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Annual Hyr'.rology Report <br />April 22, 1988 <br />Page 22 <br />spring runoff, Dewatering procedures take usually less than one day with <br />the exception of NID-5 which is responsive to a high spring groundwater <br />table and sometimes has to be dewatered more often. <br />Ponds P'IB-3 and NB-4 have not discharged during 1987 and recrords indicate <br />they have not discharged since they were constructed. MB-4 sometimes <br />catches hydraulic oil spills from the Unit Train Loadout and is pumped by a <br />licensed contract hauler or the WE1CC vacuum truck which deposits the oil in <br />the shop waste oil tank which is in turn pumped by a licensed waste oil <br />recycling firm. This is a standazd procedure. <br />i <br />Flowmeters have been installed on all discharge points from sediment ponds <br />which discharge intermittently to continuously recrord flows. <br />The Quarterly Hydrology Reports contain information on flows, sampling <br />points, and quality of water discharge from the mine site sediment ponds in <br />1986. All water dischazged was in compliance with NPDES permit effluent <br />limitations. <br />During spring runoff conditions as well as some precipitation events <br />quality of water in the North Fork of the Gunnison is much horse than the <br />quality of discharges from F1ECC sediment ponds and well outside NPDES <br />effluent limitations. <br />During winter baseflow and summer conditions water quality in the North <br />Fork is better and is within NPDFS effluent limitations, however, this is <br />the time of year when WFXC's ponds are rarely discharged. <br />Flow amounts from WE~OC sediment ponds are low in comparison to the North <br />' Fork of the Gunnison flows. Ewen during low flow conditions on the North <br />Fork F7EOC discharges represent an imperceptible difference in stream <br />quality. <br />' It is apparent from the analyses that sediment pond discharges have had no <br />adverse impact on the North Fork of the Gunnison River. The quality of <br />discharges usually exceeds the quality of the North fork; and discharge <br />' flows are so small that incremental changes in croncentrations in the North <br />Fork are imperceptible. <br />' Discharges of surface runoff is 1987 are expected to be similar to 1986. <br />