My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
REP11244
DRMS
>
Back File Migration
>
Report
>
REP11244
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/24/2016 11:42:33 PM
Creation date
11/27/2007 12:37:53 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1982057
IBM Index Class Name
Report
Doc Date
1/20/2004
Doc Name
2003 Annual Hydrology Report Letter/Report thru Appendix C
From
Seneca Coal Company
To
DMG
Annual Report Year
2003
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.
/
134
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
at Well WWC17 have been on the increase since 2000. Well WWC24 exists in <br />the south area, monitoring began in September 2001. This well failed due <br />to a landslide that occurred in April 2003. A replacement well will be <br />drilled in 2004. Water levels observed this year for all these wells, <br />except WWC17, fell within their historic ranges. <br />- Wolf Creek Underburden. Well WWCU24 monitors this stratum in the <br />south area. Monitoring began in September 2001. This well failed due to <br />a landslide that occurred in April 2003. A replacement well will be <br />drilled in 2004. <br />Ground Water Level Summary. Most aquifers at Seneca II-W exhibit a <br />typical seasonal fluctuation. Water levels are highest after the spring <br />runoff, which recharges the aquifer. Often, bedrock aquifers exhibit a <br />lag time between spring runoff and highest water levels. Water levels <br />then decrease as late summer or fall approaches. Wells WHAL6-1, 6-2, <br />WSAL12 and WW16 experienced the lowest water levels on record this year. <br />Wells WSAL14, WW14, WW17 and WWC17 experienced the highest water levels <br />on record this year. <br />Ground Water Quality. Table 3, Summary o£ Ground Water Monitoring <br />Wells, describes the wells that were sampled, the sample frequency <br />during this year, and site characteristics. Table 4 shows the ground <br />water parameter list used for all wells. Analyses have been performed by <br />ACZ Laboratory in Steamboat Springs, Colorado since May 31, 1983. ACZ <br />Laboratory performs all analyses by SPA or equivalent methods. Samples <br />are delivered the day of collection to the lab in an iced cooler. <br />Monitoring frequencies for ground water quality may be found in Appendix <br />15-3a of the Seneca II-W PAP. <br /> The following discussion of the analytical data collected during the <br /> reporting period is arranged by strata being monitored and coincides <br /> with the format (by aquifer type) in which the analytical data are <br /> presented in Appendix D. The following discussion of water quality will <br /> limit itself to a descript ion of total dissolved solids (TDS). A <br />5 <br />
The URL can be used to link to this page
Your browser does not support the video tag.