0434

1 DIVISION OF ADMINISTRATIVE HEARINGS

2 DEPARTMENT OF ADMINISTRATION, STATE OF FLORIDA

3

4 SUGAR CANE GROWERS COOPERATIVE OF FLORIDA, )

5 ROTH FARMS, INC., and WEDGWORTH FARMS, INC.,)

6 -and- )

7 FLORIDA SUGAR CANE LEAGUE, INC., UNITED )

8 STATES SUGAR CORPORATION, and NEW HOPE ) DOAH

9 SOUTH, INC., ) CASE

10 -and- ) NOS.

11 FLORIDA FRUIT AND VEGETABLE ASSOCIATION, ) 92-3038

12 LEWIS POPE FARMS, W. E. SCHLECHTER & SONS, ) 92-3039

13 INC., and HUNDLEY FARMS, INC., ) 92-3040

14 Petitioners, )

15 -vs- )

16 SOUTH FLORIDA WATER MANAGEMENT DISTRICT, )

17 Respondent, )

18 -and- ) Volume 4

19 MICCOSUKEE TRIBE OF INDIANS, THE UNITED )

20 STATES OF AMERICA, FLORIDA DEPARTMENT OF )

21 ENVIRONMENTAL REGULATION, and FLORIDA )

22 WILDLIFE ASSOCIATION, )

23 Intervenors. )

24

25 DEPONENT: ROBERT H. KADLEC

0435

1 DATE: Thursday, March 25, 1993

2 TIME: 9:15 a.m.

3 LOCATION: Sheraton Hotel, 3200 Boardwalk

4 Ann Arbor, Michigan

5 REPORTER: Rhonda L. Reppert, CSR-3468, RPR, CM

6

7 APPEARANCES:

8

9 MR. GARY V. PERKO

10 Hopping, Boyd, Green & Sams

11 123 South Calhoun Street

12 Post Office Box 6526

13 Tallahassee, Florida 32314

14 Telephone: (904) 222-7500

15 Appearing on behalf of Petitioner, Sugar Cane

16 Growers Cooperative of Florida.

17 MR. RICK BURGESS

18 Peeples, Earl & Blank

19 One Biscayne Tower, Suite 3636

20 Two South Biscayne Boulevard

21 Miami, Florida 33131

22 Telephone: (305) 358-3000

23 Appearing on behalf of Petitioners, Florida

24 Sugar Cane League, Inc., United States Sugar

25 Corporation, and New Hope South, Inc..

0436

1 APPEARANCES: (Cont.)

2

3 MR. DANIEL J. McGRATH

4 Popham, Haik, Schnobrich & Kaufman, Ltd.

5 4000 International Place

6 100 S.E. 2nd Street

7 Miami, Florida 33131

8 Telephone: (305) 530-0050

9 Appearing on behalf of Respondent, South Florida

10 Water Management District.

11

12 MR. GEOFFREY GARVER

13 United States Department of Justice

14 Environment & Natural Resources Division

15 General Litigation Section

16 P.O. Box 663

17 Washington, D.C. 20010

18 Telephone: (202) 272-4692

19 Appearing on behalf of Intervenor, United States

20 of America.

21

22

23

24

25

0437

1 APPEARANCES: (Cont.)

2

3 MR. CARLOS MARIN

4 Law Office of Carlos Marin

5 1101 E. Harrison

6 Harlingen, Texas 78550

7 Appearing on behalf of Ambiotec.

8

9 ALSO PRESENT:

10 Mr. Curtis J. Richardson

11

12

13

14

15

16

17

18

19

20

21

22

23

24

25

0438

1 C O N T E N T S

2 Witness: Page

3 ROBERT H. KADLEC

4 Examination by Mr. Burgess 439

5

6

7 E X H I B I T S

8 Number Identification Page

9 No. 10 Review of the Everglades Protection

10 Project, Conceptual Design,

11 December, 1992 440

12 No. 11 Conference Materials, Phosphorus

13 Uptake in Wetlands 499

14 No. 12 FAX Transmittal - 11/9/92 514

15 No. 13 FAX Transmittal - 5/21/91 548

16 No. 14 FAX Transmittal - 6/14/92 585

17

18

19

20

21

22

23

24

25

0439

KADLEC

1 Ann Arbor, Michigan

2 Thursday, March 25, 1993

3 * * *

4 E X A M I N A T I O N

5 BY MR. BURGESS:

6 Q. Good morning, Dr. Kadlec.

7 A. Good morning.

8 Q. You were telling us before we went on the

9 record that you don't feel you fully answered one of

10 the questions at the end of the day yesterday?

11 A. That's correct. You had, I believe, asked a

12 question in connection with the sites that I might rely

13 on for forming opinions, and we then proceeded to refer

14 to the Kadlec-Newman report, identified sites in that

15 report, but I believe your question as originally

16 phrased was broader than that, and you wished to know

17 all of the sites, and there are perhaps other sites

18 that are not in the Kadlec-Newman report.

19 Q. And what would those include?

20 A. Those would include perhaps, among others, a

21 site at Humboldt, Saskatchewan.

22 Q. Any others?

23 A. I cannot think of any significant others. I

24 had alluded in my reply, I believe, to possible data

25 arriving from an Australian project and a Texas

0440

KADLEC

1 project.

2 Q. And were those projects previously identified

3 in your response to my question concerning Paragraph 11

4 of your vitae?

5 A. Yes.

6 Q. Dr. Kadlec, with respect to those sites you

7 identified yesterday and in response to my questions

8 concerning Question 11 of your vitae, what is it that

9 you're going to rely on from those sites? Is it data

10 from those sites?

11 A. Yes.

12 Q. And in support of what proposition will you

13 rely on that data?

14 A. I don't understand the meaning of the word

15 "proposition".

16 Q. Okay. For what basis -- I'm sorry. For what

17 portion of your testimony that you anticipate giving at

18 the final hearing will you rely upon the data from

19 these various sites?

20 A. The data from these sites will be relevant to

21 testimony on hydrology and phosphorus removal in

22 wetlands.

23 (Deposition Exhibit No. 10

24 marked for identification.)

25 Q. Dr. Kadlec, I show you what's been marked as

0441

KADLEC

1 Exhibit 10 and ask you if you can identify that

2 document.

3 A. Yes.

4 Q. Have you seen it before?

5 A. I believe so, yes.

6 Q. I would refer you to the executive summary,

7 which is viii I believe on the bottom.

8 This document, Dr. Kadlec, talks in

9 terms of review of a settling rate of 8 meters a year.

10 I believe it's your testimony that you no longer feel

11 that that settling rate is applicable as a design

12 criteria for the STAs; is that correct?

13 A. Yes.

14 Q. And is it your opinion, Dr. Kadlec, as you

15 sit here today, that a settling rate of around 10 would

16 be an appropriate basis for design for the STAs?

17 A. Yes.

18 Q. And do you intend to do additional

19 calculations to verify or confirm in your mind what an

20 appropriate settling rate would be for a basis for

21 design?

22 A. I may.

23 Q. And if you do those calculations, do you

24 intend to testify concerning what, in your opinion, is

25 a relevant settling rate for the STAs?

0442

KADLEC

1 A. Yes.

2 Q. What method -- by that I mean data and

3 model -- do you intend to use if you do decide to

4 determine a settling rate value?

5 A. I don't know that I can project at this time

6 what I may do in a future calculation.

7 Q. If you had to estimate that K value today,

8 what model would you use to do that?

9 A. I would consider -- I guess I should first

10 ask what you mean by "model" in this context.

11 Q. Yesterday we identified in one of the

12 exhibits three different phosphorus mass balance

13 equations which you said had applicability to

14 determination of a settling rate constant, correct?

15 A. We did.

16 Q. That is the -- strike that. I don't want to

17 limit my question to those three equations, but when I

18 speak in terms of a model to estimate K, I'm speaking

19 in terms of those type of equations that you have

20 testified to.

21 A. I'm sorry. I don't understand what the

22 question was.

23 Q. Do those phosphorus mass balance equations

24 that we spoke about yesterday -- are they used to

25 estimate settling rate constants?

0443

KADLEC

1 A. Those equations we spoke of yesterday could

2 be used to estimate settling rate constants under the

3 mixing scenario and other assumptions built into the

4 development of those equations.

5 Q. How would you go about -- if you had to today

6 estimate K, how would you go about doing it?

7 A. I would have several choices available to me.

8 Q. Okay. And they would be --

9 A. I could presume that the operation of area 2A

10 was plug flow, and use the corresponding equation to

11 estimate a settling rate coefficient. That would be

12 one option.

13 Do you wish me to go on?

14 Q. Yes. Thank you. I'm trying to determine

15 what options are available to you and what -- if you

16 had to do it today, what option you would select.

17 A. Under a different option, I could represent

18 the mixing in area 2A by a series of well mixed units

19 of some number, and use the corresponding equations to

20 estimate a K.

21 Q. Are those your two options? Any others?

22 A. Well, as I indicated in a line of questioning

23 yesterday, there are an almost limitless number of

24 series and parallel connections of such idealized

25 components of the system that could be presumed.

0444

KADLEC

1 Q. If you had to choose today among the options

2 you just listed, which one would you select as the most

3 appropriate with respect to WCA2A?

4 A. I would choose the most conservative, which

5 would be the plug flow version.

6 Q. Now assuming that utilizing that version gave

7 you your estimate for K, what model would you use to

8 estimate acreage?

9 MR. GARVER: I object to the form. Are

10 you talking about acreage of STAs?

11 MR. BURGESS: Yes.

12 MR. GARVER: I object to the form.

13 A. Well, in estimating acreage in the design

14 mode of calculations, I would most probably utilize

15 more than one model.

16 Q. Why would you utilize more than one model?

17 A. Because in the design mode I would want to

18 understand the sensitivity of design calculations to

19 different model assumptions.

20 Q. What models might you use?

21 A. Because there is a very large number of

22 potential series of parallel combinations of the ideal

23 units I have alluded to, and because those calculations

24 need in some sense to reflect the potential

25 configuration of an STA, it's difficult to answer that

0445

KADLEC

1 question in a broad sense.

2 Q. I'm just trying to find out, if you assume

3 that you have your estimate for K, in other words you

4 have satisfied yourself that the specific number which

5 you testified to yesterday could be around ten, what

6 would you do next if someone asked you to design the

7 STAs for the Everglades, given the K value that you

8 have determined and given the necessity of having those

9 STAs achieve a 50 parts per billion outflow

10 concentration of the water conservation areas?

