© Distribution of this video is restricted by its owner
Transcript ×
Auto highlight
Font-size
00:03 Let me go ahead and uh obviously um I think I'll be doing this

00:10 anytime soon. Uh Obviously did this the pandemic. So, uh

00:14 but here we are. Um let go ahead. Yeah, as I

00:20 uh promised, uh I did uh thought I was gonna get a

00:24 Thanks. Thanks for the compliments, couple of compliments. Um uh

00:29 so let's um uh start uh with , let me share the screen so

00:35 can get this going. Ok? uh let me uh to this.

00:48 we go. Ok? And uh here. Ok. So, um

01:02 you already can see the screen. let's um ok. So thanks.

01:07 sent an email uh earlier. Uh got exam later this week. Um

01:14 we're gonna start you at 3 21 . It's relatively, there's only two

01:19 . So it's not like we're talking two complete chapters here. So it's

01:21 couple of sections in each one all . Uh We did the, this

01:26 . Um I know you got an as well. You can just,

01:29 mean, the list is relatively You can just do that on,

01:32 Monday. Um uh, but obviously you put it into however you

01:37 do it, but the smart work due for another couple of weeks.

01:41 , um, so what we're gonna is, uh, today is

01:49 Um, so again, just, to reiterate that you've only got a

01:54 of sections covering not a lot of , right? So we're gonna go

01:58 a couple of things. One um, just touching on a little

02:02 on a couple of aspects of, guess you say microbial ecology. Uh

02:07 being the water cycle, but mostly in the context of two things,

02:11 wastewater treatment and two the um kind the, the flow of water and

02:19 organic material is, is carried this and you can have some kind of

02:24 effects with that. Uh The other of this is kind of focusing on

02:28 nitrogen cycle which you talk about a of times already. Uh But then

02:33 of just uh I'm gonna let you out a little bit more uh talking

02:39 nitro fixation a little bit. uh you know, basically getting a

02:43 uh the complete story on that. . So we've talked about it bits

02:46 pieces throughout, but kind of just the whole story with, with

02:50 OK. So we do have uh , we can use the,

02:56 the, the Clicker app, the . So, um but, but

03:01 attendance, I'm I'm kind of I mean attendance is not, is

03:06 on figures, but I'm not gonna use that for today because some people

03:10 not, may not feel like even because of what's been going on and

03:14 to touch briefly on that. I actually don't know much more about

03:18 than I'm sorry you went on. muted again, sir. Ok,

03:47 about that. Ok. So, , so you know, people write

03:52 to these kinds of things. So you feel you need help there in

03:55 syllabus, is this section on Ok. So do if you feel

04:01 need help are available, you can them, information's in the syllabus and

04:06 sure you already been reached out by by the Provost and other U H

04:12 anyway. So and I, and don't know yet. Uh if we're

04:16 still be in the same mode on , but you know, for now

04:21 to show up and fast Thursday. but that's as much as I

04:25 Ok. So uh so let's go , so the hydro hydrologic or water

04:34 . Um I think we're all aware the basics of this really. I

04:38 , you know, uh how does water get around the globe?

04:42 Well, uh by water, water , right? Um forming uh clouds

04:50 precipitation, rain, flowing down precipitation and then of course, water

04:55 earth. Um it also goes through , ok. Uh imagine any kind

05:01 a deluge rain you have here in , right? Everything is flowing,

05:05 , going in through uh uh uh through uh grain gutters and this and

05:12 uh basically, you know, out bodies of water and of course,

05:16 can be processed through wastewater treatment Ok. So, you know,

05:22 hitting earth, of course, will up and pick up and carry whatever

05:25 on top of the ground or ground , through the soil. And uh

05:29 course, organic material uh is picked as a result. OK. And

05:35 really what the focus here is gonna . It's about this parameter called B

05:41 D biochemical oxygen demand. OK. so um B O D relates to

05:52 content, the quantity of organic material in a body of water.

05:59 And that can have different detrimental effects many cases as we'll see as we

06:05 through this. OK. And that's what wastewater treatment is about is about

06:13 the levels of organic materials, reducing O D. Um And so that's

06:20 of what the first part of this is about. It centers on

06:23 OK. And so, and it absolutely goes back to the concept we

06:29 about in unit two, right Um And, and uh uh aerobic

06:37 respiration, those things will come up as we go through this.

06:42 So, um so here's a question C uh is, and this is

06:50 B O D. OK. So have four water samples subjected to B

06:55 D. OK. Um Analysis, O D analysis, which sample has

07:02 lowest or had the lowest B O ABC or D OK. The lowest

07:08 O D. So remember the B D correlates to the content of organic

07:14 in, in the um water. ? And so this absolutely correlates to

07:24 respiration you, OK. Let's uh gonna go ahead and I'm gonna go

07:43 and uh start the timer. yeah, and again, the,

08:00 points for these are, are, is just more or less just for

08:05 um what I call it fun, ? So, uh these aren't gonna

08:09 posted, All right. 5 3, 2 1. OK.

08:23 , uh I figured it would be be between A and B. So

08:26 actually going to be uh OK. um d uh has really no

08:36 right? There's no reduction in So when you have organic material,

08:40 of respiration, right? Aerobic what's happening as you eat something you're

08:46 oxygen? OK. And so if nothing there to organic material there to

08:52 , then you're not gonna consume any because you're not respiring. So D

08:55 represent the lowest level of B F , right? The highest would be

09:00 , right? Because it's going what are, one is respiring uh on

09:04 organic material A has the most and goes away and you utilize oxygen very

09:10 because of the amount of organic material . OK. And so in,

09:15 a way for a treatment, you're to really get B O D down

09:20 zero or as low as you OK. So, and that's um

09:25 , all correlates to respiration. So, uh so, and this

09:33 , this up up here shows so one of the, one

09:37 one of the, one of my I wore when I was, uh

09:42 , when I was in the biotech was actually working with a business that

09:46 some of this wastewater treatment and B D analysis. And uh what you

09:50 up the upper left is typical. those, all those bottles are different

09:54 samples that uh are being subjected to O D testing and who,

09:59 who gets these kind of tests What waste uh wastewater treatment plants

10:03 And so um and environmental samples and like that, these are, are

10:09 are measuring B O D and the black um uh pro or instrument

10:16 see here, right? That's uh a B O D, that's a

10:21 a oxygen Pro, right? So the amount of oxygen present.

