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00:12 OK. Um As geologists and uh maybe Geophysics even more than in

00:19 past because they're doing things now that to uh reservoir management. Um A

00:27 of you will at some point in career, get involved with um uh

00:33 facility locations like platforms and that sort thing. If you're working with a

00:37 company, maybe drilling 11 well and pad and there, maybe somebody within

00:42 company that's really good at setting up uh your pad, your pad uh

00:47 and whatnot onshore and uh trying to things up. But uh oftentimes the

00:55 and, or the geophysicist can get in some of this. And uh

01:00 a whole um a large number of types of wells. You know,

01:06 of the wells we drill here here the list. It says uh production

01:15 , injection wells, but you can have dry hole wells where you just

01:19 it because it's the first uh you're drilling in a particular uh acreage

01:24 you've acquired from somebody and it's, kind of like a Strat graphic um

01:31 and you're, you're drilling it to what the section is, and if

01:34 actually can find any oil, sometimes a AFE application for expense to uh

01:41 cover uh the cost if you decide turn it into a production well or

01:46 . But a lot of times you may have dry hole, hole

01:51 . And in that case, uh that case, uh you,

01:58 you and your engineer, reservoir engineer uh get together and, and have

02:03 , both scenarios costed out. So , there's uh injection wells for enhanced

02:09 recovery. Uh You're gonna have utility uh to produce fluids or dispose of

02:19 . And of course, it depends where you're at and what you're

02:22 You may, you may have a well, just to add a gas

02:26 to a gas cap, that kind thing or uh there's water uh disposal

02:32 all around. And unfortunately, too of these, well, uh water

02:36 wells are, are shallow and they're they're susceptible to breakthrough to the surface

02:43 you can get uh all sorts of uh collapse structures and that sort of

02:50 , creating sinkholes that can be dangerous to people. And uh and sometimes

02:55 cities then of course, the relief which uh when I was working on

03:00 , they were kill wells two that worked on and kind of controlled were

03:05 East Cameron 81 and number nine. uh then it sort of on the

03:12 got involved with Macondo number two. , uh, so tho those are

03:17 kinds of things that, uh, you can drill then, then of

03:21 , uh, you start to worry a lot of the well ge geometries

03:24 the geometry of the well patterns and that sort of thing that you

03:29 up and, uh, often you to worry about things like shallow gas

03:33 , especially if it's, uh, . Um, another whole group of

03:39 is overpressure and under pressure. And , in a given region, a

03:44 of people have drilled a few wells uh oftentimes they know which intervals are

03:49 pressured or under pressured. And uh could always be in a regime.

03:54 , you know, it's not there the Macondo Well was drilled, they

03:57 they had a high pressure system at considerable depth which is always dangerous and

04:03 they kind of got sloppy with which didn't help. And um there

04:08 things in places uh where you can have mud slides. You know,

04:11 talk about the uh turbidity currents, uh sections of the uh shelf edge

04:20 uh a actually up on the shelf a little bit of a tilt and

04:24 there's a, a bit of a or whatnot, either due to storm

04:29 and, or, you know, in places where we have earthquakes,

04:33 that would create some kind of uh whole sections and in like hundreds

04:38 acres of uh substrate can start sliding a hill. And uh one place

04:45 that was real, uh common where mud slides in, uh on the

04:50 where main passes, they actually had build, diverter to uh, to

04:55 the uh the mud to pass around , uh the rigs, the legs

05:01 the rigs and the platforms to uh keep them from being destroyed. It

05:06 on. They uh they lost a uh platforms back in the sixties

05:11 and early seventies until they got this out. Folks at LSU did AAA

05:17 of uh research on um these types things where you could get mud slides

05:23 . Uh There's also things that you have to worry about. If

05:26 a lot of uh be paic things other uh metal rich uh grains in

05:35 uh formation, you have to be with it. Uh If you acid

05:39 , you can turn, it can turn into a gel that clogs up

05:43 the porosity nol and actually destroys And there's other things that you have

05:48 be careful with, with hydrofracking. normally not with a vertical well,

05:52 with the horizontal wells, you have be very careful. And uh,

05:56 then of course, uh you will all sorts of uh logging runs and

06:02 certain types of production data you might depending on whether it's an appraisal well

06:07 something in, in a mature you might uh have, have uh

06:12 uh request logs that you need that include production data. This is just

06:18 you uh west of Shetland Islands. is out of your textbook. Uh

06:25 when it's just showing you a spider of what was often very common and

06:30 is uh offshore where we'll have a located platform and we drill deviated wells

06:37 in many directions. In this it's showing you they have injection wells

06:42 this little arrow symbol. Here's another over here, one over there,

06:46 over there. And uh again, whether or not you need an

06:51 well, depends on whether you need sweep some bypassed oil. And also

06:57 it's economically feasible to do such sometimes it can cost more than um

07:03 the uh potential recovery of the bypassed . And this is just showing you

07:10 in the book, I think it's black and white diagram. I got

07:14 and it's a little bit different. got this from Lewis uh back around

07:20 where he was showing how uh we now have ways to uh graphically

07:27 the well bores and where they're, they're penetrating and the target interval and

07:33 what's underneath them so on and so and showing you some seismic lines.

