My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
REP41515
DRMS
>
Back File Migration
>
Report
>
REP41515
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/25/2016 12:43:21 AM
Creation date
11/27/2007 9:02:57 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981010
IBM Index Class Name
Report
Doc Date
3/16/2006
Doc Name
2005 Annual Hydrology Report Cover Letter to Section 2.8
From
Trapper Mining Inc.
To
DMG
Annual Report Year
2005
Permit Index Doc Type
Hydrology Report
Media Type
D
Archive
No
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
61
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
View images
View plain text
The water-level changes for the HI aquifer have generally been influenced less by slightly <br />less than average recharge during the previous seven years prior to the above average precipitation in <br />2005. The mining upgradient of HI well GF-4, which occurred several yeazs ago, has been long <br />enough in the past to allow water levels to fully recover. The water levels in this HI aquifer well <br />seem to be varying only slightly with changes in recharge rates. Water levels in this well were <br />slightly higher in 2005 with the above normal precipitation. The elevation of the backfill springs <br />likely limits the head buildup in the backfill aquifer, which, in tum, limits the maximum head in the <br />downgradient coal aquifer. Fairly steady water-level responses were observed in the two backfill <br />equivalent HI aquifer wells GF-5 and GF-7. Water levels seem to have reached recovered levels in <br />these two wells. The development of backfill springs may limit the maximum water level in some of <br />these azeas of the A pit. <br />The water levels in the three GE wells stabilized in approximately 1990. This is thought to • <br />be due to the length of time since dewatering stopped at the adjacent underground operation. <br />Gradually declining water levels were observed in these three wells with the above normal <br />precipitation. <br />Water levels in the backfill azeas are depressed and are not likely to ever recover to pre-mine <br />levels except near the northern end of the mine azea. Map 2-1 shows that the levels in the backfill <br />and downgradient aquifers are similar. Well pairs GD-3 & GD-2 and GF-11 & GF-6 present water <br />levels that aze very similaz in water-level elevation for the backfil] and downgradient QR aquifer <br />well. Mining is significantly increasing the permeability of the backfill aquifers which is a benefit <br />relative to potential yields from the aquifer. The increased permeability will likely not allow water <br />levels to recover to pre-mine levels in the reclaimed pits except near the northern (down-dip) end of <br />Trapper Mining Company 6-2 • <br />2005 Annual Report <br />
The URL can be used to link to this page
Your browser does not support the video tag.