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<br />' 14. <br />' 7. CONCLUSIONS <br />1. Aquifer analysis of Stollsteimer Creek alluvium indicates the <br />formation is highly permeable and has a transmissivity of <br />' approximately 100,000 gpd/f t. <br />' 2. Utilizing data from a constant discharge test and computer simu- <br />lation of actual site conditions, representative values for thel.o~¢~ <br />' Fruitland ~rmation hydrologic properties were within one order <br />of magnitude. Transmissivity values ranged from a low value of <br />' 30 gpd/ft to a high value of 500 gpd/f t. Most representative <br />values are within the range of 130 to 320 gpd/ft with a median <br />value of 210 gpd/f t. <br />3. Calculated inflows to the active pit area as determined by corn- <br />' puter simulation indicates inflow of about 10 gpm. <br />' 4. Estimated inflow to the proposed Barren Ridge pit, as determined <br />by using climatic data and hydrogeologic aquifer properties, is <br />in the range of 0.5 to 1 gpm. <br />Respectfully Submitted <br />D.R. PITEAU & ASSOCIATES LIMITED <br />1 <br />' Robert L. Tr lorYE.Enq-' <br />~ ~~~ <br />' R. Allan Dakin, P.Eng, <br /> <br />D R PI BEAU 6 ASSOCIA LES L141 EED <br />