10:25 And so you see how, what the rate is of the,

10:29 , the uptake of oxygen and that to the B O D levels.

10:34 . And so sewage, OK. As a, as you might guess

10:40 super high in organic content as it a very high B O D.

10:43 this is kind of a typical value see for something like raw sewage.

10:49 . And so uh and that thing the, on the left over

10:53 that's an example of like an, in line B O D system where

10:58 is consuming, flows in and you're like a real time B O D

11:03 . Um And so what's, what are levels that are dangerous?

11:07 , we, we have low levels oxygen. Where is it when uh

11:12 life can be affected? Ok. And these are uh levels that you

11:17 here. So air is saturated eight mg liter. So remember,

11:21 don't dissolve great in liquids. Uh that's the ability of of oxygen if

11:27 water saturated with it. Ok. it becomes da a danger for aquatic

11:33 when it begins to be like 54 of, of oxygen. That's when

11:40 they're threatened. OK. And so , there's um and so there are

11:46 if you dump in high B O material into bodies of water, um

11:54 actually ends up depleting oxygen because you this activity that feeds on it and

11:59 uses oxygen from the water and it it. And that's when you get

12:03 like fish kills and things like OK. And so uh so what

12:09 see here is just such, such thing as I've been talking about.

12:14 , you have, um, dead zones can occur, zones of

12:19 , right. These are areas that , that are, uh, the

12:23 of, not, not necessarily down zero, but certainly low levels of

12:29 , where fish and other types that in these waters can't, can't at

12:33 levels and they have to go elsewhere they can't. And, uh,

12:38 so, um, and so what these kind of things? So an

12:42 , an influx of nutrients into these of water, um knowingly or

12:49 right? It could be an oil , that's lots of organic material.

12:52 so there are uh bacteria that can this material and in doing so,

12:58 respiration, right? They're gonna eat material and then as they do,

13:02 use oxygen and the oxygen comes from water which depletes it and then affects

13:08 lives. That's, that's in the . And so, uh so this

13:12 we've been talking about time and again even two heterotrophic aerobic restoration, what

13:18 do, right? And so, and so there's other other factors should

13:25 to this as well. Ok. So if you look here, particularly

13:32 this area here, lower Mississippi right, which goes into the Gulf

13:38 Mexico all along, all along the River here, right? Heavy,

13:45 even going all the way up in , northern northern part of the

13:48 all along the river, especially down , uh heavy agricultural areas using,

13:54 fertilizers further up or lots of, , of different types of manufacturing plants

14:00 along the river dumping out, you , uh waste and things. And

14:06 this is all organic material or, things like nitrogen and phosphorus from fertilizer

14:13 gets dumped out from, from water . Those are, are nutrients that

14:18 , that are critical to, to things like algae and plants and it

14:23 cause bad effects. OK. So is kind of how these things

14:27 right? Influx obese organic materials that to these effects. And so here

14:31 one here. This question coming up relates to that process of provocation.

14:39 . So take a look at this this relates to what we've been talking

14:44 is kind of a um cascade All right, first one thing happens

14:51 that triggers the next thing and that the next thing and, and so

14:54 and the end result is back. ? In different ways. Let me

15:02 a look at that. Sure. . Yeah. Try a, let's

16:01 the timer here. OK. Let's down from 98. OK.

16:38 d seems to be the consensus. Yeah, that is actually true.

16:48 . And so, so um is . So the way to kind of

16:56 this is uh in this is a aquatic, we're talking about an

17:03 Uh And so ultimately, what happens oxygen gets depleted from the water.

17:13 . Now, um very common uh commonly what initiates this is, let's

17:22 look at the diagram here here. . Very common scenario is what you

17:27 here where you have a pond, stream or river. OK. And

17:32 have uh adjoining land of courses. uh we have water runoff of say

17:38 . OK. And that uh and fertilizer of course, is high in

17:45 which can be converted to nitrate nitrates we'll see, right? Of

17:50 all I'm gonna say is phosphate. so these elements are limiting in

17:57 OK? And so if there happens be an influx of this like a

18:02 excess of this, that will greatly the growth of photosynthetic types, photo

18:10 . OK? Particularly your algae sano . Um They because you know,

18:17 these are photosynthetic, right? They CO2, they need light um and

18:22 need these minerals and so uh where can fix CO2 and they can um

18:28 um convert light to energy. Uh can't make nitrogen phosphorus, they have

18:34 get that from the environment. So need that obviously. And so when

18:38 have an excess of it, their just explodes. OK? And you'll

18:45 what are called me uh a a Al Al bloom because they're really like

18:50 and growing to high levels. And so, and you will see

18:54 as a green mat on top of body of water in many cases,

18:58 , where this doesn't happen. And what happens is then of course,

19:03 these nitrogen and phosphorus elements are, used up at some point, even

19:08 they're in excess are gonna be used . And then the, the algae

19:11 san here and others will grow, then there's no more phosphorus to sustain

19:18 . And so that blue then will . Ok. And so that,

19:26 this now will serve as the food for the next, the next

19:31 OK. So I will bloom. they die, falls to the bottom

19:38 then the sediments will be bacteria. . So here is where um now

19:44 have your heterotrophic aerobic respiration occurring. ? And so they'll feed on a