11 MR. GARVER: I object to the form.

12 A. Well, what I'm trying to indicate in reply to

13 that question is that the settling rate coefficient

14 must then be utilized in mass balance calculations

15 which should, in design, reflect the sensitivity of

16 such calculations to factors other than the settling

17 rate constant. By that I mean the configuration of a

18 proposed STA would have implications as to the mixing

19 patterns that might occur in that particular STA.

20 Q. So assuming you then do these mass balance

21 calculations, what do you do after you complete those?

22 How do you get to the acreage, your estimate of

23 acreage?

24 I'm trying to understand your testimony,

25 Dr. Kadlec, and I'm asking you for what you would do

0446

KADLEC

1 next in order to estimate acreage if someone asked you

2 to do that, and I think you just said you have to do a

3 series of mass balance calculations.

4 Okay. After you do that, then what do

5 you do? Does that series of mass balance calculations

6 give you estimates of acreage?

7 A. It could, but given the complexity of the

8 calculations for a multiple cell STA, it is more likely

9 that the calculations would be done in a manner in

10 which the area of the system was varied, each cell in

11 the system was varied, until the design goal for the

12 STA was achieved.

13 So it is a more -- I'm having

14 difficulty, because this is not a straightforward

15 simple calculation, and it's difficult to answer a

16 brief question on how this is done.

17 Q. Is it your understanding that the STAs will

18 be of the multi cell variety?

19 A. Yes.

20 Q. Is that a Burns & McDonnell design criteria,

21 as far as you know?

22 A. That has been an element of the conceptual

23 design, and it is my belief that it will continue to be

24 so.

25 Q. What equation or equations do you feel would

0447

KADLEC

1 be most appropriate to perform these mass balance

2 calculations?

3 A. I would ask you what you mean by "these

4 mass --

5 Q. The ones that you testified to after you had

6 your value for K you would need to perform.

7 I thought I understood you to say after

8 you had your estimate for K and on your way to

9 determining the acreage, you would have to perform a

10 series of mass balance calculations.

11 A. That's correct.

12 Q. What equation or equations would you

13 anticipate using for those mass balance calculations?

14 A. It would depend on what the presumption of

15 flow pattern was for that particular iteration of

16 design calculations that is being done.

17 Q. How many different flow patterns would you

18 estimate you would examine, performing these mass

19 balance calculations?

20 A. That's difficult to answer in advance of the

21 fact.

22 MR. GARVER: You shouldn't speculate.

23 Q. What are your choices?

24 A. What are my choices concerning --

25 Q. Flow patterns.

0448

KADLEC

1 A. The choice for a cell in an STA, the choices

2 would range between a single well mixed unit to a

3 single plug flow unit.

4 Q. And would you anticipate examining both of

5 those and others?

6 A. I would anticipate using more than one of the

7 options available, yes.

8 Q. And what type of flow pattern, among those

9 that you just identified and whatever others might

10 exist that you haven't identified but that you might

11 consider, do you envision would be used in the design

12 configuration for the STAs?

13 MR. GARVER: Objection; calls for

14 speculation.

15 A. If you would rephrase the question. I did

16 not understand the question.

17 Q. Okay. What flow pattern do you consider in

18 your opinion to be most appropriate to use in the

19 calculations which you're going to perform for the

20 design configuration?

21 A. Well, the trouble I have with the question is

22 the calculations do not calculate the design

23 configuration.

24 Q. Okay. What do they calculate?

25 A. The calculation can be made for a given

0449

KADLEC

1 mixing assumption in a given STA cell of the

2 concentration change to be expected in that cell.

3 Q. Okay. I want to go back. In response to one

4 of my questions you said it would depend upon the flow

5 pattern that was used or that was chosen, and in that

6 context do you remember -- do you recall that answer?

7 A. Not explicitly.

8 Q. Okay. Why is flow pattern important for --

9 is flow pattern important for these calculations?

10 A. Yes.

11 Q. Okay. Why is it important for the

12 calculations?

13 A. Because the expected performance of a unit in

14 an STA depends upon flow pattern.

15 Q. What flow pattern do you feel is most

16 appropriate for the calculations?

17 A. In the absence of detailed information on

18 configuration of that particular unit in the design of

19 that particular STA unit, it's difficult to answer that

20 question.

21 Q. Are you familiar with Burns & McDonnell's

22 conceptual design?

23 A. I believe I know which document you refer to,

24 yes.

25 Q. If I asked you to assume configurations that

0450

KADLEC

1 are in that document, does that help you answer my

2 question?

3 A. It helps in some degree, yes.

4 Q. Can you tell me what type of flow pattern you

5 would feel would be most appropriate, if the design

6 were to design to the Burns & McDonnell STA design

7 criteria?

8 A. Well, the Burns & McDonnell conceptual

9 design, which does contain some projected layouts of

10 STAs, would be of assistance in answering the

11 question. However, there are four STAs laid out in

12 that document, and within each of those there are a

13 number of cells. Those cells are of different shapes

14 and sizes. To answer your question, I would have to

15 know which of those I am to estimate my opinion of the

16 flow pattern.

17 Q. Do each of those STAs need to be designed

18 separately?

19 A. Yes.

20 Q. Do each of them require a separate

21 calculation of a settling rate?

22 A. The design calculations do not involve a

23 calculation of the settling rate.

24 Q. Okay. Independent question. I'm going back

25 to calculations of settling rates.

0451

KADLEC

1 Based upon your testimony that each of

2 the STAs need to be designed separately, in your

3 opinion, do you need -- strike that.

4 In your opinion, is it necessary to

5 calculate -- to independently calculate settling rates

6 for each of the four STAs that Burns & McDonnell have

7 in their STA conceptual design?

8 A. I don't understand the question. The reason

9 I don't understand the question is that the design

10 process will utilize a value of the settling rate.

11 Q. Yes, sir. And in your opinion, since you

12 have testified that each of those four STAs should be

13 designed separately, I'm asking you whether in your

14 opinion you feel the predecessor calculation of the

15 settling rate should be independently performed for

16 each of the four STAs.

17 MR. GARVER: I object to the form.

18 Q. Can you answer that?

19 A. I think that a single value of the settling

20 rate may be used for the four STAs.

21 Q. What is the -- thank you. What is the basis

22 for that opinion?

23 A. The basis for that opinion is that there is

24 sufficient similarity in the intended nature of these

25 STAs, in terms of water depth, vegetation, and the

0452

KADLEC

1 parameters which influence performance, to warrant that

2 statement.

3 Q. Have you visited any of the areas where you

4 understand the four STAs are going to be constructed?

5 A. Yes.

6 Q. Which of the four or all of the four?

7 A. I have visited the area of STA 1.

8 Q. Have you done any field sampling in any of

9 the areas where the STAs are going to be constructed?

10 A. No.

11 Q. Do you know of anyone that has taken soil

12 samples -- other than where STA 1 is going to be

13 constructed -- in areas where STAs 2, 3 or 4 are going

14 to be constructed?

15 A. No.

16 Q. Have you yourself reviewed any data or soil

17 cores from those areas?

18 A. No.

19 Q. Back to my question about STA design

20 process. Is it your understanding that a mixing

21 assumption needs to be made as part of the design

22 process?

23 A. Yes.

24 Q. Which mixing assumption would you recommend

25 be used and why?

0453

KADLEC

1 A. As I think I have answered on previous

2 occasions, I think that several mixing assumptions

3 should be explored in the design process.

4 Q. And as you sit here today, do you have an

5 opinion as to which is the most appropriate for the

6 STAs, for design of the STAs?

7 A. In general terms, I believe that a degree of

8 mixing intermediate between plug flow and well mixed is

9 appropriate.

10 Q. Is that the same as or different from what

11 you understand Burns & McDonnell is recommending?

12 A. It is the same as Burns & McDonnell have used

13 in the conceptual design.

14 Q. Have you had discussions with anyone from

15 Burns & McDonnell as to whether they are going to

16 continue to recommend that through the conceptual

17 design process?

18 A. I have not.

19 Q. Have you recommended to Burns & McDonnell

20 that they utilize that mixing assumption -- strike

21 that.

22 Did you recommend to Burns & McDonnell

23 that they utilize that mixing assumption for the

24 conceptual design process?

25 A. What do you mean by "that mixing

0454

KADLEC

1 assumption"?

2 Q. The one that I asked you to identify what you

3 thought would be the most appropriate.

4 A. The intermediate degree of mixing?

5 Q. Right.

6 A. Yes.

7 Q. And was that a recommendation that was made

8 at or near the time you were on the STA design

9 committee?

10 A. Yes.

11 Q. And as far as you know, that is the mixing

12 assumption that Burns & McDonnell is continuing to

13 recommend in their conceptual design process?

14 MR. GARVER: Do you mean the general

15 design process, Mr. Burgess?

16 MR. BURGESS: General design process.

17 A. I can't answer for what Burns & McDonnell are

18 doing at the present time.

19 Q. When did you last speak with anyone from

20 Burns & McDonnell?

21 A. It was late February of this year.

22 Q. And in what context did you meet or speak

23 with --

24 A. There was a meeting at the South Florida

25 Water Management District.

0455

KADLEC

1 Q. Have you recommended any cell layout

2 configuration to Burns & McDonnell?

3 A. No.

4 Q. What cell layout configuration would you

5 recommend should be used in the STA design process?

6 A. That question cannot be answered without

7 understanding the site specific conditions of the STA

8 in question.

9 Q. In your opinion, it is going to vary between

10 and among the four separate STAs?

11 A. Yes.

12 Q. Okay. Well, what cell layout configuration

13 would you recommend with respect to STA 1? Strike

14 that. Strike that.

15 Are you familiar with the

16 recommendations for cell configurations that Burns &

17 McDonnell have included in their conceptual design?

18 A. Yes.

19 Q. Okay. Do you agree with them?

20 A. I have not formed an opinion.

21 Q. Do you anticipate at the time of trial that

22 you will testify concerning the cell configurations of

23 the various STAs?

24 A. I may.

25 Q. Do you intend to review the general design of

0456

KADLEC

1 Burns & McDonnell with respect to cell configurations

2 in the STAs?

3 A. I expect so.

4 Q. Was the last cell configuration that you saw

5 from Burns & McDonnell contained in their conceptual

6 design document?

7 A. I'm sorry. Could you please repeat the

8 question?

9 Q. What was the last cell configuration that you

10 recall seeing from Burns & McDonnell, their

11 recommendation? Was it in their conceptual design

12 document?

13 A. Yes.

14 Q. Do you know the timetable for their

15 production or completion of their general design

16 document?

17 A. In a rough way.

18 Q. When do you understand that that document is

19 due?

20 A. In early summer.

21 Q. This year?

22 A. Yes.

23 Q. Have you seen a draft of the document?

24 A. I have seen a small portion of what I believe

25 to be a draft of such a document.

