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REP50671
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Last modified
8/25/2016 12:55:35 AM
Creation date
11/27/2007 12:54:56 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981018
IBM Index Class Name
Report
Doc Date
1/4/1993
Doc Name
1992 AHR
From
Western Fuels-Utah, Inc.
Annual Report Year
1992
Permit Index Doc Type
HYDROLOGY REPORT
Media Type
D
Archive
No
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1 <br />' detected, the water level will be measured and samples collected quarterly to be analyzed for the <br />parameters listed in Table 2-1. <br />During October 1984, the Taylor Draw Reservoir facilities were completed and the reservoir began <br />filling with water. The area around the alluvial groundwater holes has become a shallow water mud <br />' flat area with the deposition of mud, silt and sand at high reservoir levels. AS a result, alluvial <br />groundwater monitoring holes Qal-1, Qal-2, Oal-3, Qal-4 and Qal-6 have been destroyed and are <br />no longer available for monitoring. Alluvial hole Qal-5 is still being monitored. <br />During May 1987, longwall panel 1 was mined past the location of 2-12U. The location was <br />' subsided and the monitoring hole could no longer provide usable data. Accordingly, Western Fuels <br />submitted an application for a Technical Revision on 6/7/88 to eliminate groundwater monitoring at <br />2-12U. The Technical Revision has subsequently been approved. <br />2.2 Summary and Analysts of Deserado Mlne Hydrology Data <br />t Data collected during this water year (Oct. 1, 1991 to September 30, 1992) have been summarized <br />' and compared with the data from the baseline hydrology inventory. Surface water and ground water <br />discussions are presented separately in the following sections. <br />' 2.2.1 Surface Water Data Surface water data has been collected from five (6) stations in the <br />Deserado Mine area. The locations of these stations are shown on Plate 1 in the pocket of this <br />report. With the exception of the White River, stream flow in the Deserado Mine area is ephemeral <br />t with flaws occurring only in response to rapid snow melt or during heavy thunderstorms. Gaging <br />stream flow and collecting water samples is therefore dependent upon being able to collect samples <br />' and gauge flow while the flow event is occurring. Heavy thunderstorms can result in flash floods <br />which destroy the sampling and gauging stations. Station SW24-1 has been destroyed twice, the <br />last time in the Spring of 1983. Up until July 1986, this station was a °grab sample' location where <br />samples were taken as soon as possible after significant thunderstorms and during snow melt run <br />off. Anew single stage sampler was installed in July 1986. Other stations have been plagued with <br />' problems such as the samplers silting in and the gauging apparatus silting in. These problems are <br />corrected as soon as possible but there is no guarantee that the next flow event will not also plug <br />the sampling and gauging apparatus. <br />The data collected from the surface water monitoring program during the hydrology reporting year <br />t is contained in Appendix B. The statistical summary of the data is also included in Appendix B. <br />These data are compared with the original baseline data to determine if changes have occurred. <br />The baseline data is reported in the "Deserado Mine First Annual Hydrology Report', 1985. <br />' S <br /> <br />
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