00949 1 MANITOBA CLEAN ENVIRONMENT COMMISSION 2 3 4 5 6 7 RED RIVER FLOODWAY EXPANSION PROJECT 8 9 10 11 12 ======================================= 13 Monday, February 21, 2005 14 Oakbank United Church 15 Oakbank, Manitoba 16 ======================================== 17 18 Volume 5 19 20 21 22 23 24 25 00950 1 APPEARANCES: 2 Clean Environment Commission: 3 Mr. Terry Sargeant - Chairman Mr. Barrie Webster - Member 4 Mr. Wayne Motheral - Member Mr. Doug Abra - Counsel 5 Mr. Dave Farlinger - Technical consultant Ms. Cathy Johnson - Secretary to Commission 6 Ms. Joyce Mueller - Secretary 7 Manitoba Conservation: 8 Mr. Trent Hreno - Chair, Project Admin Team Mr. Bruce Webb - Chair, Tech Advisory 9 Committee Mr. Stewart Pierce - Counsel 10 11 Manitoba Floodway Authority: 12 Mr. Rick Handlon - Counsel Mr. Jim Thomson 13 Mr. Doug McNeil Mr. Doug Peterson 14 Mr. Cam Osler - Intergroup Consulting Mr. John Osler - Intergroup Consulting 15 Mr. David Morgan - TetrES Consulting Mr. George Rempel - TetrES Consulting 16 Mr. Robert Sinclair - KGS Ms. Marci Friedman-Hamm - KGS 17 18 Participants: 19 Mr. Bob Starr - Ritchot Concerned Citizens Mr. Bob Bodnaruk - RM of Springfield 20 Mr. Steve Strang - RM of St. Clements Mr. Orvel Currie - Counsel to Municipalities 21 Mr. Doug Chorney - Coalition for Flood Protection North 22 Mr. Kerry McLuhan - Coalition for Flood Protection North 23 Mr. Rob Loudfoot - 768 Association Mr. Y. Shumuk - 768 Association 24 Paul Clifton - Paul Clifton Mr. Jeff Frank - Rivers West 25 Gaile Whelan Enns - Manitoba Wildlands Earl Stevenson - Peguis Indian Band 00951 1 Participants: (continued) 2 3 Mr. Jake Buhler - Cooks Creek Conservation Mr. Lloyd Crooks - Cooks Creek Conservation 4 Mr. Jon Stefanson - Cooks Creek Conservation Mr. Daryl Chicoine - Counsel 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 00952 1 INDEX OF PROCEEDINGS 2 Presentation by James Bezan 1068 3 Cross-examination of Floodway Authority 4 5 Cross-examination by Mr. Currie 967 6 Cross-examination by Mr. Millman 1099 7 Cross-examination by Mr. Stinson 1125 8 Cross-examination by Mr. Arkley 1189 9 Cross-examination by Ms. Fuga 1200 10 Questions by Reeve Strang 1218 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 00953 1 INDEX OF EXHIBITS 2 3 48 Errata for EIS 963 4 49 Response by SCN Lavalin on Feb 21, 963 5 2005 6 50 Department of Agriculture and 967 7 Conservation, Water Control and Conservation Branch, Red River 8 Floodway, Inlet Controls works, Memorandum on Preliminary Design, 9 July 28, 1962 10 51 Red River Floodway Expansion 1081 11 Concerns Raised by the People of Selkirk-Interlake. Presentation to 12 the Clean Environment Commission. By: James Bezan, Member of 13 Parliament, Selkirk-Interlake 14 15 16 17 18 19 20 21 22 23 24 25 00954 1 INDEX OF UNDERTAKINGS 2 UNDERTAKING NO. PAGE 3 No undertakings given 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 00955 1 MONDAY FEBRUARY 21, 2005 2 UPON COMMENCING AT 9:00 A.M. 3 4 THE CHAIRMAN: Good morning, ladies 5 and gentlemen. Could we come to order, please. I 6 would just like to remind you, before we get 7 going, I would like to remind people who weren't 8 in attendance at all last week, that I'm a maniac 9 about two things; cell phones and conversation in 10 the audience while hearings are going on. So 11 please turn off your cell phones and please don't 12 engage in any side conversations when others are 13 trying to make their presentations or answer 14 questions. 15 I would like to welcome you all to the 16 second week of our hearing. I would like to 17 welcome a lot of people in the audience who are 18 here today for the first time, and I would like to 19 welcome back all of the participants who were here 20 last week and seem to be very keen to get back at 21 it. 22 On the agenda this morning, Mr. McNeil 23 informs me he has some undertakings to respond to 24 off the top. That will be followed by what I 25 believe is the final cross-examination from a 00956 1 participant group, and that's Mr. Currie on behalf 2 of the three municipalities. 3 Following Mr. Currie's 4 cross-examination we will allow members of the 5 general public who might have questions of the 6 Floodway Authority to do so at that time. Then we 7 begin with presentations. The first presentation 8 this morning, later this morning will be by the 9 Cook Creeks Conservation District. The local 10 member of parliament, Mr. James Bezan, has also 11 asked for an opportunity to make a brief 12 presentation which we will hear sometime this 13 morning, and then following that, whether it is 14 morning or afternoon, we will get into the 15 presentation on behalf of the three 16 municipalities. 17 So, first order of business, Mr. 18 McNeil. 19 MR. REMPEL: Mr. Chairman, I would 20 like to clarify, with your permission, we have 21 three housekeeping items we would like to take 22 care of. One is an errata on the EIS and some 23 groundwater statements that Dr. Morgan would like 24 to speak to. Then Mr. McNeil has a number of 25 clarifications from the record of last week, and 00957 1 then Mr. Smith would like to respond to an 2 undertaking that he gave with regard to inlet 3 structure bedrock quality. So with your 4 permission, we would like to do those three items 5 now. 6 MR. MORGAN: Yes. I think you had 7 received an errata sheet and memo. This is for 8 page 514 of the EIS. This section on existing, 9 the existing groundwater quality in the EIS states 10 that while data along the Red River at the 11 floodway inlet and at the Selkirk bridge on the 12 Red River may show influence of river water in 13 wells along the river. This description of 14 variation water quality is actually meant to refer 15 to the Red River water quality and not the water 16 quality data. 17 There is an errata in appendix M which 18 makes the correction, and an EIS sheet. 19 Just to be clear, that this discussion 20 on the existing situation along the Red River does 21 not change the effects assessment in any matter. 22 THE CHAIRMAN: Thank you. Mr. McNeil. 23 MR. MCNEIL: Thank you, Mr. Rempel. 24 Mr. Chairman, I have got, I believe four things to 25 bring to your attention this morning. First of 00958 1 all we were in error when we mentioned last week 2 about summer operation. It is not 22 times in 36 3 years, had we the ability to operate in the summer 4 in the past. Manitoba Water Branch had indicated 5 to me late Friday that that was incorrect. They 6 are working on the new numbers and we will get 7 back to you in the next couple of days on that. 8 Page 699 of the February 17 9 transcript, line 8, indicated that the inlet 10 structure was not designed to 778, in fact, that's 11 an error, it should have been quoted as the inlet 12 structure was designed to 778. 13 Also Manitoba Water Stewardship 14 advises that in spring operation, contrary to what 15 I indicated, they do in fact operate the gates, 16 both on the rising and receding limbs of the 17 hydrograph, in other words, when the gates are 18 being raised and when the gates are being lowered 19 during spring operation they mimic nature in terms 20 of the rate of rise and fall as much as possible. 21 I had indicated last week that they couldn't do 22 that on the rising limb. In fact they do. 23 You were asking us about our 24 environmental management system last week and we 25 are preparing some information that will report in 00959 1 the next couple of days on that item. 2 THE CHAIRMAN: Just on that item, Mr. 3 McNeil, subsequent to my asking those questions, I 4 did learn there is an ISO 1400 or 1401 that sets 5 out environmental management systems criteria. 6 MR. MCNEIL: That's true, and we will 7 make a presentation generally that follows that 8 process. 9 THE CHAIRMAN: Thank you. 10 MR. MCNEIL: And the last thing, and I 11 will ask Mr. Rick Carson to report on the 12 undertaking to discuss the application of the 13 Canadian Dam Association Guidelines with respect 14 to the floodway. Mr. Carson. 15 MR. CARSON: Yes. As you recall, the 16 question regarding the dam safety issue was what 17 portions of the Canadian Dam Association 18 Guidelines were used and what portions were not 19 used. And as we said on Thursday, the company 20 that did the dam safety review was SNC Lavalin, and 21 we thought that we would be able to bring them in 22 to speak to that question, so that it would be the 23 original authors of the appendix that would be 24 giving you the answer. But unfortunately, on 25 short notice they were not able to have a 00960 1 representative here. But we came to a compromise, 2 that they wrote a document here that I have in 3 front of me, and they asked that I read it out to 4 you. I have hard copies if you would like to see 5 them while I read it? 6 THE CHAIRMAN: Please. 7 MR. CARSON: The response that SNC 8 Lavalin provided is as follows: The dam safety 9 review carried out for the floodway expansion 10 project was generally based on the Canadian Dam 11 Association Dam Safety Guidelines, herein called 12 the CDA guidelines, as indicated in annex C, 13 section 3.1.1.1 of the preliminary engineering 14 report. As indicated in paragraph 4, section 1.1, 15 scope and applicability of the CDA guidelines, it 16 states that the CDA guidelines are intended to 17 cover the majority of normal requirements for dam 18 safety. However, it is recognized that other 19 requirements could exist for a particular dam 20 site, and the responsible engineer must identify 21 considerations not included herein, and determine 22 the appropriate dam safety requirements. 23 That's a direct quotation from the CDA 24 guidelines. 25 Now this principle was applied to the 00961 1 dam safety investigations for the floodway 2 expansion as there are characteristics of the 3 project that require appropriate interpretation of 4 the CDA guidelines to meet the intent of the CDA 5 guidelines. Examples with respect to the floodway 6 expansion project include; 7 Number 1: A dam safety review 8 typically covers investigation of existing 9 facilities. The dam safety review for the 10 floodway expansion project covered both, (a), a 11 review of the existing facilities and procedures 12 in the context of the proposed operation after 13 completion of the project, as well as (b), a 14 review of preliminary designs for components of 15 the project, such as the west dyke, which are 16 planning to undergo substantial upgrades. 17 Number 2: The water retaining 18 structures for most dams are subjected to 19 continuous submergence of the upstream slopes and 20 hydrostatic loading from the impounded reservoir. 21 The water retaining structures for the floodway 22 are only subjected to intermittent and relatively 23 short term loading during major floods. This 24 reduces the significance of factors such as 10.4, 25 sedimentation and silting. 00962 1 Number 3: Section 6, called Floods 2 from the CDA guidelines, indicates that the 3 magnitude of the inflow design flood to be used 4 for evaluation of the design or safety evaluation 5 of the dam should increase with increasing 6 consequences of failure. This aspect of the CDA 7 guidelines is based on the fact that the 8 consequences of failure of water retaining 9 structures, in most dams, typically increase with 10 increasing flood magnitude, and increasing 11 upstream water levels. 12 In the case of the floodway, the 13 maximum difference in water level across the 14 structures and the highest consequences of failure 15 would occur for floods of relatively modest 16 magnitude. Both the difference in water level 17 across the structures and the consequence of 18 failure would decrease very substantially with 19 floods approaching the probable maximum flood, due 20 to prior inundation of areas downstream of the 21 structures. 22 In order to meaningfully apply the 23 intent of the principles of dam safety for the 24 floodway project, it was necessary to adapt the 25 templates provided in the guidelines for flood 00963 1 passage requirements during extreme events. 2 SNC Lavalin's interpretation of the 3 application of the CDA guidelines to appropriately 4 reflect the specific characteristics of the 5 Floodway Expansion Project was guided by the 6 chairperson for the working group responsible for 7 preparation of section 6 of the guidelines called 8 Floods. He was also a member of the working group 9 for preparation of section 7 of the CDA guidelines 10 called Discharge Facilities. 11 THE CHAIRMAN: Thank you. 12 MS. JOHNSON: Mr. Chairman, since 13 there is a small break I would like to enter the 14 errata as exhibit 48, and the response from SNC 15 Lavalin as exhibit 49. 16 17 (EXHIBIT 48: Errata for EIS) 18 19 (EXHIBIT 49: Response from SNC Lavalin 20 Feb 21, 2005) 21 22 THE CHAIRMAN: Mr. Rempel. 23 MR. REMPEL: We would like now to 24 proceed with Mr. Bert Smith commenting on the 25 bedrock issue. 00964 1 MR. SMITH: Mr. Chairman, this is in 2 response to your question regarding the bedrock 3 conditions at the inlet structure. And we had 4 discussed both the inlet and outlet structure and 5 the question was really related to is there a 6 difference there. We reviewed some of the 7 original reports and information that is 8 available, and I have here a report on the 9 memorandum on preliminary design dated July 28, 10 1962, by H.G. Acres, on the inlet control works. 11 And this was an investigations and preliminary 12 design for the structure. And I will read a few 13 of the pages here just for the record. 14 In fact, just to address the question 15 on the upstream water level of increased elevation 16 of 778.3 for -- so this was in the design work, 17 and it is on page 2 of this report, item 3 at the 18 bottom of the page. So that's just to clarify 19 that that was in the design planning from the 20 early stages. 21 On page 9 of the report, there is a 22 statement that the bedrock surface ranges from 23 elevation 683 to 690. This is at the proposed 24 site for the inlet structure. It is flatlined, 25 fine grained massive dolomite which exhibits 00965 1 little effect of solution or leaching in the cores 2 recovered from the most recent exploration 3 drilling. They drilled holes 20 feet in depth. 