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REV00812
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REV00812
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Entry Properties
Last modified
8/25/2016 12:58:28 AM
Creation date
11/21/2007 8:48:09 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981018
IBM Index Class Name
Revision
Doc Date
7/26/1995
Doc Name
PRELLMINARY ADEQUACY REVIEW TR 37 DESERADO MINE C-81-018
From
WESTERN FUELS UTAH INC
To
DMG
Type & Sequence
TR37
Media Type
D
Archive
No
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Ms. Barbara L Pavlik <br />Division of Minerals 8 Geology <br />July 24, 1995 <br />Page 2 <br />Monitor hole 36-2L is the only monitor hole located in the lower sandstone facies form which water <br />samples were collected. The average TDS for the monitoring period was 604 mg/I. This compared <br />with a range of TDS identified during baseline studies of 810 mgfl to 2100 mg/I. <br />The bedrock water quality analysis for the monitoring period 1981 through the third quarter of 1984 <br />indicated that the water quality had remained within the ranges identified during the baseline studies. <br />Hence, this requirement was apparenty dropped as per a letter and attachment, dated October 10, <br />1984, from Mr. Dan Mathews of the Division. Unfortunately, both WFU and DMG have been unable <br />to locate this correspondence. However, it should be noted that subsequent annual hydrological <br />reports followed the revised monitoring program which did not require bedrock water sampling and <br />analysis. It appears that such a change in monitoring program was not formalized through a <br />technical revision in 7985. <br />WFU requests that based upon the data collected during 1981-1984 which showed water quality <br />remained within the ranges identified during the baseline studies, and the current practice which is <br />in continuance since 1985, the requirements for bedrock water qualiiy sampling and analysis be <br />formally eliminated. <br />If you have any quesfions, please call. <br />MPSlg <br />cc: Raja UpadhyayNVFA <br />Jeff Dubbert/WFU <br />Sincerely, <br />,- <br />l <br />Murari P. Shrestha, P.E. <br />Assistant Manager of Engineering <br />
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