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REV09226
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REV09226
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Entry Properties
Last modified
8/25/2016 1:09:45 AM
Creation date
11/21/2007 10:00:46 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1980007
IBM Index Class Name
Revision
Doc Date
10/14/1997
Doc Name
REVIEW OF TECHNICAL REVISION NO 80 WEST ELK MINE PN C-80-007
From
J E STOVER & ASSOCIATES
To
DMG
Type & Sequence
TR80
Media Type
D
Archive
No
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David Berty - 2 - October 10, 1997 <br />expected since the NW Sealed sump continued to fill'. Bear is concerned the <br />flow between the mines may exceed 30 gpm since MCC began to pump and <br />store huge quantities of water in the NW Sealed Sump in November 1996. <br />2. MCC presents a compelling argument that the maximum seepage rate from the <br />NW Sealed Sump to the Bear No. 3 Mine would be 0.7 to 8.4 gpm. These <br />calculations are based on measured permeability values for the B-3eam that <br />range from 5.0 x 10'5 to 4.0 X 10~cm/sec and values for hydraulic cfradient and <br />maximum head. Bear has no reason to dispute these calculations except they <br />apparently are not applicable to at least one isolated area between the West Elk <br />Mine and the Bear No. 3 Mine. Bear's only concern is whether the maximum <br />head will increase upon final abandonment of the West Elk Mine. Are hydraulic <br />seals to be installed ir, the Lene Pine Gulch entries? If the maximum head dces <br />increase, the Bear No. 3 Mine could be inundated with water from the West Elk <br />Mine. <br />3. The isolated area between the West Elk Mine and the Bear No. 3 Mine was <br />discovered in 1994. It is located around cross-cut 24 - 25 in the 3'' West Mains <br />(=500 feet west of the south quarter corner of section 17). These rtlains were <br />developed during July 1993 and were virtually dry during development. <br />Approximately one year later, Bear noted wet spots and small flows in this <br />isolated area. The water emerged from the floor and lower half of the rib. <br />Apparently the barrier pillar between the two mines is fractured in tf)is isolated <br />area. It is the only area in the Bear No. 3 Mine where MCC's water storage <br />practices have produced any discernable impacts. <br />It may be instructive to determine when MCC actually began to store water in the <br />small capacity sumps in the 1 NW - 5NW longwall panels. If the Bear No. 3 Mine <br />is an effective barometer of MCC's water storage practices, then the bleeder <br />entries and set-up rooms for longwall panel 5NW were developed during mid <br />1994. <br />MCC presents a detailed discussion of how the water will flow from the NW <br />Sealed Sumps to the Bear No. 3 Mine, outcrop/subcrops, etc (page 13). MCC <br />concludes that there is insufficient cross-sectional area within the B-Seam to <br />pass the estimated inflows of 31 to 38 gpm. The water would therefore <br />eventually discharge though the Bear No. 3 Mine, C-Seam portals. <br />'Bear previously assumed the Oow increased from l6 l0 30 gpm lxcause MCC staved to rapidk rill the <br />NW Scaled Sump. Apparcndc the rowine use of the NW Scaled Sump to siorc opcnlional and other inno+v +vatcr <br />increased the head on tlu Bcar No. 3 Mine su0icicmk to cause the Oo++ to mcrcase. <br />
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