19:51 algae and that's organic material. And as they feed on it,

19:57 taking oxygen out of the water. ? And of course, there's,

20:02 fish and other aquatic life in this body of water besides bacteria, et

20:08 . So, um and it takes , they take a lot of lowering

20:13 oxygen in the water to begin to this life fish and whatnot. And

20:18 , um uh so that's how these occur. Um The uh off the

20:24 of Galveston, you've, we've had uh um uh red tide, you

20:30 have heard uh these, these types allergy that all these toxins uh that

20:37 , and they, and they, blown up in terms of their growth

20:40 a very similar manner, an influx nutrients has caused them to, to

20:44 . And uh in some cases, , can be these types of allergy

20:48 produce these toxins. And so, so this is, this happens time

20:52 again, are, are around the where you have these, you

20:56 whether it's fertilizer runoff or, or in or excess of other types

21:01 nutrients that, you know, pollutant things that get dumped into, into

21:07 of water. Ok. So it's , let me just go over to

21:13 and see any questions at this Ok. Um It, it's really

21:21 boils down to kind of really the content we've been talking about in,

21:27 his previous, in the previous And so, uh you know,

21:31 all about, you know, nutrients then can they will just eat them

21:35 what can be the effects of And so it's, it's really what

21:37 boils down to. Ok. So then see what, how do you

21:45 um counteract this? Ok. These , what can you do? So

21:50 where uh wastewater treatment comes in. so, you know, if,

21:56 you drive around your, if you to where the folks are, you

21:59 around the subdivision, whatever you'll, , if you keep your eyes

22:03 you might see one of these, ? Every each one of on a

22:07 scale, one of these little plants maybe serve 100 and 50 homes or

22:13 like that. Uh, but they're typically be hidden behind, they're

22:17 of hidden. So, um, , but they do the job

22:22 of, um, cleaning up the and, and to make, not

22:28 all cases, not in all cases this, is this process about providing

22:32 drinking water. Certainly that's, it be. But the other thing point

22:36 make here is that, uh, , you know, waste water treatment

22:40 residential homes is one thing, but are so many uh other wastewater treatment

22:46 that are used by al, probably almost every manufacturing uh has some

22:55 of wastewater treatment associated with their business they produce things that you can't just

23:02 into the water. And so very these are around, uh they,

23:07 , they, they um treat them then put them in bodies of

23:10 but they're treated to a level that's toxic. OK? And that was

23:14 of the stuff I was involved in I was working in this field

23:18 um, especially things like uh Georgia , a paper and cardboard box making

23:23 , uh produces tons of this kind waste and they have their own waste

23:26 treatment systems to handle this stuff. so, but it's all kind of

23:30 on the same concept. OK. about, um, uh and so

23:35 can see here in this tank, right, right there that you see

23:41 structure here and that will rotate And that's meant to create turbulence.

23:48 like taking a shake class of media shake it. Right. It's the

23:51 idea you're creating turbulence to promote aerobic , right? Because that's if you

23:57 promote Baros of those types to knock the organic content, the B O

24:03 OK. Uh Up here on this is kind of just a top down

24:08 . You can see it's a bit , here are the tanks here.

24:13 That's what we call secondary um treatments for the microbes are doing their

24:19 Uh But you know, you get , there's something happens before you get

24:22 that point. But really the, , the, the emphasis of the

24:27 system are, are those tanks and growth of microbes. OK. And

24:34 and in a air radiate the elastic we're ready to get lots of aerobic

24:41 to knock down that organic um OK? And you know, it's

24:48 just about bacteria either. It's also also very important in the process as

24:53 . OK. So in which for you're gonna have again, if I

24:59 to boil this down, maybe uh things, it's about obviously promoting microbial

25:06 because that's there. Those are the that are gonna knock down the organic

25:10 E O D. That's one, is to um promote settling.

25:21 So it's one thing to have the growing and, and they're, and

25:24 chewing up their organic content. Um then they're gonna, you wanna

25:29 you wanna have water coming out that relatively clean, OK? Not a

25:39 mass of stuff still in there. settling, settling up particles is

25:44 a big part of this. Um And then of course, uh

25:50 may, if it's a, if is for to supply drinking water chlorination

25:54 to knock down uh uh pathogens that be in there. So, um

26:01 really the promoting growth of microbes to down the B O D and settling

26:05 really the two, the two big here, ok. But of

26:09 as stuff comes into a wastewater treatment and you'd be surprised when that comes

26:15 one of these things, um everything animal car dead on animal carcasses

26:19 to, to tires and you can . And so you have what's called

26:25 preliminary treatment. It kind of was to weed out this kind of larger

26:30 . Ok. Uh Primary treatment then as what then then comes through,

26:36 is more like a mesh screens to of remove more inside of particles.

26:42 then um and then finally you get secondary treatment, that's where, that's

26:48 you get your microbial growth going, aerobic respiration um knocking down the organic

26:56 in the water. Ok. systems vary but all systems will pretty

27:03 have, have have that primary uh , primary treatment, secondary treatment.

27:08 may have material that they also, addition, have anaerobic respiration going

27:14 It's kind of, I think what's on over here, but it's

27:19 not, not always a part of system. Uh, it,

27:23 it can be, uh, but , we're gonna be focusing on,

27:27 this right here, right? ultimately, you're trying to discharge

27:33 uh, if it's not for drinking , you're trying to, you

27:35 discharge this into a body of water . And of course, you don't

27:40 kill the things that are in So you want, you're, you're

27:43 to knock down your organic content, and, and make it safe so

27:48 you can, you can discharge OK. And so, um and

27:53 tertiary treatment, this is where you kind of chlorination is very common

27:58 to eliminate pathogens. There may be other kind of chemicals you can use

28:01 well for that. OK. Um , uh so here again, it's

28:07 of a flow chart if you will process uh differentiating the primary, the

28:15 and uh the tertiary. OK. so, again, clarification, this

28:20 where we're materials settling out, So you have um high B O

28:26 coming in. Uh obviously you want B O D coming out.