4 Further along in the same report on 5 page 24, they indicate that in the event that any 6 clay seams or solution channels are uncovered in 7 the excavation, that if such a condition should 8 exist, a moderate decrease in foundation level or 9 provision of a shear check may be required. 10 Solution cavities, if found, would be excavated 11 and filled. In fact, during the design the inlet 12 structure was countersunk six feet below the 13 bedrock surface as a requirement for the type of 14 gate that was used. So it was well -- it was well 15 set into the bedrock, and there were minimal 16 seepage conditions observed during construction. 17 I spoke to the design engineer in 18 charge of that structure at the time, and he 19 indicated there was no grouting beneath the 20 bedrock structure and it was not required. And he 21 did add that there was a 20-foot thick clay 22 blanket built on the upstream side of the 23 structure covering the bedrock in the river bottom 24 as a further protection against any seepage under 25 the structure. 00966 1 So, I guess in summary, we certainly 2 don't see any concerns with the bedrock integrity 3 at the inlet structure site, and I would not 4 anticipate that a problem could have developed 5 in -- the groundwater conditions at that site are 6 primarily of a saline nature coming from the 7 southwest of Manitoba, very high dissolved solids, 8 so very limited potential for a solutioning, and 9 as well a very flat gradient across the structure. 10 THE CHAIRMAN: Thank you, Mr. Smith. 11 Could you make copies of the relevant parts of 12 that report available to us, please, later on 13 today or -- 14 MR. SMITH: Yes. 15 THE CHAIRMAN: Thank you. 16 MR. MORGAN: We do have copies of 17 those pages and the whole report that we can 18 submit to you. 19 THE CHAIRMAN: Thank you. Does that 20 conclude your introductory comments? 21 MR. REMPEL: Yes, it does. 22 THE CHAIRMAN: Before I turn it over 23 to Mr. Currie, we were much more popular this 24 morning than we anticipated. We have people 25 crowding in the back door and setting up chairs 00967 1 around the doorway. Maybe we could get everybody 2 to move up in this corner along the side and make 3 a bit more room available, please. There is 4 plenty of chairs over there, if we could just 5 move. 6 MS. JOHNSON: Mr. Chairman, if we 7 could add the report of memorandum on preliminary 8 design as exhibit number 50. 9 THE CHAIRMAN: Thank you. 10 11 (EXHIBIT 50: Department of 12 Agriculture and Conservation, Water 13 Control and Conservation Branch, Red 14 River Floodway, Inlet Controls works, 15 Memorandum on Preliminary Design, July 16 28, 1962) 17 18 THE CHAIRMAN: Okay, thank you for 19 that. We will come back to order now. We are 20 proceeding to cross-examination by Mr. Currie on 21 behalf of his clients, the municipalities of East 22 St. Paul, St. Clements and Springfield. Mr. 23 Currie. 24 MR. CURRIE: Thank you, Mr. Chairman. 25 I guess as to the panel, the first few questions 00968 1 that I would like to ask are sort of general in 2 scope. And the first question that I would ask 3 is, probably whoever wants to jump in and discuss 4 it, is in your proposal, can you tell us exactly 5 what are you expecting to have licensed here? Are 6 you in fact going to have the whole project 7 licensed, that is stem to stern, for lack of a 8 better word, or are you proposing to have only the 9 new infrastructure licensed? 10 MR. REMPEL: Mr. Currie, the 11 application under the Manitoba Environment Act was 12 filled out for the expansion of the project and it 13 includes the inlet structure, the outlet 14 structure, the bridges, the entire project is 15 being proposed for licensing under the Manitoba 16 Environment Act. And in doing this there will be 17 approvals required from Canada. So, when the 18 Government completes their screen report, we would 19 expect that the approvals associated with 20 fisheries, habitat alteration, Navigable Waters 21 Protection Act approvals -- and what else is 22 there -- any other approvals associated with the 23 Federal legislation would also flow. 24 MR. CURRIE: I understand that you 25 have other approvals that you have to seek and you 00969 1 have just listed those approvals for me which 2 relate to the Federal level. But what I'm asking 3 you specifically today is, is it your anticipation 4 that your project will license this floodway from 5 the beginning of the inlet to the outlet, and not 6 just the changes? 7 MR. REMPEL: There would be a licence 8 for this expanded project and its operation. 9 MR. CURRIE: Yes. And was your 10 application designed or did it exclude out the old 11 floodway? 12 MR. REMPEL: The application did not 13 exclude the existing floodway. It made an 14 application for the expansion project. 15 MR. CURRIE: Now, the next question 16 that I want to move forward to is the authority 17 itself. At this point in time, when do you 18 anticipate the authority to come to an end, or is 19 this something that's going to exist so far as we 20 know forever? 21 MR. MCNEIL: Doug McNeil speaking. 22 The Floodway Authority was proclaimed as a Crown 23 corporation on November 1, 2004, and it is not 24 expected to come to an end, because as part of the 25 Floodway Authority Act, the Floodway Authority is 00970 1 responsible not only for expansion of the floodway 2 but for long term maintenance as well. 3 MR. CURRIE: And I take it that you 4 have distinguished that, from what I can read in 5 the transcripts, I wasn't here for the hearings, 6 but what I understood was you distinguished 7 maintenance and construction from operation, am I 8 correct? 9 MR. MCNEIL: That's correct. 10 Government decided to let operation remain with 11 Manitoba Water Stewardship because they have the 12 resources, the knowledge, the expertise in 13 operating the floodway in addition and in 14 conjunction with the Shellmouth dam and reservoir 15 and the Portage diversion. 16 MR. CURRIE: With regards to the 17 assessment of mitigation factors, whose 18 responsibility will that be? 19 MR. MCNEIL: The Manitoba Floodway 20 Authority, as part of this expansion project and 21 the environmental assessment, is also responsible 22 for mitigation of any impacts. 23 MR. CURRIE: Is that answer to mean 24 that both parties? 25 MR. MCNEIL: I repeat, the Manitoba 00971 1 Floodway Authority has the responsibility for 2 expanding the floodway, and is also responsible 3 for mitigating any impacts. 4 MR. CURRIE: As I understand it, you 5 have $11 million for these mitigation strategies? 6 MR. MCNEIL: The $11 million 7 environmental mitigation fund is for unpredicted 8 events that may occur during construction. 9 Through this project, and the EIS clearly states, 10 that after mitigation this project will have no 11 significant adverse effects. But the fund -- and 12 so we are doing things under the program through 13 the expansion. For example, not deepening but 14 widening. So that's already included in the base 15 budget for the project. But if there should be 16 any unpredicted effects during construction or 17 afterwards, that's what that fund is for. 18 MR. CURRIE: You've mentioned 19 deepening versus widening. Let's get into that 20 issue since you bring it up. With regard to 21 deepening, I understood that the original proposal 22 was 1.5 metres, to .5 metres, is that correct, 23 deepening? 24 MR. MCNEIL: The original proposal was 25 in the range of 0.6 metres to 2 metres of 00972 1 deepening. That was in the concept stage of 2 design, and that was included in the original 3 project description. That is no longer true, 4 though. 5 MR. CURRIE: When did that change? 6 MR. MCNEIL: It has evolved through 7 the predesign process and also as we get final 8 design underway. As we announced a week ago 9 today, we are no longer undertaking deepening. We 10 are going to achieve the capacity increase of the 11 floodway by widening only. 12 MR. CURRIE: I understand your point, 13 you make it several times, you feel that you are 14 not deepening, you are widening. I guess I'm back 15 to my earlier question. At what point in time did 16 you make the conclusion that you would not go in 17 any deepening whatsoever? 18 MR. MCNEIL: We made the final 19 conclusion just prior to last Monday. So 20 February 11 to 13th time frame. 21 MR. CURRIE: Thank you very much. Now 22 prior to that date you had at least two feet of -- 23 sorry, about .5 metres, or roughly two to three 24 feet of deepening, in your mind, as a possibility. 25 Is that correct? 00973 1 MR. MCNEIL: That's correct. 2 MR. CURRIE: And maybe even earlier to 3 that you had a possibility of going even deeper 4 than that, correct? 5 MR. MCNEIL: In the original concept 6 design it was indicated that we could go 0.6 to 2 7 metres of deepening. And I would add that since 8 that time, when we announced that it would be no 9 more than 0.6 metres, that was at select 10 locations, not throughout the whole length of the 11 floodway. 12 MR. CURRIE: Now, I would like to ask, 13 I guess, the environmental side of your team, when 14 did they do their assessment? When did they do 15 their portion of the EIS? 16 MR. REMPEL: Are you referring in 17 particular to groundwater? 18 MR. CURRIE: Yes, thank you. 19 MR. REMPEL: Dr. Morgan will respond. 20 MR. MORGAN: The preliminary 21 engineering design, as shown in all of those 22 documents behind them, was done in July of 2004, 23 and our assessment in the EIS was done in August 24 of 2004. And as Mr. McNeil has said, and we've 25 discussed this with the community in May and June 00974 1 when we went out to public events, is that the 2 goal of the Floodway Authority was to have no 3 deepening, except in selected areas there may be 4 .5 metres of deepening. And in those selected 5 areas, Mr. Smith can get into more details, maybe 6 around some of the bridges, there was some in the 7 upstream end around St. Mary's, it was not 8 expected that there would be effects outside of 9 the right-of-way. The effect in the channel 10 actually decreases as you move away from where 11 that initial effect was. And it decreases towards 12 no effect as you get to the right-of-way. There 13 is sketches of that in the EIS, and you have a 14 groundwater specialist that you can refer to. 15 So at the time that we made it, the 16 assessment, we had also thought there would be no 17 significant effects. However, there is still a 18 lot of concern in the community, and so we've 19 always said that the best thing to make it simple 20 for people to understand is to not deepen along 21 the channel. And Mr. Smith can even fill you in a 22 bit on the process that went on from August 23 through until a few weeks ago of how they arrived 24 at modifying the design in order to be no 25 deepening. 00975 1 MR. CURRIE: Mr. Chairman, my question 2 was when did they decide that deepening would take 3 place. It wasn't necessarily a full defence of 4 why they have now retreated from their position. 5 We will get into that question perhaps later on. 6 MR. SMITH: Mr. Chair, maybe I can add 7 to that discussion. The preliminary design, you 8 have to understand, was an optimization process, a 9 sensitivity study looking at various depths versus 10 widening combinations to come up with the best 11 final design. And that involved the bridge 12 heights -- and it was a very complicated process, 13 it is not just a simple answer. But the thing to 14 appreciate is that when the preliminary 15 engineering reports went out, the decision had 16 been made not to deepen the main channel. 17 However, we did reserve some flexibility to 18 locally deepen as much as .6 of a metre, and the 19 focus on that was really in the low flow channel, 20 the narrow ditch in the middle of the floodway. 21 However, the wide base of the channel at that 22 point, the decision had been to widen the sides, 23 not deepen the bottom of the main channel. I 24 think it is important to understand that. 25 And there were a few points along the 00976 1 low flow channel where we did want to verify 2 elevations before we came to that final position 3 to say no deepening. 4 There is a diagram up on the board 5 now. You can see where the low flow channel is in 6 the middle, the little ditch, that's designed to 7 handle surface runoff from the various perimeter 8 drains. And the blue areas on the sides are where 9 the widening is proposed. The widening, as I say, 10 when the preliminary engineering report came out 11 there was no intent to deepen the base of the main 12 channel at that point. 13 Maybe that helps you, Mr. Currie, in 14 understanding the timing. 15 MR. CURRIE: Mr. Chairman, if every 16 time I ask a question, asking for a specific date 17 or a range of dates, I go on for 20 minutes in an 18 answer, I will say to you the cross-examination 19 will go considerably longer than I anticipate. 20 Answering fully and fairly is one thing, but 21 answering on a full-based defence -- we have heard 22 this evidence already. All I wanted was a 23 specific answer to when they decided. What they 24 did in their defence of that position, I might ask 25 or I may not ask. So I'm going to submit that I'm 00977 1 going to ask the chair to -- 2 THE CHAIRMAN: Could you ask your 3 question again in very simple terms, and hopefully 4 you can get your straight answer. 5 MR. CURRIE: I did, in fact, within 6 two sentences. 7 THE CHAIRMAN: You don't need a 8 preamble, just say it again. 9 MR. CURRIE: Yes, I got it, but it 10 took us quite a while. 11 So in any event, let's go on to the 12 next question now. You've indicated, as I 13 understand it, that you did the assessment in July 14 of '04 and then further work in August of '04; 15 correct? 16 MR. MORGAN: No, that is not correct. 17 MR. CURRIE: Okay. Then I didn't get 18 my answer. 19 MR. MORGAN: David Morgan. The 20 assessment started in December 2003. It was, we 21 started reviewing the engineering and talking with 22 the engineers at that time. There was an 23 iterative process in the project design. This was 24 laid out to the public in January, and then there 25 is an iterative process in the design. 00978 1 We had input from the public 2 consultations very early on that groundwater was a 3 major concern. And from that, we brought that 4 information to the engineers who worked on the 5 preliminary results. 