07:38 is like having a A two D to help you grasp the uh the

07:45 dimensionality of this diagram which is, is plotted on a 22 D

07:51 but it's plotted in such a way it looks like it's three dimensional.

07:57 . Uh Everybody's heard an awful lot um horizontal drilling in Texas and in

08:04 Pennsylvania and North Dakota. But what lot of people aren't aware of is

08:10 the, the long reach uh horizontal really got started uh in the North

08:19 and in the early 19 nineties, this is uh which farm field in

08:24 UK. And uh aside from uh this, in the early eighties,

08:32 were also drilling horizontal wells in the to improve the cross sectional area uh

08:38 the uh of the pipe, the pipe so that you have more surface

08:44 between the rock and the differential pressure you find in the well board that

08:48 actually help it flow out and up the surface. Anyway. Um This

08:54 one of the uh the longest ones was ever drilled. Um And uh

08:59 the time and here you can see over five kilometers and um and so

09:08 uh a good close to three I guess of distance. And uh

09:16 kind of thing was, was not that well heard of even in the

09:20 chalk wells, they didn't drill them that far, but technology had to

09:25 , to do this. This was done for environmental reasons. Um They

09:31 a farm site and uh they wanted offshore, get some offshore oil,

09:36 were able to get surface rights and underneath everybody else's acreage and get something

09:42 without putting a platform offshore. Because a, um, a part of

09:46 the UK where uh they had nice and whatnot. And here you can

09:51 the kinds of things they were And um, this is where uh

09:56 of those first wells came and it way out here past this peninsula

10:01 And uh they managed to keep the the area looking, uh uh naturally

10:08 looking. And uh and at the time, they were able to capture

10:12 resources that were out here without uh a lot of uh uh structures and

10:21 into the North Sea. And on of that, the water out here

10:25 get pretty rough. And uh I any platform that had to go out

10:30 would have been a rather significant structure to be able to withstand some of

10:34 storm waves. One of the uh problems, of course, with uh

10:41 doing this kind of thing and um sorry about some of my distractions,

10:48 uh had a little problem with the group ongoing before the class started

10:54 Um Nothing serious. One of, of the key things is to uh

11:00 a kickoff point and of course, I don't know if they still call

11:04 a kickoff point because they can um the, the drilling assembly, uh

11:10 uh turn it and whatnot a lot than they used to actually have a

11:15 that would kick these things off and and help it get into angle.

11:22 uh we could steer some but not as much as they can

11:25 but almost all wells. And I think still a lot of them

11:29 dri drill a pilot hole, at , at least a few of the

11:33 in a given area so that they get a really good idea of the

11:37 section. It's really critical that you this vertical section, not only the

11:42 zone, but what's above it and below it if you know what's above

11:46 and you know, it's below Um It, it really helps you

11:51 understand how close you are to the and where you have to turn.

11:54 of course, you need to have idea of the Strat gray here so

11:58 you can start turning at this point than this point or that point or

12:03 way up here and, and have . And uh this is kind of

12:08 you one in another part of the Sea uh that, that got down

12:15 into these uh Jurassic sandstones. And , and you can see how they've

12:22 these channel sands, it was able sort of corkscrew its way through this

12:27 hit sort of the sweet spot. before that there would have been something

12:31 drilled into it to make it possible them to, to see they were

12:35 the tar and uh then getting down the uh sands within the nest and

12:41 below that. And uh and of , if for some reason, they

12:46 below this, they have, they have a good Strat graphic section to

12:50 out exactly where they were at in of being below the target area.

12:58 um from a reservoir management uh a lot of these things uh go

13:07 . And of course, again, the reservoir is extremely homogeneous and high

13:11 permeability, you don't need to do lot of this. But what the

13:15 tend to do is something called the model. In other words, it's

13:19 on the rocks as they sit in ground. And the uh engineers do

13:23 reservoir simulation, it's called a dynamic because it's based on changes through time

13:30 uh formation pressure, uh gas oil , all sorts of things that,

13:36 let them know that fluids are being . And uh I showed a few

13:42 that went over some of the things they actually look at. Uh Another

13:46 we can do with geophysics is uh , they'll do something that uh a

13:55 um size mix so that they can of characterize where the fluid mass

13:59 And especially if they have um converted which includes uh S uh excuse

14:06 P waves and S waves. They of do that at the beginning of

14:11 production and they start doing it on yearly to multiple year basis to see

14:19 the oil water contacts moving and how they can actually see it. And

14:24 so they can get some real vis . This is something geophysics were uh

14:30 involved in, in the past. now they're um over the last few

14:34 , the, the last decade for . In the decade before this

14:39 uh they looked at it quite a . Uh Then after, after

14:44 of course, if product production drops , you start to sorting out where

14:49 might have uh bypassed uh oil or . And uh if something like a

14:55 flood helps, sometimes infill wells can uh something that you consider other things

15:01 fracturing and acid around the well Uh The well bore can, can

15:07 very helpful. Of course, uh fracturing is, is famously known about

15:13 uh unconventional resources as that's uh part the horizontal well fracturing um ct or

15:23 couple that uh that help us really a lot of these shales that have

15:27 permeability. And of course, there's uh enhanced oil recovery methods and we

15:33 go into all of them, but will mention a few. And uh

15:38 course, primary production is basically considered you can get with natural flow,

15:44 often choked. In other words, not letting it flow out at full

15:49 if, uh, you just kind open. In fact, you almost

15:53 do this. Open the, well bore to a natural flow.