28:30 And so here is kind of in primary, preliminary and primary, they're

28:35 rid of the larger kind of insight . OK. And so um the

28:43 is kind of just a, just a mass of that kind of really

28:47 material which can actually be used for or you may be able to digest

28:52 further anaerobically. Uh But, but remainder then uh goes through into here

28:59 aeration. So this is what we're to uh have some mechanism to create

29:05 in the water, right? Um it up, right? Get air

29:09 in and that's gonna promote growth. ? Of the types that will be

29:13 to then chew on that organic material uh lower the B O D,

29:19 ? And so of course, um , you want to have AAA kind

29:23 a clear uh super if you will out, right? So that's what

29:30 clarification tank is about, right? so uh so cells and things will

29:35 right in the sludge. So they it activated sludge because that represents the

29:40 portion of the bacteria that are doing work of breaking this material down.

29:45 ? But also has, has does protozoans in there too and they have

29:48 role in the process as well. so this can this, this is

29:54 , as you know, cleaner, water comes out of the clear fire

30:00 then the the cells that were used break down B O D can be

30:06 . OK? And we can keep it going. OK? And

30:11 if tertiary treatment is part of the is where you can introduce disinfection,

30:16 common things like chlorine, uh even light, OK. And then

30:21 what you're getting at the end is low B O D uh water

30:25 fairly clean, OK? And, , and not, and, and

30:28 , clear, OK. And um and so healthy sludge and so

30:34 throughout this process, this is uh those that are in this business

30:40 and, and monitor these things. they can look and smell, look

30:46 the microscope and, and kind of the state of the system uh because

30:50 system doesn't always, these things run 7, but they don't um always

30:55 , you know, there's times when , when they, when they don't

30:58 optimally, right? And that's the of business we were in that I

31:01 I work for, we would add bacteria or things when systems did kind

31:06 because things can, can come in types of toxins and stuff may be

31:10 there that aren't being monitored and they just knock out your system.

31:15 you kind of have to restart And it's literally like just re seeing

31:18 with, with, with microbes. so it's even uh not an uncommon

31:24 to go to because you was for treatment plants are, you know,

31:27 not, they're in proximity to each . So one may be kind of

31:32 and the, the you may go to the next treatment plant that's close

31:37 and get some of their activated sludge use that to inoculate your system.

31:42 you can do those things. And kind of like just having a,

31:45 big culture if you will, that can use to inoculate. And

31:50 uh of course, who are in business of providing uh bacteria as well

31:53 the, for this kind of um . But um in any case,

31:58 it's a waste water treatment and the involved, there's a whole other universe

32:04 I that I discovered. So it's uh it is interesting, but it's

32:09 definitely a um a uh uh unlike anything I've, I've experienced

32:17 but nonetheless, obviously very critical And so, um so, Sara

32:23 the types, they know that feed the matter, that's kind of a

32:26 thing. Um But, you you can't ignore the protozoan in there

32:32 , you know, you can look a system and you can kind of

32:35 the health of the system by, know, are you seeing protozoic,

32:38 you seeing these bacteria that are, are that are eating up the organic

32:43 ? And this, are you seeing intact ecosystem? And if you

32:47 it's probably an indicator that the system operating like it's supposed to be

32:51 And typically it's protozoon that are gonna more sensitive to things that are coming

32:57 and maybe that can be toxic. so the first thing you'll see under

33:00 microscope is that you know, the zones are wiped out though, they're

33:04 present, that's an indicator that something's going on. So,

33:10 but any case, so as the, the thing you want to

33:13 is to. So here's some examples types of Pro and you see,

33:18 , what do you call are kind fixed in place? Uh, they

33:22 have that kind of these rotating mouse that bring in. That's how they

33:27 . Uh, you have types that along these, these types of.

33:31 it's a, it's a mixture of . Um And so here's kind

33:36 yeah, a question that kind um, gets to why,

33:41 why the pros are important. And so what you're trying to do

33:48 is to with a promote, you , these bacteria that will be able

33:53 aspire and, and eat up your material. That's one but two is

33:59 promote this kind of, this is beginning of how we form a

34:05 we're called flocks. OK? And are the particles that will form because

34:11 will settle out, ok by And so you're gonna get the,

34:17 enrichment of filamentous bacteria. Ok. filaments long, long strings is how

34:24 grow. And, uh, they'll things like P H B or starch

34:29 we talked about previously and these kind can help connect these filaments together,

34:36 . And so these will form and flunks are what will settle out,

34:42 ? And that's how you get a water in the process. So you

34:46 lower B O D and they settle and the water becomes clear clearer.

34:53 , what are the role of of the protozoans? Ok. So

34:56 you, you, you're gonna have that are these types, filamentous

35:01 right? They're the ones that promote flac, that's what we call

35:05 These, this kind of mesh network these filaments held together by these kinds

35:10 different um uh actual cellular material that's by the cells. And then you

35:18 have these types. We talked about in, in the context of

35:21 right? So you have the, swimmers and the stickers, right?

35:24 these will be swimming kind of cells that's what protozoans feed on,

35:29 So they feed on uh these OK. And in doing so because

35:36 these planktonic types, you're trying to stuff to settle out, OK?

