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REV08078
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REV08078
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Entry Properties
Last modified
8/25/2016 1:08:46 AM
Creation date
11/21/2007 9:50:21 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1983194
IBM Index Class Name
Revision
Doc Date
7/8/1985
Doc Name
INDUSTRIAL RESOURCES INC REGULAR MINING PERMIT MODIFICATION MLRB
From
Industrial Resources Inc.
Type & Sequence
AM1
Media Type
D
Archive
No
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As noted earlier, the 11 wells drilled by Multi Mineral Corp. provide the <br />basis of the information provided hereing. Also, wells 14-1, 20-1, 24-1 and <br />28-1 are of definite interest since they have been permitted by IRI for <br />groundwater rights. The locations of all of these wells are shown in Figure <br />G-22. <br />G.2.3.2.4 Aquifer Testing <br />Two extended pumping tests were conducted by U.S. Geological Survey (USGS) <br />personnel in wells located on the maxi-pad. One test each was conducted in <br />the Lower Aquifer and the Upper Aquifer. Test results are presented in <br />Table G-2. Calculations and curves are contained in Appendix A. <br />The Lower Aquifer test was conducted in July 1981. Well MMC-IRI-B served as <br />the pumping well, producing approximately 60 gallons per minute (gpm) over <br />the 10,000 minute pumping portion of the test. Wells MMC-IRI-4, -5, -6, and <br />-7 simultaneously monitored drawdown in the Lower Aquifer and the Upper <br />Aquifer. Because 1;he Lower Aquifer piezometers experienced measurable <br />drawdown, transmissivity and storage coefficient were calculated. There was <br />no meaningful drawdown evidenced in any of the Upper Aquifer piezometers, <br />indicating an absence of significant communication between aquifers. <br />However, if the test: had been conducted over a longer period of time it <br />would be expected theft the drawdown would be more significant. <br />The Upper Aquifer was tested in November 1981, again using well MMC-IRI-8 as <br />the pumping well. During the 2,000 minute test duration, a discharge of <br />approximately 20 gpm was achieved. Upper Aquifer water levels were <br />simultaneously monitored for drawdown in wells MMC-IRI-4, -5, -6, -7 and <br />Lower Aquifer levels in wells MMC-IRI-S, -6, and -7. Because the Upper <br />Aquifer piezometers experienced measurable drawdown, transmissivity and <br />storage coefficient vrere calculated. No changes were observed in the water <br />level in the Lower /lquifer piezometers, again indicative of an absence of <br />communication. <br />~• <br />G-35 <br />
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