15:58 it's at great depth, you're gonna significant pressures and you'll overproduce the well

16:06 , and because of that, the you pull on the oil, the

16:11 the water behind it can move and water can outpace because it has a

16:17 higher relative permeability to oil and it'll run past the oil. So you

16:22 choke Tokyo uh production at the well to make sure that uh that you're

16:30 uh overproducing it and reducing the pressure quickly because that's pretty much the worst

16:36 you can do during World War which happened even before I was

16:42 Um Sometimes they needed oil so They uh they actually stopped choking a

16:49 of wells and they damaged a lot wells, but they needed the oil

16:53 a hurry to uh outs supply the the foes that they were dealing with

16:57 that time. Next step would be water uh secondary recovery. And that's

17:05 what we call water injection or gas . So it's some, usually when

17:08 sent uh putting something natural in there add reservoir uh energy back into the

17:16 reservoir. And that's what secondary production . And tertiary is when we do

17:20 things to uh try to help the mix better with some of the

17:26 And that alleviate some of the issue relative permeability. And uh and also

17:33 their thermal methods which uh which they to kind of uh heat things up

17:41 to uh try to make viscus oils viscous. And in some cases,

17:46 actually used to uh in uh in shales. Some of the thermal methods

17:53 actually used to uh to uh try , to mobilize and, and actually

17:59 alter the carriages to some extent so they're actually liquids instead of uh just

18:07 . OK. Here's an example um 40 seism from slumber and this was

18:14 in 2002 and it's getting a whole better. I'm sure it's uh better

18:19 . But this is a really good . Uh the tools as they

18:25 uh you're able to come up with than one or two examples that can

18:28 you something that's so clearly working. the old water contact at one point

18:33 time. And uh let's see, can't quite see it, but it

18:37 like it's see if I can uh , 1985 to uh OK,

18:55 And of course, this was one the best examples they had to show

18:59 2002. And of course, as has continued to get better every

19:06 uh this method is working better and places and of course it's not

19:11 So, um, so it's gonna in an area where, where,

19:16 , knowing exactly what's going on with royal water contact is important to

19:21 Uh, and they, and they have an example here, but I'm

19:24 there are examples now where, you might be able to see where

19:28 have been flushed and where things have been flushed, uh, which would

19:32 direct you to drilling a new primary . Well, a fill in.

19:36 , and that sort of thing, , uh, thing that can

19:45 uh, important for geologists to understand , um, we always have to

19:52 gravity and, uh, we're we're gonna try to pro,

19:56 have a water sweep. This is good sort of a good cartoon right

20:01 that I have the cursor on. an injection. Well, and it's

20:04 , pushing water up into this Uh, and you're trying to produce

20:08 just, just, uh, up of it. And here you've got

20:13 one pushing oil up dip of Um, here's an example,

20:20 from the surface of that same but they have other, uh,

20:25 . Here's like a four spot where have a production well, in the

20:29 , this might be if you um, sort of like,

20:33 some attic oil that's trapped and you're to squeeze it from all sides and

20:37 top of the top of the anticline , or the structure might be right

20:43 where this is and you're trying to , uh get that to uh push

20:46 oil uphill. So it's a little different map model than that. And

20:52 the thing called the Seven Spot one the Nine spot. One of the

20:56 that relates to. Um And I know if I've, if they've actually

21:03 it, but if, if you , um this is a horizontal

21:09 and you had another horizontal well over and another horizontal, well over

21:14 one of the things I know Schlumberger working on around 2005 and six.

21:20 I, I don't know if they uh got people interested in it,

21:25 some of those wells, they they'll have um a horizontal well

21:31 And then instead of having water flow that direction, they have the water

21:35 shooting in this direction and in this , they basically have um a primary

21:43 well in the middle, then they'll a side track, that's an injector

21:47 here on this side and another side , that's an injector over here.

21:52 I'm kind of uh without having another . I'm trying to explain to you

21:56 uh uh that could be much more in, in the fact that you're

22:01 um going down and uh immediately from beginning of your uh horizontal.