35:41 the planktonic types aren't the type that do that. They're kind of just

35:46 in the water growing and swimming around eating. Ok. So protozoans eat

35:53 guys, OK. And they contribute getting a, a clearer water,

35:59 ? Uh A clarification of the OK? Because on their own,

36:03 things won't settle out. Ok. But as protozoans growing up and grow

36:08 eat them, they'll, they But um so that's kind of what's

36:13 on here is to get a, um Hey, hey, next filamentous

36:20 that will come together, settle out in these planktonic types that will then

36:26 lead to clarifying the water we call and you know, altogether producing uh

36:34 effluent water that comes out of the . That's, that's clearing and

36:38 Ok. OK. With low B B obviously. And so, so

36:43 , that's what this is about is forming, this is forming together,

36:48 of these networks of filamentous bacteria that see here, right? You cardia

36:54 another type and they have this kind filamentous branching forms and then they'll come

37:01 and settle out and of course, proto that are, that are eating

37:05 the planktonic type. So in then just kind of what you're trying

37:10 do here is to promote, you , uh a balance of these

37:14 which promotes good fluctuation and good then they eat, which leads to

37:19 clear effluence. Ok. So it's kind of works together, right?

37:24 this is just this is just to kind of test, there's lots of

37:29 , one does when they're monitoring their treatment system and this is one of

37:34 basically just a settling test. And you do is you scoop out some

37:38 , pour it in a um graduated and then you just hit a stop

37:43 and you just see, well, long is it taking for settling?

37:48 we see, you know, a um clearing the water and the material

37:54 settling out down here. You can it's kind of very dark down here

37:58 the bottom and you just see, how fast is this happening. This

38:02 of, you know how well your working. It looks like this one

38:05 the right seems to be settling You see how it's more clear compared

38:11 that side. So yeah, it's one of the parameters you look

38:15 to see. Are you getting are you getting settling good if you

38:18 and how fast this is occurring? . And there's different things you can

38:22 . Uh, you can even increase turbulence, you get more, more

38:28 and, um, uh, uh can add different chemicals and things to

38:33 of help it out. So it's uh even you can even add

38:36 if you wanted to, to kind balance the growth. So there's different

38:39 you can do while one it's monitoring things, we don't need to go

38:42 all that. But, um, , but it, it's basically,

38:46 a continuous system. Obviously, it flowing 24 7, right, going

38:50 flowing. Um And of course, can be upsets and of course you

38:54 to, you know, there are kinds of mechanical adjustments you can

38:58 uh you can manipulate flow rates, fast stuff is flowing through. And

39:02 are different adjustments you can make to of optimize your system OK. Um

39:08 obviously you worry about that. But it, it's, you know,

39:12 , it's a, it's a, involves many parts and, and

39:16 you know, everything working together to promote again the basics here,

39:20 ? Uh microbial growth, uh aerobic , right? Uh knocking down B

39:26 D settling out of material and producing clear with low B O D.

39:33 basically the bottom line here. So let me just switch back um if

39:40 any questions, OK. Uh Oops , um if you do, you

39:49 always type, type it in if want, if you wish.

39:53 uh so the next part is going be on um nitrogen cycle. So

40:04 , let's look at these questions We've um gone through this. Um

40:12 gone through this uh More than right? We actually mentioned it in

40:18 Chapter one uh lecture. We mentioned the uh at different times in,

40:25 China, you know, too. , you know, we're kind of

40:27 of put it all together here. And so, of course, uh

40:32 think we, it was presented as triangle, right? Three sides.

40:37 so we have uh 11 side is conversion of night trait to uh N

40:44 , right? So there's a name that. I go ahead and start

40:50 time. There's, there's gonna be question that will pop up on the

40:55 slide. OK. Let's see Yeah, it is gentrification let's look

41:27 the next one here. Figured everybody get that one. All right,

41:34 . Ammonium ion would be the end of which process processes. Ok.

41:50 , let me open. Sorry. . Now you can, ok,

42:13 start the timer here. Ok. it is. Um, it certainly

42:45 nitrogen fixation and I figured everybody would that one. Uh, but the

42:49 we haven't talked about is a Ok. So that too produces

42:56 OK. So, modification is, uh I think that's how we,

43:01 we get our uh nitrogen. Uh really just breaking down of organic

43:06 So think of a protein and you down proteins, proteins have amine groups

43:12 it. And that's essentially ammonia. you, when you break it

43:15 it releases uh lots of ammonia. that's what the modification. So e

43:20 the correct answer here uh because it's um that fixation and the amun.

43:29 . So um so as we, know, talked about maybe a week

43:34 two ago. Uh well, prior spring break, we went through um

43:40 , the nitrogen molecule and its various , right? Oxidized, reduced

43:45 And um so remember that the reduced are used as energy sources by

43:52 right? They can assimilate this uh uh where more uh oxidized forms become

43:59 , this disy processes. Although we mention a a uh nitrogen uh nitrate

44:09 and actually can be assim toy. haven't, we haven't mentioned that

44:13 Um But in any case, the here is that, you know,

44:16 forms of nitrogen span the spectrum of used in different ways, right?

44:20 it's lito or respiration, uh what you, OK. And of

44:25 it's all based on so, media enzymes I would and, and organisms

44:31 different capabilities uh within this whole OK. So, um all

44:39 So obviously, I'm sure we all that the different um elements that are

44:44 our atmosphere, nitrogen is is In highest quantity right near the 80%.

44:51 uh Heber bach process is still in . Uh I think it was invented

44:56 the turn of the century or turn the 20th century um as a way

45:02 make uh ammonia for fertilizers and um uses nitrogen gas and hydrogen gas.

45:11 it uses it under conditions of extreme , extreme pressure, different types of

45:18 catalyst, I think. Um And , uh I, I think it

45:23 accounts for half of the nitrogen that's on earth. Uh The other half

45:29 course comes from bacterial activity. um and so as we've mentioned

45:38 right, we have this as a with the three sides and various forms

45:43 nitrogen are, are part of OK. So, atmospheric nitrogen

45:49 right? So they're three and symbiotic , right? So we'll look a

45:54 bit at Uh and that's your So, um of those two the

46:01 types have the greater contribution in terms amount of N2 fixed on Earth.

