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00:12 | OK. Um As geologists and uh maybe Geophysics even more than in |
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00:19 | past because they're doing things now that to uh reservoir management. Um A |
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00:27 | of you will at some point in career, get involved with um uh |
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00:33 | facility locations like platforms and that sort thing. If you're working with a |
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00:37 | company, maybe drilling 11 well and pad and there, maybe somebody within |
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00:42 | company that's really good at setting up uh your pad, your pad uh |
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00:47 | and whatnot onshore and uh trying to things up. But uh oftentimes the |
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00:55 | and, or the geophysicist can get in some of this. And uh |
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01:00 | a whole um a large number of types of wells. You know, |
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01:06 | of the wells we drill here here the list. It says uh production |
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01:15 | , injection wells, but you can have dry hole wells where you just |
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01:19 | it because it's the first uh you're drilling in a particular uh acreage |
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01:24 | you've acquired from somebody and it's, kind of like a Strat graphic um |
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01:31 | and you're, you're drilling it to what the section is, and if |
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01:34 | actually can find any oil, sometimes a AFE application for expense to uh |
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01:41 | cover uh the cost if you decide turn it into a production well or |
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01:46 | . But a lot of times you may have dry hole, hole |
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01:51 | . And in that case, uh that case, uh you, |
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01:58 | you and your engineer, reservoir engineer uh get together and, and have |
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02:03 | , both scenarios costed out. So , there's uh injection wells for enhanced |
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02:09 | recovery. Uh You're gonna have utility uh to produce fluids or dispose of |
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02:19 | . And of course, it depends where you're at and what you're |
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02:22 | You may, you may have a well, just to add a gas |
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02:26 | to a gas cap, that kind thing or uh there's water uh disposal |
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02:32 | all around. And unfortunately, too of these, well, uh water |
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02:36 | wells are, are shallow and they're they're susceptible to breakthrough to the surface |
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02:43 | you can get uh all sorts of uh collapse structures and that sort of |
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02:50 | , creating sinkholes that can be dangerous to people. And uh and sometimes |
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02:55 | cities then of course, the relief which uh when I was working on |
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03:00 | , they were kill wells two that worked on and kind of controlled were |
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03:05 | East Cameron 81 and number nine. uh then it sort of on the |
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03:12 | got involved with Macondo number two. , uh, so tho those are |
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03:17 | kinds of things that, uh, you can drill then, then of |
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03:21 | , uh, you start to worry a lot of the well ge geometries |
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03:24 | the geometry of the well patterns and that sort of thing that you |
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03:29 | up and, uh, often you to worry about things like shallow gas |
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03:33 | , especially if it's, uh, . Um, another whole group of |
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03:39 | is overpressure and under pressure. And , in a given region, a |
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03:44 | of people have drilled a few wells uh oftentimes they know which intervals are |
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03:49 | pressured or under pressured. And uh could always be in a regime. |
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03:54 | , you know, it's not there the Macondo Well was drilled, they |
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03:57 | they had a high pressure system at considerable depth which is always dangerous and |
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04:03 | they kind of got sloppy with which didn't help. And um there |
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04:08 | things in places uh where you can have mud slides. You know, |
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04:11 | talk about the uh turbidity currents, uh sections of the uh shelf edge |
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04:20 | uh a actually up on the shelf a little bit of a tilt and |
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04:24 | there's a, a bit of a or whatnot, either due to storm |
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04:29 | and, or, you know, in places where we have earthquakes, |
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04:33 | that would create some kind of uh whole sections and in like hundreds |
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04:38 | acres of uh substrate can start sliding a hill. And uh one place |
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04:45 | that was real, uh common where mud slides in, uh on the |
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04:50 | where main passes, they actually had build, diverter to uh, to |
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04:55 | the uh the mud to pass around , uh the rigs, the legs |
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05:01 | the rigs and the platforms to uh keep them from being destroyed. It |
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05:06 | on. They uh they lost a uh platforms back in the sixties |
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05:11 | and early seventies until they got this out. Folks at LSU did AAA |
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05:17 | of uh research on um these types things where you could get mud slides |
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05:23 | . Uh There's also things that you have to worry about. If |
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05:26 | a lot of uh be paic things other uh metal rich uh grains in |
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05:35 | uh formation, you have to be with it. Uh If you acid |
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05:39 | , you can turn, it can turn into a gel that clogs up |
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05:43 | the porosity nol and actually destroys And there's other things that you have |
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05:48 | be careful with, with hydrofracking. normally not with a vertical well, |
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05:52 | with the horizontal wells, you have be very careful. And uh, |
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05:56 | then of course, uh you will all sorts of uh logging runs and |
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06:02 | certain types of production data you might depending on whether it's an appraisal well |
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06:07 | something in, in a mature you might uh have, have uh |
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06:12 | uh request logs that you need that include production data. This is just |
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06:18 | you uh west of Shetland Islands. is out of your textbook. Uh |
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06:25 | when it's just showing you a spider of what was often very common and |
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06:30 | is uh offshore where we'll have a located platform and we drill deviated wells |
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06:37 | in many directions. In this it's showing you they have injection wells |
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06:42 | this little arrow symbol. Here's another over here, one over there, |
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06:46 | over there. And uh again, whether or not you need an |
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06:51 | well, depends on whether you need sweep some bypassed oil. And also |
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06:57 | it's economically feasible to do such sometimes it can cost more than um |
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07:03 | the uh potential recovery of the bypassed . And this is just showing you |
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07:10 | in the book, I think it's black and white diagram. I got |
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07:14 | and it's a little bit different. got this from Lewis uh back around |
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07:20 | where he was showing how uh we now have ways to uh graphically |
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07:27 | the well bores and where they're, they're penetrating and the target interval and |
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07:33 | what's underneath them so on and so and showing you some seismic lines. |
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07:38 | is like having a A two D to help you grasp the uh the |
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07:45 | dimensionality of this diagram which is, is plotted on a 22 D |
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07:51 | but it's plotted in such a way it looks like it's three dimensional. |
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07:57 | . Uh Everybody's heard an awful lot um horizontal drilling in Texas and in |
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08:04 | Pennsylvania and North Dakota. But what lot of people aren't aware of is |
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08:10 | the, the long reach uh horizontal really got started uh in the North |
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08:19 | and in the early 19 nineties, this is uh which farm field in |
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08:24 | UK. And uh aside from uh this, in the early eighties, |
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08:32 | were also drilling horizontal wells in the to improve the cross sectional area uh |
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08:38 | the uh of the pipe, the pipe so that you have more surface |
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08:44 | between the rock and the differential pressure you find in the well board that |
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08:48 | actually help it flow out and up the surface. Anyway. Um This |
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08:54 | one of the uh the longest ones was ever drilled. Um And uh |
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08:59 | the time and here you can see over five kilometers and um and so |
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09:08 | uh a good close to three I guess of distance. And uh |
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09:16 | kind of thing was, was not that well heard of even in the |
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09:20 | chalk wells, they didn't drill them that far, but technology had to |
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09:25 | , to do this. This was done for environmental reasons. Um They |
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09:31 | a farm site and uh they wanted offshore, get some offshore oil, |
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09:36 | were able to get surface rights and underneath everybody else's acreage and get something |
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09:42 | without putting a platform offshore. Because a, um, a part of |
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09:46 | the UK where uh they had nice and whatnot. And here you can |
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09:51 | the kinds of things they were And um, this is where uh |
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09:56 | of those first wells came and it way out here past this peninsula |
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10:01 | And uh they managed to keep the the area looking, uh uh naturally |
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10:08 | looking. And uh and at the time, they were able to capture |
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10:12 | resources that were out here without uh a lot of uh uh structures and |
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10:21 | into the North Sea. And on of that, the water out here |
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10:25 | get pretty rough. And uh I any platform that had to go out |
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10:30 | would have been a rather significant structure to be able to withstand some of |
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10:34 | storm waves. One of the uh problems, of course, with uh |
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10:41 | doing this kind of thing and um sorry about some of my distractions, |
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10:48 | uh had a little problem with the group ongoing before the class started |
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10:54 | Um Nothing serious. One of, of the key things is to uh |
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11:00 | a kickoff point and of course, I don't know if they still call |
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11:04 | a kickoff point because they can um the, the drilling assembly, uh |
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11:10 | uh turn it and whatnot a lot than they used to actually have a |
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11:15 | that would kick these things off and and help it get into angle. |
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11:22 | uh we could steer some but not as much as they can |
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11:25 | but almost all wells. And I think still a lot of them |
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11:29 | dri drill a pilot hole, at , at least a few of the |
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11:33 | in a given area so that they get a really good idea of the |
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11:37 | section. It's really critical that you this vertical section, not only the |
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11:42 | zone, but what's above it and below it if you know what's above |
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11:46 | and you know, it's below Um It, it really helps you |
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11:51 | understand how close you are to the and where you have to turn. |
