Laserfiche WebLink
r <br />The amount of water entering the mine as ventilation intake air humidity is based on monthly <br />mean temperatures from Figure II.C-2 on page II.C-9 of the Mining Permit and the yearly <br />mean relative humidity of 56% found on page II.E-1 of the Mining Permit. The absolute <br />humidity, the actual amount of water in the air, is calculated from these data and an average <br />ventilation quantity of 450,000 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 <br />1994, a survey of the accessible areas of the mine workings was conducted to identify the <br />location and flow rates of all seeps. The locations and flow rates of the seeps are shown on <br />Plate 1. Due to the very low flow rates measured, the flow rates are shown in gallons per <br />day. Most, if not all, of this water leaves the mine in the form of humidity in the ventilation air <br />flow. There are very few locations in the mine that produce water over the long term. Most <br />wet areas encountered during mining flow for relatively short periods (hours or days), in the <br />form of profuse drips, and then gradually dry out as the flow stops and the ventilation air <br />carries the moisture out of the mine. These areas are generally associated with stackrock in <br />the roof. stackrock is a sandstone laminated with very thin layers of silty carbonaceous <br />' material. These laminations range in thickness from a few inches to a few millimeters thick. <br />Water in the stackrock appears to be connate in origin and not from the rechargeable <br />groundwater systems. Virtually all of the geologic water enters the mine from the surounding <br />strata from broken rock in the gob behind the longwall face. BME believes there was <br />insignificant amount of seepage during the 1997-1998 water year. <br />The smallest quantity of water entering the mine is the incidental category. This category <br />includes leakage from water lines, dust control watering in the haulage entries, and <br />washdown water used in the slope and other locations. It has been assumed that 10% of the <br />water used for production equipment will be used under this category. <br />' Outnoinst Water As coal is mined, it is wet by dust control sprays on the continuous miners, <br />the longwall shearer and at transfer points along the conveyor belt system. This water is then <br />carried out of the mine as surface moisture on the raw coal. This added coal surface <br />moisture represents a 2% increase in the raw coal moisture content. The raw coal tonnage <br />A produced during this reporting period was 2,031,983 tons. <br />Water leaving the mine as ventilation humidity represents a large quantity in the water <br />balance. The temperature of the exhaust ventilation air is almost constant, at 60° F. <br />' No underground water is being pumped out since the fire episode. For the remaining life of <br />the D-Seam mine, the underground water will be left to fill the mined out areas. <br />1 <br />12 <br />