6 Preliminary results were made in 7 April, May, and presented to the public in May, 8 June. At that time, you know, over that time the 9 assessment was made. And as I just discussed 10 earlier, the engineering report was finalized in 11 August -- the engineering reports finalized in 12 July, the EIS was finalized in August. 13 MR. CURRIE: Thank you. With regards 14 to that then, my analysis of you going through 15 your assessment is that regardless of the 16 deepening or not, you came to the conclusion in 17 your assessment that there would be no significant 18 impact on the groundwater by deepening or not 19 deepening, it really didn't matter? 20 MR. MORGAN: That's incorrect. 21 MR. CURRIE: Okay. 22 MR. MORGAN: A deepening of two metres 23 would have had an effect. We brought that, we 24 brought that to the engineers and they understood 25 that. What we said is that deepening in selective 00979 1 insensitive areas throughout the channel of 2 .5 metres or less would have no significant -- 3 would likely have no significant adverse effect. 4 MR. CURRIE: So if I can -- 5 MR. MORGAN: Selected areas, you have 6 to understand that. 7 MR. CURRIE: I'm going to now repeat 8 it back to you to see if I have got it and 9 understood it. You are saying that if the 10 engineers had come to you and said, we are going 11 to deepen it generally, that was a problem for 12 you; but if they came to you and said, we have 13 selected areas that you have determined are not 14 sensitive, you would not have a problem with them 15 deepening in those areas? 16 MR. MORGAN: Yes. 17 MR. CURRIE: So I understand it now. 18 MR. MORGAN: It is the magnitude 19 that's important, though. 20 MR. CURRIE: Sorry? 21 MR. MORGAN: The magnitude is also 22 important, not just the location, the location and 23 magnitude is important. 24 MR. CURRIE: Correct. Okay. Now, can 25 you point to, I guess, specific documents or pages 00980 1 in your EIS where you discuss, if you will, the 2 deepening issue and the fact that you can't deepen 3 generally, but only -- you feel you might be able 4 to deepen only in select areas. 5 MR. MORGAN: Page 5-37 in the EIS 6 under erosion control, figure 5.5-5. 7 MR. CURRIE: Yes. 8 MR. MORGAN: This figure shows a 9 profile from the inlet to the outlet. It states 10 that the only area at that time that requires low 11 flow deepening was an area upstream around St. 12 Mary's Road. This area is underlined with clay, I 13 can't remember the exact detail, but it is not a 14 sensitive area. 15 If you look at that diagram also you 16 will see what that they are looking at doing is 17 filling the channel, the low flow channel in the 18 sensitive areas, so improving the current 19 baseline. So by filling and improving the current 20 baseline, we do not see an adverse effect in those 21 areas. 22 MR. CURRIE: Now, with that 23 assessment, are you able to tell us today roughly 24 how many springs might be throughout the floodway? 25 MR. MORGAN: I think that's in the 00981 1 documentation. We can find that and put it up. 2 MR. CURRIE: And how did you do that 3 assessment? Did you use Provincial Government 4 data or did you use anecdotal data? 5 MR. MORGAN: What do you mean by the 6 assessment? 7 MR. CURRIE: Well, essentially, how 8 did you get the data, how did you get the data of 9 the number of the springs from one end of the 10 floodway to the other, where did you get it from? 11 MR. MORGAN: Mr. Smith can get into 12 the details, but it is shown in appendix M, there 13 is a graph there, those were located, I think by 14 KGS staff, they can confirm that, but we also had 15 people out there doing aquatic studies which noted 16 those springs also. 17 The data is presented, or the diagram 18 is presented in appendix M, annex H, is it? 19 MR. CURRIE: Do you have an electronic 20 version available? 21 MR. MORGAN: Yes, we are looking for 22 that. 23 MR. CURRIE: Let's take our time and 24 get it up there. Is Mr. Smith able to tell us 25 where the data comes from? I mean, I understand 00982 1 that you are going to present for us a document or 2 a diagram that's going to show what you believe to 3 be springs occurring, but I guess the question is, 4 where did you get the data from, or where is that 5 data generated from? 6 MR. MORGAN: We will get into the 7 details -- it is a very detailed question, and you 8 are looking towards -- there is also base flow 9 studies done last year about this time. 10 MR. CURRIE: Sorry? 11 MR. MORGAN: There was base flow 12 studies which determined the base flow in the 13 floodway. These are done in the winter time so as 14 not to be interfered with by runoff, et cetera, 15 and that gives indication of the groundwater flow 16 getting into the floodway. So that's how the 17 quantification was done. 18 MR. CURRIE: I don't mean to quibble 19 with you too much, Mr. Morgan, clearly that would 20 tell us how much water is flowing through the 21 floodway, but it may not necessarily pinpoint 22 where springs might be or otherwise? 23 MR. MORGAN: No, the springs are -- 24 MR. SMITH: Mr. Currie, maybe I can 25 expand on that a little bit. We have just lost 00983 1 that section. 2 In the report we have a drawing in 3 appendix M, drawing H5C, I'm sure you have seen 4 it, it is a profile along the floodway from the 5 inlet to the outlet, and the location of the major 6 springs are shown on that profile. Now, that's 7 based on the historical data at the time of 8 construction, also on published literature. And 9 in addition, we, during the course of our work we 10 were out in the field walking the floodway to 11 examine spring locations. 12 I might add, on that figure we did 13 miss one spring location at the TransCanada 14 Highway, and we are aware of other springs right 15 near the outlet. 16 I guess the scale of that -- it 17 doesn't really highlight it, but just for the 18 record, we show springs in the vicinity of Highway 19 15, CNR Redditt, CPR Keewatin, through the Birds 20 Hill area, and north of Dunning Road. And as I 21 mentioned earlier, at Highway 1 we are also aware 22 of springs there. 23 MR. CURRIE: Maybe in the analysis 24 here, I guess, is that looking at this document, 25 can you tell me -- when I look at it, maybe it is 00984 1 just me -- can you tell me where those springs are 2 occurring from that document, just looking at it 3 yourself? 4 MR. SMITH: They are occurring in the 5 bottom of the channel, and there is in our report, 6 again, appendix M, section 8, there is a 7 discussion on the groundwater discharge areas that 8 describes them in more detail. 9 MR. CURRIE: Okay. But looking at 10 that diagram, can you pinpoint those springs for 11 me off that diagram now? 12 MR. SMITH: Well, you can't on the 13 drawing that's in the report. 14 MR. MORGAN: We will get a paper copy 15 to show the Commission. It just doesn't show up 16 very clearly because it is a light blue arrow. 17 MR. CURRIE: Light blue arrow -- I 18 don't see one there. 19 MR. MORGAN: It doesn't show clearly 20 on the screen. 21 MR. CURRIE: I see one there now, yes. 22 Okay. 23 Is that an indicator then to us that 24 that's where you've identified a spring coming 25 out? 00985 1 MR. SMITH: The arrows on that drawing 2 indicate springs of 100 gallons per minute or 3 greater, as noted on the drawing. 4 MR. CURRIE: And 100 gallons per 5 minute or less, you didn't note them? 6 MR. SMITH: In general where we show 7 these arrows there is a zone of springs occurring, 8 so there will be also smaller ones adjacent to it, 9 we didn't show every arrow. 10 MR. CURRIE: I understand that there 11 may be other springs, but I guess generally 12 speaking, your analysis or your data doesn't 13 show -- or at least on this, it may not mean that 14 you didn't go get the data, I'm not suggesting 15 that you didn't, what I want to know is that you 16 didn't put on this particular diagram anything 17 less than 100 gallons per minute; correct? 18 MR. SMITH: Well, the arrows show 19 approximate areas where there is groundwater 20 discharge of 100 gallons per minute or greater. 21 That doesn't mean that it has to be all one 22 spring, there could be a collection of springs of 23 lesser flow that total 100. 24 MR. CURRIE: Let's get back to -- 25 okay, so you are saying what you have anticipated 00986 1 the blue arrow now to mean is that it could be a 2 collection of small springs equalling 100 gallons 3 per minute? 4 MR. SMITH: I'm clarifying that for 5 you, yes. 6 MR. CURRIE: Okay, I understand that. 7 Now, just so I understand this, and I 8 mean, again, you are going to correct me I'm sure 9 if I don't, but basically when we see these 10 springs they are conduits to the groundwater, 11 correct, possible conduits to the groundwater? 12 MR. SMITH: That's correct. There has 13 to be an interconnection to the aquifer. 14 MR. CURRIE: Yes, and as I understand 15 it, we have got these conduits, possible conduits 16 to the groundwater, and from what we see here, 17 this is the upper aquifer; correct? We are not 18 talking the lower carbonate aquifer at this point, 19 or are we? 20 MR. SMITH: No, we are dealing with 21 the upper carbonate aquifer. 22 MR. CURRIE: Right. And I note there 23 that aside from the springs that we have, that you 24 show a sand and gravel, I guess geography for lack 25 of a better word, I don't know the actual 00987 1 engineering term; is that correct, we have sand 2 and gravel here? And that appears to be coming 3 right out to the top of the -- to the top of the 4 floodway itself where you are actually at ground 5 level? 6 MR. SMITH: That sand and gravel 7 deposit is projected on to the profile. It 8 actually represents the Birds Hill sand and gravel 9 Kame Esker deposit which occurs east of the 10 floodway. 11 MR. CURRIE: I see. So that's the 12 actual Birds Hill sand and gravel aquifer? 13 MR. SMITH: That's correct. 14 MR. CURRIE: Okay, good. 15 Now, along this diagram, aside from 16 the Birds Hill sand and gravel aquifer that we see 17 in here, on the length of the floodway, do you 18 have any data regarding any other smaller, 19 insignificant sand and gravel deposits in there 20 which would be a conduit to the groundwater 21 itself? 22 MR. SMITH: The spring areas that 23 occurred initially were developed at the time of 24 construction in the 1960s, when the bedrock 25 aquifer was still under its higher head. So you 00988 1 had that 20-foot or 6-metre head, as you know, 2 that has dissipated or dropped at current levels. 3 At the time of construction that still existed, so 4 you had a significant differential pressure, if 5 you will, from the bedrock aquifer up through the 6 till and the overlying clay. So in areas, 7 particularly where there was a thin clay or a till 8 exposure, that's where the springs would develop. 9 So it is not a sand conduit up from 10 the till necessarily. It actually was a high 11 differential pressure that forced openings through 12 the clay. And I might add that a lot of those 13 openings since construction, since the pressure 14 has dissipated, have partially or totally rehilled 15 or infilled. 16 MR. CURRIE: Right. Now just so I 17 understand this, I mean, if we are talking about 18 groundwater protection in the state of nature, 19 clearly certain types of clay are the best, almost 20 the best natural protection we can find; am I 21 incorrect on that, I mean, short of a bedrock 22 aquifer, or a bedrock that has absolutely no 23 cracks in it? 24 MR. SMITH: What you are looking for 25 is a low permeability layer that the water can't 00989 1 pass through readily. So certainly the lacustrine 2 clays are very low permeability. The till here is 3 in fact a clay till for the most part and is also 4 relatively low permeability. 5 MR. CURRIE: And then we just go up 6 from there to higher permeability? 7 MR. SMITH: That's correct, into silts 8 or sands. 9 MR. CURRIE: Yes. Now, with the 10 baseline of your assessment, I have read through 11 the transcripts and as I understand it, and again 12 I need to be educated, your baseline is the 13 existing floodway as it exists with all of the 14 springs in it, with all of the conduits to the 15 groundwater that may exist. Am I to understand 16 that's where you are starting with your project, 17 and then we will move forward from there? 18 MR. MORGAN: Baseline is similar but 19 it is a little bit more than that. It is the 20 condition that would occur currently and in the 21 future with the project. So it includes the -- 22 sorry, without the project. It is the -- I will 23 say that again. The baseline is the environment 24 now and into the future without the project. So 25 it includes existing conditions now, plus 00990 1 potentially further erosion. That's one of the 2 reasons why when we looked at the assessment we 3 also looked at the erosion control measures and 4 infilling of the existing floodway when making the 5 assessment that there should be no likely adverse 6 effects. There should be potentially beneficial 7 effects in some areas. 8 MR. CURRIE: With regards to that 9 then, I guess what I'm understanding you saying is 10 that the baseline is the existing conditions, plus 11 what you anticipate might be further conditions 12 created by this specific project itself? 13 MR. MORGAN: No, I don't think it 14 is -- you can clarify me if it is on -- the future 15 conditions is future expected, not any 16 anticipated, but expected. 17 MR. CURRIE: I see, so it is just more 18 of actual expected changes, not -- 19 MR. MORGAN: We can't anticipate any 20 future event. 21 MR. CURRIE: Right, what you expect 22 will happen based on the historical process that 23 has occurred already? 24 MR. MORGAN: Yes, continued erosion. 25 MR. CURRIE: And in particular erosion 00991 1 being a good example of that? 2 MR. MORGAN: Yes, and other activities 3 in the area too. 4 MR. CURRIE: And other activities in 5 the area meaning other development that has 6 occurred on the fringes of this particular 7 floodway that might have an impact on it, or are 8 we talking about other developments just specific 9 to the floodway? 10 MR. MORGAN: No, other activities and 11 developments in the area which could have an 12 overlap in effects. 