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11:54 | of course, you need to have idea of the Strat gray here so |
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11:58 | you can start turning at this point than this point or that point or |
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12:03 | way up here and, and have . And uh this is kind of |
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12:08 | you one in another part of the Sea uh that, that got down |
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12:15 | into these uh Jurassic sandstones. And , and you can see how they've |
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12:22 | these channel sands, it was able sort of corkscrew its way through this |
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12:27 | hit sort of the sweet spot. before that there would have been something |
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12:31 | drilled into it to make it possible them to, to see they were |
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12:35 | the tar and uh then getting down the uh sands within the nest and |
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12:41 | below that. And uh and of , if for some reason, they |
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12:46 | below this, they have, they have a good Strat graphic section to |
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12:50 | out exactly where they were at in of being below the target area. |
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12:58 | um from a reservoir management uh a lot of these things uh go |
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13:07 | . And of course, again, the reservoir is extremely homogeneous and high |
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13:11 | permeability, you don't need to do lot of this. But what the |
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13:15 | tend to do is something called the model. In other words, it's |
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13:19 | on the rocks as they sit in ground. And the uh engineers do |
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13:23 | reservoir simulation, it's called a dynamic because it's based on changes through time |
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13:30 | uh formation pressure, uh gas oil , all sorts of things that, |
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13:36 | let them know that fluids are being . And uh I showed a few |
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13:42 | that went over some of the things they actually look at. Uh Another |
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13:46 | we can do with geophysics is uh , they'll do something that uh a |
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13:55 | um size mix so that they can of characterize where the fluid mass |
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13:59 | And especially if they have um converted which includes uh S uh excuse |
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14:06 | P waves and S waves. They of do that at the beginning of |
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14:11 | production and they start doing it on yearly to multiple year basis to see |
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14:19 | the oil water contacts moving and how they can actually see it. And |
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14:24 | so they can get some real vis . This is something geophysics were uh |
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14:30 | involved in, in the past. now they're um over the last few |
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14:34 | , the, the last decade for . In the decade before this |
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14:39 | uh they looked at it quite a . Uh Then after, after |
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14:44 | of course, if product production drops , you start to sorting out where |
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14:49 | might have uh bypassed uh oil or . And uh if something like a |
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14:55 | flood helps, sometimes infill wells can uh something that you consider other things |
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15:01 | fracturing and acid around the well Uh The well bore can, can |
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15:07 | very helpful. Of course, uh fracturing is, is famously known about |
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15:13 | uh unconventional resources as that's uh part the horizontal well fracturing um ct or |
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15:23 | couple that uh that help us really a lot of these shales that have |
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15:27 | permeability. And of course, there's uh enhanced oil recovery methods and we |
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15:33 | go into all of them, but will mention a few. And uh |
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15:38 | course, primary production is basically considered you can get with natural flow, |
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15:44 | often choked. In other words, not letting it flow out at full |
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15:49 | if, uh, you just kind open. In fact, you almost |
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15:53 | do this. Open the, well bore to a natural flow. |
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15:58 | it's at great depth, you're gonna significant pressures and you'll overproduce the well |
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16:06 | , and because of that, the you pull on the oil, the |
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16:11 | the water behind it can move and water can outpace because it has a |
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16:17 | higher relative permeability to oil and it'll run past the oil. So you |
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16:22 | choke Tokyo uh production at the well to make sure that uh that you're |
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16:30 | uh overproducing it and reducing the pressure quickly because that's pretty much the worst |
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16:36 | you can do during World War which happened even before I was |
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16:42 | Um Sometimes they needed oil so They uh they actually stopped choking a |
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16:49 | of wells and they damaged a lot wells, but they needed the oil |
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16:53 | a hurry to uh outs supply the the foes that they were dealing with |
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16:57 | that time. Next step would be water uh secondary recovery. And that's |
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17:05 | what we call water injection or gas . So it's some, usually when |
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17:08 | sent uh putting something natural in there add reservoir uh energy back into the |
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17:16 | reservoir. And that's what secondary production . And tertiary is when we do |
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17:20 | things to uh try to help the mix better with some of the |
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17:26 | And that alleviate some of the issue relative permeability. And uh and also |
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17:33 | their thermal methods which uh which they to kind of uh heat things up |
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17:41 | to uh try to make viscus oils viscous. And in some cases, |
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17:46 | actually used to uh in uh in shales. Some of the thermal methods |
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17:53 | actually used to uh to uh try , to mobilize and, and actually |
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17:59 | alter the carriages to some extent so they're actually liquids instead of uh just |
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18:07 | . OK. Here's an example um 40 seism from slumber and this was |
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18:14 | in 2002 and it's getting a whole better. I'm sure it's uh better |
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18:19 | . But this is a really good . Uh the tools as they |
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18:25 | uh you're able to come up with than one or two examples that can |
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18:28 | you something that's so clearly working. the old water contact at one point |
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18:33 | time. And uh let's see, can't quite see it, but it |
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18:37 | like it's see if I can uh , 1985 to uh OK, |
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18:55 | And of course, this was one the best examples they had to show |
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18:59 | 2002. And of course, as has continued to get better every |
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19:06 | uh this method is working better and places and of course it's not |
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19:11 | So, um, so it's gonna in an area where, where, |
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19:16 | , knowing exactly what's going on with royal water contact is important to |
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19:21 | Uh, and they, and they have an example here, but I'm |
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19:24 | there are examples now where, you might be able to see where |
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19:28 | have been flushed and where things have been flushed, uh, which would |
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19:32 | direct you to drilling a new primary . Well, a fill in. |
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19:36 | , and that sort of thing, , uh, thing that can |
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19:45 | uh, important for geologists to understand , um, we always have to |
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19:52 | gravity and, uh, we're we're gonna try to pro, |
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19:56 | have a water sweep. This is good sort of a good cartoon right |
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20:01 | that I have the cursor on. an injection. Well, and it's |
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20:04 | , pushing water up into this Uh, and you're trying to produce |
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20:08 | just, just, uh, up of it. And here you've got |
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20:13 | one pushing oil up dip of Um, here's an example, |
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20:20 | from the surface of that same but they have other, uh, |
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20:25 | . Here's like a four spot where have a production well, in the |
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20:29 | , this might be if you um, sort of like, |
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20:33 | some attic oil that's trapped and you're to squeeze it from all sides and |
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20:37 | top of the top of the anticline , or the structure might be right |
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20:43 | where this is and you're trying to , uh get that to uh push |
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20:46 | oil uphill. So it's a little different map model than that. And |
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20:52 | the thing called the Seven Spot one the Nine spot. One of the |
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20:56 | that relates to. Um And I know if I've, if they've actually |
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21:03 | it, but if, if you , um this is a horizontal |
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21:09 | and you had another horizontal well over and another horizontal, well over |
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21:14 | one of the things I know Schlumberger working on around 2005 and six. |
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21:20 | I, I don't know if they uh got people interested in it, |
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21:25 | some of those wells, they they'll have um a horizontal well |
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21:31 | And then instead of having water flow that direction, they have the water |
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21:35 | shooting in this direction and in this , they basically have um a primary |
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21:43 | well in the middle, then they'll a side track, that's an injector |
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21:47 | here on this side and another side , that's an injector over here. |
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21:52 | I'm kind of uh without having another . I'm trying to explain to you |
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21:56 | uh uh that could be much more in, in the fact that you're |
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22:01 | um going down and uh immediately from beginning of your uh horizontal. |
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22:07 | trying to figure out a way to , push the uh hydrocarbons in this |
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22:12 | . In this direction. But in the, in these low permeability |
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22:18 | that can be difficult. This uh might work even in high permeability ones |
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22:24 | some of the chalk fields and some those sandstones I was showing in the |
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22:28 | where they already have horizontal wells. . This, this uh kind of |
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22:38 | uh uh a nice 3d uh representation the problem with relative permeability and how |
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22:48 | can cause coning of the water. the well bore and uh because the |
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22:54 | bore is drawing down pressure here, , uh all the fluids are gonna |
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22:58 | screaming up here. And of the uh the water with that, |
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23:02 | higher relative permeability is going to try cone up into it. This is |
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23:07 | it would look like in one cross uh pretty much on strike with the |
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23:13 | of the reservoir. This is this looking at a dip section of the |
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23:18 | and then this is looking at it the map view from the map |
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23:21 | You get an idea of what's happening your reservoir as this water is coning |
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23:27 | . In other words, vertically, trying to go up uh laterally, |
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23:30 | trying to move up, dip in an arrow sense. You can |
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23:34 | that also and of course, that's cusp. And um you can have |
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23:42 | like this uh where your initial oil contact is down here. You've got |
