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2017-05-24_REVISION - C1981041
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2017-05-24_REVISION - C1981041
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Last modified
11/1/2022 8:34:56 PM
Creation date
11/1/2022 8:14:59 AM
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DRMS Permit Index
Permit No
C1981041
IBM Index Class Name
Revision
Doc Date
5/24/2017
Doc Name
MLRB Hearing Transcripts
Type & Sequence
TR69
Email Name
JDM
Media Type
D
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No
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101 <br /> 1 Palisade, Colorado. 1 looking at the bulk resistivity distribution, you <br /> 2 Q. What was your role in the preparation 2 can make an estimate of the geology of the <br /> 3 of the first report marked Exhibit A-29? 3 substance. <br /> 4 A. From the beginning I was responsible 4 Q. Okay. You said a little while ago <br /> 5 for developing the program to do the exploration 5 that you didn't do the actual data collection? <br /> 6 survey to meet the objectives of Huddleston- 6 A. Physically, no, I did not. <br /> 7 Berry/Snowcap. I also -- I did not collect the 7 Q. Okay. Is that a general -- how do I <br /> 8 data, but I did analyze the data, and-- through 8 describe it? Do you normally rely upon data <br /> 9 using a series of commercial, state-of-the-art 9 collected by other professionals within your <br /> 10 programs. At the completion of the data analysis, 1 10 organization? <br /> 11 wrote the report that is presented here. 11 A. Yes. <br /> 12 Q. Okay. Why don't we go ahead and 12 Q. Okay. <br /> 13 review that first report, and you've already 13 A. At this point in my career, yes. <br /> 14 answered a number of my questions. 14 Q. Okay. I understand. Would you be <br /> 15 Why don't you first start by 15 able to tell the Board the names and titles of those <br /> 16 summarizing the objective of the initial 16 individuals within Fugro who did take care of <br /> 17 investigation in the exhibit marked A-29, being your 17 that? <br /> 18 April 28, 2016, report? 18 A. Yeah. In this particular — the <br /> 19 A. We were approached in trying to 19 first survey is was Jim Pfeiffer and Lincoln Steele <br /> 20 identify if there were any physical pathways from i20 who did the field work. Do you want to discuss the <br /> 21 the surface to a coal mine at depth at the site -- 21 second one too? <br /> 22 at the Snowcap mine site, Palisade, Colorado. 22 Q. Why don't we just go ahead and focus <br /> 23 It was requested, is there any 23 on the first report. <br /> 24 geophysical methods that may be useful in 24 A. Okay. <br /> 25 identifying these pathways. We went through several 25 Q. Why don't we turn to Figure 2 of this <br /> 101 103 <br /> 1 discussions on this particular scope that was 1 work. I think we've already had a lot of discussion <br /> 2 required. 2 regarding the site and the location and the <br /> 3 We recamenbed using an ERT survey, 3 Fontanari trench. <br /> 4 which is an electrical resistivity tomography 4 What does Figure 2 represent? <br /> 5 survey, in which we lay out a surface array of 5 A. Figure 2 shows the lines which we <br /> 6 electrodes, inject current into the ground, and from 6 acquired data -- the M data along. <br /> 7 the feedback are able to make evaluations of the 7 Q. And were you here for the testimony <br /> 8 distributions of the electrical resistivity of the 8 of Mr. Stark and Mr. Boulay earlier? <br /> 9 sub -- changes along the line both vertically and 9 A. Yes. <br /> 10 horizontally. 10 Q. Is the trench they described shown in <br /> 11 Q. Would you be able to tell the Board 11 this figure? <br /> 12 why that technique was chosen? 12 A. From the best of my knowledge, it is, <br /> 13 A. Yes. It's got some advantages. 13 yes. <br /> 14 There are obviously otter geophysical techniques 14 Q. Okay. What about the structure <br /> 15 that may be used. We settled on an -- excuse me -- 15 referred to as the Carey Pond? <br /> 16 an electrical method because it is -- two things. 16 A. That was not clear. I'm assuming <br /> 17 One is what we're looking for is water movement fron 17 that this (indicated) is the Carey Pond. <br /> 18 the surface to the ground. 18 Q. Okay. Where would that be on this <br /> 19 The electrical resistivity -- the 19 figure? <br /> 20 bulk electrical resistivity of subsurface units are 20 A. That would be along line 2 -- along <br /> 21 greatly affected by the amount of fluid, the amount 21 line 2. <br /> 22 of water within the unit you are measuring. In 22 Q. Are there any other, I guess, items <br /> 23 addition, the lithology of the different units -- 23 that are identified in this figure? <br /> 24 the clays, sands, sandstone, shales -- normally have 24 A. Yes. We do show sane surface <br /> 25 a different electrical bulk resistivity, and by 25 sinkhole expressions. At least our crew identified <br /> 102 104 <br />
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