0457

KADLEC

1 Q. Is that something that has been publicly

2 available, to your knowledge?

3 A. I don't know.

4 Q. How did you get it?

5 A. It was given to me by Galen Miller.

6 Q. When did he give it to you?

7 A. I can't give you the exact date, but it was

8 early in this year, January or February of this year.

9 Q. And what was the document called?

10 A. It had no name.

11 Q. What was contained in the document?

12 A. The document contained, among other things,

13 the reproduction of the equations that I had

14 transmitted to Galen Miller in December of 1992.

15 Q. Did it contain any cell configurations for

16 the STAs?

17 A. No.

18 Q. Did you have any comments back to Galen

19 Miller with respect to what he provided to you?

20 A. No.

21 Q. Dr. Kadlec, in your opinion will the ENR

22 project, for which you have attended two workshops I

23 believe you have testified, assist you with the future

24 design of these cells in the STAs?

25 MR. GARVER: I object to the form. I

0458

KADLEC

1 believe Dr. Kadlec said he was going to design those

2 cells.

3 MR. BURGESS: Okay.

4 Q. Well, assist you in your review of the design

5 work of Burns & McDonnell.

6 A. But what do you mean by -- I believe you said

7 ENR project.

8 Q. Yes.

9 A. What do you mean, will it help? What's "it"

10 in this case?

11 Q. Given what you know about the ENR project,

12 what configuration would you recommend for STA 1, what

13 cell configuration?

14 A. Well, I believe --

15 MR. GARVER: I object to the form.

16 A. Well, I believe I have answered that cell

17 configuration is determined by site specific factors.

18 Q. Like?

19 A. The potential possibility of citing pump

20 stations and outflow structures, among other things,

21 physical site constraints.

22 Q. Earlier this morning, Dr. Kadlec, when I

23 asked you if you had to estimate K today what model

24 would be used, I believe you said that in your opinion

25 the plug flow model would be most appropriate; is that

0459

KADLEC

1 correct?

2 A. Yes.

3 Q. What is the basis for that opinion?

4 A. The basis for that opinion is twofold.

5 Firstly, as I have indicated several

6 times, I believe that is the conservative presumption

7 for the estimation K, and secondly, my best

8 understanding of flow patterns in area 2A.

9 Q. Why, in your opinion, is the plug flow model

10 the most conservative?

11 A. Because it returns the smallest value of the

12 settling rate constant.

13 Q. Why is it important that the settling rate

14 constant be the smallest value?

15 A. The importance is my personal preference, in

16 a process involving parameter estimates and subsequent

17 design in the face of uncertainty as to mixing either

18 in the prototype or in the final system, to stay on the

19 conservative side when assumptions must be made.

20 Q. And do conservative K values yield larger or

21 smaller amounts of acreage when those K values are used

22 in design equations?

23 A. Larger.

24 Q. You have testified previously that in your

25 opinion the flow patterns in WCA2A are sheet flow; is

0460

KADLEC

1 that correct?

2 A. I don't believe I said that.

3 Q. Then I didn't want to repeat your testimony,

4 so then I do need clarification.

5 You said there were two reasons

6 supporting your use of the plug flow model, the second

7 one of which was your assumptions of the flow patterns

8 in 2A. What is your understanding of the flow patterns

9 in 2A?

10 A. That it is approximated by plug flow.

11 Q. What does that mean, I mean in layman's

12 terms, "approximated by plug flow"?

13 A. In layman's terms, that means that an element

14 of water enters through an inlet structure and proceeds

15 on a course toward the outlet structure, with small, if

16 any, mixing, with preceding or succeeding elements of

17 water.

18 Q. What is sheet flow?

19 A. In the wetland hydrology context, that is

20 used to refer to a shallow depth of water over a broad

21 expanse, in motion.

22 Q. And do you think WCA2A hydrologic conditions

23 approximate sheet flow?

24 A. The term "sheet flow" is not an absolute

25 quantifiable term. I personally do not often use the

0461

KADLEC

1 term "sheet flow". It would be my understanding, if I

2 were to use it, that yes, that's what exists in area

3 2A.

4 Q. Okay. And what, in your opinion, is the

5 direction of flow in 2A?

6 A. In general terms, from north to south.

7 Q. And the basis for that opinion?

8 A. Because the inlet structures are on the north

9 and the outlet structures are on the south.

10 Q. Is there any lateral variability to the

11 magnitude of flow in 2A?

12 A. Well, as we went through this yesterday, this

13 needs a referent of time in question, the depth in

14 question, but in general terms, there is variability in

15 the magnitude of flow in area 2A.

16 Q. You say in general there is variability in

17 the magnitude of flow in 2A. Have you attempted to

18 quantify that variability?

19 MR. GARVER: I believe this area was

20 covered in some detail already.

21 MR. BURGESS: I don't think that

22 specific question was.

23 A. I have not taken data on flows in area 2A.

24 Q. Is that one way, in your opinion, to quantify

25 the variability of flow?

0462

KADLEC

1 A. Yes.

2 Q. What type of data would be taken?

3 A. I'm sorry. The referent for the question is

4 unclear. I don't know why I would be taking data.

5 Q. In an attempt to quantify the variability in

6 flow in 2A.

7 A. Well, there are several types of variability,

8 and so the answer to the question, I would need to

9 know --

10 Q. Variability in the direction of flow.

11 A. In the direction of flow?

12 Q. Yes.

13 A. Would you repeat the question at this point,

14 please?

15 Q. Dr. Kadlec, you have been testifying for the

16 last five minutes that in your opinion there is

17 variability in the direction of flow in 2A; is that

18 correct?

19 A. No, I think it was the magnitude.

20 Q. Okay. Thank you.

21 Is there variability in the magnitude of

22 flow in 2A?

23 A. I would expect so, yes.

24 Q. That's right. Okay.

25 And one way to quantify the variability

0463

KADLEC

1 in magnitude is through the collection of data; have

2 you testified to that?

3 A. Yes.

4 Q. What data would you seek to collect to

5 determine that variability in the magnitude of flow?

6 A. There are different approaches that could be

7 taken to make such a determination. One such approach

8 could be to make local velocity measurements in 2A.

9 Q. Do you know of anyone who has attempted to

10 take local velocity measurements in 2A on behalf of the

11 Department of Justice?

12 A. No.

13 Q. Do you know anyone who has done that on

14 behalf of the South Florida Water Management District?

15 A. No.

16 Q. Have you seen any data referencing local

17 velocity measurements?

18 A. No.

19 Q. Do you know if that is a work step planned by

20 the United States prior to the time of trial?

21 A. No.

22 Q. Is it important to you, in either your

23 calculation of the K rate or estimation of the acreage

24 to achieve compliance with 50 parts per billion outflow

25 requirement, to know the magnitude of flow in WCA2A?

0464

KADLEC

1 MR. GARVER: Well, I don't believe

2 Dr. Kadlec said he was going to make those

3 calculations.

4 MR. BURGESS: I think he said he may.

5 MR. GARVER: It calls for speculation.

6 Q. Were you to make those calculations,

7 Dr. Kadlec, would the variability in the magnitude of

8 flow be important to you?

9 A. I cannot tell at this time.

10 Q. Why not?

11 A. Because that is dependent on the relative

12 importance of the size of those variations.

13 Q. Would it make a difference to the accuracy of

14 your plug flow model if 50 percent of the water in

15 WCA2A moved east/west and not north/south?

16 A. Well, I would return to an answer that I made

17 I believe yesterday, which is, it is not possible in

18 general terms for that to occur, because although water

19 can move on preferential paths from north to south, all

20 of the water eventually has to make it through the

21 outlet instructs to the south, so your hypothetical

22 situation I don't believe is possible.

23 Q. If it happened, would it make a difference?

24 MR. GARVER: I believe Dr. Kadlec said

25 he doesn't believe it would be possible.

0465

KADLEC

1 MR. BURGESS: I'm asking him to assume.

2 A. Well, in order to understand your question, I

3 would need to know what area of 2A you are referring

4 to, and in what way, which side, in what way there can

5 be an east/west flow out of whatever area it is we're

6 describing.

7 Q. Do you anticipate that you would conduct a

8 sensitivity analysis with respect to the magnitude of

9 flow in 2A prior to undertaking your calculations to

10 determine K?

11 A. Yes.

12 Q. Have you done such sensitivity analysis?

13 A. No.

14 Q. As you sit here today, do you anticipate as a

15 contemplated work step before the trial of this matter

16 that you are going to conduct such sensitivity

17 analysis?

18 A. Yes.

19 Q. Do you know of anyone on the department -- do

20 you know of any consultant to the Department of Justice

21 that has made such a sensitivity analysis with respect

22 to the flow in 2A?

23 A. No.

24 Q. Other than conducting a sensitivity analysis,

25 do you anticipate evaluating the magnitude of flow in

0466

KADLEC

1 any other manner between now and the trial of this

2 matter?

3 MR. GARVER: You mean the flow in 2A?

4 MR. BURGESS: Yes.

5 A. Only in the sense that such a sensitivity

6 analysis would avail itself of all information at my

7 disposal.

8 Q. If there were preferential paths in 2A that

9 routed 50 percent of the water east/west, would this

10 affect your plug flow model?

11 MR. GARVER: I object to the form.

12 A. I would have to know where in 2A, to answer

13 that question. 2A is an area larger than the area used

14 to estimate the parameter K.

15 Q. Let's say 50 percent of the water initially

16 entering Water Conservation Area 2A through the ten

17 structures.

18 MR. GARVER: I object to the form.

19 A. I don't understand your scenario for where

20 that water then goes.

21 Q. East/west and then north/south.

22 A. Well, the difficulty I have with your

23 question is that water goes one way, it doesn't go

24 east/west and then north/south, so I just would ask you

25 to explain what you mean by that.

0467

KADLEC

1 Q. What effect would preferential paths have on

2 your plug flow model?

3 MR. GARVER: I object to the form.

4 A. As I understand that question, preferential

5 paths are one of the ways in which a nonplug flow

6 mixing pattern can obtain in a given wetland.

7 Q. Have you conducted sensitivity analysis with

8 respect to the magnitude of flow in 2A already?

9 A. No.

10 Q. Do you know of anyone else besides yourself

11 that anticipates evaluating the magnitude of flow in 2A

12 for the Department of Justice?

13 A. No.

14 Q. Okay.

15 MR. GARVER: About ready for a break,

16 Mr. Burgess?

17 MR. BURGESS: Okay.

18 (Recess taken: 10:10 - 10:22)

19 Q. Dr. Kadlec, in the Kadlec-Newman paper which

20 is Exhibit No. 8, did you find that depth should not be

21 a model parameter because there was no correlation

22 between depth and performance of a given wetland?