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23:49 | injector pushing water up here. uh, you can see that at |
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23:54 | point that injector well down here, is a, is a perm |
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23:59 | an impermeable barrier. And, so you have this kind of trap |
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24:04 | to the side, this particular producer produce until the water gets up |
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24:09 | uh, up to here. But one's gonna be trapped off, |
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24:12 | down to there. So this may leaving some attic oil behind and, |
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24:18 | , that would be a type of bypassed oil or uh oil that uh |
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24:23 | additional um uh drainage on it. , you didn't have preparations all the |
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24:30 | to the top of this thing. they were down here, you, |
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24:32 | might leave even more attic oil which happens quite frequently and this is |
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24:37 | showing you what the sweep looks like from a map view relative to this |
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24:43 | section. Here's another thing that you know, we, we always |
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24:48 | about these fining upwards and coarsening upward . And uh this is like a |
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24:55 | Gama log in a way. But here, here, it's showing your |
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25:00 | um is higher here and it gets down here in this one. The |
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25:07 | is higher and it's lower down So this could be a coursing upward |
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25:12 | and this is a binding upwards And uh just uh I hope somebody's |
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25:22 | attention. I like this diagram because gives me a chance to ask the |
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25:27 | a question which one first of and anybody can answer which one of |
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25:34 | looks like it's getting better sweep of reservoir. Would it be the top |
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25:50 | ? Yeah, I would say the one. And why, why do |
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25:53 | think that, assuming it's a good ? Why would you think that, |
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26:06 | , because of the migration direction of oil, the water, the impact |
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26:10 | the water on the oil? And, and, but, |
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26:13 | one, you know, because we're at a cross sectional area, cross |
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26:17 | area is not everything, but it's part of a volume. It's two |
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26:21 | of a volume you can see the cross sectional area that's, that's |
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26:25 | flushed is much greater than this cross area. And uh and that's why |
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26:31 | was obvious to you, I And uh and so that's absolutely |
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26:36 | So having said that um what is about coarsening upwards that seems to work |
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26:44 | better than um binding upwards? what physical factor do you think is |
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27:00 | this happen? Gravity? Absolutely. said that me, Stephanie the |
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27:12 | Of course, yes. Gravity. has a role in everything. |
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27:17 | now I'm sitting here thinking about but what if the sweep was too |
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27:22 | ? Um If we looked at this a different perspective, this could be |
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27:29 | a thief zone up here if it , if it breaks through too |
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27:32 | right? And uh so it's, know, that this is the right |
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27:39 | in one in one way. But could be the wrong answer. For |
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27:43 | , if this was happening, happening , what we could find out is |
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27:48 | water would break through and just block the entire, uh, production of |
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27:53 | . Well, and you'd leave all oil behind. However, this |
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27:59 | uh, if you think about thief because it's on the bottom, it's |
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28:04 | , the water is not breaking So it's gonna take it a |
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28:06 | but it's gonna sweep the rest of area eventually after it gets put. |
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28:11 | other words, you know, it's slow process, but it's, it's |
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28:15 | be a greater and greater aerial Whereas this, this could come right |
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28:20 | here and if your perps are all here, uh you're in trouble if |
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28:25 | down here, uh You could still some issues because, but the gravity |
|
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28:30 | actually trying to help you in that . So, um it always depends |
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28:36 | , you know, what the problem could be. Uh If this happens |
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28:40 | a long period of time, it's much more efficient sweep and would be |
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28:44 | good thing. Uh And better than . But if this was happening |
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28:49 | this could be a thief zone to off a lot of this oil down |
|
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28:53 | . Whereas this one is gradually gonna in this direction and get all the |
|
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28:58 | and especially if you have perps all this pipe, which you probably |
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29:03 | but uh I don't think they're trying show you that this is ground |
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29:06 | This is the formation itself uh where finding upwards and this is the formation |
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29:12 | where it's coarsening upwards. OK. , um oh yeah, I put |
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29:20 | over here too, you know, been there for a long time and |
|
|
29:24 | is the first class that got it . OK. Um Here we have |
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29:31 | just more examples showing this kind of . And uh here you can |
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29:36 | uh here's high permeability at the top here you're gonna end up getting |
|
|
29:44 | um, a better sweep because gravity , is actually doing the exact opposite |
|
|
29:50 | . Um But here it's shooting through and so it sounds like I'm saying |
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29:55 | different thing but for different reasons, , this one definitely looks like it's |
|
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30:02 | lot better. Uh, in terms a coursing upward sequence versus a finding |
|
|
30:08 | sequence. And here again, you see this gravity is also the gravity |
|
|
30:14 | the water is actually working against Here, it's working with you here |
|
|
30:20 | long as it's not too fast. . And here, here's just another |
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30:28 | of, uh, I like to a couple of these things are really |
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30:32 | same thing, but this is trying show you that tonguing doesn't, doesn't |
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30:36 | to be, you know, so like this. Um, tongue can |
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30:46 | more like this too where you get pods of bypassed oil. And here |
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30:56 | , uh this is the barrel of questions and uh this doesn't equal 100% |
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|
31:04 | it says, you know, maybe of the recovered oil is gonna be |
|
|
31:07 | . I think in your example, have 34 you may be able to |
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31:12 | another 15% out this way, another that way, another 20 you may |
|
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31:17 | do all of these things either. whatever the in place amount was, |
|
|
31:22 | can get 30% out this way especially with a nice, with good |
|
|
31:27 | abilities. Uh then uh this could another 15%. All these different things |
|
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31:34 | help you. And it's talking uh, you know what it is |
|
|
31:37 | here, of course, the Eeor thermal and surfactants and polymers and that |
|
|
31:43 | of thing. And uh here we water and gas injection down here and |
|
|
31:48 | of course, infill horizontal wells can redirected primary recovery. Um And so |
|
|
31:57 | primary, this is another primary. this is what, you know, |
|
|
32:01 | we have a recovery factor. This what we're hoping for when we put |
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|
32:04 | first wells in. But after someone can come back and do some |
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|
32:09 | these things. One of these two of these things, three of |
|
|
32:11 | things and try to get more I don't think it's likely that you |
|
|
32:15 | do all of them and get all the oil. Uh, but 1 |
|
|
32:18 | work better in a particular setting than . Uh, sometimes it has to |
|
|
32:23 | with, you know, gas If you've got a lot of extra |
|
|
32:26 | coming out of the gas cap, an easy source. And, |
|
|
32:31 | water injection could relate to, uh, waste if you have waste |
|
|
32:36 | . But sometimes it's an issue putting in a pipe. So, |
|
|
32:39 | there can be a lot of different that you normally wouldn't think of. |
|
|
32:45 | here's a section of what's going on what these are called. So this |
|
|
32:51 | be bypassed oil, which would um, could be pods of oil |
|
|
32:55 | are left behind or it could um, something like the attic oil |
|
|
33:00 | you might see up here, at the end of it. So |
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33:03 | would be types of bypassed oil and bypassed oil here that, uh, |
|
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33:09 | some reason, uh, they couldn't a sweep on, on this and |
|
|
33:12 | it to drilled based on the I'm seeing, it looks like they |
|
|
33:16 | . But, uh, again, , they're trying to point out that |
|
|
33:20 | near the top of a, of system. You can have attic oil |
|
|
33:23 | gets trapped because water starts coning somewhere the well is. Ok, |
|
|
33:29 | like this, uh, leg of right here, could be one of |
|
|
33:38 | in your wells right here. But your well starts up dip, once |
|
|
33:43 | well starts producing that water, you're gonna be able to get that |
|
|
33:46 | That's next to it. Simple But there's some complications that you must |
|
|
33:53 | aware of. Here's water injectors going . And of course, you |
|
|
33:57 | they didn't put them up here, put them down here to try to |
|
|
34:00 | all the bypassed oil. Uh, other type of oil that we have |
|
|
34:04 | residual oil. And, uh, is microscopic and of course we use |
|
|
34:10 | , uh, things like polymers and to try to uh reduce surface tension |
|
|
34:15 | , or um surfactant surface tension and of the polymers to uh make the |
|
|
34:21 | missable with the water and uh, get stuff at the interstitial level, |
|
|
34:29 | what we call residual oil. So good test question is something about what |
|
|
34:33 | residual oil, what is bypassed oil , um, and what might be |
|
|
34:40 | bypass oil, be added oil, kind of thing. And, |
|
|
34:48 | there's the answer to that one and , here's just some others. Um |
|
|
34:55 | won't go through this in great uh , but I think what you should |
|
|
35:01 | is just look at it and see we can have. Uh, here's |
|
|
35:04 | Strat graphic uh potential uh attic oil in up here. And here's one |
|
|
35:13 | , um, um, you um, perforation such that it, |
|
|
35:19 | that it come through and left a lot of oil behind you. And |
|
|
35:24 | would be, uh definitely be a infill well in here somewhere which could |
|
|
35:29 | up this attic oil, this Strat attic oil and this sun swept oil |
|
|
35:34 | . And this, this right here be something, uh, similar to |
|
|
35:39 | a different direction what this was In other words, you know, |
|
|
35:44 | this water gets over here to the , it's gonna shoot right up the |
|
|
35:48 | bore and it's gonna get there quicker . Which one of these ones, |
|
|
35:57 | , this, this could win for lot of reasons and this could win |
|
|
36:01 | other reasons and vice versa. It's and the reservoir engineers are good at |
|
|
36:07 | out what will work in a given and a given uh permeability. Uh |
|
|
36:14 | between the water and the oil or other fluids. If you have |
|
|
36:19 | it's not usually a problem. Um Here is, um, again |
|
|
36:27 | just a better diagram of what attic will look like. It's a type |
|
|
36:31 | ba bypassed oil. And, you know, and what I, |
|
|
36:36 | I was trying to point out earlier that in the slide or coming out |
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|
36:40 | the slide? Uh This could be tongue that actually misses the well bore |
|
|
36:47 | , but there might have been a bore in or out of here that |
|
|
36:50 | up some of the oil in between even this one. And here's just |
|
|
36:57 | example of um, um, different of attic oil that you can, |
|
|
37:03 | configurations. Here's, here's a whole of compartments, this was totally unsw |
|
|
37:10 | one needs to be swept more. one needs to be swept more, |
|
|
37:14 | this is all um bypassed or un oil. And uh and uh you |
|
|
37:21 | end up with a lot of it a row like this, you can |
|
|
37:25 | up with these things being stacked. so I shared some diagrams that I |
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|
37:29 | myself and this would be what it look like. If you had ones |
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|
37:33 | were side by side, you could a horizontal well to come in and |
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|
37:37 | a whole bunch of them. You a deviated well to come in and |
|
|
37:40 | get several of them this way. in fact, um one of the |
|
|
37:46 | Hill Corp has in some of these that have been highly produced is to |
|
|
37:50 | in and do this kind of And uh and take advantage of the |
|
|
37:56 | to uh the, it's much easier deviate wells now or drill horizontal wells |
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38:03 | it used to be. And you use this in conventional resources that have |
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38:07 | oil uh that can, can be with one be well, uh well |
|
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38:14 | could actually penetrate all these pods in row. And uh and sometimes, |
|
|
38:21 | sometimes there's rules against it, but you can have multiple per preparations and |
|
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38:27 | the multiple perforations at one time. there's rules against that and you can't |