46:08 . These are in association with certain . OK. Uh there are free

46:13 types. Uh the free living types , are, are span the spectrum

46:18 different bacterial types. They're not just confined to one group. Um

46:24 that, that is evidence really that the uh metro fixation property itself

46:32 likely passed on through different mechanisms of transfer. We'll talk about that

46:38 in, in Chapter nine. but um in any case, so

46:43 types are ones that are have contributed more in terms of uh nitric fixation

46:49 li types uh in any case. , um so fixation provides ammonia and

46:55 various nitro fires utilize that. So are liu right? We'll oxidize that

47:02 things like nitrate, uh nitrate which then can be utilized for anaerobic

47:08 , right? Deification. OK. so, um and so am ification

47:14 mentioned previously. So uh cantab um like proteins will release ammonia and that's

47:22 uh ammonia can be utilized by OK. So we'll look at each

47:27 these three sides here um starting with fixation. OK. So um the

47:38 so the process of metric fixation is that's very sensitive to oxygen.

47:45 And so uh for that reason, kind of has to operate, you

47:51 where there's they are relatively no OK. Now, the other thing

47:58 it requires a lot of A T and a lot of N A E

48:03 or N AD P H depending on type um bond lines, a lot

48:07 energy to do this. OK. so, uh so remember that,

48:12 N two itself, right? That's bond, right? There's three bonds

48:17 those two N N atoms together, ? So you're gonna have to transform

48:22 into a pneumonia so that it's no it takes into is very stable.

48:27 it's no wonder it takes a lot energy to convert this into ammonia.

48:31 ? But nonetheless critical, right? that's how you know, you get

48:35 nitrogen into the environment. OK? converting it from nitrogen gas, so

48:42 critical. OK. So uh So you don't need to know these

48:50 uh gene genera Slamon. Uh You or may not know this, but

48:57 three types are very different from each . Klebs Y is a gram negative

49:01 is a gram positive and those four is a gram negative that's very different

49:07 Pepsi. So they're all the point is that you see this property

49:11 very different bacterial types. OK. All three of these are what we

49:17 free living types. And so Rizo a type that's, that's a symbiotic

49:23 fixer. OK? He has associations plants. So leguminous plants are things

49:28 um uh clover if you're affording um alfalfa, uh soybean, uh

49:38 plants. These are all in OK? And you can see the

49:43 up here, the soybean plant. the little, the little knobby

49:47 those are the nodules where the bacteria in there fixing nitrogen. OK.

49:55 uh Santa bacteria which are uh of course, uh they too can

50:02 this uh but they have little specialized structures. Uh So What we call

50:09 . So every it's like every 10th is a heteros. So you see

50:13 chain here. So these would be photos photosynthetic types that produce oxygen,

50:22 ? Excuse me. So remember that nitro fixation is poisoned by oxygen.

50:27 the hetero cyst evolved to be a where where nitrogen fixation takes place since

50:32 compartment will be devoid of oxygen. it's CYO bacteria is a way of

50:38 being able to do this by having own special compartment for it called the

50:43 . OK. Um Yeah. So focus here is on symbiotic, a

50:50 . OK. So it's not just random association between bacteria that do this

50:56 and plants. It's it's very OK. Uh The the species of

51:03 and the species of plants, very interactions, right? So these are

51:07 involve different chemical signals between the two bring them together. OK. And

51:13 again, types of plants that do . So things like soybean and particularly

51:17 plants, uh peanut plants grow and nutrient poor soil plant. Practically,

51:23 can sandy soils and they can do . You often find these kinds of

51:29 in nutrient poor soils where other plants necessarily be able to grow. But

51:34 can because they have their own little of nitrogen with them. Ok.

51:40 so, um, so here's an of a root of a, just

51:46 a, a plant that can fix symbiotically with, with these bacteria.

51:52 again, it's all about chemicals that this OK, chemical um uh signals

51:59 bring them together. So uh chemo , right? These are uh these

52:04 the chemical form of being called flavonoids time. And so the plant sends

52:08 out these tracts of bacteria that are to it. And um they

52:14 the bacteria itself has um uh proteins produces uh one of these being a

52:20 factor. And so root hair curling a very important part of this

52:27 Uh mutant plants that can't do this will not, will not form these

52:32 of what are called infection threads. . So, curling of the root

52:38 right? From something like this to like that is based on these kinds

52:44 chemicals, right? And that promotes initiates the um invasion by the cells

52:51 then formation of an infection thread. ? And so um and then be

52:58 beginnings of a nodule as you see , OK. And the beginnings

53:04 So we go like that to that flying to a fully developed or what's

53:09 a bactero. So basically this is this is an example of a

53:14 type that's basically differentiating. So what , what it is here is zum

53:20 as you see here, all Is now differentiating into this form called

53:24 factoid. OK. And so it's an N2 fixing factory. That's

53:29 it does. OK. And so and so we've seen these kind of

53:37 before. think of a of a forming cell, right? It's a

53:41 cell that can form into an endo , right? That's another type of

53:45 . So this is uh analogous to . OK. So the uh the

53:51 form uh provides protection to the to cell but then com compartmentalize it.

53:56 remember, fixation is sensitive to So by putting it in a particular

54:02 of structure like this, it can it minimize the the exposure to

54:08 There's actually another thing that helps with uh too. So, excuse

54:15 so again, very energy expensive, can see the amount of of A

54:19 P S needed. OK. So so we look closer up at

54:24 close up at this here is here be a a bao you see

54:30 OK, that has developed inside of plant. And so um get the

54:39 production needed. So they're gonna have they have a T C A cycle

54:43 on. So the bao is again into this me fixing form if you

54:50 . And uh and so it needs of energy. So N A DNA

54:55 , right? Uh in the creb , OK. Um A T P

55:02 right through, here's a respiratory right? Components. We've gone through

55:08 before. All right, the A P A s and production of A

55:11 P. So I just going to here's nitrogenous enzyme to fix nitrogen.