13 MR. CURRIE: Okay. 14 MR. MORGAN: That's why we went 15 towards the no effect condition of no deepening, 16 infilling, control erosion, widening instead of -- 17 MR. CURRIE: Right. I guess we are 18 going to quibble, you and I, about whether there 19 is a no effect result, but I understand your 20 position, you take it that there is a no effect 21 result. 22 MR. MORGAN: No likely significant 23 adverse effects is the position that we state. 24 MR. CURRIE: Yes, and I understand 25 that. 00992 1 With regard to actual numbers, aside 2 from the blue arrows that we are having a hard 3 time distinguishing, were you able to put in the 4 report somewhere a quantitative number where I 5 could point to the Commission and say, there are 6 34 springs, there are 31, there are none, there 7 are 14? 8 MR. SMITH: As indicated earlier in 9 appendix M, section 8, we do discuss some of the 10 major springs, and I think it is important to 11 appreciate that, as we brought out in the earlier 12 discussions in this hearing, we have an ongoing 13 program to monitor the springs along the channel. 14 And when you have flow in the channel 15 from surface runoff, you can't identify those 16 springs in terms of actual total flow of the 17 springs. So we have been in fact monitoring again 18 this winter to pick up flows along the channel at 19 various locations, and that will give us a better 20 quantitative number on the contributions at 21 various stations along the channel. However, the 22 initial work that we did was consistent with that 23 completed back in the early '70s when the channel 24 was constructed. 25 MR. CURRIE: Mr. Smith, so the answer 00993 1 is no, you do not have a document that points to 2 the number of springs that are found in that 3 aquifer, that I can point the Commission to and 4 say there is 34 springs there, there is 10, there 5 is none, there is 22? 6 MR. SMITH: The number of springs will 7 vary from season to season, depending on the 8 amount of pressure and the conditions. 9 MR. CURRIE: So the answer is no, you 10 do not have a written document in your EIS that 11 says there are 34 or less, and give or take, 12 because there are changes in the environment? 13 MR. SMITH: We do identify the major 14 areas where springs occur, we did not quantify the 15 exact number of springs, and that's not realistic 16 to do that. 17 MR. CURRIE: Did you quantify the 18 number of springs that had a significance? 19 MR. MORGAN: You seem to be missing 20 the point on significance here. Significance is 21 what we do when we assess the project, not when we 22 assess the baseline. So we can look at this and 23 say, by not deepening, by having erosion control 24 we do not expect this condition of springs from 25 the aquifer to the floodway to increase 00994 1 significantly. 2 MR. CURRIE: Okay. Let's get into 3 that then. 4 MR. SMITH: Excuse me, Mr. Currie, 5 maybe I need to clarify. The springs are 6 primarily occurring in the bottom of the low flow 7 channel. The low flow channel has water in it, so 8 you can't walk along the flow channel and say, I 9 see all of the springs, clearly they are masked by 10 the flow. So the intent is you measure the flow 11 at different locations along the channel, and then 12 you get a quantification of the contribution of 13 springs in various sections. And that's what we 14 have done and we have identified the major zones 15 of contribution. 16 MR. CURRIE: And it is not possible, I 17 take it, Mr. Smith, to do the reverse of that, 18 which is to stop the flow at a certain point, to 19 hold it back in a particular low flow period, 20 watch what occurs past that point to determine 21 where your springs are at, and then do the 22 calculation? 23 MR. SMITH: In the period that we did 24 our investigations, it was probably the wettest 25 summer on record and that was not done. 00995 1 MR. CURRIE: So the answer is, it was 2 just not convenient at the time that you did your 3 assessment to do that? 4 MR. SMITH: I wouldn't say convenient, 5 I would say not practical. 6 MR. MORGAN: I guess the answer is 7 also that it is not necessary, in order to make 8 the assessment of the project, that by infilling 9 and erosion control we do not expect this to have 10 a likely adverse effect, infilling and erosion 11 control. 12 MR. CURRIE: My understanding is that 13 the number of springs and the conduits between the 14 floodway -- or sorry, the floodway channel and the 15 lower carbonate aquifer, your model takes into 16 account these springs. Your modeling, when you 17 went to use it, was taking into account the number 18 of conduits to come to the conclusion there was 19 going to be no significant adverse effects? 20 MR. SMITH: That's correct. The 21 regional model identified the locations of the 22 springs by the interconnection that we applied to 23 the model at the appropriate locations. 24 MR. CURRIE: Well, you may not agree 25 with me, but if your data is wrong, that you don't 00996 1 have the number of springs correct, that you have 2 more conduits between the aquifer and the 3 floodway, that throws your model a little bit off? 4 MR. SMITH: What we have is very 5 detailed measurements of the piezometric pressure 6 or pressure level all along the floodway, and 7 that's matched in our model in the contours which 8 allows us then to have the proper -- if we have 9 the proper interconnections then we can mirror the 10 levels in the model. And that was done both for 11 construction for year 2000, and for the '97 flood. 12 So we did represent that to a reasonable level. 13 MR. CURRIE: Your model, though, 14 however, would have to make sure that all other 15 geophysical conditions were exactly as your model 16 in order to make it a reality? That is, in order 17 to simulate reality, your model had to have a 18 pretty good geophysical description of what you 19 were dealing with; correct? 20 MR. SMITH: I suspect you mean 21 geotechnical. Geotechnical mean soils. And 22 that's correct, we did have that, we did a lot of 23 drilling along the channel, well over 300 holes 24 with both lab testing and field permeability 25 testing. So we have a reasonable representation 00997 1 of the geotechnical or hydrogeological conditions 2 along the floodway. 3 MR. MORGAN: Another point you have to 4 understand is that the model is calibrated, and 5 there is also sensitivity analysis done on 6 modeling. Exactness, precision is not what a 7 groundwater model does. I mean, your expert 8 should be able to counsel you on this. But, 9 again, you also have to see mechanisms for 10 significance. By infilling and erosion control, 11 I'm not sure where you see the mechanism for 12 adding adverse effects? 13 MR. CURRIE: I will get to that, Mr. 14 Morgan, and that's something for me to argue with 15 the Commission. In the meantime, I'm entitled to 16 explore the evidence and make my own conclusions 17 and arguments to the Commission. 18 The next issue I would like to address 19 is how many of those 300 test holes were done at 20 springs? How many of your test holes -- 21 MR. SMITH: Well, I'm glad you asked 22 that because in fact the detailed sections that we 23 present in this report were selected specifically 24 at areas of major springs, such as CPR Keewatin, 25 Springhill, and in the Dunning Road area. And in 00998 1 those locations we did detailed drilling, both in 2 the bedrock, the till and the clay, usually on 3 either side of the floodway, and testing at those 4 locations in order to use that information in our 5 model to have a confidence level of the response. 6 Again, those are selected as representative 7 sections. Clearly, you can't do a section on 8 every mile along the floodway. But, in addition, 9 those were selected in areas where the province 10 had installed monitoring wells and they had 11 continuous water level readings in the bedrock, 12 water pressure levels from pre-construction up to 13 current date. In other words, on a daily basis 14 they recorded what the levels were, they respond 15 to the water, the changes in the seasons, to the 16 floods that pass. So we had an excellent data 17 base in order to calibrate our models and have a 18 confidence level in the response. 19 MR. CURRIE: I don't care who answers 20 the question, but what is the definition that your 21 assessment, your environmental assessment uses for 22 sensitive areas? What is the definition? 23 MR. MORGAN: I don't understand. Can 24 you repeat the question? 25 MR. CURRIE: Well, earlier you 00999 1 indicated to us that you were going to look at, 2 your concerns were that you would not deepen in 3 sensitive areas, and that you had somehow decided 4 that there was some form of sensitive areas within 5 the floodway. And I'm just asking now, what is 6 your definition of sensitive areas? 7 MR. MORGAN: I guess a sensitive area 8 would be an area, as Mr. Smith discussed, the 9 areas where there is potential for higher 10 permeability material. Like an area with eight 11 metres of clay is less sensitive than an area with 12 two metres of silt, and an area with potentially 13 sandy silt is more sensitive. So those are the 14 areas which more, as he said, more testing was 15 done, and we actually looked at specific modeling 16 in three of the areas, more detailed modeling. 17 MR. SMITH: Maybe I can add to that, 18 Mr. Morgan. There was drilling done along the 19 entire length of the channel. We initially 20 interpreted the stratigraphy, the soils 21 conditions, identified areas where there is more 22 likely to be groundwater infiltration, such as 23 areas with a thin clay or no clay cover, and then 24 focused on more drilling and testing and 25 ultimately modeling those areas. 01000 1 In addition to that, when we did the 2 models, not only did we first run what was a 3 representative value for the till permeability, 4 which in this case is a clay till, right from the 5 Highway 59 north to Lockport, but we also did 6 sensitivity analysis where we reduced -- or sorry, 7 increased the permeability to the equivalent of a 8 sand. So we said what if there was a sand pocket 9 here, not a till, but pure sand connection to the 10 bedrock, and then analyzed that case to see how 11 quickly might surface water infiltrate under an 12 extreme condition of the 1997 flood, which is the 13 most extreme on record. 14 MR. CURRIE: Right. I read that in 15 your earlier evidence, Mr. Smith, that you had 16 done your sensitivity to basically what you felt 17 was the most sensitive you could put in there, 18 still running a realistic model. 19 MR. SMITH: And I will add to that 20 when you put those values in, the model didn't fit 21 the observed pressure levels in the nearby 22 piezometres. So clearly it was two orders, you 23 know, 100 times more permeable. Certainly you can 24 hypothesize even higher permeability connections, 25 you can carry on forever. It achieved our 01001 1 purpose. 2 MR. CURRIE: The next question that I 3 have is, there is really to my understanding two 4 types of erosion occurring in this particular 5 aquifer. Am I wrong in that? 6 MR. MORGAN: I don't understand the 7 question. 8 MR. CURRIE: Good, let's go on. 9 MR. MORGAN: Could you clarify it? 10 MR. CURRIE: There is the first type 11 of erosion which we call channelization, correct? 12 As the water flows down you are deepening the 13 channel simply by erosion of the water, and that's 14 the one form of erosion that we talked about this 15 morning; am I correct in that? 16 MR. SMITH: Are you referring to the 17 erosion at the base of the low flow channel? 18 MR. CURRIE: Yes. 19 MR. SMITH: That has occurred, yes, 20 that's in the report, we show a profile of that. 21 In fact, that erosion typically occurred in the 22 clay zones, not in the till zones. It is the clay 23 that's more susceptible to erosion. 24 MR. CURRIE: Yes. That's the one form 25 of erosion that we have identified this morning; 01002 1 correct? 2 MR. SMITH: That's correct, and we 3 have proposed to rectify that. 4 MR. CURRIE: But there is a second 5 form of erosion, as I understand it, and that is, 6 as you pointed out, you have hydraulic pressure 7 coming up from the bottom, from the aquifer 8 itself; correct? 9 MR. SMITH: I wouldn't expect there 10 would be a lot of erosion there. In fact, as I 11 indicated, in a lot of cases those are anticipated 12 to have been infilling since the original 13 development, with silt deposition. 14 MR. MORGAN: There could be the 15 opposite of erosion, there can be sedimentation 16 also in natural mechanisms. 17 MR. CURRIE: I would agree with you, 18 in a drought year we could have sedimentation, or 19 the aquifer is drained out to a level that it 20 doesn't have the pressure any further, sure, you 21 can have that reverse. And I'm going to make that 22 argument that in fact you now have a conduit going 23 the other way, that you can have in fact water 24 flowing down that same channel, in effect? 25 MR. MORGAN: That's an argument or a 01003 1 question? 2 MR. CURRIE: Is that correct? 3 MR. SMITH: During a flood scenario 4 with the high level in the floodway, in fact, in 5 the fairly high silt sand base load in the water, 6 when you have water going down there, as I said, 7 you would start to infill that opening. 8 MR. CURRIE: And so your suggestion is 9 that this would help stop contaminating the 10 aquifer by the fact that you have silt and sand in 11 your Red River water, and as it flows backwards in 12 the system that it would in fact now, so to speak, 13 design its own plug? 14 MR. SMITH: To some extent, yes. If 15 you hypothesize that it has opened up, I'm 16 indicating that in fact during a flood that would 17 tend to replug. So the sands and the silt, the 18 silts in particular would be a lower permeability 19 and reduce significantly any inflow. 20 MR. CURRIE: What about places where 21 there is bedrock exposure and very little till? 22 MR. SMITH: In the channel there is 23 very -- in fact, the areas where we had bedrock 24 exposure were during construction at the inlet 25 structure and the outlet structure, and possibly 01004 1 in the immediate area upstream of the outlet 2 structure. And I note that I have seen a 3 reference to bedrock outcropping one and a half 4 kilometres upstream of Springhill. And I have 5 spoken to the design engineers at the time the 6 floodway was constructed, a contractor engineer 7 who worked in that area, and a construction 8 supervisor in that area, and none of them recall 9 bedrock in that area. So I appreciate -- to the 10 best of our understanding, there is not bedrock 11 exposures along the floodway channel. 