22:07 trying to figure out a way to , push the uh hydrocarbons in this

22:12 . In this direction. But in the, in these low permeability

22:18 that can be difficult. This uh might work even in high permeability ones

22:24 some of the chalk fields and some those sandstones I was showing in the

22:28 where they already have horizontal wells. . This, this uh kind of

22:38 uh uh a nice 3d uh representation the problem with relative permeability and how

22:48 can cause coning of the water. the well bore and uh because the

22:54 bore is drawing down pressure here, , uh all the fluids are gonna

22:58 screaming up here. And of the uh the water with that,

23:02 higher relative permeability is going to try cone up into it. This is

23:07 it would look like in one cross uh pretty much on strike with the

23:13 of the reservoir. This is this looking at a dip section of the

23:18 and then this is looking at it the map view from the map

23:21 You get an idea of what's happening your reservoir as this water is coning

23:27 . In other words, vertically, trying to go up uh laterally,

23:30 trying to move up, dip in an arrow sense. You can

23:34 that also and of course, that's cusp. And um you can have

23:42 like this uh where your initial oil contact is down here. You've got

23:49 injector pushing water up here. uh, you can see that at

23:54 point that injector well down here, is a, is a perm

23:59 an impermeable barrier. And, so you have this kind of trap

24:04 to the side, this particular producer produce until the water gets up

24:09 uh, up to here. But one's gonna be trapped off,

24:12 down to there. So this may leaving some attic oil behind and,

24:18 , that would be a type of bypassed oil or uh oil that uh

24:23 additional um uh drainage on it. , you didn't have preparations all the

24:30 to the top of this thing. they were down here, you,

24:32 might leave even more attic oil which happens quite frequently and this is

24:37 showing you what the sweep looks like from a map view relative to this

24:43 section. Here's another thing that you know, we, we always

24:48 about these fining upwards and coarsening upward . And uh this is like a

24:55 Gama log in a way. But here, here, it's showing your

25:00 um is higher here and it gets down here in this one. The

25:07 is higher and it's lower down So this could be a coursing upward

25:12 and this is a binding upwards And uh just uh I hope somebody's

25:22 attention. I like this diagram because gives me a chance to ask the

25:27 a question which one first of and anybody can answer which one of

25:34 looks like it's getting better sweep of reservoir. Would it be the top

25:50 ? Yeah, I would say the one. And why, why do

25:53 think that, assuming it's a good ? Why would you think that,

26:06 , because of the migration direction of oil, the water, the impact

26:10 the water on the oil? And, and, but,

26:13 one, you know, because we're at a cross sectional area, cross

26:17 area is not everything, but it's part of a volume. It's two

26:21 of a volume you can see the cross sectional area that's, that's

26:25 flushed is much greater than this cross area. And uh and that's why

26:31 was obvious to you, I And uh and so that's absolutely

26:36 So having said that um what is about coarsening upwards that seems to work

26:44 better than um binding upwards? what physical factor do you think is

27:00 this happen? Gravity? Absolutely. said that me, Stephanie the

27:12 Of course, yes. Gravity. has a role in everything.

27:17 now I'm sitting here thinking about but what if the sweep was too

27:22 ? Um If we looked at this a different perspective, this could be

27:29 a thief zone up here if it , if it breaks through too

27:32 right? And uh so it's, know, that this is the right

27:39 in one in one way. But could be the wrong answer. For

27:43 , if this was happening, happening , what we could find out is

27:48 water would break through and just block the entire, uh, production of

27:53 . Well, and you'd leave all oil behind. However, this

27:59 uh, if you think about thief because it's on the bottom, it's

28:04 , the water is not breaking So it's gonna take it a

28:06 but it's gonna sweep the rest of area eventually after it gets put.

28:11 other words, you know, it's slow process, but it's, it's

28:15 be a greater and greater aerial Whereas this, this could come right

28:20 here and if your perps are all here, uh you're in trouble if

28:25 down here, uh You could still some issues because, but the gravity

28:30 actually trying to help you in that . So, um it always depends

28:36 , you know, what the problem could be. Uh If this happens

28:40 a long period of time, it's much more efficient sweep and would be

28:44 good thing. Uh And better than . But if this was happening

28:49 this could be a thief zone to off a lot of this oil down

28:53 . Whereas this one is gradually gonna in this direction and get all the

28:58 and especially if you have perps all this pipe, which you probably

29:03 but uh I don't think they're trying show you that this is ground

29:06 This is the formation itself uh where finding upwards and this is the formation

29:12 where it's coarsening upwards. OK. , um oh yeah, I put

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

29:31 just more examples showing this kind of . And uh here you can

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

29:55 different thing but for different reasons, , this one definitely looks like it's

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

30:28 of, uh, I like to a couple of these things are really

30:32 same thing, but this is trying show you that tonguing doesn't, doesn't

30:36 to be, you know, so like this. Um, tongue can

30:46 more like this too where you get pods of bypassed oil. And here

30:56 , uh this is the barrel of questions and uh this doesn't equal 100%

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

31:12 another 15% out this way, another that way, another 20 you may

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

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

32:04 first wells in. But after someone can come back and do some

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

33:03 would be types of bypassed oil and bypassed oil here that, uh,

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

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

37:29 myself and this would be what it look like. If you had ones

37:33 were side by side, you could a horizontal well to come in and

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

38:03 it used to be. And you use this in conventional resources that have

38:07 oil uh that can, can be with one be well, uh well

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

38:27 the multiple perforations at one time. there's rules against that and you can't