55:19 . So uh interestingly, they have plant, this is a plant

55:26 produced protein called leg hemoglobin. So know what hemoglobin does. Hemoglobin binds

55:33 . Leg hemoglobin does the same thing the plant. OK? And so

55:39 helps to minimize the um the the oxygen getting inside the bactero,

55:48 You don't want N two inside right? No 02, right?

55:56 so it's like hemoglobin kind of helps it out, right? So it

56:00 aerobic respiration out here, right? part of the respiratory chain. So

56:05 hemoglobin kind of helps to regulate that prevents it from coming inside the back

56:11 will where it would poison this process fixing nitrogen. Ok. So,

56:17 interesting really evolutionary development on the, the part of these two where the

56:22 plant has, has formed this to the process. OK? And so

56:29 the, and you can see here the individual rights over cell.

56:34 Let me put my power cord sorry. And so you can see

56:40 how it differentiates in two, the excuse me plugging in my power cord

56:55 . Ok. So, um so , it's a very energy expensive

57:01 Um and, and uh but the , you know, has it has

57:06 part in the process where it can minimize exposure of oxygen to the

57:11 Uh But then, of course, the the supply of nitrogen through by

57:17 nitrogen fixation process. Of course, plant uses that right to,

57:22 to form its amino acids and, um both coexisting. And so

57:28 the, the plant relies on that . Um So uh let me just

57:35 back real quick if there's any. , here we go. Ok.

57:41 How can these dead zones recover to good B O D? Good

57:47 So, uh oftentimes because they, can persist for quite a while.

57:55 I would have to just be a of time. I mean, you

57:57 , it would be impractical to kind , uh I'm not sure on a

58:02 basis how you, how you could the levels of oxygen in those

58:07 Um um I, I, I'm sure, I don't know uh because

58:15 are still areas that persist even since uh uh what was that called horizon

58:21 in the Gulf. There are still that are, that are dead

58:23 So I, I don't have a answer to that one. Unfortunately.

58:27 What did you miss with sensitive of ? Yes, the nitrogen A is

58:30 is sensitive to oxygen. OK. The uh it's uh that's why we

58:38 this leg hemoglobin, the plant producers kind of help keep oxygen away from

58:43 bactero, but still be able to it for respiration outside that bactero.

58:50 OK. So, uh back All right. So, OK.

58:56 the other side of the triangle, ? So that was the N two

59:00 ammonia. So now, nitrification, we talked about before. Um and

59:05 this is lit, right? using ammonia, uh oxidizing to

59:10 nitrate can be oxidized to nitrate. And as it says, there you

59:15 two different genera, bacteria do, these uh side note. Um

59:22 that same company I worked for, we actually grew uh nitro fires as

59:27 product. Uh So those of you have aquariums may be familiar with

59:32 that in aquariums, you have to monitor the water, especially for ammonia

59:38 because of fish waste. And so can become toxic. And so we've

59:42 had a product that contained nitro fires would sell to like to like to

59:48 restaurants and things that have like these aquariums or even like for coid ponds

59:52 things like that to reduce the levels ammonia in the fish that produced from

59:56 fish waste. And um of the nitrate nitrate produced could be used

60:01 the plants in, in the, the system. And So um prove

60:05 be a, a useful product. of course, um if you have

60:12 ex excess, right, an excess ammonia um in a in an

60:19 uh this activity can produce lots of nitrate which can be acidic and can

60:25 soil P S. OK. This the example I I think I mentioned

60:29 , we haven't looked at this one . This is an example of Asim

60:32 nitrate reduction. So that remember the we looked at before was where this

60:37 to N 20 and then two N . OK. That was the dissimulator

60:47 here. This is, we'll see on the next slide. That's the

60:50 deification, right? But this is one is Asim toy because it's producing

61:00 that then is used by the cells make amino acid. So they're,

61:04 holding on to it right? From toy means you hold on to

61:08 you're not letting it go. And so this is a example of

61:12 toy nitrate reduction. OK? And course, for, for the use

61:18 amino acids, OK? To make acids. So um so you

61:24 metabolism, nitrogen can take lots of forms here. And um and depending

61:29 the bacterial type, it, you , you can do some of these

61:32 not others and, and so OK? Um Just Murray talked about

61:38 uh as well. So um now we're also talking about this as

61:46 right. So here's what we call , nitrate reduction because we're going

61:51 to products ultimately nitrogen that's going to let go to the atmosphere. So

61:56 not holding on to these, hence dissimulator. Right. And so

62:02 so it rates of de electrification, how fast that process process works up

62:11 on top. Uh can um there factors that can, that can influence

62:19 . And so this is, remember is and aerobic, OK? And

62:29 anaerobic respiration, remember that? And so uh in areas that are

62:35 , right? Um it can, activity can be quite vigorous and one

62:40 the 11 of the components in this , the N 20 right is a

62:48 gas. OK? And so levels this can be quite high in areas

62:53 you have these dead zones, Dead zones. So these these this

62:57 deportation can coincide in these areas on that are hy toxic due to these

63:05 effects we've talked about, right? influx of nutrients, aerobic tropes use

63:10 the oxygen, right? Oxygen levels down, right? And so then

63:13 can lead to this uh and and increase in electrification. OK. And

63:21 an increase in levels of this three gas. OK. Um So we

63:28 about another one, right? methane is a greenhouse gas, nitrous

63:32 , right? So these these bacterial are are ones that can are producing

63:37 things. Uh IKEA in case of . But um and so as

63:43 so we can see this uh here's one, a different one. This

63:49 using a nitrate as uh as a becoming reduced. OK. And uh

64:01 two, right? So we've seen one before, right? Hydrogen a

64:04 , right? So it oxidizes OK. And uh and then the

64:12 reduces nitrate right to ammonia. So see this typically in areas that are

64:18 kind of in stagnant areas typically that anaerobic um but may have an influx

64:23 organic material, for example. Um don't know how major of the process

64:28 is, I don't think it's, that big but it can be in

64:31 environmental niches. It can, it , it can form again another way

64:38 bacterial type that can use nitrogen in different way each time. But back

64:43 this right here, we can see . Uh this is data from a

64:50 done in India. So, off coast of India is a hypoxic zone

64:55 , due to the things we talked before, right, influx of uh

64:59 material like the pollutants of some sort creating the, creating the,

65:07 the uh effect of growing and then even taking oxygen from the water

65:14 and creating uh a dead zone. And so now it's anaerobic.