12 MR. MORGAN: There is though bedrock 13 exposure along Lister Rapids in the Red River. 14 MR. CURRIE: Yes. My understanding 15 is, even reading your own documents, that for sure 16 in the '97 flood, and almost invariably when you 17 run the floodway there is going to be a 18 contaminant event in the groundwater. 19 MR. MORGAN: I don't think -- I don't 20 think that was in the document, a contaminant -- 21 there is intrusion, and we can clarify that, we 22 have some slides that -- are you talking about the 23 river? 24 MR. CURRIE: No, I'm talking about the 25 floodway itself. When you operate the floodway, 01005 1 you are going to have surface water come into 2 contact with groundwater. That is almost with 3 certainty. Is that correct? 4 MR. SMITH: Yes. 5 MR. MORGAN: Yes, but that does not 6 mean it is at a well or anything like that, so I 7 don't want to alarm people. That surface water 8 and groundwater along the river are always in 9 contact, along every river stream, that's an 10 interface. So, you know, you have to be clear 11 when you make statements like that. 12 MR. CURRIE: My next question is that 13 each time then we see the contact between 14 groundwater and surface water, and if you want to 15 argue with me about whether the Red River comes in 16 contact with groundwater or it doesn't, the fact 17 of the matter is right now you have got a man-made 18 event occurring where you have more surface water 19 coming into contact with groundwater. Would you 20 agree with me or disagree with that? Not more in 21 the sense of traditional volumes, but certainly 22 more opportunity. You have created another 23 structure which relates to a possibility of 24 groundwater and surface water interaction? 25 MR. MORGAN: Possibility, yes. 01006 1 MR. SMITH: And maybe to clarify, Mr. 2 Currie, that's correct, and for the most part that 3 groundwater is flowing upward discharging into the 4 channel, so there is that contact. But for the 5 most part, the pressure coming up from the ground 6 exceeds the water level in the channel. 7 MR. CURRIE: What you are suggesting 8 to me is that you are of the position that even 9 though you have created this additional source of 10 contact, not you personally but necessarily the 11 construction itself has created this second form 12 of possible contact, you have now said to us, but, 13 because you have springs in there, you have 14 hydrological pressure which really prevents that 15 contact. Is that essentially -- 16 MR. SMITH: That's not correct. The 17 contact is there. What I'm saying is it is an 18 upward gradient, flowing upward, so it would be 19 localized to the base of the channel. 20 MR. CURRIE: I see. So you are saying 21 it is not flowing down into the bedrock aquifer? 22 MR. SMITH: When there is an upward 23 gradient from the groundwater, that's correct. 24 MR. CURRIE: What happens when there 25 is no upward gradient, when you have a drought 01007 1 that may have occurred? 2 MR. SMITH: Then there is no flood and 3 there is no water in the channel. 4 MR. CURRIE: Where does the flood 5 waters come from, do they come only from Manitoba? 6 MR. SMITH: The floods on record of 7 concern, when the water level in the channel 8 exceeds the pressure in the wells -- and again I 9 remind you that we have records from day one of 10 the flood operation -- the pressures, the water 11 levels in those wells are for the most part, 12 adjacent to the floodway, are higher than the 13 water level in the floods. So that's real data. 14 MR. CURRIE: I guess the question that 15 I asked is, do the flood waters only come from 16 Manitoba? 17 MR. MORGAN: No. 18 MR. SMITH: The flood basin, as you 19 know, extends into the States. 20 MR. MORGAN: But floods usually come 21 when there is a regional wet period. 22 MR. CURRIE: A significant flood such 23 as the 1997 flood was impacted because we had 24 significant water or precipitation within the 25 region; correct? 01008 1 MR. MORGAN: Correct. 2 MR. CURRIE: But it doesn't mean that 3 you aren't seeing, in effect, the use of the 4 floodway without that additional precipitation? 5 In other words, the basin, as you have pointed 6 out, extends into the U.S. and it may well be 7 their amount of precipitation which determines the 8 amount that the floodway is used, or at least has 9 a significant impact on it? 10 MR. MORGAN: I'm not sure -- that the 11 floods can come from the U.S., yes. 12 MR. CURRIE: And in those 13 circumstances, when we have that event coming from 14 the U.S. and we use the floodway, and I wouldn't 15 say even on a drought, but even on a normal year, 16 it is possible for those conduits between the 17 channel and the upper aquifer to reverse the flow. 18 Correct? 19 MR. MORGAN: Yes, we have a whole 20 section on surface water intrusion in the EIS 21 where we have assessed this existing condition 22 with the expanded condition, so I'm -- 23 MR. CURRIE: I guess I'm confused 24 because Mr. Smith just seemed to eliminate where I 25 was going with this by simply saying that the 01009 1 hydrological pressure is such as you would never 2 reverse the flow into the aquifer, it is likely to 3 remain up and the contact will be within the 4 channel? 5 MR. MORGAN: He was talking in the 6 inactive condition when the floodway is not in 7 operation, which is most of the year, even during 8 a flood. 9 MR. CURRIE: On an active condition of 10 usage of the floodway, does that flow reverse 11 itself? 12 MR. MORGAN: Yes, we modeled that. It 13 was very much of a concern of ours. We took it 14 very seriously. We did an extensive amount of 15 work, calibrated models, did sensitivity analysis 16 and made our assessment. 17 MR. CURRIE: As a matter of fact, you 18 came to the conclusion that there was potential 19 surface water groundwater interaction out to the 20 boundaries, I guess, of your floodway, or 21 essentially to that depth, that you would see the 22 effects of surface water through the groundwater, 23 to the boundaries of your floodway; that was your 24 conclusion? 25 MR. MORGAN: We can go through this 01010 1 again and I can explain it to you. Well, 2 actually, we can explain it to you in a sensitive 3 area if you like? 4 MR. CURRIE: No, I would just like you 5 to tell me, did you come to the conclusion that 6 you had surface water come -- or appear at the 7 boundaries of your floodway in the groundwater 8 aquifer? 9 MR. MORGAN: Okay. I hope you 10 understand that all groundwater comes from surface 11 water. So in any time, that's where it comes 12 from. So what we did is we looked at a modeling 13 to determine the rate of flow of surface water 14 from the floodway into the -- not into the till, 15 and expected that in most cases along the floodway 16 it would turn back after the flood. We then 17 looked at an unrepresentative highly sensitive 18 case and said, yes, there is potential for it to 19 get into the aquifer. We then looked at rates of 20 travel and -- 21 MR. CURRIE: Are you suggesting -- 22 MR. HANDLON: Let him finish. 23 Mr. Chairman, I'm going to interject, 24 because Mr. Morgan was going through his answer 25 and it is a responsive answer, and he should be 01011 1 allowed to complete it before he is interrupted or 2 another question posed. 3 THE CHAIRMAN: I would agree. 4 MR. MORGAN: Maybe it would be easier 5 if we showed some diagrams of the surface water 6 intrusion modelling. I mean, in a sensitive area 7 we did look at this, we did have concerns. Let's 8 go through a presentation of surface water 9 intrusion, because that seems to be the concern. 10 THE CHAIRMAN: I would like to note, 11 Mr. Currie, that a lot of this was canvassed on 12 Thursday, and this explanation was covered on 13 Thursday as well. 14 MR. MORGAN: What we have shown, 15 though, is an area which may be of a concern to 16 the people in the East St. Paul area where their 17 wells are. We didn't show that example, it is the 18 EIS, and we can talk about that one also. 19 This is the regional groundwater flow, 20 and this is Birds Hill area here, and we have 21 shown this one. We did show this, we just want to 22 show it again to put people's mind frame back to 23 where we are. So what we did, next slide, is -- 24 sorry, I can't put the laser through people -- 25 what we did is, there was groundwater modeling to 01012 1 expressly look at the potential for surface water 2 intrusion at three locations along the floodway. 3 These are locations that were selected because 4 they were potentially sensitive; the Keewatin 5 bridge around Highway 59, which is the Springhill 6 area and Dunning Road. I showed the Dunning Road 7 one earlier, and I will show this Springhill area 8 also. 9 Next slide. This is the sand and 10 gravel aquifer. As we have said, this recharge 11 comes from the Birds Hill area. This higher 12 piezometric head here is from a well which would 13 be located in the carbonate aquifer, and the lower 14 one is the water table in the sand and gravel 15 aquifer. The flow goes through into the carbonate 16 aquifer, and there is upwelling here. During 17 inactive conditions, the flow is into the 18 floodway. 19 What we wanted to look at was a flood 20 condition, so what was modeled was the flood of 21 1997. 22 Next slide. Now, upon reviewing the 23 documents provided by Conestoga-Rovers, they make 24 comment about GUDI studies. And I want to just 25 explain this a little bit more. There is concern 01013 1 that the existing floodway or expansion project 2 may affect wells. The Ministry of the Environment 3 in Ontario, the MOE, has developed a terms of 4 reference for a hydrogeologic study to examine 5 groundwater sources under the direct influence of 6 surface water -- those are often called GUDI 7 studies -- for a public water supply. And the 8 appendix C of the Conestoga report has the full 9 protocols. This is done to ensure that 10 appropriate treatment is provided to the public 11 water supply. If there is evidence of direct 12 influence of surface water on groundwater, then a 13 full treatment should be done of the water supply. 14 Next slide. Now, looking at that 15 terms of reference, a critical part of a study 16 like this is to assess the hydrogeology in the 17 region of the municipal wells to assess water 18 capture zones, i.e. this is to determine where the 19 water is coming from. They give examples. They 20 say a preferred method is to use a numerical model 21 called "mod flow." This is the model that was 22 used in this case, in the EIS. 23 The assumptions, they you say should 24 submit reports which show your assumptions and 25 your sensitivity analysis. This is in the EIS and 01014 1 is documented in appendix P, engineering reports, 2 the model and the sensitivity. 3 Now there is a potential -- the 4 potential for the floodway to be within the 5 capture zone for the 1997 flood condition was 6 looked at. We did not -- I don't want to make a 7 mistake, but this is not a GUDI study, the 8 hydrogeology was based on the same principles and 9 the rigour of doing a GUDI study, but it is not. 10 Other features outside of the 11 floodway, to east of the wells -- and we will show 12 an air photo of this area so you can get a good 13 feel for what is there. But this is not a GUDI 14 study. A GUDI study is the responsibility of the 15 water supplier to understand whether they need to 16 have further treatment. But it is just saying 17 that the model used, the rigour in terms of 18 calibration and sensitivity analysis was done in 19 terms of the floodway intrusion assessment. 20 If you can put up an air photo of the 21 region which will show more specifically where the 22 modeling was done. 23 This is the region, this is the 24 floodway here, Highway 59, the Oasis Road is along 25 here, and the RM has wells in this region here 01015 1 right along the Oasis Road. Modeling study -- we 2 are just saying what we did do was only look at 3 the floodway impacts. A GUDI study would be done 4 to look at the region, so it would be more in all 5 directions looking at the potential water capture 6 from gravel pits, residences in this area here. 7 We looked at -- the model of the study that we did 8 was to look at effects at baseline conditions and 9 effects of the floodway expansion, and that was 10 done in this region here. 11 Go back to the presentation here. 12 This is in the EIS figure 5.4-4. It 13 is also in appendix P, which has the details of 14 the modeling studies. This is a 1997 flood 15 condition. This is looking east over here, west 16 over here, through the floodway. East St. Paul's 17 municipal wells are located over here. This is 18 following the flood to the furthest extent of the 19 intrusion for the calibrated model. 20 Remember, this model was calibrated so 21 that the wells located around the floodway match 22 the conditions in '97. So the wells are over 23 here, this is the furthest extent during the 24 flood. 25 Now after the flood, next slide -- 01016 1 just a second, one point. Even at the flood here, 2 the water levels in the sand and gravel aquifer 3 over here, this is the carbonate aquifer, the sand 4 and gravel and the pressure from the carbonate 5 aquifer in the East St. Paul wells and this region 6 here is higher in the floodway. There is an area 7 here where the flood is higher, but as you go 8 towards the wells the groundwater levels rise and 9 they are actually higher. But there is a point 10 for some intrusion to go from the floodway, some 11 water to go from the floodway into the till, or 12 the silty sand and into the floodway. 13 The yellow part is -- next slide 14 please, I will show you one thing. This water 15 here in this location where it is sloping down is 16 flowing this way, even though this water is 17 flowing that way. 18 Next slide. When the flood is 19 finished, flood waters go down, next, and at that 20 point this yellow water here is recaptured back in 21 the floodway. The pressure from here flows back 22 up, the water is recaptured back in the floodway. 