23 MR. GARVER: You should review that

24 document if you wish, Dr. Kadlec.

25 A. Well, there is a work element on that in this

0468

KADLEC

1 document. I need to refer -- it's in the appendices

2 section.

3 I have reviewed the section that I think

4 you're alluding to, and I would ask you, please, to

5 repeat the question.

6 Q. Do you have any findings or conclusions in

7 that exhibit concerning the relationship between

8 wetland performance and depth?

9 A. Yes.

10 Q. What are those conclusions or findings?

11 A. The conclusion reached from that particular

12 section was that evidence from Boney Marsh and Iron

13 Bridge did not support the hypothesis that a volume

14 specific uptake or settling rate was to be preferred to

15 an area specific rate.

16 Q. And what does that say about the

17 consideration of depth of a wetland?

18 A. That implies that depth is a factor in

19 hydrology, but probably not in wetland function.

20 Q. Do you utilize depth as a parameter in your

21 plug flow model for WCA2A?

22 A. Not directly.

23 Q. How is it used indirectly?

24 A. That I would have to review. Could I please

25 review the exhibit in question?

0469

KADLEC

1 Well, I slightly misspoke. This is a

2 steady state version in which depth does not appear

3 indirectly either.

4 Q. Does your plug flow model for 2A use

5 hydraulic loading rate as a model parameter?

6 A. To which model do you refer?

7 Q. The plug flow model that you have utilized

8 for your various calculations for 2A.

9 A. I draw a distinction between "model" and

10 "equation".

11 Q. Okay.

12 A. So I would ask you what you mean by that.

13 Are you referring to equations 10 or 11 --

14 Q. Yes, sir.

15 A. -- in Exhibit 6?

16 Q. Yes.

17 A. And so in that context question was --

18 Q. Is hydraulic loading rate a parameter?

19 A. Yes.

20 Q. Is hydraulic detention time a parameter?

21 A. No.

22 Q. Let me refer you to Exhibit 7 from

23 yesterday. The last sentence in the first paragraph

24 reads "Attempts to correlate wetland performance for

25 pollutant reduction with very simple design variables

0470

KADLEC

1 such as hydraulic loading rate, detention time, and

2 pollutant loading rate, have all failed to produce

3 satisfying results".

4 I think I asked you yesterday whether

5 that was a true statement when made and whether you

6 agreed with it today, and you said yes; is that

7 correct?

8 A. Yes.

9 Q. Why, if that statement is true -- and the way

10 I read it, it indicates that attempts to correlate

11 performance with a design variable of hydraulic loading

12 rate hasn't produced satisfactory results. Why, if

13 that is a given, do you use hydraulic loading rates as

14 a parameter for your plug flow equation for 2A?

15 A. Because the equations in Exhibit 6 that we

16 were referring to are not an attempt at a correlation.

17 Q. What are they an attempt to do?

18 A. Those equations are mass balances, not

19 correlations.

20 Q. So in your opinion it is a valid exercise to

21 use a hydraulic loading rate in equations such as 10

22 and 11 in contradistinction to utilizing them to

23 correlate wetland performance or to evaluate wetland

24 performance?

25 A. It's inescapable in the acknowledgment of

0471

KADLEC

1 conservation of mass.

2 Q. Do all of the models in Exhibit 7 utilize

3 detention time as a parameter?

4 MR. GARVER: Did you say do all of the

5 models?

6 MR. BURGESS: Yeah, the models.

7 Q. Or the equations. Again, I'm sorry. I will

8 refer you to the equation on No. 3, No. 5. I don't see

9 any others, but maybe you do.

10 A. The equations in Exhibit 7 contain contact

11 time or detention time, yes.

12 Q. Does the data that you have reviewed with

13 respect to 2A validate the use of detention time?

14 MR. McGRATH: I object to the form.

15 A. I have not attempted to validate the use of

16 detention time for data from 2A.

17 Q. If you used a hydraulic detention time

18 model -- or equations, I'm sorry -- instead of a

19 hydraulic loading rate equation for 2A, in your opinion

20 would it lead you to a higher or lower value of K?

21 A. Since the two procedures lead to a different

22 K, a different type of K, the two cannot be compared.

23 Q. Why do they lead to different types of K?

24 A. Because they are used in different equations

25 and different units, different meanings.

0472

KADLEC

1 Q. What type of K would you get if you used

2 hydraulic detention time as opposed to hydraulic

3 loading rate?

4 A. A mass balance model that utilizes detention

5 time necessarily involves a rate constant that I refer

6 to as a volume specific rate constant. A model that

7 utilizes hydraulic loading rate is the same mass

8 balance, but in that case it is an area specific rate

9 constant. Two different quantities.

10 Q. If you used a hydraulic detention time model

11 instead of a hydraulic loading rate model for 2A, would

12 it lead to higher or lower acreage for the STAs?

13 MR. GARVER: I object to the form.

14 A. I don't know.

15 Q. Well, why don't you know? Is there other

16 information that is required before you can answer the

17 question?

18 A. Yes.

19 Q. What information would that be?

20 A. An estimate of the volume specific value of

21 an uptake coefficient.

22 Q. What is a volume specific value for an uptake

23 coefficient?

24 A. It is the coefficient in a rate equation that

25 presumes that phosphorus uptake is proportional to the

0473

KADLEC

1 concentration of phosphorus in the water and to the

2 volume of water in question.

3 Q. Do you anticipate before the trial of this

4 matter that you would conduct such an analysis to

5 determine what the K value would be so you could answer

6 the question that I have posed?

7 A. I have no such plans at this time.

8 Q. Why did you use detention time in the models

9 in Exhibit 7 and not in the models for 2A?

10 MR. GARVER: Are you referring to models

11 or equations, Mr. Burgess?

12 MR. BURGESS: I was referring to

13 equations earlier, but I think Dr. Kadlec has been

14 answering my questions in the terms of these as

15 models.

16 A. Well, I'm now aware that we need not make too

17 careful a distinction apparently, and I have been, I

18 think, interpreting correctly what you mean.

19 Q. Okay.

20 A. In Exhibit 7, equations 1 through 5 occur in

21 a section on reactor theory taken from the literature,

22 and in that literature the common practice, because of

23 the nature of chemical reactors in general, is to use

24 volume specific reaction rates. That's equations 1

25 through 5.

0474

KADLEC

1 Equations 6 and 7 are taken from other

2 literature from a reference by Reed, et al, which is

3 reproduced elsewhere.

4 So those are not models that I'm using.

5 They are models that I'm quoting from the literature.

6 And I believe those are all of the equations listed in

7 this document.

8 Q. If I can refer you to Page 5, the top of the

9 paper, is that model depicted in the top figure

10 utilizing hydraulic detention time or hydraulic loading

11 rate?

12 A. Figure 4 depicts a hydrologic situation. It

13 depicts dye concentration versus time. It does not

14 purport to represent a model of concentration of a

15 reactive species.

16 Q. For the Des Plains, Illinois site, which I

17 think you said was one of the ones that you might rely

18 upon at the time of trial, did you estimate a hydraulic

19 loading rate or a hydraulic detention time?

20 Do you utilize a hydraulic loading rate

21 based parameter or hydraulic detention time based

22 parameter?

23 A. Well, you have asked two questions. I would

24 ask you to please repeat the first and I'll attempt to

25 answer it.

0475

KADLEC

1 Q. I think the one that I need an answer to is,

2 with respect to Des Plains, Illinois, that site which I

3 think is the one you said you might rely upon at the

4 time of trial, did you utilize a hydraulic loading rate

5 based parameter or a hydraulic detention time based

6 parameter?

7 A. Well, the answer is that in this particular

8 document, which is Exhibit 7, I'm attempting to model

9 the movement of a noninteractive tracer which moves

10 with the water, through the wetland. There is no

11 uptake process being modeled in this connection at all,

12 and consequently the model in question is simply one of

13 liquid movement through the system. It has nothing

14 whatsoever to do with an uptake model. The concepts of

15 hydraulic loading rate and detention time are not

16 operative in the context we have been discussing them.

17 Q. For any of the work that you have done at

18 Des Plains, have you utilized a hydraulic loading rate

19 based model or a hydraulic detention time based

20 model --

21 MR. GARVER: I object to the form.

22 Q. -- for describing the movement of phosphorus?

23 MR. GARVER: I object to the form.

24 A. In my work in attempting to describe

25 phosphorus at the Des Plains site I have used a

0476

KADLEC

1 hydraulic loading rate model in the sense I believe you

2 mean it.

3 Q. Have you made any attempts to utilize a

4 hydraulic detention time model for WCA2A?

5 A. I believe I may have.

6 Q. When would you have conducted that effort?

7 A. It would have been very early in my work with

8 data sets from 2A, and there's a possibility I -- at

9 that point in time I may have attempted to extract the

10 volumetric rate constant. I can't recall as I sit here

11 today.

12 Q. You would have attempted that through a

13 series of calculations; is that correct?

14 A. Yes.

15 Q. Do you know whether those calculations were

16 made available with your documents?

17 A. I would have produced them, given them to the

18 Department of Justice for production, yes.

19 Q. And do you know where among your documents

20 and how we may be able to identify such calculations?

21 A. I would assume that they would be in a file

22 that has designation WCA2A.

23 Q. Do you recall any of the results of those

24 calculations?

25 A. No.

0477

KADLEC

1 Q. Do you know whether the calculations produced

2 a K?

3 A. Yes.

4 Q. Do you know what the K was?

5 A. I cannot recall any numerical values.

6 Q. Do you know whether it was lower than 8

7 meters a year?

8 A. That is not possible. The units are not

9 meters per year for volumetric rate constant.

10 Q. What are the units?

11 A. It would be reciprocal time; for example, one

12 over years.

13 Q. And you don't recall what that value might

14 have been?

15 A. No, if in fact I made such calculations.

16 That's some time ago.

17 Q. Why would you -- if you made such

18 calculations, why would you not have pursued those

19 calculations?

20 A. Because it's my belief that the phosphorus

21 uptake potential of a wetland is more appropriately

22 described as area specific than volume specific.

23 Q. And the basis for that opinion is?

24 A. That a given square meter of wetland should

25 not remove twice as much phosphorus if the water is

0478

KADLEC

1 twice as deep.

2 Q. Is depth important for phosphorus removal in

3 a wetland?

4 A. It may have effects on phosphorus removal.

5 Q. And what factors of depth would affect

6 phosphorus removal?

7 A. What do you mean by the word "factors" of

8 depth?

9 Q. I'm trying to -- I think we have agreed that

10 depth may be important in your opinion to a wetland,

11 and I guess I would rephrase my question to say how

12 might depth be important in a wetland?