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38:32 | mangle in which, which cases you , you would open up one at |
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38:35 | time, then just open up the one and the next one, |
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38:38 | if each one of these was like contested unit, part of this block |
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38:42 | in somebody's acreage, but this one , uh, you might have to |
|
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38:46 | it out that way. And this is just um, another, |
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38:53 | thing that can happen, you can gas coating. If you have |
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38:56 | um, the upside ver upside down of, of water coning, you |
|
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39:01 | , you have, have the gas , you wanna keep your preparations away |
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39:04 | your gas cap in the course of in a situation like this and you |
|
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39:13 | gas up here and you have oil here, which one of these you |
|
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39:18 | is gonna be really important and uh the bottom one would be better if |
|
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39:22 | had a gas cap in it. there's simple things to think about, |
|
|
39:29 | there's no right answer unless you know the details on this. Ok. |
|
|
39:37 | there's another issue of uh dealing with problem of landing horizontal wells. And |
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|
39:46 | you remember uh earlier on, I about um you know, when |
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39:52 | when we drill a well, it's very hard to um see ahead of |
|
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39:58 | drill bit, but when you, you work on a horizontal, |
|
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40:04 | it seems very complicated except that you have layers through here uh that you |
|
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40:10 | pick up. So um here is somebody heather kickoff point, too |
|
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40:17 | So the target was high and they it here. Their kickoff point was |
|
|
40:23 | , too, too early. And it took him a while to get |
|
|
40:26 | to it. So these kinds of can happen. But, but |
|
|
40:30 | as we're drilling this way, we always have that predictability. But if |
|
|
40:34 | do drill this way here, you see where they, you're gonna have |
|
|
40:41 | with this. The dip being different what you think it is. Here's |
|
|
40:45 | where you go through faults and this offset can make you miss it. |
|
|
40:50 | now there's a lot of la lateral that have improved. And uh one |
|
|
40:54 | the, one of the students, Sheikh Iqbal was um a phd student |
|
|
41:00 | Rice University. He came here and into the program. You're in the |
|
|
41:05 | uh in petroleum geology. So, know, a little bit more about |
|
|
41:10 | and it, it helped him, think I mentioned, helped him save |
|
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41:13 | job beyond his boss and his boss's . Anyway, um Here, I'm |
|
|
41:20 | show you a couple of things. of the alternatives of course is bio |
|
|
41:25 | uh to this old scenario of trying guess where to do this first. |
|
|
41:32 | uh that is to have some idea what the vertical section looks like. |
|
|
41:38 | bio zone four, for example, be your sweet spot in here and |
|
|
41:42 | a paleontologist can do is come in figure out what some really high detailed |
|
|
41:47 | localized by zones are. So that actually as, as you're drilling |
|
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41:52 | you know, exactly where you And of course, if you want |
|
|
41:55 | predict where you're gonna start kicking uh, you could get some of |
|
|
41:59 | bioz ons sooner and, and figure the geometry of when you needed to |
|
|
42:03 | turning. But once you get you'll know you're in one, you |
|
|
42:06 | , you're in two, you need keep going down. And when you |
|
|
42:08 | to three, you need to start slow down. And when you get |
|
|
42:12 | four, you wanna level off and you go too far, you'll see |
|
|
42:17 | uh that sort of thing. And , so you have this vertical profile |
|
|
42:22 | in a way allows you, you , if, if you're, if |
|
|
42:26 | on target in, in a well, everything's great. But what |
|
|
42:30 | want is something that can help you ahead of the drill bit and what's |
|
|
42:34 | ahead of the drill bit here is what's a, what's next to the |
|
|
42:39 | , the drill bit on this way in this way. So the lateral |
|
|
42:44 | now becomes the vertical. And we tools that can see laterally which will |
|
|
42:50 | the vertical for us to help us if we're getting too close to this |
|
|
42:54 | we're getting too close to that. uh and so this is the kind |
|
|
42:59 | thing is you know, you, keep adjusting it in this manner. |
|
|
43:05 | , here, um with these uh these lateral tools that we have with |
|
|
43:11 | higher, higher reach into the you, you do the same kind |
|
|
43:15 | thing. You come up with with a trophy zone nation like |
|
|
43:21 | This is done in the chalk wells the time and uh last like just |
|
|
43:26 | COVID, they were still doing I know for sure. And I'm |
|
|
43:29 | they might still be doing it with owns. But now, now with |
|
|
43:33 | tools that they can see farther put them on their side laterally, |
|
|
43:38 | seeing what you need to see vertically keep you on target. And so |
|
|
43:45 | is, this is kind of why drilling works because in, in some |
|
|
43:51 | you're seeing ahead of the drill bit in the sense that you wanna know |
|
|
43:55 | going on laterally to keep you aligned here. Now. And um and |
|
|
44:04 | that's why uh uh these new tools reach farther out into the formation help |
|
|
44:10 | because you can see through those zones , and so on and so forth |
|
|
44:15 | that we'll be done with that Any questions, um push the wrong |
|
|
44:37 | there. Is anybody there? Uh you know, um like |
|
|
44:51 | I, I think everybody in, the class prefers in class and I |
|
|
44:54 | I do too. It's a whole easier when I can see you let's |
|
|
45:04 | . But you're, you're a whole quieter um, online as well. |
|
|
45:18 | . Now we're gonna talk a little about some of the types of unconventional |
|
|
45:22 | resources. Everybody knows about the And, uh, and of |
|
|
45:32 | when you're working with unconventional, you the same primary task as somebody working |
|
|
45:36 | conventional wells. And, uh, of course, in that vein, |
|
|
45:43 | know, the conventional things with high and high porosity, you know, |
|
|
45:48 | , have put us, you pretty much focused on the coarse |
|
|
45:53 | And of course, now we've, know, I say new tech technologies |
|
|
45:57 | what, what's really, I think most amazing are the, are the |
|
|
46:02 | the ways they can turn the drill now that they couldn't do before and |
|
|
46:07 | way they managed to uh to get into the well board that's horizontal |
|
|
46:12 | and a lot of other things which uh absolutely amazing how they do |
|
|
46:17 | But uh but the hydrofracking that they is something that was done routinely, |
|
|
46:25 | least, at least in the late , if not earlier, that was |
|
|
46:30 | vertical wells. And of course, horizontal wells were being done in the |
|
|
46:38 | . And then these, these long ones, especially uh in the UK |
|
|
46:44 | what sort of forced people to figure some technology to do some of these |
|
|
46:49 | reach wells which were probably very difficult do. And the technology had some |
|
|
46:56 | , but over the past 20 the improvements have gotten, uh, |
|
|
47:00 | much better. So, it, a lot's happened, uh, over |
|
|
47:04 | last 20 years, terms of helping to get into these things and, |
|
|
47:10 | I've already shown you this, but , to me it's still remarkable |
|
|
47:15 | you know, if you look at the sedimentary rocks covering the earth's |
|
|
47:20 | uh, it's a pretty big, big area, uh, for the |
|
|
47:26 | and we've been ignoring all the fine sediments for the most part. And |
|
|
47:31 | and that is the reason why it's . And uh I know I gave |
|
|
47:36 | lectures with this slide before 2010 ish uh things were just starting to happen |
|
|
47:44 | people had no idea. I don't at the time of how profound it |
|
|
47:49 | certainly people like uh Floyd C Wilson exactly how profound it was and uh |
|
|
47:56 | guess it was Mitcham uh that also a pretty good handle on, on |
|
|
48:02 | was gonna happen. And uh even today, we haven't even, I |
|
|
48:08 | think we've touched even a small fraction the resource plays that are out there |
|
|
48:15 | around the globe. Um You a lot of the technology is, |
|
|
48:19 | still focused here in the United States it's just slowly creeping um to other |
|
|
48:25 | of the world where uh a lot the fields, for example, that |
|
|
48:29 | being developed, even like in places surname and Guyana, those are all |
|
|
48:36 | productivity. Those are all conventional You know, they're going after |
|
|
48:41 | uh, the big, the big that uh, that are easy to |
|
|
48:46 | and they haven't gotten to the, the point of uh turning some of |
|
|
48:50 | uh resource plays into real assets. , anyway, uh there's a whole |
|
|
48:57 | of them. Um, she plays oil and gas, of course, |
|
|
49:04 | then there's these other things, tar , oil shales. So we'll talk |
|
|
49:08 | little bit about these, a little about the tar sands and the oil |
|
|
49:13 | and some of these tight gas sands that are not typical. Um But |
|
|
49:21 | what we call basin centered gas gas , the BC GM. And um |
|
|
49:34 | things that we can do with, uh drilling and wells, the geologist |
|
|
49:38 | geophysicists might be involved in or carbon wells, gas storage, heat, |
|
|
49:46 | , uh lithium is probably gonna become soon. And of course helium and |
|
|
49:53 | for all the different uses, I think this map has changed much since |
|
|
49:58 | came out. And um, this published in 2016. I think there |
|
|
50:05 | something identical to this almost every but some of these uh other fields |
|
|
50:11 | starting to develop a little bit But some of the uh the biggest |
|
|
50:15 | are the Marcellus, the Utica. uh this Antrum over here is glacial |
|
|
50:22 | which one of my students worked Here's the Bakken up in North Dakota |
|
|
50:28 | a little bit in Idaho. uh, mostly in here in, |
|
|
50:33 | , in the, um, this of, uh, northern, |
|
|
50:41 | North Dakota rather. And, and of course, the Barnett has |
|
|
50:45 | a big one. that's some of acreage that, uh, one of |
|
|
50:49 | students worked on that made a lot money for his company. And, |
|
|
50:54 | , and some of these other things , are picking up this. Uh |
|
|
50:59 | is where some of the tight gas might be in here because even the |
|
|
51:03 | stuff in Mobile Bay over here related it uh was tight gas. And |
|
|
51:13 | it's pretty extensive in the US and no shortage of things like this. |
|
|
51:18 | one thing that's really obvious to anyone worked in the oil industry for any |
|
|
51:23 | of time is that these things are right underneath a lot of places where |
|
|
51:28 | been producing oil and gas forever. that's why they're there. They're the |
|
|
51:34 | through the source rocks which are now plays to uh to basically go back |
|
|
51:39 | and get the bypassed oil that hasn't generated and, and uh expelled into |
|
|
51:46 | secondary migration and uh into a And uh I like to use this |
|
|
51:56 | uh some of these diagrams were pretty , but uh things got hopping and |
|
|
52:00 | kind of slowed off. But uh think this kind of explains what |
|
|
52:05 | This is in 2013 here, you see 2011. And uh this person |
|
|
52:11 | today, he probably couldn't get a that looked like the one that he |
|
|
52:16 | uh what he used for this But he said two years later, |
|
|
52:20 | way up here. So it was a boom. After that point in |
|
|
52:24 | , you can see here that people getting into it. Uh You |
|
|
52:29 | just one place, um the Barnett a while, but you can see |
|
|
52:37 | happened here in uh 20 07, know, it started to pick up |
|
|
52:43 | people didn't realize it was gonna be over the place as well as the |
|
|
52:48 | that had the vision to do this invest some money to do this, |
|
|
52:51 | had the vision and um pretty pretty good calls actually. And uh |
|
|
52:58 | then it just exploded after that. of course, some of this relates |
|
|
53:02 | the technology was getting better every day uh here is in 2012, how |
|
|
53:10 | all of this was. And, these, um and this is looking |
|
|
53:15 | expenditures, of course, uh the expenditures actually would have a lot to |
|
|
53:20 | with what ended up happening and how production moved forward. And here they |
|
|
53:25 | talking about $54 billion into this and much more than that's come out of |
|
|
53:31 | areas. And uh and so, it's pretty significant, I think what's |
|
|
53:37 | significant to notice is, um, Ford is predominantly in Texas, |
|
|
53:44 | um, the Permian basin, of , it's in West Texas and some |
|
|
53:49 | uh, New Mexico and here the washes in Texas, Oklahoma. |
|
|
53:57 | uh, and of course, some these uh, smaller things that aren't |
|
|
54:00 | listed on here also are in So, an awful lot of, |
|
|
54:04 | , of these resource players are in where we, we found oil and |
|
|
54:08 | for primary production of conventional. Here's a scattering of what's going on in |
|
|
54:17 | Permian basin. And uh many, years ago before any of you were |
|
|
54:23 | , I actually did a study on Delaware and the Midland Basin. And |
|
|
54:29 | but I was looking at uh pretty the, the conventional resources uh |
|
|
54:35 | in graduate in a class in graduate . OK. Um Some of the |
|
|
54:44 | in some of these areas was uh already been, uh you know, |
|
|
54:49 | a, a lot of the development based on the conventional and, and |
|
|
54:54 | the Delaware Basin was one of the one people started to go back |
|
|
55:00 | Uh one thing that's interesting is that on the highs here, I have |
|
|
55:05 | also um come into their own as are some source rocks up up across |
|
|
55:13 | high. And uh that's a completely thing. But uh uh here, |
|
|
55:21 | , it's saying, you know, 20% develop, here's 3% since, |
|
|
55:28 | uh that period of time, you , it's, it's developed a lot |
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55:31 | but there's still a lot to Here's showing uh cap Capex past. |
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55:38 | Here, here is what Capex was to be in 2012. Here's just |
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55:44 | you a diagram, bar diagrams. know, I, I wish when |
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55:49 | made a diagram like this, they make one the next year and the |
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55:52 | year. So you could show people . It's very difficult to find uh |
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55:58 | uh graphics. I think it's But uh but it would be helpful |
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56:02 | an instructor, but you can see uh what's going on and of |
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56:08 | uh a lot of stuff uh that projected for 2020 2021 obviously didn't |
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56:15 | And some of that, a lot that had to do with COVID, |
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56:17 | of it had to do with uh the oversupply that we had starting to |
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56:22 | in 2019. And here again, projections pass 2020 this was released in |
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56:32 | . So this was assuming a dip COVID and then some build up uh |
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56:37 | that. And um here's sort of um the gap is uh being projected |
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56:49 | the future. Um as we see in conventional, we're gonna see uh |