38:32 mangle in which, which cases you , you would open up one at

38:35 time, then just open up the one and the next one,

38:38 if each one of these was like contested unit, part of this block

38:42 in somebody's acreage, but this one , uh, you might have to

38:46 it out that way. And this is just um, another,

38:53 thing that can happen, you can gas coating. If you have

38:56 um, the upside ver upside down of, of water coning, you

39:01 , you have, have the gas , you wanna keep your preparations away

39:04 your gas cap in the course of in a situation like this and you

39:13 gas up here and you have oil here, which one of these you

39:18 is gonna be really important and uh the bottom one would be better if

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

39:46 you remember uh earlier on, I about um you know, when

39:52 when we drill a well, it's very hard to um see ahead of

39:58 drill bit, but when you, you work on a horizontal,

40:04 it seems very complicated except that you have layers through here uh that you

40:10 pick up. So um here is somebody heather kickoff point, too

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

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

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

55:31 but there's still a lot to Here's showing uh cap Capex past.

55:38 Here, here is what Capex was to be in 2012. Here's just

55:44 you a diagram, bar diagrams. know, I, I wish when

55:49 made a diagram like this, they make one the next year and the

55:52 year. So you could show people . It's very difficult to find uh

55:58 uh graphics. I think it's But uh but it would be helpful

56:02 an instructor, but you can see uh what's going on and of

56:08 uh a lot of stuff uh that projected for 2020 2021 obviously didn't

56:15 And some of that, a lot that had to do with COVID,

56:17 of it had to do with uh the oversupply that we had starting to

56:22 in 2019. And here again, projections pass 2020 this was released in

56:32 . So this was assuming a dip COVID and then some build up uh

56:37 that. And um here's sort of um the gap is uh being projected

56:49 the future. Um as we see in conventional, we're gonna see uh

56:56 in the unconventional resources. And uh , here's where we are right about

57:03 and uh we're still really just a bit better in here. And

57:09 I'm not sure the unconventional are outstripping conventional right now. But uh

57:15 this is in the US, the Basin is still a monster. And

57:21 and that's all unconventional, which which is driving a lot of our

57:24 and ability to export oil and gas this time. And I think exporting

57:30 when, when you can send it the refineries that can produce that lighter

57:35 , uh you're actually creating an efficiency the system that ultimately uh at least

57:41 a global and a national scale should the prices relatively lower as long as

57:45 happening. OK. And uh this just a diagram showing you that,

57:53 know, it's not just going on the US, it's happening all over

57:56 world. And um some of these in Brazil and Argentina are pretty

58:03 Um Some of the ones in um this area here relate to high uh

58:11 geothermal um low, which uh which actually mature things that are shallower than

58:18 would normally expect and uh still be the, the source rock itself.

58:26 this is showing you the same kind thing with gas. Again. Uh

58:32 key to this is to just point uh there are lots of places uh

58:37 where we have reserves that aren't aren't being produced really uh at high

58:42 yet. But um there's a lot reserves out there in terms of uh

58:48 and it's a matter of uh getting technology spread around the world so that

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

59:03 of having enough energy to uh keep electricity on. I was over there

59:08 times and we had a professional master's over there and over the course of

59:13 16 months, they had blackouts, , all sorts of things because,

59:18 their grid, their na their grid a national scale was uh was not

59:22 able to keep up. And I'm sure they, they, they have

59:29 very little to no uh nuclear They're trying to, trying to keep

59:33 as clean as possible. And of , natural gas would be a good

59:36 for them because natural gas produces more per CO2 output. OK. So

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

60:04 that, you know, if you a, if you have a vertical

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

60:28 the formation and the rise up And of course, it's gonna be

60:33 , uh, if you're doing things . And, uh, until you

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

60:50 a Coke bottle. He was in , in a, um, plastic

60:54 bottle. It was coming from well, that's producing four barrels of

60:58 a day. He was really excited it. Um, you know,

61:03 , it is, it is extra if you can get it without um

61:08 having to spend much apex uh with shallow wells that that happens often in

61:13 . So, um but nevertheless, know, when you get uh this

61:18 surface area in here, uh and you frac it, you're increasing the

61:24 area dramatically at all these critical So you're getting flow into it from

61:31 formation over a greater area. In words, all through here, all

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

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.

62:11 uh keeping it opened up, others . But the uh the percentage and

62:16 amount of these things are really As long as, as long as

62:20 unit that you're producing is not near valuable aquifer or not near salt,

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

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

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

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

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

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

85:39 are, this is sort of a scale cartoon and there are faults and

85:46 in here. But the normal conventional and traps are up here and up

85:52 . But down here, there's this mass of natural gas, it's pretty

85:57 trapped by something like a dynamic, like a dynamic seal that we were

86:02 about where pressure on either side of is closing the po throats and making

86:06 difficult for migration to happen. And , this looks even harder to understand

86:17 you've done a lot of geology. , uh, but here you can

86:23 water and there's gas underneath the What could possibly be wrong?