13 MR. GARVER: For P removal?

14 MR. BURGESS: Yes.

15 A. Well, one such way would be as an influence

16 on the type of vegetation that could be sustained in

17 such a wetland.

18 Q. Is it your opinion that there is no

19 correlation between depth and performance of a

20 wetland -- is it your opinion that there is no

21 correlation between depth and performance of a wetland?

22 A. No.

23 Q. What is your opinion with respect to

24 correlation between depth and performance?

25 MR. GARVER: Do you mean performance

0479

KADLEC

1 with respect to phosphorus removal?

2 MR. BURGESS: Yes.

3 A. I'm sorry. Please repeat the question.

4 Q. Referring back to your testimony a short

5 while ago with respect to the Kadlec-Newman paper, I'm

6 asking you what your opinion is with respect to the

7 correlation or say with respect to the relationship

8 between depth and performance of a wetland.

9 MR. GARVER: With respect to phosphorus

10 removal?

11 MR. BURGESS: Yes.

12 A. In what connection are you referencing the

13 Kadlec-Newman document?

14 Q. Just your former testimony or your earlier

15 testimony today in response to some of my questions.

16 You cited to that report with respect to support for an

17 opinion concerning the relationship between depth and

18 performance.

19 A. No, the conclusion in that report I believe

20 is that there was no support for a hypothesis that a

21 volume specific uptake rate was to be preferred to an

22 area specific uptake rate. The issue of a depth

23 dependence of performance is in several ways separate

24 from that. I do believe that there is an effect of

25 depth on phosphorus removal in more than one way, as I

0480

KADLEC

1 have indicated.

2 Q. Is there an optimum depth in your opinion for

3 water in a wetland for optimum P removal?

4 MR. GARVER: I object to form.

5 A. There may be.

6 Q. Do you have an opinion with respect to

7 whether there is for WCA2A?

8 A. There may be.

9 Q. Your opinion is that there may be?

10 A. An optimum depth for P removal in WCA2A.

11 Q. And what in your opinion is that optimum

12 depth?

13 A. I don't know.

14 Q. Do you have an opinion as to what an optimum

15 depth might be for P removal in the W -- I'm sorry --

16 in the STAs?

17 A. I think there's a range of possibilities.

18 Q. And what are those ranges?

19 A. I think that range would be from a fairly

20 shallow depth, something perhaps approximating a foot

21 or thereabouts, on up to an upper range where the

22 system would become aquatic, which might be on the

23 order of perhaps four feet.

24 Q. And in your opinion, should that -- should

25 that -- strike that.

0481

KADLEC

1 How, if at all, does your model account

2 for the effects of depth that you have testified to?

3 MR. GARVER: I object to the form.

4 A. I would ask you to define what you mean by

5 "your model".

6 Q. Plug flow model for 2A.

7 A. Depth dependence in the model represented in

8 part by the equations 10 and 11 in Exhibit 6, which I

9 believe is what you're referring to, the depth effects

10 are imbedded in the rate constant, the uptake constant,

11 settling rate constant, KE.

12 Q. How does that settling rate constant account

13 for depth?

14 A. That was not my answer. My answer was that

15 depth effects are contained within KE, and that KE is

16 expected to depend in some way upon depth.

17 Q. Does the depth of water in the STAs change

18 the size of STAs to treat the water to the target

19 levels of the SWIM plan?

20 MR. GARVER: I object to the form.

21 MR. BURGESS: I withdraw the question.

22 Q. Dr. Kadlec, how do variations in depth of up

23 to on the order of four feet -- which I think you have

24 testified to -- affect the phosphorus removal

25 performance of a wetland?

0482

KADLEC

1 MR. GARVER: I don't believe Dr. Kadlec

2 testified to variations up to four feet.

3 MR. BURGESS: I think he said depths of

4 up to four feet.

5 A. I believe that I said that depths could be

6 imagined for phosphorus uptake in wetlands. They could

7 operate at depths between a foot and four feet.

8 Q. Well, I guess my question is, how do

9 variations in depth on the order of up to four feet,

10 the fluctuation in the depth of the water, how does

11 that affect the phosphorus removal performance of a

12 wetland?

13 A. Wetlands which undergo depth fluctuations in

14 that range would be expected to have some particular

15 performance, and I would anticipate that if a different

16 depth fluctuation were imposed on the same wetland,

17 that there would be a difference in phosphorus

18 removal. I could not quantify it at this point.

19 Q. For answering my question did you assume that

20 we had a constant depth of water and then fluctuation

21 of four feet for a period of time?

22 A. Well, I believe we are talking within a

23 general context of Conservation Area 2A and similar

24 systems --

25 Q. Right.

0483

KADLEC

1 A. -- which do undergo fluctuations in water

2 depths about a mean over some time period in question,

3 yes.

4 Q. Okay.

5 A. So my answer was relative to what WCA2A, for

6 instance, was doing at a depth of four feet, as

7 distinguished from what it was doing at a depth of one

8 feet -- one foot. I would have to analyze information,

9 if sufficient information were available, to make such

10 a determination.

11 Q. If I recall your testimony earlier, you had

12 no opinion as to what the optimum depth of WCA2A would

13 be for phosphorus removal; is that correct?

14 A. Yes.

15 Q. And what do you base your opinion on with

16 respect to design of STAs with a range of depth of one

17 to two feet?

18 MR. GARVER: I'm not sure that's what

19 Dr. Kadlec stated.

20 A. I don't believe I did make such a statement.

21 Q. What is the basis for your opinion as to the

22 optimum design parameter of depth in the STAs, in view

23 of the fact that you have testified you don't know what

24 the optimum depth is in 2A for a phosphorus removal?

25 A. In the absence of information on the depth

0484

KADLEC

1 dependence, it's my opinion that a utilization of the

2 same depth variability into A should be utilized in the

3 design of the STAs.

4 Q. And is it your understanding that that depth

5 variability has been incorporated into the conceptual

6 design of the STAs by Burns & McDonnell?

7 A. With one exception, yes.

8 Q. What is that exception?

9 A. With the exception that the dry end of the

10 water depth range has been removed; in other words, the

11 STAs should not be allowed to dry out.

12 Q. Do you agree with that design parameter?

13 A. Yes.

14 Q. Why?

15 A. By the design parameter, I think your

16 referent is the no dryout period; is that correct?

17 Q. Yes, sir.

18 A. I agree with that, because I believe that

19 dryout has the effect of removing a period of time of

20 possible phosphorus removal for the wetland, as well as

21 perhaps bringing into play sediment oxidation

22 processes.

23 Q. And why should that period of time be

24 removed?

25 A. So that the STA would be operational as large

0485

KADLEC

1 a fraction of the time as possible.

2 Q. In your opinion, is phosphorus not being --

3 strike that.

4 With respect to the Everglades, do you

5 have an opinion as to when plants grow best, growing

6 season?

7 MR. GARVER: I object to the form.

8 A. Well, do you mean during what period of the

9 year?

10 Q. Yes, sir.

11 A. It is my general impression that growth

12 proceeds throughout the year, but to differing degrees.

13 Q. Do plants in the Everglades grow best when

14 the soil is moist or when there is standing water on

15 the soil?

16 A. I would presume that that would depend on

17 which plant species you're referring to.

18 Q. Okay. Let me refer you to Exhibit 10.

19 A. I have Exhibit 10 in front of me.

20 Q. Thank you. In Paragraph 2 --

21 A. Excuse me. What page?

22 Q. I'm sorry. In the executive summary.

23 A. Paragraph -- Item 2.

24 Q. Yes.

25 A. Okay.

0486

KADLEC

1 Q. The second sentence begins: The degree of

2 confidence in the 8 meter a year value involves three

3 major concerns; the validity of the 8 meter a year in

4 describing phosphorus removal determined from the

5 transects studied in 2A, the transferability of the 8

6 meter a year value from the WCA2A to the proposed STA

7 sites, and support for the 8 meter a year value from

8 independent data sources.

9 Dr. Kadlec, substituting for 8 meter a

10 year the term "close to 10 meters a year", would you

11 agree that the degree of confidence in 10 meters a year

12 would involve those three factors?

13 A. Yes.

14 Q. Any other factors that bear upon the degree

15 of confidence in that settling rate constant?

16 A. I'm sure there may be, but I can't at this

17 point in time speculate on all of them.

18 Q. Okay. Paragraph B down further on the page,

19 again, substituting 10 for 8, The transferability of 10

20 meters a year to the STAs is based on similitude

21 between the conditions in the STAs and the WCA2A site.

22 Would you agree with that statement?

23 A. Not entirely.

24 Q. What, in your opinion, is the transferability

25 of a settling rate constant derived from WCA2A data

0487

KADLEC

1 dependent upon?

2 A. Well, there needs to be a definition of the

3 word "transferability" before this question can be

4 properly addressed.

5 Q. Are you utilizing -- for purposes of your

6 calculations arriving at the 10 meter a year K value,

7 are you using data from 2A?

8 A. Yes.

9 Q. And are you attempting to transfer that K

10 value, arrived at from using that 2A data, to an

11 estimation of the size for stormwater treatment areas

12 to be constructed on lands that are not located within

13 WCA2A?

14 A. Yes.

15 Q. That is the context in which I mean

16 "transfer". Does that help?

17 A. Well, I would ask one further question as to

18 whether or not you mean transferability in the sense of

19 the basis of design of the STAs.

20 Q. It is for the determination of acreage. Is

21 that what you're asking?

22 A. The reason that I'm asking you for

23 clarification is the basis of design is the long-term

24 sustainable removal of phosphorus as opposed to the

25 start-up period of such a system, and I draw a

0488

KADLEC

1 distinction between the two in the context of the word

2 "transferability".

3 Q. Will the systems operate differently over the

4 long-term than during the short-term start-up period?

5 MR. GARVER: Asks for speculation.

6 Objection.

7 Q. Do you have an opinion?

8 A. What do you mean by "the systems"?

9 Q. In the context that you used the word, the

10 STAs.

11 A. It's my opinion that the long-term

12 sustainable phosphorus removal potential of WCA2A is

13 transferable under appropriate conditions,

14 knowledgeable conditions of hydrology and other design

15 parameters to the STAs.

16 Q. I guess what are those -- what are those

17 factors that you just mentioned, hydrology among

18 others, that are transferable to the STAs?

19 A. They are the other design factors such as the

20 nature of vegetation, depth, hydraulic loading that we

21 have alluded to in previous lines of questioning.

22 Q. Do factors such as vegetation, depth and

23 hydraulic loading, in your opinion need to be similar

24 between the STAs and the WCA2A?

25 A. To some degree, yes.

0489

KADLEC

1 Q. To what degree does the vegetation need to be

2 similar?