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56:56 | in the unconventional resources. And uh , here's where we are right about |
|
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57:03 | and uh we're still really just a bit better in here. And |
|
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57:09 | I'm not sure the unconventional are outstripping conventional right now. But uh |
|
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57:15 | this is in the US, the Basin is still a monster. And |
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57:21 | and that's all unconventional, which which is driving a lot of our |
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57:24 | and ability to export oil and gas this time. And I think exporting |
|
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57:30 | when, when you can send it the refineries that can produce that lighter |
|
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57:35 | , uh you're actually creating an efficiency the system that ultimately uh at least |
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57:41 | a global and a national scale should the prices relatively lower as long as |
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57:45 | happening. OK. And uh this just a diagram showing you that, |
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57:53 | know, it's not just going on the US, it's happening all over |
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57:56 | world. And um some of these in Brazil and Argentina are pretty |
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58:03 | Um Some of the ones in um this area here relate to high uh |
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58:11 | geothermal um low, which uh which actually mature things that are shallower than |
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58:18 | would normally expect and uh still be the, the source rock itself. |
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58:26 | this is showing you the same kind thing with gas. Again. Uh |
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58:32 | key to this is to just point uh there are lots of places uh |
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58:37 | where we have reserves that aren't aren't being produced really uh at high |
|
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58:42 | yet. But um there's a lot reserves out there in terms of uh |
|
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58:48 | and it's a matter of uh getting technology spread around the world so that |
|
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58:53 | can, can uh get these Of course, South Africa I think |
|
|
58:58 | is, is doing a lot uh they're always sort of on the teetering |
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59:03 | of having enough energy to uh keep electricity on. I was over there |
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59:08 | times and we had a professional master's over there and over the course of |
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59:13 | 16 months, they had blackouts, , all sorts of things because, |
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59:18 | their grid, their na their grid a national scale was uh was not |
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59:22 | able to keep up. And I'm sure they, they, they have |
|
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59:29 | very little to no uh nuclear They're trying to, trying to keep |
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59:33 | as clean as possible. And of , natural gas would be a good |
|
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59:36 | for them because natural gas produces more per CO2 output. OK. So |
|
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59:45 | we're gonna get into hydrofracking and, , again, we're just looking at |
|
|
59:56 | , but uh I think the most thing that you have to think about |
|
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60:04 | that, you know, if you a, if you have a vertical |
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60:07 | up here and you're trying to produce own, that's all the surface |
|
|
60:15 | But the circumference of that well, times the thickness of your PFS, |
|
|
60:21 | perf zone is all the surface area have uh that creates that differential impress |
|
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60:28 | the formation and the rise up And of course, it's gonna be |
|
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60:33 | , uh, if you're doing things . And, uh, until you |
|
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60:38 | to, uh, something that's producing slowly. Um, Rob Stewart, |
|
|
60:45 | of the geophysics professors was teaching today he, he brought me some oil |
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60:50 | a Coke bottle. He was in , in a, um, plastic |
|
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60:54 | bottle. It was coming from well, that's producing four barrels of |
|
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60:58 | a day. He was really excited it. Um, you know, |
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61:03 | , it is, it is extra if you can get it without um |
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61:08 | having to spend much apex uh with shallow wells that that happens often in |
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61:13 | . So, um but nevertheless, know, when you get uh this |
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61:18 | surface area in here, uh and you frac it, you're increasing the |
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61:24 | area dramatically at all these critical So you're getting flow into it from |
|
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61:31 | formation over a greater area. In words, all through here, all |
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61:35 | way down here, uh You're getting , the sand grains that are put |
|
|
61:40 | here are supposed to be suggesting um prop which is glass beads or sand |
|
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61:48 | anything that uh can create a uh higher permeability uh and kind of hold |
|
|
61:55 | fractures open once they're made. And there's a lot of concern about the |
|
|
62:02 | things that go into this. A of the unnatural chemicals are to help |
|
|
62:07 | from clogging things up on the way and really have nothing to do. |
|
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62:11 | uh keeping it opened up, others . But the uh the percentage and |
|
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62:16 | amount of these things are really As long as, as long as |
|
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62:20 | unit that you're producing is not near valuable aquifer or not near salt, |
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62:28 | that you could actually dissolve and cause um a sinkhole to form above it |
|
|
62:35 | that sort of thing. So most the time, this can be a |
|
|
62:38 | uh very efficient way to get more out in a very safe way. |
|
|
62:42 | long as all the players are paying to the reality of what they're |
|
|
62:49 | there's a different uh types of uh , something's called the passy method and |
|
|
62:54 | everything in geology, it doesn't work everywhere, but it works really well |
|
|
63:00 | a lot of places and it can very well with different tools. Um |
|
|
63:08 | original, original uh thing that was was uh looking to see um uh |
|
|
63:16 | your resistivity. Uh And also your trying to give you uh a hint |
|
|
63:24 | uh various things like, like uh creating resistivity versus um uh volume issues |
|
|
63:37 | might be related to density and uh that sort of thing. So you |
|
|
63:41 | a density log and you have something looking for organics. And here it's |
|
|
63:46 | you kind of uh um the gamma is showing you um a higher level |
|
|
63:52 | organics down here versus up here. this is definitely more organics than anywhere |
|
|
63:58 | . The resistivity is a, is uh a function of uh of some |
|
|
64:06 | that porosity that you're getting. And this density is showing you um here |
|
|
64:12 | there's, there's a drop there um , in the density. And |
|
|
64:20 | um what's filling that porosity is gonna organic material as opposed to uh to |
|
|
64:27 | something like like uh rocks or In other words, you're visualizing the |
|
|
64:34 | and the resistivity at the same time . And when you get here, |
|
|
64:39 | you kind of see that there's, no gap in that log and the |
|
|
64:44 | in that same area did, did of the same thing where he, |
|
|
64:47 | had this and he was tying the um uh S two uh values and |
|
|
64:55 | to CTO C values based on the data and how it lines up with |
|
|
65:01 | the log data was trying to show at the same time. And so |
|
|
65:05 | worked out really well and uh sometimes doesn't. And uh originally uh they |
|
|
65:11 | Sonic, but you can also um can also use uh a density or |
|
|
65:16 | neutron log if it works better in lithograph and sort out an algorithm that'll |
|
|
65:22 | you see this um this separation between two things and the overlap that opens |
|
|
65:28 | uh and allows you to see that hydrocarbons in a poorer system. |
|
|
65:34 | If we uh look at the Eagle play which is, they go way |
|
|
65:40 | here is this thing that we're gonna at. Um, you know, |
|
|
65:56 | is one of these unique places where had a source rock that they knew |
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66:02 | had hydrocarbons in it. And uh the shell, the shell can be |
|
|
66:10 | to 400 ft thick. Uh 250 , what the average is in the |
|
|
66:14 | prolific areas. Um It can have content as high as 70%. So |
|
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66:22 | has a low V shell and that it's more highly frac, it also |
|
|
66:28 | that there's some grain support so that you're, if you're removing some of |
|
|
66:31 | hydrocarbons, it's not gonna necessarily So you have, you have kind |
|
|
66:38 | a rock that's a little bit it's frack, but it also doesn't |
|
|
66:44 | need as much uh prop naturally uh keep, keep those uh fractures that |
|
|
66:50 | push open uh in, in the that some of the natural fractures could |
|
|
66:57 | uh work alongside with the uh the fractures that you put in there. |
|
|
67:04 | a lot of it had to do uh an isolated basin uh behind the |
|
|
67:10 | Sligo Reef trend. And uh and lot of these different things uh kind |
|
|
67:16 | combined to make this really incredible sweet and the producing interval is found over |
|
|
67:23 | . Of course, some of the , the deeper parts are gonna be |
|
|
67:27 | gas prone. And um and as come up the section, it's gonna |
|
|
67:32 | less and less mature to where you into the, uh, condensate in |
|
|
67:37 | gas zones and then into oil and further up, you're gonna have a |
|
|
67:42 | amount of oil production in some early . And, um, here you |
|
|
67:52 | see, um, the Eagle Ford this Strat graphic column. Of |
|
|
67:58 | they have a timescale over here and don't show any gaps for these un |
|
|
68:02 | , which I know it probably means to you guys, but it, |
|
|
68:05 | hurts, hurts my feelings to see . But what's interesting here is you've |
|
|
68:10 | something with natural frock fracking, the chalk up above it and you have |
|
|
68:15 | other stuff. Uh The Del Rio here also has natural fracturing. So |
|
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68:21 | you're, when you're perf in you have to make sure that uh |
|
|
68:25 | of these systems depending on how they're with each other structurally in that particular |
|
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68:30 | where you're at, you. Um have to be really careful um uh |
|
|
68:37 | you don't have uh fracturing going into above, into the Austin chalk or |
|
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68:43 | into the uh into the Buddha. , the, the shale part that |
|
|
68:49 | gonna be working on in the Eagle is well below some of the other |
|
|
68:53 | . So usually you don't have to about Austin chalk. But if |
|
|
68:55 | if you, if you're near faults stuff like that, it could be |
|
|
68:59 | issue OK. Here. Um It's of showing you um where the shelf |
|
|
69:09 | were. And uh so you have basins behind the Sligo and the Stewart |
|
|
69:16 | shelf margins. And, uh and have the thickness uh here, you |
|
|
69:21 | see it gets thicker over here in East Texas Basin. It's a little |
|
|
69:25 | thinner over here. But uh what it normally mean when we have a |
|
|
69:32 | section in a given area? Really rocks? Remember what we were talking |
|
|
69:36 | ? Net degross anybody uh when it suggest or think about, you |
|
|
69:46 | you're, we're trying to make you , petroleum geologist and some of you |
|
|
69:52 | . Uh but what is it about area? It's behind this, this |
|
|
69:57 | break. It looks like a big center over here. It's less of |
|
|
70:03 | depot center over here. And you've me say that a lot of times |
|
|
70:08 | go to the Depot center, but is the Depot center a bad thing |
|
|
70:12 | here? What is it about this structural scenario here that makes this bad |
|
|
70:25 | this better when, if you stop think about it, normally, we're |
|
|
70:29 | for thicker sections with more, with plastics and more sand. Why might |
|
|
70:38 | automatically be a bad place for producing Ford? Maybe it has um minerals |
|
|
71:02 | aren't sand. Ok. Over over , we do have more carbonate. |
|
|
71:10 | have more plastic sands and shales over , but this is a much thicker |
|
|
71:17 | . I mean, 12,000 ft versus is a lot, right? |
|
|
71:23 | um if we have all that sediment compassion be an issue and then that |
|
|
71:31 | affect like pro permeability. Is that we're going for? Ok. |
|
|
71:40 | well, let me, let me uh back up and um, so |
|
|
71:44 | , we have this space in here uh it's obvious there's more accommodation space |
|
|
71:49 | here, there's less over here. , but what is it also obvious |
|
|
71:54 | more of in here? Remember this , this is, you know, |
|
|
72:01 | is the thickness of it. It have uh the structure, the an |
|
|
72:06 | like the other side does. And rem remember I'm asking you, |
|
|
72:14 | know, in the past, I've out when we're looking at conventional, |
|
|
72:19 | wanna see exactly this kind of thing opposed to that kind of thing. |
|
|
72:25 | want to see that Depot Center when , when we're looking for thicker Depot |
|
|
72:30 | , what are we looking for? , what part of the uh there's |
|
|
72:36 | things but what's the first kind of , um I don't know how to |
|
|
72:41 | this. Um I'm trying to get guys to think, but it's hard |
|
|
72:45 | telling you the answer. How do , um there's like a more period |
|
|
72:53 | subsidence, more period of subsidence, have more subsidence. But what's happening |
|
|
73:00 | that side of subsidence? It, know, is, is it just |
|
|
73:08 | and not being filled up. Is um not collecting like the combination? |
|
|
73:25 | , it's being pushed over into the space. Ok. Um I guess |
|
|
73:33 | stop trying but um you guys are to, trying to get there. |
|
|
73:38 | no, you know, in conventional looking, you know, a lot |
|
|
73:41 | times we, we want to make one reason we look for high net |
|
|
73:45 | gross is because we're looking for reservoir , ok? But in this |
|
|
73:53 | we're looking for a source rock that also the reservoir. What does high |
|
|
73:59 | rate do to a potential reservoirs Excuse me, a potential source |
|
|
74:05 | What would hide uh depositional depositional rates to uh accumulation of organic rich |
|
|
74:25 | It's a big picture thing. It , in this case, the sedimentation |
|
|
74:31 | the organic material and the concentrations of material that you see over here can't |
|
|
74:38 | over here because it's diluted. Do remember uh the example of the ridge |
|
|
74:42 | that I showed you where it was 1009 kilometers, 9000 m. I |
|
|
74:50 | time I say it, I don't it's true, but it is there's |
|
|
