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2008-12-09_PERMIT FILE - C1996083A (4)
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2008-12-09_PERMIT FILE - C1996083A (4)
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Last modified
8/24/2016 3:38:45 PM
Creation date
2/27/2009 9:27:05 AM
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Template:
DRMS Permit Index
Permit No
C1996083A
IBM Index Class Name
Permit File
Doc Date
12/9/2008
Section_Exhibit Name
2.04 Information on Environmental Resources
Media Type
D
Archive
Yes
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2.04.7 Hydrology Description <br />• <br />Water right 83 is a perennial spring with a shallow pond that is typically full and <br />overflowing. The spring associated with water right 83 has an average and <br />maximum flow of 0.08 and 0.50 gallons per minute respectively. The Operator <br />considers the pond associated with water right 76 to be a good pond because it <br />contains water in the spring and into the summer under normal weather <br />conditions. <br />Additionally, high value springs have been identified on USDA-FS managed land <br />within the permit boundary. They are shown on the following table. <br />Spring Rate GPM Spring Rate GPM <br /> Ave to Max Ave to Max <br />SP33-5 0.2 to 2.5 S34-4 1.2 to 4.8 <br />S33-2 3 to30 S34-5 1.2 to 10.7 <br />S34-1 0.6 to 4.3 SP34-11 2.8 to 18.8 <br />SP34-2 3.0 to 22.2 S34-22 1.5 to 35.0 <br />S34-3 0.2 to 1.7 <br />• <br />The seasonal quantity and quality of the water within each aquifer is presented in <br />Volume III, Exhibit 3 and on Maps 10 and 11. The Operator does not have down <br />gradient baseline monitoring wells in the northern section of the permit area <br />because of technical difficulties. Ground water monitoring wells in the northern <br />portion of the permit area may be technically infeasible to implement because of <br />extreme depth. In addition, it is technologically impracticable and extremely <br />problematic to obtain representative water samples at depths that exceed 2,000 <br />feet. To partially compensate for the lack of down gradient wells the Operator had <br />HydroGeo, Inc. prepare a report that uses existing up gradient baseline data to <br />predict down gradient water quality in the B-Seam and the water bearing zone <br />above the B-Seam. The report provides expected ranges in values for pH, total <br />dissolved solids, total Iron and total Manganese. HydroGeo's September 2, 2008 <br />report is located in Volume III, Exhibit 3. <br />The USDA-FS controls surface access to any potential monitoring well sites. A <br />few years ago the USDA-FS made a formal decision, with public input, to close <br />Hubbard Creek road beyond the location of the DH-67 monitoring wells. <br />Therefore, they strongly discourage re-opening Hubbard Creek road for access <br />to a lower depth monitoring well site. The USDA-FS has approved one site (DH- <br />68) on Iron Point as a potential monitoring well site. <br />• <br />The location of DH-68 is shown on Map 9. Map 11 and Map 11-1 present a <br />prediction of the depth of the water bearing zone above the upper B-Seam. The <br />depth to the water bearing zone is 2,350-feet and the coal seam is 2,450 feet <br />deep at DH-68. The extreme depth dictates two separate monitoring wells. A <br />dual completion well would not be attempted at the required depth. One well <br />would need to be installed in the formation above the B-Seam and one well in the <br />B-Seam. The estimated cost to attempt to install the two wells is in excess of one <br />million dollars. <br />PR-10 <br />~pPRaV6A <br />lrzy ~a ~ <br />2.04 - 24 - 09/26/08 <br />
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