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REP45364
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Entry Properties
Last modified
8/25/2016 12:48:04 AM
Creation date
11/27/2007 10:34:24 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981018
IBM Index Class Name
Report
Doc Date
2/24/1997
Doc Name
1996 AHR
Annual Report Year
1996
Permit Index Doc Type
HYDROLOGY REPORT
Media Type
D
Archive
No
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<br />operate about 3 hours per shift (the rest of the time is spent moving, etc.). The longwall <br />equipment uses 140 gpm of water for about 7 hours per shift. <br />' The amount of water entering the mine as ventilation intake air humidity is based on monthly mean <br />' temperatures from Figure II.C-2 on page II.C-9 of the Mining Permit and the yearly mean relative <br />humidity of 56% found on page II.E-1 of the Mining Permit. The absolute humidity, the actual <br />amount of water in the air, is calculated from these data and an average ventilation quantity of <br />' 525,000 cubic feet per minute. <br />' The amount of water entering the mine from the surrounding strata is partially estimated by <br />identifying all known seep areas and estimating the flow rate from each. During January 1994, <br />a survey of the accessible areas of the mine workings was conducted to identity the location and <br />' flow rates of all seeps. The locations and flow rates of the seeps are shown on Plate 1. Due to <br />the very low flow rates measured, the flow rates are shown in gallons per day. Most, 'rf not all, of <br />this water leaves the mine in the form of humidity in the ventilation air flow. There are very few <br />' locations in the mine that produce water over the long term. Most wet areas encountered during <br />mining flow for relatively short periods (hours or days), in the form of profuse drips, and then <br />gradually dry out as the flow stops and the ventilation air carries the moisture out of the mine. <br />These areas are generally associated with stackrock in the roof. Stackrock is a sandstone <br />laminated with very thin layers of silly carbonaceous material. These laminations range in <br />' thickness from a few inches to a few millimeters thick. Water in the stackrock appears to be <br />connate in origin and not from the rechargeable groundwater systems. Vrtually all of the geologic <br />water enters the mine from the surrounding sfrata from broken rock in the gob behind the longwall <br />face. <br />' The smallest quantity of water entering the mine is the incidental category. This category inGudes <br />leakage from water lines, dust control watering in the haulage entries, and washdown water used <br />' in the slope and other locations. <br />Outaol~y Water As coal is mined, it is wet by dust control sprays on the continuous miners, the <br />longwall shearer and at transfer points along the conveyor bek system. This water is then carried <br />out of the mine as surface moisture on the raw coal. This added coal surface moisture represents <br />' a 2% increase in the raw coal moisture content. The raw coal tonnage produced during this <br />reporting period was 527,130 tons. <br />' Water leaving the mine as ventilation humidity represents a large quantity in the water balance. <br />The temperature of the exhaust ventilation air is almost constant, ranging from 60° in winter <br />months to 63°F in summer months. The relative humidity of this air ranges from f30% in the <br />' summer to 95% in January and February. Throughout the year, except for the months of June, <br />12 <br /> <br />
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