86:27 there's a lot of pressure in There's pressure coming down over here and

86:32 a capillary issue which is kind of this in and, uh you reach

86:36 point to the pressure, uh abnormal down here. And of course,

86:42 expansion of this has caused sort of uh a pressure seal pushing up and

86:47 depth in the well is pushing on uh capillaries down with the water.

86:53 so you kind of get something that's similar to a dynamic uh pressure

86:59 And this is what it looks like cross section. And um um if

87:08 was to try to explain this to people I worked with in the

87:11 they think I was insane. But this is basically what we think's going

87:17 is the pressure across this, this . This cap, it's a capillary

87:22 between here and here and uh some of it leaks out but,

87:29 a lot of it is still trapped . And as, as um some

87:35 pressure is released, you know, little bit escapes and then, then

87:41 generation occurs, more builds up and lateral to these things, we,

87:48 do end up having tight sands that , uh, the normal,

87:54 geometry of what we would expect you know, water down here,

88:00 , water and gas bearing zone down with minimum to no food flow and

88:04 the gas all stuck up here. still, there's this funny issue

88:10 uh, of a pressure of a war going on between things that shouldn't

88:15 be, uh, uh, at with each other. And here's kind

88:20 what it looks like again, at a, at a larger

88:23 And here you can see this might one of the conventional reservoirs up

88:28 This is a diagram that helped me believe it. And I can't doubt

88:32 because I know it's happening, but still hard for me to uh understand

88:38 . But you, you have the the higher over pressure down here.

88:43 have capillary pressure in conflict here and through faults and some other things,

88:49 little bit of it leaks out and all these, these uh conventional reservoirs

88:55 have a funny configuration like this with similar kind of thing since there's all

89:00 gas involved. Uh And, uh know, the, the water is

89:05 top and the gas is trying to around it. Ok. If uh

89:14 anybody understand this better than me? I, I thought it would be

89:21 to point out to you that uh , uh even when we think we

89:26 that gravity is simple. Here's a case of gravity, um capillary pressure

89:36 overpressure fighting each other at some Uh That's making it very difficult uh

89:45 this gas to actually get out of bases, the center of the

89:49 In other words, it's a barrier migration. I guess that's the best

89:52 of looking at it. OK. Then the other thing that we were

90:02 look at, I used to love when professor actually, I didn't ever

90:09 to worry about professors doing this because didn't have Power point. They drew

90:14 on the board. OK. um you know, we looked at

90:21 , we've looked at this. we're gonna take a look at these

90:24 things here, car sands and oil . OK? So the tar

90:42 you know, are mixtures of clay and, and bitumen and uh and

90:51 the bitumen at least can be processed , with uh with the different types

90:58 organic solvents. And uh and so kind of how this works. And

91:06 um the oil gets extracted from this turning it into um something called a

91:13 sin fuel. And uh that in has a pretty good footprint, hydrocarbon

91:19 and a and an environmental footprint You can see uh Venezuela's got some

91:24 big resources here. Of course, have the um in the subsurface,

91:29 have the heavy oils and then you're to the surface uh they have some

91:34 sands up here. Alberta has really things very close to the surface.

91:41 uh of course, Saudi Arabia also places um that, um, and

91:48 are billions of barrels, by the , that's 265 billion barrels. So

91:53 a lot of uh a lot of tar sands and asphalt out there that

91:58 , that we can use as a . And uh this is showing you

92:04 it is in uh in Alberta, , obviously a little bit of it

92:09 over into the next province and uh never have enough time to go into

92:19 in, in great detail. But I'd like you to just go through

92:23 and, and read it uh when get a chance. But I highlight

92:27 because steam assisted gravity drainage, which SAGD uh produces uh recovery rates of

92:36 to 60%. Uh One of the why this is one that they like

92:42 most is because it's slightly in the and you still get a pretty high

92:49 rate. That's actually a phenomenal recovery . Uh strip mining, you get

92:55 recovery rate, but it's um you have to imagine if you have

93:00 much area of tar sands near the and you have rivers and streams cutting

93:06 it and even lakes uh forming around . You have to imagine that automatically

93:13 natural existence of these uh deposits actually an environmental problem in itself. It's

93:22 , uh, it's, it's um, damage free just in

93:27 But if you go in there and stripping it, stripping whatever cover there

93:31 be on it off, uh, makes it even more catastrophic.

93:37 uh, and of course, it carbon to the carbon footprint that's not

93:42 . Um, it's hard to say this is a problem because we've always

93:46 it here. To me that excuse pretty weak. That's the excuse for

93:52 . But uh but nevertheless, um a lot of reasons, this particular

93:59 is one of the ones that is strip mining, which is, which

94:03 very um uh which is very damaging the environment. Re releases lots and

94:10 of uh CO2 in the process. this is kind of the, the

94:15 that's favored by most people. They're to uh generate these sin fuels.

