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2014-05-13_PERMIT FILE - C1996083A (3)
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2014-05-13_PERMIT FILE - C1996083A (3)
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Last modified
8/24/2016 5:43:58 PM
Creation date
5/21/2014 9:22:10 AM
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Template:
DRMS Permit Index
Permit No
C1996083A
IBM Index Class Name
Permit File
Doc Date
5/13/2014
Doc Name
pages 2.05-84 to 2.05-165
Section_Exhibit Name
Volume I 2.05 Operation and Reclamation Plans Part 2
Media Type
D
Archive
Yes
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Flooded mine workings could also impact the water quality in the area. When the <br />mines are sealed they will slowly fill with water. Although no data for permeability or <br />transmissivity of the saturated portions of the coal bearing member of the Mesaverde <br />Formation are available within the permit area, the experience by others (Brooks, <br />1983) suggests the Mesaverde Formation transmits little water. Therefore, the <br />abandoned mine workings would not be expected to transmit water to the <br />surrounding strata. Based on the above discussion, if the mine workings fill with <br />water and discharge through the portals, the impact on the North Fork of the <br />Gunnison River would be less than or equal to the mine water discharge analysis <br />presented above. <br />The flooded mine workings could also affect the ground water quality and quantity in <br />the overlying Upper and Lower Perched Water Zones. However, as stated above, <br />the Mesaverde Formation transmits little water. Therefore, the impact the flooded <br />mine workings will have on the quantity and quality of the surrounding strata should <br />be minor. <br />The Rollins sandstone, as monitored in DH -34B, NM4X98 -29 and P- TC- 03 -01(R) <br />has pH in the range of 7.5 to 9.6, conductivity in the 1,200 to 7,900 umhos /cm range <br />and total recoverable iron in the 0.2 to 62.0 mg /I range. The Rollins sandstone is a <br />confined aquifer under piezometric head. The confining shale layers above the <br />Rollins sandstone and piezometric head should prevent any integration of waterfrom <br />either the D -Seam or B -Seam into the Rollins sandstone. There are two drill holes <br />(G -15) located near the mouth of Dove Gulch and DH 98 -57 located in the central <br />portion of the east mine workings that provide documentation of the hydraulic <br />isolation of the Rollins sandstone from the B -1 Seam, the lowest coal seam to be <br />mined. The following table shows the extent of the hydraulic isolation. <br />Hole (Interburden) <br />Mudstone <br />Sandy Mudstone <br />Sandstone <br />Coal <br />Lost Core <br />G -15 (89.8) <br />64.3 <br />8.3 <br />11.0 <br />6.2 <br />0.0 <br />DH 98 -57 (94.9) <br />68.0 <br />10.6 <br />9.0 <br />0.0 <br />7.3 <br />In the western mine plan area, west of Terror Creek, drill holeTC- 03 -03, CWI- DH -50, <br />51 and 62 document the hydraulic isolation between the Rollins sandstone and the <br />lowest coal seam to be mined. DH- CWI -51 is located in the northern portion of the <br />western mining district. The following table shows the extent of the hydraulic <br />isolation. <br />Hole (Interburden) <br />Mudstone <br />Sandy Mudstone <br />Sandstone <br />Coal <br />Lost Core <br />TC -03 -03 (74.5) <br />23.0 <br />28.3 <br />4.0 <br />19.2 <br />0.0 <br />CWI -DH -50 (70.6) <br />31.7 <br />17.7 <br />10.0 <br />8.0 <br />3.2 <br />CWI -DH -51 (70.0) <br />16.2 <br />47.1 <br />0.0 <br />6.7 <br />0.0 <br />CWI -DH -62 (105) <br />9.0 <br />60.0 <br />15.5 <br />20.5 <br />0.0 <br />PR -13 2.05-115 02/13 <br />
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