65:19 And so that can promote deification. . And so um that um will

65:31 to production of this is N N 20 uh greenhouse gas that is

65:38 potent. And so you see the starting with nitrate here, then it

65:48 utilized, right? Uh First step deification becomes reduced to uh nitrite.

65:56 so then that goes up right down up. And then, so we're

66:01 , then here, then here, to N O and N 20 as

66:06 see this going up. And so a cascade effect, right? And

66:12 are being this can produce significant amounts this N oxide and greenhouse gas.

66:19 And so all, all, all this occurring because of the generation of

66:24 hypo zones to these effects we talked earlier. So everything can kind of

66:28 , build one, builds on the thing. OK. Um I

66:32 not good but uh it's, it's what can happen in these kind

66:38 situations. OK. Um So the animo reaction, OK. So it

66:51 de de deification, this process right. Right. Here. This

66:59 been known for quite some time. ? And for that reason, it

67:03 thought to be the way the the that contributes to the loss of nitrogen

67:11 the Environment. OK? Until the , I don't know, 15,

67:17 years. Um The animo reaction is one that's been shown to be the

67:25 uh generating the greatest amount of into so both in marine environments, terrestrial

67:34 , uh bacteria that can do this numerous and it wasn't really known uh

67:39 I said, maybe 10 years ago , as how much it contributes

67:43 to the release of N two into environment. And so it's basically using

67:50 ammonia, uh oxidation of pneumonia and of nitrate. And so it's a

67:58 as I said, it's, it's one that accounts for mostly in two

68:02 the atmosphere, not, not but rather this process. OK.

68:07 these plank of my seeds, I to put a picture of this on

68:11 . Uh They're kind of really odd looking bacteria that kind of on

68:16 larger size scale, uh kind of amorphous Bobs, almost not really uniform

68:23 and often have um specialized structures in . Uh In this case for

68:29 for the type that actually carries out reaction, they have specialized structures.

68:34 kind of a an odd um an group in, in that respect.

68:39 But there are other types besides them do that, but they seem to

68:42 one of the, one of the ones, main ones that do

68:45 Um So again, a reaction is can can, can um lead to

68:52 loss of nitrogen uh in tune back the atmosphere. OK. Um

69:00 uh oh I should mention also it is an anaerobic process.

69:04 It's anaerobic process. So this does involve was, so you see this

69:09 , in deep sea sediments in um terrestrial environments. Is where you see

69:14 activity? Ok. Um So uh, let me before we just

69:23 a couple of questions and that's Let me just, um,

69:27 um, there any more questions? . Um Professor, you're muted

70:42 Ok. So, um, so I said, there's a quiz uh

70:48 what we talked about today, that's weekly quiz this week. Um It

70:53 have some, it's gonna have, have a little bit of stuff on

70:55 and eight, but it's, I it's not that many, not that

70:57 questions. Um Like I said, , just nothing that difficult. So

71:02 take it on them Sunday or Monday you finish exam too. Um

71:11 so let's uh this right. So the Flimm treatment uh that's gonna be

71:28 really taking out the big stuff, ? That comes through primary treatment,

71:33 kind of the smaller and soluble Uh Secondary treatment, which of course

71:38 the correct answer. That's, that's your bacteria. Are you promoting growth

71:42 them in secondary treatment? Ok. is a big part of that,

71:47 ? So it's aerobic res aerobic heterotrophic going on there. Tertiary treatment

71:53 the, if it's done is the to be at atl chlorination and that

71:58 of stuff. Um And so, , activated sludge correlates also to secondary

72:05 . So when you see activate sludge activated is kind of the word

72:09 If you wanna focus on a, a on that term. So,

72:14 . So it's microbial activated, let's it that. OK. So activate

72:17 correlates to the secondary treatment. So two uh go hand in hand.

72:25 . So, uh so that's uh all I wanted to cover today.

72:30 I remember it's two, it's chapter , but we're only talking about a

72:36 of sections out of each of right? So just uh focusing on

72:40 cycle, hydrologic cycle. Uh And , it's really, as you saw

72:45 , you kind of just built on uh concepts we talked about previously in

72:52 two and respiration, right? a respiration, um stay in and

73:01 measure molecules and their different uses uh , in an action triangle.

73:07 um is there any questions? Um Well, I hope that we're

73:19 , we're back in the classroom on Thursday and I haven't seen any emails

73:26 from the host uh mentioning, mentioning change Thursday. Uh I'm sure you'll

73:34 the same time I do. But you know, for now, plan

73:38 being back in class uh Thursday. hope I don't wanna continue this

73:44 But um anyway, so, uh , I'll pull up the recording um

73:51 in a second. Uh And then no questions, folks, I will

73:55 you, hopefully see you in person time. OK. Uh uh That's

74:02 folks. So I'll shut her down we'll see you, like I

74:06 uh whatever happens, I'll send you an email so just keep your eyes

74:09 . But for now uh see you . Thank you. You have a

74:16 day. Thank

-
+