23 So the water does not continue moving on to an 24 area where it can effect the wells. 25 Next slide. This pink area, as it 01017 1 said down here, the water is not captured within 2 the floodway within one year. Some of it does go 3 back, but not all of it. And we will talk a bit 4 more about the analysis done to some of this water 5 even in an unrepresentative case. 6 Next slide. This is what the 7 sensitivity analysis -- as we talked about 8 earlier, the calibrated model, this is what you 9 expect to happen. You do sensitivity analysis to 10 understand what areas should we continue on with 11 further monitoring in case there is something 12 unrepresentative? Sort of, it is a sort of the 13 belt and suspenders, we don't know what we are 14 doing in terms of calibration, but we are going to 15 make sure by monitoring if we find it is 16 potentially a sensitive area. 17 So in this case, the unrepresentative 18 case, the silty till in this area is replaced by, 19 soon to be replaced by sand. So in this case the 20 extent of the intrusion would be further. The 21 flow though of this condition is still going this 22 way. That's why even though you do a very highly 23 unrepresentative low permeability sanding here, 24 water does not flow up hill, it still only goes so 25 far and then it will return. 01018 1 Next slide. So after the flood, this 2 water here will return to the floodway. Some of 3 this will go back in, but it could take longer 4 than a year. Some of this could move to the west. 5 This is where -- this is what we agree upon. 6 Next slide. But this is a potential, 7 remember, this is an unrepresentative condition. 8 On the east side, just to clarify, these wells are 9 up gradient, the floodway is not influencing these 10 wells even during a major flood such as 1997. On 11 the west side, even for unrepresentative cases, 12 the travel times are expected to be long. 13 Now the project in this area is 14 widening, but as we have presented in evidence 15 last week, and I haven't got it here, there is 16 going to be a clay cutoff wall put in on that east 17 side. That is done to keep the water levels up 18 higher on the -- the groundwater levels higher on 19 the east side, and that will maintain the same 20 sort of resistance between the floodway and the 21 wells. 22 Another thing, when you widen the 23 floodway for the same flood of 1997, the water 24 levels in the floodway would be about one metre 25 lower, so there would be less pressure pushing it 01019 1 towards the east. So the project is not expected 2 to significantly affect well quality, the project, 3 the expansion project. 4 Next slide. This was done at the 5 sensitive areas, CPR Keewatin Bridge, as I said, 6 the Springhill area and Dunning Road which we 7 talked about earlier. And the key there, as we 8 showed earlier, the flow generally is from east to 9 west, so the area of concern where we are looking 10 at more monitoring wells, but we did look at this 11 local area model. 12 Next slide. This is the Dunning Road 13 one we showed earlier. In the Dunning Road the 14 expected case is you will widen a bit, they don't 15 show it here but it will be a little lower. You 16 will get no more vertical intrusion. You will get 17 a little bit of expanded contact here I guess you 18 could say with the groundwater, although after the 19 flood it goes back. So that was just a reminder 20 of what we went through last time. 21 Next slide. The travel times to the 22 west of the right-of-way were estimated. This 23 information is selected from appendix P, the table 24 is annex C. At Springhill Oasis Road -- for the 25 expected case in all of these ones, the 01020 1 groundwater -- Springhill is different than the 2 other two. The other two it is all expected to 3 return to the channel within a year. At 4 Springhill it may take more than a year to return, 5 after a 1997 flood, which is a one in 100 year 6 flood. 7 So we also looked at the unrepresented 8 sensitivity case. In that case, going west of the 9 right-of-way at Springhill, it would take greater 10 than ten years to get to the right-of-way. You 11 will recall those GUDI studies that we talked 12 about earlier. When they look at that they are 13 looking at wells in Ontario and they say you 14 should have at least 50 days travel time to your 15 municipal well. So in these cases it is much 16 higher. 450 days -- and this is the 17 unrepresented, I keep reminding myself and 18 everybody, this is potential but not expected -- 19 450 days at Dunning Road and 145 days at CPR. 20 And the comments, these are areas that 21 we said continue monitoring in all of these 22 sensitive areas. 23 THE CHAIRMAN: Thank you, Dr. Morgan. 24 That's an appropriate place to take a break. We 25 will break for 15 minutes, and come back at 10 to 01021 1 sharp. 2 (Proceedings recessed at 10:30 a.m. 3 and reconvened at 10:50 a.m.) 4 5 THE CHAIRMAN: Order, please. People, 6 please take your seats quickly, please. 7 Mr. Currie. 8 MR. CURRIE: Mr. Chairman, before I 9 start again, I noted that you had made a comment 10 midway through that this stuff had been covered on 11 Thursday. There is two things that I'd like to 12 ask the Commission to consider. The first is 13 that, one, we're in this community and this 14 information, while it's readily available on the 15 transcripts for us professionals and we realize 16 it, this community wants to hear and see what 17 actually is going on in that channelized floodway. 18 So that's the first thing, that it's a little 19 broader and perhaps a little overlapped may not 20 hurt. 21 Secondly, I'm going to submit that 22 it's not necessarily me who is going into the 23 Thursday presentation. I may be asking questions, 24 but the Floodway Authority is taking every 25 opportunity they can to restate their case in a 01022 1 much more broader context than the question I 2 asked. And I'm going to submit that those are two 3 things that I don't want saddled, if you will, on 4 my questioning doorstep. 5 THE CHAIRMAN: I won't comment on your 6 second point, Mr. Currie. On your first point, I 7 agree that there is a great amount of value in 8 recanvassing some of this area for the benefit of 9 the local citizens. So I will allow you some 10 latitude. 11 MR. CURRIE: Thank you. 12 We have heard a lot about your change 13 in design from considering any deepening to more 14 of a process of widening. And you pretty much 15 stated, I guess, that there will be no deepening. 16 I'm just wondering, with what certainty can you 17 provide the residents of this community and 18 perhaps the participant municipalities that there 19 will be no deepening? 20 MR. MCNEIL: Mr. Chair, as I mentioned 21 earlier, the design to increase the capacity of 22 the channel was an evolutionary process. We 23 started out at 2 metres, up to 2 metres deepening 24 when we submitted the concept design with the 25 original environmental licence. As Mr. Morgan had 01023 1 indicated, through public consultation and because 2 of the overriding concern of groundwater, we 3 jumped to the step of no more than 2 feet or 0.5 4 or 0.6 metres at select locations. And we had 5 publicly announced last week at the beginning of 6 the hearings that we will not be deepening to 7 increase the capacity of the channel and we stand 8 firm on that. 9 MR. CURRIE: I have read in your EIS 10 that if design and construction require it, you 11 would in fact consider deepening at that point? 12 MR. MCNEIL: The EIS was drafted in 13 July and submitted on August 3, 2004, and so 14 that's old news. 15 MR. CURRIE: I understand it's old 16 news, but the principle still stands today, if 17 design and construction require it, you will 18 deepen? 19 MR. MCNEIL: We are confident, and 20 that's why we made the announcement, that we will 21 not be deepening. 22 MR. CURRIE: Now, by widening the 23 channel, I suppose it might be somewhat semantics 24 to say that you're not also deepening some of the 25 channel in the sense that you are taking the 01024 1 channel walls and removing that dirt or 2 construction to the floor of the existing 3 floodway. Is that correct? 4 MR. MORGAN: You can point me to the 5 diagram of the widening that you make your point 6 on. Could you clarify where you think deepening 7 is occurring? 8 MR. CURRIE: Sure. I take it this is 9 the widened channel; correct? 10 MR. MCNEIL: That's correct. 11 MR. CURRIE: And I take it that the 12 area that we see, I guess where the arrow 13 starts -- yes, right there. 14 MR. HANDLON: For the purpose of the 15 record, maybe the witness or counsel can just 16 direct everyone to the slide that's on the screen 17 so that we have a record of what's being referred 18 to. 19 THE CHAIRMAN: Thank you. 20 MR. REMPEL: This slide was taken from 21 Mr. McNeil's presentation I believe on Tuesday of 22 last week. I don't have a slide number, but it's 23 in Mr. McNeil's presentation. And this particular 24 slide shows the manner in which is proposed to 25 enlarge the channel. 01025 1 MR. CURRIE: Which I'm given to 2 understand is actually this part right in here; am 3 I correct? 4 MR. REMPEL: Yes. The purple areas in 5 the cross section of the channel are conceptually, 6 the concepts are shown of widening the channel to 7 achieve the additional capacity instead of 8 enlarging it by going down. 9 MR. CURRIE: Yeah. In effect, you're 10 taking the channel itself and lowering it to this 11 bottom portion. That is a corner of the channel, 12 correct? 13 MR. REMPEL: There will be excavation 14 at the edges of the existing channel to make it 15 larger, wider, yes. 16 MR. CURRIE: And it may be semantics 17 but, in essence, as it relates to this portion 18 right here, you are deepening the channel? 19 THE CHAIRMAN: I think you are 20 correct, Mr. Currie, that it is semantics. I 21 think the point of concern here is whether or not 22 they are deepening the floor of the channel. 23 MR. CURRIE: Well, that may be one 24 aspect of it, Mr. Chairman, but there may be other 25 aspects that I'd like to explore such as, for 01026 1 example, have you now created a greater surface 2 exposure at the bottom? 3 THE CHAIRMAN: I think that that's a 4 valid point. But to sort of couch it in the 5 language of deepening, I don't see where that 6 leads us. 7 MR. CURRIE: Okay, fair game. 8 MR. MCNEIL: Mr. Chair, just for 9 clarification, the line shown here is prairie, so 10 prairie is to go all the way across here. 11 THE CHAIRMAN: By prairie you mean 12 ground level, normal ground level? 13 MR. MCNEIL: Normal ground level, and 14 this is the existing spoil pile from the original 15 excavation, and from the widening excavation, we 16 will take that spoil material and place it behind 17 and/or on top of the existing spoil piles. And 18 now Mr. Smith would like to explain the 19 differences between widening and deepening with 20 excavation, in trying to help answer Mr. Currie's 21 question. 22 MR. SMITH: Mr. Currie, I may just add 23 to that that the bottom of the main channel slopes 24 at a 1 to 20 horizontal. In other words, it's 25 sloping upward as we move outward from the 01027 1 centre -- sorry, correction, 1 to 50. So for 2 every foot you go up vertically, you move over 3 50 feet horizontally. So there is an up slope 4 throughout that. So as we widen that channel and 5 remove the side slopes of existing channel, we are 6 actually going up slope as well, so increasing the 7 thickness of cover over the aquifer. 8 MR. CURRIE: Are you suggesting that 9 at this portion of the floodway that you are, in 10 fact, increasing the thickness between the aquifer 11 and the existing floodway? Is that what your 12 position is or did I misunderstand? 13 MR. SMITH: Relative to the existing 14 floodway base, as you widen and move outward, 15 there will be an increasing thickness. So we're 16 not making it any worse in that respect. 17 MR. CURRIE: Can you assure us that, 18 given that you have seemed to take in your 19 baseline of the bedrock as being pretty level 20 there, that it is in fact, it is going to be 21 consistent from one side to the other? 22 MR. SMITH: No, our baseline is based 23 on actual drilling, so we defined the bedrock as 24 it was in the -- 25 MR. CURRIE: As it existed? 01028 1 MR. SMITH: -- existed at the sites 2 analyzed. 3 MR. CURRIE: I was wondering what part 4 of the report, as it relates to microbiology, what 5 part of the report explains at this point the type 6 and extent of microbes and other organisms that 7 might be found within the floodway waters that are 8 travelling down the floodway? 9 MR. REMPEL: You're asking about the 10 water quality characteristics of the water in the 11 floodway when it's operational? 12 MR. CURRIE: Correct. 13 MR. REMPEL: We'll take a minute and 14 find the appropriate spot in the EIS. 15 MR. SMITH: That would be in appendix 16 M. 17 MR. CURRIE: Yes. 18 MR. SMITH: We have data on the 19 coliform monitoring in the river water. 20 MR. CURRIE: Is that the extent of it 21 was the coliform content? 22 MS. FRIEDMAN-HAMM: In the report on 23 figure E.4.3 is the graph of the coliform content 24 of the Red River at the south gate of the floodway 25 from 1978 to 1985. This is data from the 01029 1 provincial database from Water Stewardship. 2 MR. MORGAN: Just to clarify, coliform 3 bacteria is an indicator of other bacteria. We 4 are in no way saying that's the only one there. 5 We are using it as an indicator that there is 6 bacteria of a variety of forms in the flood 7 waters. 8 MR. CURRIE: And am I given to 9 understand that the information you relied on, 10 given Ms. Friedman's comments, that that was from 11 '78 to '85; is that correct, or did I 12 misunderstand you? 13 MR. SMITH: Just to clarify, what did 14 you mean by information we relied on? 15 MR. CURRIE: Well, I had understood 16 her to say that there was coliform monitoring in 17 the floodway, and that there was data that you had 18 under E.4.3 that stated you had, that there had 19 been collection of provincial data from '78 to 20 '85. 21 MR. SMITH: That's correct, but what 22 is your reference -- 23 THE CHAIRMAN: That was his question. 24 MR. CURRIE: Yes, that was just 25 essentially my question. 