74:53 | kilometers of sediment in that pull apart in California and it's got lots of |
|
|
75:00 | rocks in it. But one of things that it does is dilute, |
|
|
75:06 | it's a dilution effect on the overall composition of the sediments throughout the basin's |
|
|
75:12 | . And therefore, this is the Texas Basin and you've got all sorts |
|
|
75:18 | uh, sediment coming in here from, uh, something similar to |
|
|
75:22 | the Mississippi River is today. Just stuff in here. You've got this |
|
|
75:28 | here, the San Marcos Arch here keeps it from getting into here. |
|
|
75:33 | is an isolated small basin where Anoxia prevalent. There's probably gonna be less |
|
|
75:40 | in here because it's a bigger open . And, uh, and it's |
|
|
75:45 | diluted. So the source rock over , not the, not the reservoir |
|
|
75:50 | , but the source rocks over here um on steroids over here. And |
|
|
75:57 | I don't know how I did that a pointer, but that was pretty |
|
|
76:00 | when I said steroids. And uh , the um uh and that's the |
|
|
76:07 | about being a, a geologist and geophysicist looking for oil and gas. |
|
|
76:12 | have to think about how these combinations things that are perfect in one place |
|
|
76:17 | perfectly wrong in another place. And all that's different here is that |
|
|
76:22 | we're focusing on a source rock and makes that source rock good because that |
|
|
76:27 | rock now will also be a reservoir over here. We would probably be |
|
|
76:31 | more of reservoir rocks, but we have a harder time of uh getting |
|
|
76:37 | source rock. But as it turns there are Jurassic source rocks over here |
|
|
76:42 | feed into primary uh plastic sandstones. . Um Not as, not as |
|
|
76:52 | as we want, but that's, how it works. And, |
|
|
76:54 | um, but over here we have really high graded, uh source rock |
|
|
77:00 | that's essentially, um, on steroids this part of the world. And |
|
|
77:07 | , um, like I said um, this, the lower Eagle |
|
|
77:12 | is what really is the uh very rich laminated part of this. One |
|
|
77:17 | the reasons you don't have to worry , um, um, breaking up |
|
|
77:25 | the Austin Shaw is because you've got upper Eagle Ford, which is um |
|
|
77:32 | word right here, burrowed. It's a better bedded and it's burrowed, |
|
|
77:37 | which is two unusual things I But nevertheless, um, it's been |
|
|
77:44 | a lot if it's brewed a that means the uh creatures that live |
|
|
77:47 | were eating the organics and uh making good meal out of it. And |
|
|
77:53 | what's getting preserved down here where it more anoxic and they couldn't thrive and |
|
|
78:00 | uh organic rich layer was preserved and course, it's organic rich and laminated |
|
|
78:08 | a lot of disruptions. Here. can see a lot of disruptions in |
|
|
78:12 | laminate because it's being bioturbated like Ok. Now, the bottom |
|
|
78:19 | you have to worry about fracking into bottom because the Buddha has natural fracturing |
|
|
78:23 | there could be aquifers that you have watch out for, depending on where |
|
|
78:28 | at. Ok. Here is a structure during the deposition of the Eagle |
|
|
78:36 | and you can see you have these shelves. There's a salt ridge here |
|
|
78:42 | . Uh There's this arch here, this basin in here is primarily the |
|
|
78:46 | Basin and the rest of this um are isolated here. It says organic |
|
|
78:57 | , uh less organic concentration, Why we have these, the wood |
|
|
79:03 | fluvial axes is coming in here and in sandstones and shales and clay, |
|
|
79:09 | silts and clays to uh further dilute uh potential organic rich things that might |
|
|
79:16 | in here. And so there's a of constriction of a bay and this |
|
|
79:22 | a bigger broader area uh that can uh water circulation that can prevent anoxia |
|
|
79:29 | happening. And also dilution of the material. You deposit a whole lot |
|
|
79:35 | sediment with the organic rain that's coming to make your source rock. It's |
|
|
79:40 | be less rich. If you reduce sedimentation coming into a basin, then |
|
|
79:45 | have almost nothing but pure organic This is a lot, this isn't |
|
|
79:51 | good as a lake basin, but close to some of the internally drained |
|
|
79:56 | uh lake basins on a large scale uh that actually preserved a lot of |
|
|
80:01 | material. And here's a uh a uh uh ice pack map of the |
|
|
80:12 | Eagle Ford. And you can see um uh there's a lot of the |
|
|
80:17 | in here. Again, the thermal uh or the uh thermal gradient and |
|
|
80:26 | of maturation is less as you go way you have, um, the |
|
|
80:32 | out here kind of insane and, , um, and, uh, |
|
|
80:38 | gas or wet gass rather. uh, and then up here you |
|
|
80:42 | getting oil and then you start to too mature oil, immature oil up |
|
|
80:45 | . But still some oil as you to the, um, go to |
|
|
80:49 | north over here it's, it's very to find these organic rich sales. |
|
|
80:56 | where the, uh, Stewart City margin in the Georgetown Edwards are pretty |
|
|
81:01 | together here. There's a little bit a break and here's the, |
|
|
81:06 | and here's the lower Eagle Ford, Buddha, the Del Rio. This |
|
|
81:10 | kind of an isolated basin at the of the lower Eagle Ford deposition, |
|
|
81:14 | also, uh, helped make uh, more likely to develop |
|
|
81:21 | uh, ox or anoxic conditions. , here's where some of the, |
|
|
81:27 | big fields are. Um, this BHP Billiton purchase. Um, one |
|
|
81:36 | the things that you, uh, don't see on here anymore is Petra |
|
|
81:42 | because, um, they sold it to BHP and, uh, it |
|
|
81:47 | $400. He bought the acres for acres, sold it for $10,000 an |
|
|
81:53 | and made money just off of And, uh, not quite to |
|
|
81:58 | extent of 12 billion. But, , um, the student, |
|
|
82:04 | that worked up around the Dallas area I was talking about made uh somewhere |
|
|
82:09 | 2 to 4 billion barrels for his doing something very similar to that. |
|
|
82:17 | . And again, uh this is of showing you a cross section across |
|
|
82:21 | arch. And here you can see low Eagle Ford is isolated over |
|
|
82:26 | You have something sim sim similar to over here. But then you start |
|
|
82:31 | get into these um uh different The wood B is, is a |
|
|
82:36 | um sandstone rich unit uh in the here. And uh there's some things |
|
|
82:45 | to the Eagle Ford here that they it the Pete the pepper here, |
|
|
82:49 | manna here. But this uh these lighter gray because they're less organic |
|
|
82:54 | only a small part of the organic feathers off around the top of the |
|
|
82:59 | Marcos Arch. And uh so you've got uh you've got diluted organic |
|
|
83:08 | over here that certainly had more oxidation on uh in the, in the |
|
|
83:14 | . And over here it's isolated and limited influx of sediments to dilute the |
|
|
83:21 | material that was settling on the OK. We just got a couple |
|
|
83:32 | things to look at and um we have a half hour to go. |
|
|
83:38 | um tight, tight gas sands are normally uh 0.1 millis which is really |
|
|
83:48 | , I'm not sure how that But uh but that's what it is |
|
|
83:53 | of course, um what I'm gonna , look what we're gonna be looking |
|
|
83:57 | here is something that's very unusual. course, there are tight gas sands |
|
|
84:02 | , uh, are produced, similar to, um, conventional, |
|
|
84:10 | , reservoirs and things that you, , uh, you know, you |
|
|
84:14 | play and work on the normal But the basin centered ones, it's |
|
|
84:20 | the depressions that you're going for, find the guest pockets and the sweet |
|
|
84:25 | , uh, to produce from. here is, um, one of |
|
|
84:33 | classic ones here and we're looking across basin. Um, I don't know |
|
|
84:40 | , but I've always called it the Creek Basin, I guess because the |
|
|
84:43 | Creek goes through it. And, , but here is uh the formation |
|
|
84:49 | you're looking at and they say here's top of guess what's funny about this |
|
|
85:14 | ? Do you see anything in here looks like a trap? Not |
|
|
85:23 | So, um, what's interesting is , you know, normally all of |
|
|
85:32 | , if there was gas like normally it would just come out |
|
|
85:35 | It would, you'd have tertiary migration the way to the surface. Uh |
|
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85:39 | are, this is sort of a scale cartoon and there are faults and |
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85:46 | in here. But the normal conventional and traps are up here and up |
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85:52 | . But down here, there's this mass of natural gas, it's pretty |
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85:57 | trapped by something like a dynamic, like a dynamic seal that we were |
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86:02 | about where pressure on either side of is closing the po throats and making |
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86:06 | difficult for migration to happen. And , this looks even harder to understand |
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86:17 | you've done a lot of geology. , uh, but here you can |
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86:23 | water and there's gas underneath the What could possibly be wrong? |
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86:27 | there's a lot of pressure in There's pressure coming down over here and |
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86:32 | a capillary issue which is kind of this in and, uh you reach |
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86:36 | point to the pressure, uh abnormal down here. And of course, |
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86:42 | expansion of this has caused sort of uh a pressure seal pushing up and |
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86:47 | depth in the well is pushing on uh capillaries down with the water. |
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86:53 | so you kind of get something that's similar to a dynamic uh pressure |
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86:59 | And this is what it looks like cross section. And um um if |
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87:08 | was to try to explain this to people I worked with in the |
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87:11 | they think I was insane. But this is basically what we think's going |
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87:17 | is the pressure across this, this . This cap, it's a capillary |
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87:22 | between here and here and uh some of it leaks out but, |
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87:29 | a lot of it is still trapped . And as, as um some |
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87:35 | pressure is released, you know, little bit escapes and then, then |
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87:41 | generation occurs, more builds up and lateral to these things, we, |
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87:48 | do end up having tight sands that , uh, the normal, |
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87:54 | geometry of what we would expect you know, water down here, |
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88:00 | , water and gas bearing zone down with minimum to no food flow and |
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88:04 | the gas all stuck up here. still, there's this funny issue |
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88:10 | uh, of a pressure of a war going on between things that shouldn't |
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88:15 | be, uh, uh, at with each other. And here's kind |
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88:20 | what it looks like again, at a, at a larger |
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88:23 | And here you can see this might one of the conventional reservoirs up |
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88:28 | This is a diagram that helped me believe it. And I can't doubt |
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88:32 | because I know it's happening, but still hard for me to uh understand |
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88:38 | . But you, you have the the higher over pressure down here. |
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88:43 | have capillary pressure in conflict here and through faults and some other things, |
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88:49 | little bit of it leaks out and all these, these uh conventional reservoirs |
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88:55 | have a funny configuration like this with similar kind of thing since there's all |
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89:00 | gas involved. Uh And, uh know, the, the water is |
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89:05 | top and the gas is trying to around it. Ok. If uh |
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89:14 | anybody understand this better than me? I, I thought it would be |
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89:21 | to point out to you that uh , uh even when we think we |
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89:26 | that gravity is simple. Here's a case of gravity, um capillary pressure |
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89:36 | overpressure fighting each other at some Uh That's making it very difficult uh |
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89:45 | this gas to actually get out of bases, the center of the |
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89:49 | In other words, it's a barrier migration. I guess that's the best |
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89:52 | of looking at it. OK. Then the other thing that we were |
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90:02 | look at, I used to love when professor actually, I didn't ever |
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90:09 | to worry about professors doing this because didn't have Power point. They drew |
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90:14 | on the board. OK. um you know, we looked at |
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90:21 | , we've looked at this. we're gonna take a look at these |
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90:24 | things here, car sands and oil . OK? So the tar |
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90:42 | you know, are mixtures of clay and, and bitumen and uh and |
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90:51 | the bitumen at least can be processed , with uh with the different types |
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90:58 | organic solvents. And uh and so kind of how this works. And |
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91:06 | um the oil gets extracted from this turning it into um something called a |
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91:13 | sin fuel. And uh that in has a pretty good footprint, hydrocarbon |
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91:19 | and a and an environmental footprint You can see uh Venezuela's got some |
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91:24 | big resources here. Of course, have the um in the subsurface, |
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91:29 | have the heavy oils and then you're to the surface uh they have some |
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91:34 | sands up here. Alberta has really things very close to the surface. |
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91:41 | uh of course, Saudi Arabia also places um that, um, and |
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91:48 | are billions of barrels, by the , that's 265 billion barrels. So |
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91:53 | a lot of uh a lot of tar sands and asphalt out there that |
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91:58 | , that we can use as a . And uh this is showing you |
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92:04 | it is in uh in Alberta, , obviously a little bit of it |