3 A. In general terms, I would expect it would

4 need to be soft tissue emergent macrophytes.

5 Q. To what degree does the depth need to be

6 similar?

7 A. It would need to approximate the hydroperiod,

8 with the exception of the nondryout period, that exists

9 in Water Conservation Area 2A.

10 Q. And is it your understanding that that

11 hydroperiod in 2A goes from zero to four feet?

12 A. I believe those are the -- below zero in some

13 instances to approximately four feet is the best of my

14 recollection, yes.

15 Q. When you say that the dryout periods are not

16 to be considered, at what level is the water in 2A --

17 when is 2A dry?

18 A. When there's no standing water.

19 Q. So the period of time from 2A that you would

20 remove as a transferable design parameter would be when

21 the water is below the surface or when there is no

22 standing water on the surface?

23 A. I did not mean to imply at any time that the

24 dryout period was a transferable design parameter.

25 Quite the contrary. It's a perceived improvement to

0490

KADLEC

1 not use such a dryout period.

2 Q. Do you have any opinions as to whether the

3 vegetation in the STAs will in a general sense remove

4 phosphorus from the water column better than vegetation

5 in WCA2A?

6 A. I would expect the function of a given

7 macrophyte in the STA to be closely approximated to

8 that performance in WCA2A.

9 Q. So it would be your opinion that macrophytes

10 grow better under conditions of continual standing

11 water than conditions where they have been allowed

12 to -- strike that.

13 It would be your opinion that

14 macrophytes grow better under conditions of continual

15 standing water than under conditions experienced in

16 WCA2A?

17 A. I don't believe I made such a statement.

18 Q. Do you have an opinion as to whether

19 macrophytes would grow better under continual standing

20 water than under conditions where the soil is allowed

21 to dry out from time to time?

22 A. I think that would depend on which macrophyte

23 you are referring to.

24 Q. Does it make any difference to you,

25 Dr. Kadlec, with respect to answering these questions

0491

KADLEC

1 concerning transferability, and specifically with

2 vegetation, that WCA2A has been -- that the macrophytes

3 in WCA2A have been subjected to periods of drought and

4 drying, or certainly periods of no standing water, and

5 that the macrophytes in the STAs are going to be

6 subjected to continual flooding?

7 MR. GARVER: Objection to the form.

8 A. I don't know what you mean by make any

9 difference to me. I take your question to mean do I

10 believe this has an influence on design.

11 Q. Yes.

12 A. And in that case, my answer is I do not think

13 it has a significant influence on design.

14 Q. Have you attempted to quantify the influence

15 at all?

16 A. Indirectly.

17 Q. And how have you done that?

18 A. By comparison of information on the

19 phosphorus removal potential as measured by a settling

20 rate constant in Florida systems which do not undergo

21 the dryout and other phenomena that you alluded to, and

22 comparing them to the same number for Water

23 Conservation Area 2A.

24 Q. Do any of the systems that you testified you

25 might rely on at the hearing, do any of the systems

0492

KADLEC

1 from Florida, are they subjected to periods of drying

2 out?

3 A. Water Conservation Area 2A.

4 Q. Other than that.

5 A. Of those that I have said I would rely upon,

6 I don't believe so.

7 Q. On a per unit area basis, do you feel that

8 the macrophytes in the STAs will uptake phosphorus

9 better than the macrophytes in WCA2A?

10 A. I would ask you what you mean by "uptake" in

11 this context of this question.

12 Q. Remove phosphorus from the soil-poor water or

13 from the water column.

14 A. Is the premise of the question is there the

15 same vegetation density, biomass and species?

16 Q. Yes.

17 A. And it is the amount of -- you're referring

18 to the amount of phosphorus taken up by the plant or

19 the overall settling rate concept that we have been

20 talking about?

21 Q. Talking about the amount of phosphorus taken

22 up by the plant.

23 A. It would be my opinion that there might be

24 minor differences due to the minor differences in

25 hydroperiod of the growth of a macrophyte, and

0493

KADLEC

1 consequently minor differences in the macrophyte

2 portion of phosphorus uptake.

3 Q. Dr. Kadlec, in your opinion the fact that the

4 STAs are not going to be subject to drought, is that,

5 in your opinion, an enhancement over the conditions

6 which obtain in WCA2A from a macrophyte standpoint?

7 MR. GARVER: I'll object to the form.

8 A. I don't know.

9 Q. Do you have any concerns or questions about

10 whether WCA -- I'm sorry -- whether the macrophytes in

11 the STAs will remove phosphorus from the water

12 column -- strike that.

13 Do you know what the water depth or

14 range of water depths are for Boney Marsh and for Iron

15 Bridge?

16 A. I have information on water depths for Boney

17 Marsh, and I have also rough information on water

18 depths for Iron Bridge.

19 Q. How do they compare to the water depths

20 proposed for the STAs?

21 A. They are within the range proposed.

22 Q. What is your -- could I ask you to turn to

23 Exhibit 8.

24 A. What page, please?

25 Q. 9-4. Let's see if that refreshes your

0494

KADLEC

1 recollection at all with respect to water depth.

2 A. It does not.

3 Q. Okay. When you say that the water depths at

4 Iron Bridge and Boney Marsh are within the range of

5 that proposed by the STAs, what do you mean?

6 A. Well, it's my understanding from the

7 conceptual design document that the range in depths for

8 the STAs is going to approximate that for WCA2A, with

9 the exception of the dry period, so the range in depths

10 would be from zero to four feet, and Boney Marsh and

11 Iron Bridge are generally, in general terms, within

12 that range.

13 Q. Do they also fluctuate from between zero and

14 four feet?

15 A. There are fluctuations. The hydroperiod

16 curves are different.

17 Q. Is there a mean average depth for Boney Marsh

18 and Iron Bridge?

19 A. A mean depth for Boney Marsh could be

20 computed from the data available in the period of

21 record for that system, yes. I don't know that number

22 as I sit here today.

23 Q. How about for Iron Bridge; do you know what

24 the average depth is in Iron Bridge?

25 A. I do not.

0495

KADLEC

1 Q. Do you have an opinion as to whether or not

2 typha takes up phosphorus when there is no standing

3 water?

4 A. I would ask you what you mean by "takes up".

5 Is it in the nature of storage of phosphorus in the

6 plant tissues, or do you mean the long-term average

7 settling process that we have discussed in most other

8 contexts?

9 Q. Does it remove phosphorus from the soil-poor

10 water?

11 MR. GARVER: I'll object to the form.

12 A. It may.

13 Q. What is your "may" dependent upon?

14 A. Well, in the climate in which we sit and the

15 period of time of year in which we are sitting here, I

16 don't believe the typha is, as of yet, removing

17 phosphorus from poor water.

18 Q. How about in the Everglades?

19 A. I would imagine in the Everglades, in the

20 same time period, that growth of typha requires

21 phosphorus from the poor water, yes.

22 Q. Do you have an opinions as to the depth at

23 which the typha can take P from the poor water?

24 MR. GARVER: I object to the form.

25 A. Well, in general terms a plant can take

0496

KADLEC

1 phosphorus from its rhizosphere.

2 Q. So whatever the depth of the root of the

3 typha is the depth at which it can remove P from the

4 poor water?

5 A. That would be the range of possibility, yes.

6 Q. Do you have any opinions as to what, on

7 average, the depth of the root system is for typha in

8 the Everglades?

9 A. I have no direct data on typha in the

10 Everglades as I sit here today.

11 Q. Okay. Back to Exhibit 10, please. Over onto

12 the next page. Yeah. The paragraph beginning, "A

13 major issue of concern is the expected water

14 chemistry. The required implementation of the BMP

15 activities in the EAA may significantly change the

16 relative amounts of dissolved and particulate

17 phosphorus reaching the STAs".

18 Do you agree with that statement?

19 A. Not entirely.

20 Q. Do you agree that the BMPs may change the

21 relative amounts of dissolved and particulate

22 phosphorus?

23 A. Yes.

24 Q. The next sentence reads, "It is possible that

25 the particulate fraction of phosphorus reaching the

0497

KADLEC

1 STAs will be less than that experienced in WCA2A".

2 Do you agree with that statement?

3 A. Yes.

4 Q. The next sentence reads, "As a result, the

5 treatment performance of the STAs may not be the same

6 as the performance observed in 2A".

7 Do you agree with that statement?

8 A. No.

9 Q. What's the basis for your disagreement?

10 A. My basis for disagreement is that other

11 Florida systems which receive particulate fractions

12 less than Water Conservation Area 2A do not display a

13 lowered value of the settling rate.

14 Q. What systems are those?

15 A. Iron Bridge.

16 Q. Any others?

17 A. There are other systems outside Florida.

18 Q. Do you anticipate that at the hearing you

19 will render an opinion that the performance of the STAs

20 will not depend upon the amounts of dissolved and

21 particulate phosphorus which may be reaching them?

22 A. I would not expect to make that precise

23 statement, no.

24 Q. Okay. Of the other systems that you

25 mentioned are outside of Florida and that receive

0498

KADLEC

1 particulate phosphorus less than that experienced in

2 2A, were any of those systems systems which you

3 mentioned you may rely upon for the purpose of

4 expressing opinion at the area hearing?

5 A. Yes.

6 Q. Which one?

7 A. Well, I can't, as I sit here, quickly

8 identify all such systems. Would you like me to go

9 through the list? I can in general terms tell you that

10 those systems that receive a fairly highly treated

11 municipal waste water typically contain a small

12 particulate fraction, and those systems, both in and

13 out of Florida, fall in the category of those that

14 offer information on low particulate incoming waters.

15 Q. Would you expect to testify at the time of

16 the hearing that the removal rate for the STAs will not

17 depend upon the form of phosphorus between dissolved

18 and particulate phosphorus that they are going to

19 receive?

20 A. No.

21 Q. What would you anticipate your testimony to

22 be on this subject at the hearing?

23 A. I would anticipate that my testimony would be

24 of the nature that anticipated changes in the fraction

25 of particulate material coming from the EAA as a result

0499

KADLEC

1 of BMPs would not be greatly different from that which

2 exists at the present time in terms of the character of

3 the particulate material, and perhaps not greatly

4 different in the fraction of particulate material, and

5 that other information from sites which have less

6 particulate do not reflect a substantial reduction, in

7 fact, reflect no reduction in the settling rate to be

8 expected.

9 MR. GARVER: Mr. Burgess, if you are

10 about to get started, could we take a very short

11 break?

12 MR. BURGESS: Very short.

13 (Recess taken: 11:30 - 11:35)

14 (Mr. Marin exits.)

15 (Deposition Exhibit No. 11

16 marked for identification.)