94:22 uh the way that process works is lot like the horizontal whales. I

94:27 showing you in a, in a where you actually um uh surround uh

94:35 of uh the deposit with the steam , the steam chamber which has steam

94:42 and it sort of heats up the area and then very close to

94:45 You have oil production an oil well can uh not really oil but uh

94:52 this a sludge that comes off of as it uh it heats up,

94:55 becomes less viscous and you can produce at the surface. And here you

94:59 see, uh they're using um, to, to pull it out of

95:05 ground at the same time, even uh the viscosity is being reduced and

95:10 uh the float characteristics are being Ok. And so, uh

95:17 that's all I wanna say about tar . But I, I want you

95:21 be aware of this, you there's an addition to the shale plays

95:24 , that I think everybody's familiar Just trying to show you some of

95:28 . And we looked at the Eagle , I'm trying to show you a

95:31 of things that are a little bit . Uh There's certainly a lot

95:34 a lot of other uh things uh that list that I showed up front

95:40 that are considered unconventional resources. So next one is oil shale. And

95:49 the difference between oil shale and shale ? I've already asked this question,

95:53 maybe I can see if everybody remembers it is. You know, there's

95:59 thing called oil shale and there's another called shale oil. Nobody has that

96:19 oil. It's um oh, it deals with the extraction like one's

96:27 to the finish line than the other something like that. Yeah, you're

96:31 on it. And uh and I'm the geophysicist is on top of this

96:37 uh but you're, you know, absolutely right. The um the oil

96:41 . First of all, we had we called oil shell before we had

96:45 ever produced any shale oil. So shale, the term oil shale was

96:50 owned by um this carriage enrich. can't, you can't use solvents to

96:56 it out of the ground. This enrich uh uh thing that we have

97:05 uh in some of these lake The only way to turn it into

97:10 liquid is to heat it. In words, to try to advance the

97:14 maturation of the carros so that they to generate fluids. And um and

97:22 we can mine these but that's really and most of them are, are

97:26 deep and uh you could mine this actually process them by heating them up

97:33 that, of course, is Uh But uh having said that oil

97:39 , the carris will burn at the if you, if you have a

97:44 piece of oil shale, that's over toc and probably less than that,

97:49 can light it with a match and burn um I guess, sort of

97:54 Pete. But uh but nevertheless, it, it's, it's all carriage

97:59 , and um and so um they , they do strip mining but uh

98:06 other way they pull it out of ground. Uh And here's some of

98:09 big basins, the Green River basin course, and the UTA Basin and

98:13 Peons Basin are big areas and I've worked on issues of lacustrine basins

98:20 these are big latrin basins and good of um less productive, less cooked

98:28 . In other words, the deepest of these have uh matured, but

98:34 quantities of the um of these basins still have immature Carris, which is

98:41 we have oil shale, shale oil what is when we produce oil straight

98:47 of a shale. It's, it's like you said, it's farther down

98:51 line. And uh and it may viscous, it may be uh heavy

98:56 some cases. It's not. And and it's uh but it's, it's

99:02 Carro that's already been metamorphosed into uh the liquid. And here's some deep

99:11 shells and carbonates and um uh some these beds may actually be part of

99:16 mahogany ledge. Uh But the to in here uh probably range between 15

99:23 20%. And of course, these the limestones uh that fall during uh

99:30 productivity periods and deposition. So what one of the things that uh shell's

99:38 that's um they had some success with was you actually put heaters into the

99:46 wells that heat it just like he do here. And I don't know

99:51 it was steam injection, but it have probably was. And uh and

99:57 these are the heater wells then they that if they put in refrigeration

100:03 Uh And, and I'm, I'm not sure exactly how they,

100:08 , did this but they would, , but cool, cool,

100:15 chilled waters into these, into these to create sort of an isolating insulation

100:22 these would sort of block around this and help concentrate the heat through the

100:29 area and through that they were able do it. I don't think they

100:32 got to the point of, uh, making it economic, but

100:38 theory, they've, they've figured out to make it work. And here

100:41 can see this would be a, producer. Well, right here.

100:47 . And with that, we're done many questions about unconventional, even if

100:55 didn't talk about it. Ok. , um thank you guys for letting

101:04 break earlier uh on Saturday and uh I, I'm, I'm gonna send

101:12 email out to everyone and let you what the um let me open this

101:17 up again here that, so I a quick question. OK. There

101:32 go. I just stopped the Go ahead. Hey, earlier you

101:38 mentioned unconventional um sources and I think associate it with uh uh CO2 storage

101:46 carbon storage. Um No, that, that wasn't, that

101:53 that wasn't associated with, with uh it's associated with unconventional. In other

101:59 , it's a type of unconventional, not. Um um uh Let me

102:06 back to the slide. Mm I to share my screen again. What

102:15 is carbon capture OK. Hang on minute. Uh Let's see.