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92:09 | over into the next province and uh never have enough time to go into |
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92:19 | in, in great detail. But I'd like you to just go through |
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92:23 | and, and read it uh when get a chance. But I highlight |
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92:27 | because steam assisted gravity drainage, which SAGD uh produces uh recovery rates of |
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92:36 | to 60%. Uh One of the why this is one that they like |
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92:42 | most is because it's slightly in the and you still get a pretty high |
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92:49 | rate. That's actually a phenomenal recovery . Uh strip mining, you get |
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92:55 | recovery rate, but it's um you have to imagine if you have |
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93:00 | much area of tar sands near the and you have rivers and streams cutting |
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93:06 | it and even lakes uh forming around . You have to imagine that automatically |
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93:13 | natural existence of these uh deposits actually an environmental problem in itself. It's |
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93:22 | , uh, it's, it's um, damage free just in |
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93:27 | But if you go in there and stripping it, stripping whatever cover there |
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93:31 | be on it off, uh, makes it even more catastrophic. |
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93:37 | uh, and of course, it carbon to the carbon footprint that's not |
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93:42 | . Um, it's hard to say this is a problem because we've always |
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93:46 | it here. To me that excuse pretty weak. That's the excuse for |
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93:52 | . But uh but nevertheless, um a lot of reasons, this particular |
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93:59 | is one of the ones that is strip mining, which is, which |
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94:03 | very um uh which is very damaging the environment. Re releases lots and |
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94:10 | of uh CO2 in the process. this is kind of the, the |
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94:15 | that's favored by most people. They're to uh generate these sin fuels. |
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94:22 | uh the way that process works is lot like the horizontal whales. I |
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94:27 | showing you in a, in a where you actually um uh surround uh |
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94:35 | of uh the deposit with the steam , the steam chamber which has steam |
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94:42 | and it sort of heats up the area and then very close to |
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94:45 | You have oil production an oil well can uh not really oil but uh |
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94:52 | this a sludge that comes off of as it uh it heats up, |
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94:55 | becomes less viscous and you can produce at the surface. And here you |
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94:59 | see, uh they're using um, to, to pull it out of |
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95:05 | ground at the same time, even uh the viscosity is being reduced and |
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95:10 | uh the float characteristics are being Ok. And so, uh |
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95:17 | that's all I wanna say about tar . But I, I want you |
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95:21 | be aware of this, you there's an addition to the shale plays |
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95:24 | , that I think everybody's familiar Just trying to show you some of |
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95:28 | . And we looked at the Eagle , I'm trying to show you a |
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95:31 | of things that are a little bit . Uh There's certainly a lot |
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95:34 | a lot of other uh things uh that list that I showed up front |
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95:40 | that are considered unconventional resources. So next one is oil shale. And |
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95:49 | the difference between oil shale and shale ? I've already asked this question, |
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95:53 | maybe I can see if everybody remembers it is. You know, there's |
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95:59 | thing called oil shale and there's another called shale oil. Nobody has that |
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96:19 | oil. It's um oh, it deals with the extraction like one's |
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96:27 | to the finish line than the other something like that. Yeah, you're |
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96:31 | on it. And uh and I'm the geophysicist is on top of this |
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96:37 | uh but you're, you know, absolutely right. The um the oil |
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96:41 | . First of all, we had we called oil shell before we had |
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96:45 | ever produced any shale oil. So shale, the term oil shale was |
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96:50 | owned by um this carriage enrich. can't, you can't use solvents to |
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96:56 | it out of the ground. This enrich uh uh thing that we have |
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97:05 | uh in some of these lake The only way to turn it into |
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97:10 | liquid is to heat it. In words, to try to advance the |
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97:14 | maturation of the carros so that they to generate fluids. And um and |
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97:22 | we can mine these but that's really and most of them are, are |
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97:26 | deep and uh you could mine this actually process them by heating them up |
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97:33 | that, of course, is Uh But uh having said that oil |
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97:39 | , the carris will burn at the if you, if you have a |
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97:44 | piece of oil shale, that's over toc and probably less than that, |
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97:49 | can light it with a match and burn um I guess, sort of |
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97:54 | Pete. But uh but nevertheless, it, it's, it's all carriage |
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97:59 | , and um and so um they , they do strip mining but uh |
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98:06 | other way they pull it out of ground. Uh And here's some of |
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98:09 | big basins, the Green River basin course, and the UTA Basin and |
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98:13 | Peons Basin are big areas and I've worked on issues of lacustrine basins |
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98:20 | these are big latrin basins and good of um less productive, less cooked |
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98:28 | . In other words, the deepest of these have uh matured, but |
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98:34 | quantities of the um of these basins still have immature Carris, which is |
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98:41 | we have oil shale, shale oil what is when we produce oil straight |
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98:47 | of a shale. It's, it's like you said, it's farther down |
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98:51 | line. And uh and it may viscous, it may be uh heavy |
|
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98:56 | some cases. It's not. And and it's uh but it's, it's |
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99:02 | Carro that's already been metamorphosed into uh the liquid. And here's some deep |
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99:11 | shells and carbonates and um uh some these beds may actually be part of |
|
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99:16 | mahogany ledge. Uh But the to in here uh probably range between 15 |
|
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99:23 | 20%. And of course, these the limestones uh that fall during uh |
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99:30 | productivity periods and deposition. So what one of the things that uh shell's |
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99:38 | that's um they had some success with was you actually put heaters into the |
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99:46 | wells that heat it just like he do here. And I don't know |
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99:51 | it was steam injection, but it have probably was. And uh and |
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99:57 | these are the heater wells then they that if they put in refrigeration |
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100:03 | Uh And, and I'm, I'm not sure exactly how they, |
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100:08 | , did this but they would, , but cool, cool, |
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100:15 | chilled waters into these, into these to create sort of an isolating insulation |
|
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100:22 | these would sort of block around this and help concentrate the heat through the |
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100:29 | area and through that they were able do it. I don't think they |
|
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100:32 | got to the point of, uh, making it economic, but |
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100:38 | theory, they've, they've figured out to make it work. And here |
|
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100:41 | can see this would be a, producer. Well, right here. |
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100:47 | . And with that, we're done many questions about unconventional, even if |
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100:55 | didn't talk about it. Ok. , um thank you guys for letting |
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101:04 | break earlier uh on Saturday and uh I, I'm, I'm gonna send |
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101:12 | email out to everyone and let you what the um let me open this |
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101:17 | up again here that, so I a quick question. OK. There |
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101:32 | go. I just stopped the Go ahead. Hey, earlier you |
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101:38 | mentioned unconventional um sources and I think associate it with uh uh CO2 storage |
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101:46 | carbon storage. Um No, that, that wasn't, that |
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101:53 | that wasn't associated with, with uh it's associated with unconventional. In other |
|
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101:59 | , it's a type of unconventional, not. Um um uh Let me |
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102:06 | back to the slide. Mm I to share my screen again. What |
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102:15 | is carbon capture OK. Hang on minute. Uh Let's see. |
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102:33 | And you have to remember when we're about unconventional course resources. It's not |
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102:38 | shales. Ok. Unconventional resources are these different things. One is shale |
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102:46 | which I think was what your question . Hayden. And, um, |
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102:51 | , but there's other unconventional resources and tar sands have nothing to do with |
|
|
102:57 | , the oil shells have nothing to with these, the gas hydrates |
|
|
103:01 | or clathrate. Um That's a really thing but it, you know, |
|
|
103:06 | another 20 minute uh discussion to get these, but we talked about these |
|
|
103:12 | uh they relate to um um what you call it, um gas clouds |
|
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103:23 | uh that are coming up, seeping that come up to the surface, |
|
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103:26 | reach the proper temperature and uh and and they, and the uh the |
|
|
103:32 | turn into uh crystals and, and clathrate that create these structures and |
|
|
103:39 | So there are people that have actually at producing these things. There's another |
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103:42 | that's really important is coal bed And uh and that's kind of a |
|
|
103:47 | too. And we, I've actually a student drill into coal mines and |
|
|
103:54 | get carbon capture credits for burning the because the methane is worse. Uh |
|
|
104:03 | the CO2. So they turn the into Co2 so that methane doesn't get |
|
|
104:08 | the atmosphere directly leaking from mines. there's a lot of things like |
|
|
104:12 | And, um, and here's additional , uh not on this list, |
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104:18 | this would be, you know, the size of a bullet here. |
|
|
104:22 | , carbon storage is, is another in the sense of something we can |
|
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104:29 | with wells. Um, that's it's a, it's an economic resource |
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104:35 | have a place to park CO2 is, I guess a better way |
|
|
104:38 | saying it also to store uh gas you might be able to use for |
|
|
104:44 | floods and that kind of thing. then these other things, uh heat |
|
|
104:49 | uh is also an unconventional and and actually geothermal is too, but |
|
|
104:54 | didn't uh I didn't even list that , but some of these other things |
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104:58 | things that we can put in wells take out of works, essentially what |
|
|
105:03 | getting at that. And with some the gas clathrate, you have to |
|
|
105:08 | like an apron uh that would go top of it and uh and try |
|
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105:13 | produce it that way because it's, that's extremely dangerous because if you mobilize |
|
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105:20 | you know, a massive amount of frozen gas and turn it into uh |
|
|
105:26 | gas, you know, you can issues that are, are catastrophic because |
|
|
105:31 | changes the density of the water as comes to the surface in any vessel |
|
|
105:36 | on top of it can sink. it's uh it's a big thing. |
|
|
105:41 | in terms of carbon capture capture, mean, basically what people are trying |
|
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105:46 | do is to capture it where we it like at a um they |
|
|
105:50 | they've done a whole series of um things. Uh Well, not a |
|
|
105:57 | but a few where they actually have generation with coal fired plants and they're |