17 Q. Dr. Kadlec, let me show you what's been

18 marked as Exhibit 11 and ask you if you can identify

19 that.

20 A. This appears to be the hard copy of materials

21 that I used in a conference at LSU a few weeks ago.

22 Q. Can you turn to Page 1112243.

23 A. (Witness complied.)

24 Q. What does that table show?

25 A. This table was not used in the presentation.

0500

KADLEC

1 It was an initial effort to attempt to separate forms

2 of phosphorus at Boney Marsh, and I did not include it

3 in the presentation because I realized that this

4 particular breakdown should not have been carried

5 through to a settling rate constant, that that is

6 inappropriate in terms of mass balances, but it is an

7 attempt, an erroneous one in my view, to attempt to

8 partition the forms of the phosphorus in terms of the

9 settling rate.

10 Q. The figures on the right under rate constant

11 meters per year, is that equivalent to a settling rate?

12 A. That is computed in the same way as a

13 settling rate for the fraction of phosphorus indicated,

14 yes.

15 Q. Those are fractions of phosphorus that were

16 in the water column in Boney Marsh in 1986; is that

17 correct?

18 A. 1986 Boney Marsh data, yes.

19 Q. And those rate constants are not all the

20 same, are they?

21 A. Those rate constants should not have been

22 calculated.

23 Q. Why not?

24 A. Because the settling rate process by mass

25 balance can only be applied to an element or

0501

KADLEC

1 constituent like total phosphorus, not to individual

2 species which may interconvert in the wetland. Having

3 realized that, I did not use this table in the

4 presentation.

5 Q. When did you realize that, compared to when

6 you prepared the table?

7 A. Within hours.

8 Q. What did you intend to show through

9 preparation of this table?

10 A. It was an attempt to see if I could extract

11 some information on the relative rates at which the

12 forms of phosphorus interacted with the ecosystem.

13 Q. And why is it an incorrect or invalid result

14 in your mind?

15 MR. GARVER: Objection; asked and

16 answered.

17 A. Because the various forms of phosphorus

18 undergo processes not described by the settling rate

19 model, interconversions.

20 Q. How fast do those interconnections occur?

21 MR. GARVER: Interconversions.

22 Q. Interconversion?

23 A. It depends on which one or which process you

24 might mean.

25 Q. If the ratios -- no, strike that.

0502

KADLEC

1 If the form of phosphorus were to

2 change, and by that I mean particulate phosphorus were

3 to interconnect or interconvert to dissolved organic

4 phosphorus, would the rate constant associated with

5 dissolved organic phosphorus change?

6 A. I'm sorry. Repeat that. What is

7 interconverting to what, please?

8 Q. Well, I think you said the reason that this

9 exercise was not valid is you somehow discovered,

10 realized, or thought about it further and realized that

11 forms of phosphorus -- what was your term?

12 Interconvert?

13 A. Yes.

14 Q. Interconvert, such that the settling rate

15 concept wasn't valid.

16 A. Correct. Wasn't valid for individual

17 species.

18 Q. It is in your mind only valid for total P, or

19 for what? What, in your mind, is it valid for?

20 A. In my mind it should be applied to total P.

21 Q. Only?

22 A. Yes.

23 Q. Okay. Do you have an opinion as to whether

24 or not dissolved organic P would stay in the water

25 column for a longer period of time relative to ortho P?

0503

KADLEC

1 MR. GARVER: I object to the form.

2 A. I would have to ask, what water column are

3 you referring to?

4 Q. I meant it in the abstract, but I'll confine

5 it to the Everglades.

6 A. So we're referring to a water column in an

7 Everglades wetland?

8 Q. Yes.

9 A. In general terms, I believe ortho phosphorus

10 is a more reactive species than dissolved organic

11 phosphorus.

12 Q. And does that mean that in your opinion

13 dissolved organic phosphorus would remain in the water

14 column for a longer period of time relative to ortho

15 phosphorus?

16 A. That does not in my mind necessarily follow,

17 because of a wide variety of other factors which would

18 need to be known.

19 Q. Would you agree with me that the chart on

20 Page No. 111243 indicates that dissolved organic

21 phosphorus has a lower or is the lowest settling rate

22 amongst the four varieties of phosphorus listed on the

23 page?

24 A. I would agree that the incorrectly presented

25 number or incorrectly computed conceptually wrong

0504

KADLEC

1 number listed for dissolved organic phosphorus of 5.2

2 is a lower number than the same incorrectly contrived

3 number for ortho phosphorus, yes.

4 Q. How would you correctly derive the relative

5 settling rates for the various fractions of phosphorus?

6 A. I don't believe it can be done, because the

7 settling rate concept is a combination of all processes

8 operating at a locality in a wetland ecosystem that

9 does not distinguish between forms of phosphorus.

10 Q. How would one then go about determining the

11 ability of a wetland to remove one form of phosphorus

12 better than another form of phosphorus?

13 A. The ideal experiment, to answer that

14 question, would be to subject a same wetland, under

15 identical conditions of climate, hydrology and all

16 other factors, to first a flow involving particulate

17 phosphorus, and then the second part of the experiment,

18 identical conditions to another form of phosphorus to

19 assess the differences.

20 Q. Some sort of a dosing study; would that be

21 appropriate?

22 A. Not necessarily.

23 Q. Other than subjecting the wetland to two

24 different forms for a period of time, is there any

25 other way that you are aware of you can distinguish

0505

KADLEC

1 between the relative removal abilities?

2 A. One can also compare wetlands in the same

3 region receiving different types of water with

4 comparable wetlands in the same region, and evaluate

5 potential differences from their performance data.

6 Q. Okay. Is that what you intend to do at the

7 hearing?

8 A. Yes.

9 Q. Dr. Kadlec, the rate constants on the page

10 we're discussing, those were not in fact incorrectly

11 calculated, were they?

12 A. They are based on an incorrect concept.

13 Q. Okay.

14 A. They ignore interconversion rates.

15 Q. The calculations though to arrive at those

16 numbers were not invalid, were they, or incorrect?

17 A. Not to my knowledge. They were not numerical

18 errors, to my knowledge.

19 Q. Okay. Thank you.

20 Do you have any opinions as to whether

21 or not dissolved organic P moves further down the

22 gradient in WCA2A than any other fraction of

23 phosphorus?

24 MR. GARVER: I object to the form.

25 A. Well, not at this time.

0506

KADLEC

1 Q. Do you anticipate that you will be

2 investigating that before the time of the hearing?

3 A. I have no such anticipation.

4 Q. Dr. Kadlec, is it your testimony that the

5 model which you used to derive the settling rate

6 constant will not discriminate among these various

7 phosphorus forms?

8 A. Not directly.

9 Q. Okay. Is it a mechanistic model?

10 A. I don't know that I understand what you mean

11 by "mechanistic".

12 Q. Would you consider it, in your definition of

13 the term "mechanistic", to be a mechanistic model?

14 A. Okay. In order that I can be clear, what is

15 the equation representation model to which you refer?

16 Q. I'll withdraw the question.

17 Dr. Kadlec, how does your model not

18 directly discriminate among the P forms?

19 MR. GARVER: Objection to form.

20 A. I need to know what you mean by "your model".

21 Q. The model you used to derive the K to which

22 you just said it does not directly discriminate among

23 the P forms.

24 A. Well, I believe in the context in which we're

25 currently talking, you may be referring to models

0507

KADLEC

1 represented by equations in Exhibit 6.

2 Q. Yes, sir.

3 A. There is no differentiation between the forms

4 of P, because those equations and those models refer to

5 total phosphorus in the water column, as well as total

6 phosphorus removed by sedimentation processes, settling

7 processes, uptake.

8 Q. Back to Exhibit 10, if we could.

9 Dr. Kadlec, with respect to the systems

10 that you have said you might rely upon, and

11 specifically Boney Marsh, Iron Bridge, Jackson Bottoms,

12 WCA2A, have those in your opinion reached steady state

13 with respect to macrophytes?

14 A. Well, we had encountered those words earlier,

15 and I would like to be sure I understand what you mean

16 by "steady state".

17 Q. Your definition of steady state is in the

18 record, so you may answer it using your definition of

19 steady state. You mean steady state, not stationary

20 state; is that right?

21 MR. BURGESS: His definitions of both

22 are on the record, and if you would like to repeat your

23 definition, you may do so.

24 A. I think I recall what those were. Steady

25 state and stationary state must however -- I think your

0508

KADLEC

1 question refers to vegetation?

2 Q. Yes, sir.

3 A. All right. One of the systems was Boney

4 Marsh.

5 Q. Yes. Iron Bridge? If you want, we will take

6 them individually. That would be fine.

7 A. Yes, please.

8 Q. Okay.

9 A. I mean I don't remember them all.

10 Boney Marsh, it is my impression that

11 the vegetation -- first of all, let me make one

12 comment, and that is that the Boney Marsh system was

13 studied for a period up through 1986, so reference to

14 the present condition is perhaps not what you meant.

15 Q. Okay. Your anticipated testimony at trial,

16 will that discuss conditions at the Boney Marsh up

17 until 1986?

18 A. Yes.

19 Q. Then my question is with respect to

20 conditions in 1986.

21 A. So in 1986 was the vegetation at a steady or

22 stationary state? And my answer would be that the

23 major portions of it were, or close to or at what I

24 would call a stationary state.

25 Q. What portions were not?

0509

KADLEC

1 A. There's a possibility -- and I have not fully

2 reviewed all of the information at this time -- that

3 the very downstream-most end was still undergoing some

4 changes.

5 Q. The edge of the affected area?

6 A. I don't know that I associate a term like

7 "affected area" with the Boney Marsh project.

8 Q. What macrophytes were at the downstream edge

9 of that project?

10 A. I would have to refer to data to answer that

11 question.

12 Q. I think you just indicated that major

13 portions of it were not at stationary state, and my

14 question was whether they were not -- whether they were

15 at steady state, utilizing your definition.

16 Do you believe -- I'm sorry. Go ahead.

17 A. Well, I think I just said the opposite, so

18 let me try and say it again.

19 I think that the largest portions of

20 Boney Marsh with respect to vegetation may have been

21 close to steady state or stationary state, in the way

22 that I would prefer to use the terminology.

23 Q. We need to define, I think, stationary state

24 and steady state with respect to macrophytes again on

25 the record, because my understanding was that you had

0510

KADLEC

1 not previously defined them to be similar. By that I

2 mean you were not using the term interchangeably.

3 A. I would prefer not to.

4 Q. Okay.

5 A. It's my preference to refer to a steady state

6 situation as one that has no time variability

7 whatsoever on any time scale.

8 Q. Can macrophytes or vegetation in your mind in

9 a wetland ever be at steady state?