01030 1 MR. SMITH: I just wanted to clarify, 2 data we relied on for what? 3 MR. CURRIE: For determining the 4 content of microbes in that floodway? 5 MR. MORGAN: I guess that was part of 6 it, but also we do acknowledge in the EIS, page 7 519, that there is wastewater and land drainage 8 discharged to the floodway, although it's expected 9 that any wastewater discharges would be required 10 to comply to the applicable regulations. But we 11 do again acknowledge bacteria in surface water, 12 hence the assessments we did. 13 MR. CURRIE: From 1985 to the year 14 2005, are there other microbes evolving as we 15 speak today, i.e. from '85 to 2005 there are other 16 microbes that actually have come into existence? 17 MR. MORGAN: Not that I know of. 18 MR. CURRIE: No? You would 19 disagree -- 20 MR. MORGAN: But everything is 21 evolving all the time, I'm not sure what you're -- 22 MR. CURRIE: Well, I'm just talking 23 about generally. We've got 1985 data, and you're 24 talking about coliform content, and the extent of 25 that is that you are able to tell us that there is 01031 1 microbes in the water. That's what you're telling 2 us? 3 MR. MORGAN: Yes, there is microbes in 4 the water. 5 MR. CURRIE: You cannot tell me what 6 microbes beyond the coliform content? 7 MR. MORGAN: The coliform is an 8 indicator commonly used in water treatment and 9 water assessments to indicate that there is 10 bacteria. It is not common practice to do a 11 complete inventory of all potential bacteria in 12 waters, even when you're doing a water supply or 13 water treatment work. 14 THE CHAIRMAN: Perhaps I might 15 interject here. We're just looking at this graph 16 at the table. Is there similar data available 17 post 1985? 18 MR. MORGAN: There is data in the Red 19 River continuously taken at the inlet at Selkirk. 20 There is data taken throughout the City of 21 Winnipeg, mostly it's on coliforms, e.coli, total 22 coliforms, fecal coliforms. 23 THE CHAIRMAN: Now, you have these 24 half a dozen years covered on this graph in the 25 '70s and early '80s. Did you not feel it was 01032 1 necessary or advisable to -- 2 MR. MORGAN: We don't see that the 3 floodway is adding any more coliforms in the 4 pathway. In the water quality, we focused on 5 things which have potential to be added to the 6 floodway by the project. We do acknowledge that 7 there is coliforms in the water. It should be 8 treated as there is coliforms bacteria, therefore, 9 we did the analysis that I showed earlier, as you 10 would do for potential GUDI or whatever, that type 11 of thing. 12 THE CHAIRMAN: Thank you. 13 MR. REMPEL: I'd just like to add, 14 there is a database, as Dr. Morgan indicated, 15 upstream of the channel inlet which covers the 16 period post '85, and it would give water quality 17 the characteristics such as suspended solids, 18 nutrients, and on the bacterial side it would have 19 fecal coliform which is an indicator of 20 contamination. And we certainly would expect 21 during a flood that the surface water would have 22 high levels of fecal coliform indicating some 23 contamination from feed lots, lagoons, whatever. 24 MR. CURRIE: Right. I guess the 25 chairman got exactly where I was going, which was 01033 1 the prudence of relying on '85 data to the year 2 2005. And now, while he's prepared to accept the 3 answer that you've given him, I am just not in 4 this sense, that you've got evolving conditions 5 from '85 to 2005, you've got more hog farms 6 downstream from you, you've got more development 7 downstream from you. Would you disagree with me 8 on either one of those premises, that from '85 to 9 2005, that we've seen more development? 10 MR. REMPEL: Certainly there's been 11 more development. Did you say hog farms 12 downstream of the project? 13 MR. CURRIE: Well, yes -- well, 14 downstream of your project, or upstream rather -- 15 sorry, my apologies, you're right, upstream. 16 MR. REMPEL: Certainly there's been 17 developments both upstream and downstream and in 18 the floodway area itself. But if you are looking 19 for that database, we can provide that surface 20 water quality database updated to current 21 conditions in terms of -- it's an easy thing to 22 access database and provide you with that 23 information, if that's useful. 24 MR. CURRIE: I was wondering why we 25 don't have it. That's what I'm wondering. I 01034 1 mean, it's readily accessible. It tells us 2 information, puts a community at rest. 3 MR. REMPEL: Well, we would not expect 4 that the expansion project would change the 5 characteristics of the flood waters going down the 6 Red River or the floodway itself. We just didn't 7 see it as a pathway, a vector of the expansion of 8 the project, of the floodway. 9 MR. CURRIE: And that, sir, may be 10 where there's a big problem, and maybe it's a 11 misunderstanding and maybe it's just our 12 perception. But it appears that you have 13 essentially taken that portion and deemed it a 14 non-issue by virtue of having said, we didn't 15 think the expansion of the floodway will have any 16 effect on the contents of the Red River. I agree 17 with you, it will not have any effect on the 18 contents of the river. However, reverse it a bit. 19 You have now more water going through that 20 floodway, and the contents are different. You are 21 raising the level. 22 THE CHAIRMAN: Mr. Currie, you're 23 getting into a debate here, and you'll have plenty 24 of time to make debate and argument later on in 25 these hearings. Please restrict yourself to 01035 1 questioning at this point. 2 MR. CURRIE: Thank you, Mr. Chairman. 3 My question is, are you going to put more content 4 of water through that floodway? 5 MR. REMPEL: During severe flood 6 events, there will be more water flowing down the 7 floodway. 8 MR. CURRIE: Yes. And as part of 9 that, when we put more water down the floodway, is 10 that not part of an analysis of accumulative 11 effects? That is, that you have more water going 12 down the floodway and, therefore, something you 13 should analyze what is going on there? 14 MR. REMPEL: And we have done that. 15 MR. MORGAN: We have done that. 16 MR. CURRIE: But you didn't feel the 17 database had any value to you, that is the '85 to 18 2005. 19 MR. MORGAN: It wasn't required in 20 order to do the effects assessment. As we showed 21 earlier, we did assume that there would be 22 bacteria in the water and we did thorough 23 hydrogeological assessments. 24 MR. CURRIE: What I'm given to 25 understand is that as this project evolves there 01036 1 are still design and construction changes that may 2 occur; am I correct on that? 3 MR. REMPEL: The design is evolving. 4 It is common practice in designing engineering 5 projects to do a conceptual design, proceeding to 6 a more detailed design. And details do evolve, 7 even during the tendering process when the final 8 documents are issued for contractors to bid on. 9 MR. CURRIE: And at that point in 10 time, my understanding is that when we get to the 11 detailed design phase, the MFA has some 12 anticipation to have public input. Am I correct 13 on that or have I missed the point? 14 MR. REMPEL: The Authority has 15 indicated it will have ongoing public involvement. 16 I'm not sure if the design details will change 17 sufficient that the design will be a major element 18 of that involvement, but certainly the Authority 19 will be open to discussing details of bridge 20 closures, details of piling, when it will occur, 21 that kind of thing. 22 MR. CURRIE: I follow that, but my 23 question is this: Does the MFA have a plan that 24 they can present to the Commission to have them 25 assess whether the public input is going to be 01037 1 meaningful in the sense of how you are going to do 2 it? 3 MR. MCNEIL: First of all, over the 4 last 14 months, we've had significant public 5 consultation on the predesign and hence the 6 widening rather than deepening. And we've also 7 committed to future consultation as we go through 8 this project, specifically during construction. 9 With respect to road access, we have committed to 10 continuous access across each of the crossings 11 except maybe at Highway 44, but all the other 12 roads will be accessible across the floodway 13 during construction. 14 If there is any change from that, then 15 yes, we would expect to have public consultation, 16 any changes from the design that is now on the 17 table. 18 MR. CURRIE: I guess my question is, 19 do you have any plans that you put forward in your 20 proposal as to how you are going to hold your 21 public consultations, how are the public going to 22 respond, and are you obliged to hold them? 23 MR. MCNEIL: I think as managers of 24 this project, it's just good, a good approach to 25 keep the public involved. And although we don't 01038 1 have it written down anywhere specifically how 2 we're going to go forward from here, we have 3 indicated it will be more of the same which has 4 occurred in the past, and that's a commitment that 5 we are making. 6 MR. MORGAN: I can give an example of 7 I guess a commitment made in the EIS by MFEA under 8 groundwater mitigation specifically. There is 9 discussion about dewatering at the bridges and 10 that there's potential for short-term effects from 11 the dewatering. And there's a commitment made to 12 mitigate this. However, on page 5-19, they have 13 outlined the groundwater mitigation policy. And 14 in it they say that the examples of mitigation 15 include lowering of pumps and individual wells, 16 deepening existing wells, installing new wells. 17 This is if they are unable to stop the effect by a 18 number of other mitigation activities described 19 later. But the affected property owners are to be 20 involved in determining the mitigation and MFEA is 21 open to suggestions on mitigation alternatives. 22 MR. CURRIE: While I'm thinking of it, 23 on your drawing regarding the influence of water, 24 surface water on your model, remember the model 25 you put on the screen? Yes? 01039 1 MR. MORGAN: Well, that's a 2 representation of the model. 3 MR. CURRIE: At Oasis Road. 4 MR. MORGAN: Yes. 5 MR. CURRIE: While I'm there, you put 6 on a circle indicating the East St. Paul wells, 7 correct? 8 MR. MORGAN: Yeah, there was East St. 9 Paul wells that were marked to the east of the 10 floodway. 11 MR. CURRIE: Yeah. In your model 12 diagram, can you show me where the draw down cone 13 from the wells appears? 14 MR. SMITH: Maybe I can comment on 15 that, Mr. Currie. The water level at J006, which 16 is the provincial well adjacent to the municipal 17 wells, represented shall we say the net effects of 18 pumping at those wells. Actually at the time of 19 this, there was only two wells operating of the 20 municipal wells. So we recognize there will be 21 local draw down cones. You're dealing with a very 22 pervious sand and gravel aquifer drawing with flow 23 coming from up gradient. We don't show a local 24 depression there but clearly there will be. 25 Now, those wells are operated on and 01040 1 off. There is a very limited zone from the, I 2 guess the static level to where the pumps are set, 3 so they are cycled quite frequently back and forth 4 between them. 5 And then as I said, the J6 represents 6 the average impact of those over ongoing, as they 7 flip back and forth, I don't know if it's on an 8 hourly basis or something in that order. 9 MR. CURRIE: I guess my question still 10 remains; your model, at least on this diagram, 11 doesn't show a draw down cone? 12 MR. SMITH: There is no monitoring of 13 that draw down cone by the RM. 14 MR. CURRIE: I understand. 15 MR. SMITH: So we monitor the closest 16 well and that's what we show there. So it doesn't 17 show, you know, that's what we get. We've got a 18 continuous monitoring right through that period 19 and that's the level that we had. 20 MR. CURRIE: And do you -- 21 MR. SMITH: So the draw down cone 22 would be very localized around the immediate dam 23 or to the well. These municipal wells are, I 24 don't know, 400 or 500 metres probably from the 25 floodway at the point of entry and, you know, 01041 1 local draw down cone when they are operating 2 cycling on and off would be significantly less 3 than that as a radius. 4 MR. CURRIE: Yes, but let's take that 5 position further. That does change your modeling 6 somewhat, at least as to the local conditions for 7 that well? That is that that draw down cone does 8 change the gradient at the local site of the well; 9 correct? 10 MR. SMITH: Very locally, yes, for a 11 short time. As soon as the pumps turn off, it 12 fills back, recovers. 13 MR. CURRIE: And Mr. Smith, you are 14 quite certain that those pumps turn off and on? 15 MR. SMITH: Well, they have a high 16 level, low level float control, so that's why they 17 have got four in a row because one individual well 18 cannot supply the required water, so therefore 19 that's the mode of operation as they do cycle back 20 and forth. At least that's as we understood based 21 on discussions with the RM of East St. Paul, but 22 we actually have data on the operation of those 23 wells. 24 MR. CURRIE: In your EIS, can you 25 point me to the section which shows us the amount 01042 1 of anticipated or future development in any of the 2 three municipalities? 3 MR. J. OSLER: Mr. Currie, perhaps I 4 can help you. It's discussed in the future trends 5 and planning for residential land use, the section 6 of the EIS is found on page 8-22. 7 MR. CURRIE: Yes. 8 MR. J. OSLER: It has a brief 9 discussion on anticipated future trends and 10 planning based on discussions that the EA study 11 team had with municipalities in the region. It 12 does not provide detailed analysis of what those 13 forecasted anticipated future development trends 14 are. It does point out things such as within the 15 RM of St. Andrews that there is noted plans for 16 housing projects in the southern part of the RM; 17 or in the RM of East St. Paul it's indicated that 18 residential development was very important to the 19 municipality, and that growth of about a hundred 20 homes per year is a general target for the 21 municipality, if that's of any help to you. 22 MR. CURRIE: Is that the extent of the 23 information that exists regarding the amount of 24 development amongst the three municipalities, 25 within the EIS itself? 