|
|
106:03 | the CO2 at that plant and processing and shipping it into the ground. |
|
|
106:09 | There are other things that they're trying do to just uh um different ways |
|
|
106:15 | try to pull it out of the . But obviously, the quickest and |
|
|
106:21 | and biggest gain would be to um something, capture the carbon that's coming |
|
|
106:28 | of a carbon source like a uh coal fired or a gas fired uh |
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106:36 | plant. In other words, um of make it net zero. In |
|
|
106:41 | words, you would collect, you collect all that carbon that you're generating |
|
|
106:45 | push it down into the ground. you could use that for doing a |
|
|
106:50 | flood. I didn't mention CO2 but instead of uh natural gas, |
|
|
106:55 | can also flood the reservoir with uh which which puts it away in, |
|
|
107:01 | into the ground and actually helps us pump up reservoir pressure and maintain reservoir |
|
|
107:09 | as we're depleting the oil or, natural gas that we want to get |
|
|
107:13 | of it. And it has certain and characteristics that make it favorable to |
|
|
107:18 | of these other floods in terms of tension and uh and uh relative |
|
|
107:27 | And so I, I hope that the question on what is carbon |
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|
107:31 | Really? And um you know, to pull it out of the atmosphere |
|
|
107:36 | , would I think would be limited . But uh but you know, |
|
|
107:42 | you, if you could have capture it at the back end of |
|
|
107:46 | car that drives down the road, be on to something And uh and |
|
|
107:53 | um would give us more time to to cleaner energy. And I think |
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|
108:00 | basically the whole purpose of it. , I was just curious because |
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|
108:05 | I know at work we're doing a of projects for companies that are like |
|
|
108:10 | um we're doing like extra f analysis in the Permian basin. And I |
|
|
108:14 | just curious like how carbon capture would in a basin like that, that |
|
|
108:18 | was so much unregulated drilling back in day. It's like Swiss Cheese. |
|
|
108:23 | I was like, how would carbon work in an area like that where |
|
|
108:28 | just so many wells? Well, , and, and um you |
|
|
108:32 | they, there's all sorts of, mean, there must be 30 different |
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|
108:36 | you could do. And you just this idea of poking a hole |
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|
108:40 | a mine and sucking out the methane flaring it uh that reduces the carbon |
|
|
108:50 | by a factor of 52 or, the heat index rather because methane holds |
|
|
108:58 | more heat than CO2 does. So a fif, there's 50 times 52 |
|
|
109:04 | worse to let that methane out. there, there are companies that are |
|
|
109:09 | capturing, they're getting carbon credit, really storing CO2, but they're getting |
|
|
109:15 | credit. Half of that uh 52% 26 20 or 52 times. |
|
|
109:23 | they get credit of 26 times for the methane. They turn into |
|
|
109:29 | And because, you know, you to give back a little bit of |
|
|
109:31 | you take because you are burning something it's, it's the same thing with |
|
|
109:39 | biofuels. If you're, if you're recycling uh living material that's gonna biodegrade |
|
|
109:49 | , that's one thing. But if actually producing the biomaterial for biofuels, |
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|
109:56 | actually adding CO2 and the process of agriculture requires machinery and the net that |
|
|
110:04 | get out of that is, is zero just in terms of energy, |
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|
110:09 | it's actually creating more of a carbon . So I have no idea why |
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|
110:12 | think biofuels are good. And uh it's a, it's a complicated question |
|
|
110:18 | a lot of, a lot of they're doing with carbon credits is things |
|
|
110:22 | burning, burning methane to get And uh there's also uh different types |
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110:30 | places where CO2 is released, different where CO2 is released where they're trying |
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|
110:35 | figure out a way to absorb it uh into things and or push it |
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110:42 | into the ground. And uh like you would, for example, |
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110:46 | you're producing oil and gas, you're get some CO2 2. If you |
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110:50 | capture the gas and the CO2 and both of them back in the |
|
|
110:54 | you're saving on methane and you're saving , on CO2. If you naturally |
|
|
111:00 | everything that you produce, like to make an oil well, |
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|
111:06 | sometimes you have to flare uh the so that you can get that oil |
|
|
111:12 | because you don't have anywhere to put methane. Now, if they could |
|
|
111:16 | out in all cases of how to the methane rather than flaring it, |
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|
111:21 | get another 26 points out of that points for completely taking the methane out |
|
|
111:28 | the system. And that would that would be a real winner in |
|
|
111:31 | of carbon capture. And uh and I, and I don't know |
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|
111:37 | we don't do this more often, there are a lot of places where |
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|
111:40 | producing conventional resources where if we figure a way to economically take any of |
|
|
111:49 | gas that any of the associated gas comes out with it that we don't |
|
|
111:54 | for, for generation, put that into the well and put that back |
|
|
111:58 | the well energy automatically your, your you could also get 52 credit points |
|
|
112:05 | each mole of that that you put into the ground instead of flaring. |
|
|
112:11 | uh there, there's a lot of like that, that we can |
|
|
112:14 | It all takes engineering and uh every uh like right now they, they |
|
|
112:20 | , it's borderline with the, these plants that they're trying to use to |
|
|
112:26 | carbon storage. Wall Street Journal had really good article on it if you |
|
|
112:30 | the Wall Street Journal and uh when are working well, they're, they're |
|
|
112:36 | breaking even. But uh but it's, it, the engineers will |
|
|
112:41 | up with a filter or something that absorb this CO2 better and, |
|
|
112:46 | and so that they can pull it and, and put it into a |
|
|
112:51 | and send it back down. Uh know, the better we get at |
|
|
112:56 | , you know, that's some, technology that's worth spending money on, |
|
|
113:00 | , to get that stuff back into ground because if, if you |
|
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113:05 | if you can get the benefit of without the, um, the negative |
|
|
113:11 | of CO2, uh you're obviously gonna , be making a lot of money |
|
|
113:16 | somebody and, and saving the planet the same time. Does that answer |
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|
113:28 | question? It does. Thank May maybe it maybe a little |
|
|
113:35 | No, it does. I was curious. Well, I mean, |
|
|
113:38 | , it's a, uh, it's work, it's definitely a work in |
|
|
113:42 | . And uh, and there's, gotta be 1000 ways they're already trying |
|
|
113:47 | , to figure out how to, to, how to get this, |
|
|
113:51 | get the CO2 back into the ground how to figure out a way |
|
|
113:55 | to keep having such a large And, uh, you know, |
|
|
114:00 | EPA did a big thing for us the seventies to get particulate pollutants, |
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114:05 | example, out of the atmosphere. they, they didn't do such a |
|
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114:09 | job and, and everybody's resistant uh, helping them get the, |
|
|
114:15 | , the invisible pollutants that come out the uh come out of some of |
|
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114:20 | uh refineries and, and uh chemical and uh and that's been a |
|
|
114:24 | But uh again, it's, it's of these are engineering problems and uh |
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114:30 | as clever as we are and as as A I is supposed to |
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114:34 | uh you know, if we put little in a little bit of energy |
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114:38 | carbon capture and things like that, um the problem with CO2 may become |
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114:44 | moot point uh if they have some breakthroughs. And uh that's, that's |
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114:50 | of what I'm hoping for for the because I don't see us getting the |
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114:55 | alternates up to steam as quickly as want them to. Uh because there's |
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115:01 | lot of, a lot of difficulty the entire food chain, so to |
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115:05 | . And, you know, all way from producing enough cars to producing |
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115:08 | electricity, to transporting that electricity on lines. And uh and, |
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115:15 | that sort of thing that, you , we, we have a long |
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115:17 | to go to, uh, to fully electric. So, with |
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115:24 | thank you guys for paying attention. you for giving me a little break |
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115:27 | Saturday. And, uh, if you guys want me to send |
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115:33 | the schedule for the exam. um, uh, and also when |
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115:39 | , the final exercise is due or you, uh, do you, |
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115:42 | you all write it down? It's at one on Friday, right? |
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115:49 | at 1 p.m. Ok. Um, , so it is at 1 p.m. |
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115:55 | Friday. I thought it was gonna at, at, uh, 5 |
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115:58 | 7 on Friday. But we, , we can do it. I |
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116:03 | something written down wrong. Then uh, 1 p.m. That's right |
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116:08 | uh, uh, who was Anthony? Anthony couldn't make it at |
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116:16 | to 7. Is that correct? correct. Ok. So, so |
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116:20 | do it. We will do, do the online exam at one |
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116:27 | 2 30 then, um, and , uh, I, I |
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116:33 | is a here, I don't think here. He wanted to do it |
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116:41 | person at once. So that makes easier for me. I get |
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116:44 | I'll do it all at once. then the, um, let's |
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116:55 | the, well, the, excuse me, I have too many |
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117:05 | on my phone. Yeah, the , the mapping exercise is gonna be |
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117:23 | on, um, the 17th. , the exam, the final exam |
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117:30 | be Friday at 1 p.m. on the and then on the 17th, your |
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117:35 | exercise will be due. Does, that sound right? Guess? |
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117:45 | Yeah. Yes, sir. So we're all, we're all |
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117:52 | Now, now we're all on the page. Ok. I'm glad I |
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117:55 | the question because I would have messed again. Thank you for keeping me |
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118:02 | line. Ok. So, uh luck with this. And um, |
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118:09 | the, uh, I've loaded, , this past weekend's, uh, |
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118:16 | and I'll be loading this one uh, before I head out |
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118:21 | So, um, things should be . I don't know, it takes |
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118:26 | while for them to get processed uh, video points, but they |
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118:31 | be up by now. They uh, about two hours ago, |
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118:35 | hopefully they're, they're available now, if not, they should be sooner |
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118:40 | . Um, well, at uh, sometime this evening they should |
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118:44 | up and up and running. But you don't see them by tomorrow |
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118:47 | let me know and, uh, may have to reload them. |
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118:54 | Sure. Ok. Well, it's been nice having you guys in |
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118:58 | class. Um, uh, I've done a three week course before. |
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119:05 | , the last time I taught one these classes which, which was only |
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119:09 | , uh, 16 months. less than that, it was about |
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119:13 | semesters ago. Uh, I, had the last, uh, I |
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119:20 | I had the last. Well, it was bio so I only teach |
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119:23 | thirds of that course. Uh, it's been about, it's been exactly |
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119:29 | months since I taught the four week . But I've never taught the three |
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119:34 | course. So, sorry about my with timing and, uh, some |
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119:40 | the delays we had and that we to do any of this online. |
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119:44 | , uh, really enjoyed, a lot of the feedback we were |
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119:48 | in class and, uh, even questions you just asked me. |
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119:52 | so have a good, good And, um, oh, by |
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119:55 | way, your grades are all pretty in the same bucket. So, |
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120:00 | , so I have to, figure out who gets an A or |
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120:03 | A minus at this point. uh, but at the same |
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120:07 | you know, you have another exam that could affect the curve and, |
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120:12 | , and you have the exercises which help in most cases help pull up |
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120:17 | , uh, pull up your So, uh, good luck with |
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120:21 | you've done. If you haven't turned your first three exercises, get those |
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120:24 | as soon as possible as well. , sir. Yes, sir. |
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120:31 | too. Thank you. Thank Thank you. Thanks. Ok, |
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120:37 | |
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