10 A. No.

11 Q. And how do you define "stationary state"?

12 A. Stationary state is one in which the

13 vegetation, although undergoing changes, returns within

14 a specified period of time to a condition similar to

15 that at the beginning of that period of time. So it

16 may be undergoing short-term variability as well as

17 cyclic seasonal processes, but on average looks the

18 same in one year compared to the previous year, the

19 distinction being the allowance of repetitive and some

20 degree of variability.

21 Q. Given the caveat that you have said in your

22 opinion that vegetation can never be at steady state, I

23 understand your testimony with respect to Boney Marsh.

24 In your opinion, has the vegetation at

25 Iron Bridge reached stationary state?

0511

KADLEC

1 A. Some of it has. In answer, Iron Bridge is a

2 difficult system. In some cells, vegetation management

3 has been attempted, and that makes a generic or general

4 answer to your question difficult.

5 Q. Can we answer it for those cells where

6 vegetation management hasn't been attempted and those

7 cells where it has?

8 A. Well, information is not available from all

9 cells. The cells where information is available, it is

10 my impression that a close approximation of the

11 stationary state has been achieved.

12 Q. I'm sorry. In those cells where they are

13 managed?

14 A. In those cells where data is available.

15 Q. I'm sorry. Thank you.

16 A. I believe. But I would have to refer to

17 actual data to see which cells are managed, which

18 aren't, and where the data on vegetation has been

19 made -- has been taken.

20 Q. Okay. Do you anticipate at the time of trial

21 that you will be giving opinions as to whether or not

22 the vegetation in the various sites that you said you

23 might consider in your opinions has or has not reached

24 stationary state?

25 A. I would expect so, yes.

0512

KADLEC

1 Q. Do you have an opinion with respect to the

2 vegetation at Jackson Bottoms, whether or not it has

3 reached stationary state?

4 A. I have not reviewed the most recent data from

5 that system. My general impression from site visits is

6 that it may have reached a stationary state with

7 respect to biomass, but perhaps not with respect to

8 species composition.

9 Q. Does the first order model that you and

10 Dr. Walker have used to estimate the P settling rate

11 require a steady state condition in order to be valid?

12 A. The calculation procedures can be applied

13 under either condition, and I attempt to draw a

14 distinction between a stationary state description

15 resulting in a settling rate coefficient, whereas a

16 nonstationary state results in a calculation of what I

17 term an uptake coefficient.

18 Q. And what is or are the differences between

19 the two?

20 A. When an ecosystem is undergoing

21 unidirectional change, the total removal of phosphorus,

22 from the water passing through it, is being utilized in

23 transient storage compartments as well as in the

24 long-term removal mechanisms.

25 Q. If in fact, as you previously testified,

0513

KADLEC

1 vegetation in wetlands can never be at a steady state,

2 is it your opinion that an uptake of coefficient as

3 opposed to a settling rate is the factor to be applied

4 as design criteria?

5 A. In the context of STA design, a long-term

6 average settling rate has been utilized and I believe

7 should continue to be utilized.

8 Q. And how does a long-term average settling

9 rate differ from an uptake coefficient?

10 A. Again, the uptake coefficient refers to those

11 systems who are in a state of ecosystem change, and the

12 design is not -- and in my opinion should not -- be

13 focused on that period of change. It should be focused

14 on the long-term average performance.

15 Q. Have you attempted to calculate an uptake

16 coefficient for the STAs?

17 A. The STAs are not in existence and cannot

18 generate uptake or settling rate coefficient.

19 Q. Have you -- I'm sorry. For WCA2A, have you

20 calculated an uptake coefficient as opposed to a

21 long-term average settling rate?

22 A. Those two terms, when the calculation is made

23 for a period in which a stationary state occurs, there

24 is no difference. The calculation for the long-term

25 situation, which I believe pertains in the zone of 2A

0514

KADLEC

1 that we're discussing, which is the area that has

2 concentrations related to the STA design --

3 Q. How large is that zone?

4 MR. GARVER: Were you done with your

5 answer?

6 MR. BURGESS: Oh, I'm sorry.

7 A. I believe I was close to done with my answer.

8 Q. Okay.

9 A. I'm sorry. How large is what zone in 2A?

10 Q. Right, the zone that you are saying that

11 we're concerned with for calculation of the long-term

12 average settling rate.

13 A. I can't tell you an exact size as I sit here,

14 but it would be that zone which includes concentrations

15 that exceed the 50 parts per billion, which is the

16 target for the STAs.

17 MR. BURGESS: Mark this.

18 (Deposition Exhibit No. 12 marked for

19 identification.)

20 Q. How do you determine what that zone is? By

21 that I mean that zone that contains more than 50 parts

22 per billion.

23 A. Well, there is information on the phosphorus

24 concentrations on gradients from north to south within

25 Water Conservation Area 2A.

0515

KADLEC

1 Q. Is that South Florida Water Management

2 District data?

3 A. Yes.

4 Q. Any other data?

5 A. There are also data sets on various

6 parameters on those same gradients by Dr. Reddy's group

7 and by Duke University group.

8 Q. Do you have any opinion as to whether or not

9 that zone corresponds to the zone where cattails are

10 seen in WCA2A?

11 MR. GARVER: I object to the form.

12 A. I can say that there are cattails in that

13 zone.

14 Q. Do you have any intention to testify at the

15 time of trial concerning the relationship between that

16 50 parts per billion and the abundance of cattail

17 within area where that 50 parts per billion is found?

18 A. No.

19 Q. Let me show you what's been marked as

20 Exhibit 12.

21 A. Yes.

22 MR. GARVER: Can I take a look?

23 Q. What is that document, Dr. Kadlec?

24 A. This is a FAX memo of some of my work to

25 Dr. Walker.

0516

KADLEC

1 Q. And what were you attempting to do in that

2 work?

3 A. I was attempting to establish a relationship

4 between -- not a relationship, excuse me. What I mean

5 to say is I was attempting to calculate the areas

6 between the L39 levee and various contours of poor

7 water and soil phosphorus in Area 2A.

8 Q. Can you utilize any of the calculations in

9 that exhibit to tell us, referring back to your

10 testimony a moment ago, with respect to what area

11 contains the 50 parts per billion?

12 A. No.

13 Q. Okay.

14 MR. GARVER: When you say the area

15 contains 50 parts per billion, you mean area bounded by

16 50 parts per billion?

17 MR. BURGESS: I'm sorry. I'll clear it

18 up.

19 Q. Dr. Kadlec, earlier this week you testified

20 that 500 milligrams per kilogram, in your opinion,

21 represent the background levels of soil phosphorus in

22 the Everglades; is that correct?

23 MR. McGRATH: I object to the

24 mischaracterization.

25 MR. BURGESS: The record will stand for

0517

KADLEC

1 itself. I'm just trying to refresh his recollection.

2 A. That is not correct.

3 Q. Okay. What did you say?

4 A. I said I was not prepared to offer an opinion

5 on that, excepting that I believe that 500 milligrams

6 per milligram might represent an upper limit.

7 Q. On background?

8 A. On what background might be perceived to be,

9 yes.

10 Q. Okay. Would you turn to Bates numbered Page

11 1110063.

12 A. Yes.

13 Q. What is this?

14 A. It's a printout of a spreadsheet of

15 information workup in this document.

16 Q. Did you create this spreadsheet?

17 A. I did.

18 Q. Okay. What amount of hectares or acreage --

19 or let's say hectares -- is depicted to be included in

20 the area above 500 milligrams per kilogram total

21 phosphorus in the soil?

22 A. Well, I must point out that the information

23 that's in this entire document is subject to the

24 reservations about accuracy which I have expressed

25 earlier in my testimony, which is that the contours

0518

KADLEC

1 from which this information is derived are those of

2 Dr. Reddy, and the placement of those contours is, in

3 my mind, in question, and I'm awaiting information from

4 the South Florida Water Management District in order to

5 improve this calculation.

6 So in that context, this work that we're

7 inspecting is very preliminary and in my opinion quite

8 probably needs to be altered and has not been reviewed

9 by myself for accuracy and is based on information that

10 may change.

11 In that context, referring to Page

12 1110063, I have made a calculation, I believe -- I'm

13 jumping right into this work, but it appears to

14 tabulate at 600 milligrams per kilogram and above for

15 total phosphorus in whatever horizon it pertains to,

16 which appears to be 0 to 10 centimeters, 133 -- excuse

17 me -- 13372 hectares. I'm sorry. I misspoke, because

18 there's a second area.

19 Q. Yeah.

20 A. I'm sorry. I erred. I was reading a column

21 called "station area" which refers to areas what I

22 believe are upstream of a station, and I should have

23 been on the left-hand side.

24 So upstream of 500 milligrams per

25 kilogram, the number in the table is 13554 hectares.

0519

KADLEC

1 Q. That would be at 500 or above --

2 A. Yes, sir.

3 Q. -- milligrams per kilogram?

4 Okay. Do you have an opinion as to

5 whether or not, subject to the caveats that you have

6 provided, that is the amount of or the number of

7 hectares that are impacted by nutrients above

8 background in Water Conservation Area 2A?

9 A. I would form no such conclusion based on one

10 parameter, and as I said, I don't necessarily believe

11 500 is the background level; it is simply an upper

12 limit on what it may be with respect to soil

13 phosphorus.

14 Q. Do you have any intentions between now and

15 the time of the hearing in this matter to determine

16 what the background of soil phosphorus is in the

17 Everglades?

18 MR. GARVER: I believe that's asked and

19 answered.

20 A. I have no such intention.

21 Q. Do you have any intention to testify at the

22 time of trial relative to what background soil

23 phosphorus concentrations are in the Everglades?

24 MR. GARVER: I believe that's asked and

25 answered also.

0520

KADLEC

1 A. I'm sorry. The exchange caused me to lose

2 concentration. Would you repeat the last question,

3 please?

4 Q. Yes, sir. Do you have any intention at the

5 time of trial on testifying what in your opinion would

6 be the background levels of soil phosphorus in the

7 Everglades?

8 A. No.

9 Q. Could, in your opinion, background soil

10 phosphorus levels be less than 500 milligrams per

11 kilogram?

12 A. I have so stated.

13 Q. Okay. And would that, based upon the

14 document you have in front of you, necessarily increase

15 the number of hectares --

16 MR. GARVER: I object to the form.

17 Q. -- upstream of that lower background number?

18 MR. GARVER: I object to the form. I'm

19 not sure what you refer to by "lower background

20 number".

21 MR. BURGESS: Than the 13554 hectares he

22 has testified to.

23 A. Well, the techniques represented in the rough

24 work document we are inspecting cannot be extended, in

25