102:33 And you have to remember when we're about unconventional course resources. It's not

102:38 shales. Ok. Unconventional resources are these different things. One is shale

102:46 which I think was what your question . Hayden. And, um,

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

103:23 uh that are coming up, seeping that come up to the surface,

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

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,

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

104:29 with wells. Um, that's it's a, it's an economic resource

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

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

105:13 produce it that way because it's, that's extremely dangerous because if you mobilize

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

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

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

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

108:00 basically the whole purpose of it. , I was just curious because

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

108:36 you could do. And you just this idea of poking a hole

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,

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,

110:09 it's actually creating more of a carbon . So I have no idea why

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

110:30 places where CO2 is released, different where CO2 is released where they're trying

110:35 figure out a way to absorb it uh into things and or push it

110:42 into the ground. And uh like you would, for example,

110:46 you're producing oil and gas, you're get some CO2 2. If you

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,

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,

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

111:37 we don't do this more often, there are a lot of places where

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

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

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,

114:05 example, out of the atmosphere. they, they didn't do such a

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

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

114:30 as clever as we are and as as A I is supposed to

114:34 uh you know, if we put little in a little bit of energy

114:38 carbon capture and things like that, um the problem with CO2 may become

114:44 moot point uh if they have some breakthroughs. And uh that's, that's

114:50 of what I'm hoping for for the because I don't see us getting the

114:55 alternates up to steam as quickly as want them to. Uh because there's

115:01 lot of, a lot of difficulty the entire food chain, so to

115:05 . And, you know, all way from producing enough cars to producing

115:08 electricity, to transporting that electricity on lines. And uh and,

115:15 that sort of thing that, you , we, we have a long

115:17 to go to, uh, to fully electric. So, with

115:24 thank you guys for paying attention. you for giving me a little break

115:27 Saturday. And, uh, if you guys want me to send

115:33 the schedule for the exam. um, uh, and also when

115:39 , the final exercise is due or you, uh, do you,

115:42 you all write it down? It's at one on Friday, right?

115:49 at 1 p.m. Ok. Um, , so it is at 1 p.m.

115:55 Friday. I thought it was gonna at, at, uh, 5

115:58 7 on Friday. But we, , we can do it. I

116:03 something written down wrong. Then uh, 1 p.m. That's right

116:08 uh, uh, who was Anthony? Anthony couldn't make it at

116:16 to 7. Is that correct? correct. Ok. So, so

116:20 do it. We will do, do the online exam at one

116:27 2 30 then, um, and , uh, I, I

116:33 is a here, I don't think here. He wanted to do it

116:41 person at once. So that makes easier for me. I get

116:44 I'll do it all at once. then the, um, let's

116:55 the, well, the, excuse me, I have too many

117:05 on my phone. Yeah, the , the mapping exercise is gonna be

117:23 on, um, the 17th. , the exam, the final exam

117:30 be Friday at 1 p.m. on the and then on the 17th, your

117:35 exercise will be due. Does, that sound right? Guess?

117:45 Yeah. Yes, sir. So we're all, we're all

117:52 Now, now we're all on the page. Ok. I'm glad I

117:55 the question because I would have messed again. Thank you for keeping me

118:02 line. Ok. So, uh luck with this. And um,

118:09 the, uh, I've loaded, , this past weekend's, uh,

118:16 and I'll be loading this one uh, before I head out

118:21 So, um, things should be . I don't know, it takes

118:26 while for them to get processed uh, video points, but they

118:31 be up by now. They uh, about two hours ago,

118:35 hopefully they're, they're available now, if not, they should be sooner

118:40 . Um, well, at uh, sometime this evening they should

118:44 up and up and running. But you don't see them by tomorrow

118:47 let me know and, uh, may have to reload them.

118:54 Sure. Ok. Well, it's been nice having you guys in

118:58 class. Um, uh, I've done a three week course before.

119:05 , the last time I taught one these classes which, which was only

119:09 , uh, 16 months. less than that, it was about

119:13 semesters ago. Uh, I, had the last, uh, I

119:20 I had the last. Well, it was bio so I only teach

119:23 thirds of that course. Uh, it's been about, it's been exactly

119:29 months since I taught the four week . But I've never taught the three

119:34 course. So, sorry about my with timing and, uh, some

119:40 the delays we had and that we to do any of this online.

119:44 , uh, really enjoyed, a lot of the feedback we were

119:48 in class and, uh, even questions you just asked me.

119:52 so have a good, good And, um, oh, by

119:55 way, your grades are all pretty in the same bucket. So,

120:00 , so I have to, figure out who gets an A or

120:03 A minus at this point. uh, but at the same

120:07 you know, you have another exam that could affect the curve and,

120:12 , and you have the exercises which help in most cases help pull up

120:17 , uh, pull up your So, uh, good luck with

120:21 you've done. If you haven't turned your first three exercises, get those

120:24 as soon as possible as well. , sir. Yes, sir.

120:31 too. Thank you. Thank Thank you. Thanks. Ok,

120:37

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