01043 1 MR. J. OSLER: I think when you go to 2 look at the environmental assessment process, 3 Dr. Morgan has talked about it in regards to 4 groundwater, the thing that we're looking for is 5 an indication of where things are going. Part of 6 our environmental assessment, particularly as it 7 relates to future resource and land use 8 requirements, has to obviously look at where 9 future land use requirements are headed. And 10 that's part of our assessment of the process. 11 But when we look at socio-economic 12 environmental effects, they do have to follow from 13 a physical pathway. Something that Dr. Morgan 14 identifies, or Mr. Smith as regards to what -- 15 where are the pathways and changes in the 16 biophysical condition? That's a definition that 17 we have to work with under CEAA, our Environmental 18 Assessment Act. 19 So once we have determined that there 20 is growth taking place, that's one thing. The 21 effect that this project has on that is the thing 22 that we are considering. And I think in looking 23 at that reference on page 822 in chapter 8, we are 24 looking for an indication of where growth is, what 25 are the land use requirements, what are the 01044 1 current planning studies that are being 2 undertaken? But really when we're looking at 3 effects and a determination of the significance of 4 those effects, it has to follow from what does 5 this project, the Floodway Expansion Project, what 6 does it result in, where is the pathway, where is 7 the linkage and changes in biophysical 8 environment, and then associated changes in the 9 socio-economic environment? 10 MR. CURRIE: I appreciate that I've 11 heard that argument, read it many times in your 12 transcripts. I understand your point, which is 13 that you've got an existing baseline and how does 14 this new project affect the existing baseline. 15 That's essentially it. Am I correct on that? 16 That's the only analysis that you really want to 17 get through is what does this project specifically 18 affect your baseline, or have I misunderstood 19 that? 20 MR. MORGAN: It's not done in 21 isolation of current or future or past effects 22 outside the project. For example, we have talked 23 about that, if you read our transcripts from last 24 week, that we took the groundwater concerns that 25 are in this region very seriously, and for that 01045 1 reason we went to a number of steps in order to 2 have no effect. We have talked about the no 3 deepening earlier. We talked about last week in 4 this region that we had up earlier a mitigation 5 was to put a clay cutoff wall between the 6 expansion and the wells in order to have no effect 7 on water levels. We do not do assessments on 8 future projects, though, in isolation. You know, 9 it's not an assessment of a future project that 10 East St. Paul may have to withdraw water later in 11 the future. 12 MR. CURRIE: I guess I'm not asking 13 you in the sense of are you going to do an 14 assessment on some future project? I am just 15 going to ask you, do you know all the projects on 16 the horizon? Not the assessments of those 17 projects, but do you know what they are? 18 MR. REMPEL: No, we do not know all 19 the projects that might be coming forward, but we 20 have an obligation to see what is reasonably 21 foreseeable in terms of development activities, 22 and to test whether this expansion project will 23 interact with those activities. 24 MR. CURRIE: Okay. And what can you 25 tell me about the RM of Springfield and 01046 1 development within the RM of Springfield 2 particularly, let's just start with residential? 3 MR. REMPEL: In terms of development 4 in Springfield, we would ask how could this 5 Floodway Expansion Project interact with 6 residential development? And we did not see that 7 it had a pathway to affect that. 8 MR. CURRIE: Okay. So that's a fair 9 answer, is that you simply didn't see it as a 10 significant component that is impacted by your 11 expansion project? 12 MR. REMPEL: We did not see a linkage 13 between the expansion project and residential 14 development. 15 MR. CURRIE: And any other development 16 in the municipality, or for sure residential? 17 MR. REMPEL: Well, other developments, 18 we understand that service drainage was an issue 19 and that some stakeholders were interested in 20 assuring greater capacity in the future for 21 accelerated surface drainage. And the authority 22 has responded by increasing the capacity, or 23 intends to increase the capacity of some of the 24 structures allowing entry of surface water into 25 the floodway. 01047 1 MR. CURRIE: Dr. Webster carried this 2 line of questioning with you, basically, and I 3 think he had kept it significantly to those wells 4 adjacent to the floodway. And in particular, he 5 was asking you, if I recall correctly, what was 6 your baseline analysis at the floodway? Do you 7 recall those questions? I can pull them out of 8 the transcript and we can go through them again. 9 But, effectively, he has already asked you many of 10 those questions. Do you recall those questions at 11 all regarding the baseline and your establishing 12 it? 13 MR. REMPEL: This is with respect to 14 groundwater? 15 MR. CURRIE: Yes, with respect to 16 groundwater. 17 MR. REMPEL: I remember a line of 18 questioning, but I can't recall the specific 19 questions at this point. 20 MR. CURRIE: Okay. 21 THE CHAIRMAN: It's on record. The 22 questions and answers from Dr. Webster. I mean, 23 do we need to revisit it again? 24 MR. CURRIE: Well, Mr. Chairman, as 25 long as they don't tell me they don't understand 01048 1 what I'm talking about, then I wouldn't have a 2 problem to revisit it. But, essentially, it's 3 incumbent upon me to make sure that I'm clear that 4 I'm not misleading on the record, that I have 5 accurate -- that I have put accurate information 6 to them. So I don't necessarily need to go 7 through it in detail but, certainly -- I'll start 8 off and head off my questioning. And if we get 9 objected to, then we can decide what we have to do 10 at that point. How is that? 11 THE CHAIRMAN: Okay. 12 MR. CURRIE: As I understood his line 13 of questioning, it was essentially saying it would 14 be prudent to have a fairly well-established 15 baseline of infiltration because once that event 16 occurs and people start coming forward, how are we 17 to know whether it was the operation of the 18 floodway, the expansion of the floodway or just 19 normal conditions? Do you recall those kinds of 20 questions? Yes? 21 MR. MORGAN: Yes. 22 MR. CURRIE: And I guess that that's 23 essentially where I am going with my whole line of 24 questioning. We have folks who have to come 25 forward and at some point in time, I suppose, 01049 1 prove that this expansion project had some effect 2 on them. They just can't come forward and say, oh 3 no, my well is now contaminated. I doubt that 4 that's a position that you would readily accept. 5 You'd have to have some proof, correct? You'd 6 want to know that it came from the floodway? Yes? 7 No? 8 MR. MORGAN: I'm not answering for the 9 floodway, but I guess you'd want to know if there 10 is any kind of proof, or what's the reason they 11 think so? 12 MR. CURRIE: Right. 13 MR. REMPEL: There is a process to 14 that. When a person has a problem or suspects 15 that there's an issue with a well, I believe it's 16 the Manitoba Stewardship branch, the water, Office 17 of Drinking Water will investigate and advise the 18 owner. And typically if there is an issue, the 19 source of that contamination is pursued. And 20 certainly if the floodway was involved in that 21 contamination, I think Mr. McNeil has indicated 22 they would mitigate it. 23 MR. CURRIE: I understand that. But 24 if you don't take a very solid baseline, that is 25 make sure we know where we're starting from, would 01050 1 you not agree with me that you have put those 2 folks in a horrible position of having to prove 3 something, having to prove that now the floodway 4 has done this? 5 MR. SMITH: Mr. Currie, we have 6 established baseline, as we discussed, on 25 of 7 the public wells along the floodway at select 8 locations, and we are intending to continue 9 monitoring those wells, and as we indicated 10 earlier, establish additional points to build on 11 that baseline. 12 MR. CURRIE: In our submission, we 13 supplied to the MFA and your various experts a 14 copy of the groundwater study done by the Selkirk 15 planning district. 16 MR. REMPEL: Was that the study done 17 by Wardrop? 18 MR. CURRIE: Correct. 19 MR. REMPEL: Yes, that was received. 20 MR. CURRIE: And in there, their 21 analysis is that there is enough water in this 22 aquifer for development for, they see until 2030 I 23 believe? 24 MR. SMITH: That's what their 25 assessment was I believe, yes. 01051 1 MR. CURRIE: Yes. And currently, as I 2 understand it, we have 1,700 imperial gallons per 3 minute of aquifer water pouring into the floodway. 4 And I appreciate you don't want to take 5 responsibility for that, it's not your 6 construction design, all the rest of it, I've 7 heard your position. But as you are widening the 8 channel, is it your position that that 9 1,700 gallons per minute can continue to flow, 10 because all you've done is widened, you don't have 11 to mitigate that problem, it can just flow; is 12 that what I'm understanding? 13 MR. MORGAN: Are you saying we -- are 14 you talking about the baseline, 1,700? 15 MR. CURRIE: Yes. 16 MR. MORGAN: We're saying to have no 17 significant adverse effect if it remains the same 18 and that's no significant adverse effect. That's 19 what we said, yes. 20 MR. CURRIE: And you have no 21 obligation to mitigate? 22 MR. MORGAN: Remediate? 23 MR. CURRIE: Well, mitigate, put up a 24 wall, just as you did, similar, a clay barrier or 25 somehow stop that flow from going into the 01052 1 floodway. 2 MR. MORGAN: In order to assess the 3 EIS adverse significant effects, we had no 4 obligation to remediate. 5 MR. CURRIE: And that's exactly what I 6 asked you. 7 MR. SMITH: However, in fact, we are 8 proposing to do some works to reduce or protect 9 against that. 10 MR. MORGAN: We are looking at things 11 like the erosion control and the infilling on the 12 low free channel which has potential. But we're 13 not trying to say it's going to significantly 14 change that baseline. 15 MR. SMITH: Maybe for further 16 clarification, Mr. Currie, the inflow relates to 17 the head to the east or upgrading to the floodway. 18 As development continues in that area, that 19 piezometric surface will be drawn down and there 20 will be less of a gradient and, you know, there's 21 opportunity for people to develop that water east 22 of the floodway and capture it. 23 MR. CURRIE: I understand your point, 24 Mr. Smith. Can you tell us today how many wells 25 are along the floodway that are going to be 01053 1 actually impacted on a flooding event? 2 MR. REMPEL: Could you clarify your 3 question? 4 MR. CURRIE: Potentially impacted I 5 suppose? 6 MR. REMPEL: Are you referring to 7 water quality now? 8 MR. CURRIE: Yes. 9 MR. MORGAN: Potentially impact? 10 MR. CURRIE: Well, let's put that even 11 in deeper terms, realistically impact. I don't 12 want you to go off on, you know, something that's 13 not realistic. Are you suggesting I guess that 14 there are no wells that are going to be impacted 15 by a flooding event? Are you suggesting 10 will 16 be? Are you suggesting 100? 17 MR. SMITH: Can you clarify impact? 18 Are you talking water levels, piezometric level or 19 quality? 20 MR. CURRIE: Quality, let's start with 21 quality. 22 MR. SMITH: Currently, there is no 23 recorded impacts by public, you know, well, or 24 rather domestic wells to our knowledge that has 25 been submitted to the province. The intent is to 01054 1 have the monitoring program and mitigation plans 2 if in fact there are local wells impacted. At 3 this stage, we can't say that there's going to be 4 10 or 20 or 30. Based on existing modelling of 5 the representative data, we would anticipate there 6 would be very few, which is consistent with what 7 we've seen already from the operation of the 8 floodway since 1970. 9 MR. CURRIE: I guess that's the 10 question. What is very few? 11 MR. SMITH: Well, there's been none. 12 I mean, you can't rule out, as you said yourself 13 you don't want to say absolutely and positively 14 there shall be no wells ever effected to the 15 fullness of time. That's not a realistic comment 16 to make. That's why, as I say, there's a need for 17 monitoring and a mitigation plan. But, again, 18 based on our representative modeling, we don't see 19 migration of any extent beyond the floodway 20 right-of-way. 21 MR. CURRIE: With regard to the 22 conclusions that you draw about significant 23 effects, I take it that the EIS makes judgments, 24 or professional judgments based on your 25 experience, as to what the likelihood of adverse 01055 1 effects might be. Am I correct on that? 2 MR. REMPEL: Yes. We actually spent 3 quite a bit of time in our presentation on the 4 first day commenting on how we treated likelihood, 5 how we assessed an effect as to whether it's 6 adverse or not, and the judgments as to 7 significance. 8 MR. CURRIE: And in effect, it's the 9 professional team's personal judgment that it's 10 significant or insignificant; correct? 11 MR. REMPEL: There is judgment 12 involved, but we do get guidance from the 13 guidelines in terms of how to draw that judgment. 14 And there are practitioner guides put out by the 15 Canadian Environmental Assessment Agency that give 16 general guidance in that sense. And we spent a 17 number of pages certainly dealing with how we 18 treated or judged significance in terms of 19 duration, magnitude, frequency, et cetera. And we 20 discussed that in section 2, I believe it is, of 21 the EIS for both biophysical and socio-economic 22 effects. 23 MR. CURRIE: And when you're 24 exercising the personal judgment on these effects, 25 you are looking at, as I understand it, the nature 01056 1 of the effect? 2 MR. REMPEL: Certainly. 3 MR. CURRIE: The duration of the 4 effect? 5 MR. REMPEL: Um-hum. 6 MR. CURRIE: And the magnitude o