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2010-12-17_REVISION - C1981019 (140)
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2010-12-17_REVISION - C1981019 (140)
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Last modified
8/24/2016 4:28:03 PM
Creation date
1/29/2009 2:12:53 PM
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Template:
DRMS Permit Index
Permit No
C1981019
IBM Index Class Name
REVISION
Doc Date
12/17/2010
Doc Name
Exhibit 7 Item 22 Collom Pit Regional Hydrogeologic Model
Type & Sequence
PR3
Email Name
JRS
Media Type
D
Archive
No
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Model calibration D R A F T <br /> <br /> <br />4.3 Transient calibration <br />20 <br />A transient calibration was performed on a sub-region of the regional model defined in <br />the area of the pilot dewatering test by using the hydraulic response measured during <br />the pilot test as a target. The pilot test caused a wide area of drawdown in the F/G <br />sequence indicating that the coal seams are relatively permeable and that there are no <br />lateral barriers to flow in the test vicinity. Analysis of the pilot test indicated that vertical <br />leakage occurring from underlying and overlying units into the F/G sequence was very <br />low, demonstrating that the interbedded mudstone and siltstone units above (from the <br />top of the Fa coal to the bottom of the E2 coal) and below (from the bottom of the Gc <br />coal to the top of the I coals) have a very low hydraulic conductivity, especially in the <br />vertical direction. The hydraulic response to the dewatering test in these interbedded <br />materials above and below the F/G was minimal, and was only observed very near to <br />the pilot well. The response in the F/G sequence from the pilot test also indicated some <br />horizontal anisotropy with drawdown spreading more in the direction of the N66W <br />fracture sets than perpendicular to these fractures. The transient sub-region model and <br />the regional model were adjusted to reflect this horizontal anisotropy. Because of the <br />requirements of the FEFLOW code, this was achieved by rotating the model until the <br />N66W fracture set was parallel to the east-west direction in the model coordinate <br />system. <br />During the transient calibration, hydraulic parameters such as the horizontal and vertical <br />conductivity and confined storage coefficient of the bedrock units were adjusted to <br />synthesize the observed hydraulic response. The calibrated parameters are listed in <br />Table 4.2. <br />Table 4.2 Calibrated hydraulic parameters from transient calibration <br />Model Kx Ky Kz Specific Drainable <br />layer no. (along main (perpendicular (vertical) storage porosity <br /> fracture to main <br /> direction) fracture <br /> direction) <br /> (ft/day) (ft/day) (ft/day) /m) (%) <br />1 and 2 65 65 65 N/A 20 <br />3 41 20 4.1 2 x 10-7 20 <br />4 and 5 3,287 1,641 329 2 x 10-7 5 <br />6 and 7 41 20 0.4 1 x 10-6 5 <br />8 3,939 1,967 3,939 2 x 10-7 5 <br />9 952 476 95 2 x 10-7 5 <br />10 and 11 68 34 0.7 1 x 10-6 5 <br />12 819 411 82 2 x 10-7 5 <br />13 0.01 0.01 0.01 2 x 10-7 5 <br />14 309 154 31 2 x 10-7 5 <br />15 and 16 615 309 61 2 x 10-7 5 <br />2572-R3 Colowyo Coal Company, L.P. <br />Water Management Consultants
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