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ditches are flowing and flood irrigation is occurring. Water level responses to <br /> precipitation events are indistinguishable, as the effects of recharge from the ditch <br /> irrigation system have masked any evidence of recharge that could be attributable to <br /> precipitation. Mining at the Nucla Mine area has had no discernible affects on the water <br /> levels of the overburden monitor wells. <br /> Dakota Coal Water Levels. Eight monitor wells have been installed to monitor water levels <br /> in the Dakota coal aquifer. Two of the monitor wells (GW-N4 and GW-N4R) are located at <br /> the Nucla Mine and the remaining six monitor wells (GW-N14, GW-N17, GW-N17P1, GW-N20, <br /> GW-N29 and GW-N30) are located at Nucla East (Exhibit 7-1). Water level data for Well <br /> GW-N4 has been collected since August, 1979 and collecti"on of water level data for Wells <br /> GW-N14, GW-N17, GW-N17P1, and GW-N20 began in July 1986. The remaining three wells <br /> (GW-N4R, GW-N29 and GW-N30) were recently installed (September, 1987) and collection of <br /> water level information began immediately after they were completed and developed. <br /> Exhibit 7-3 shows the Dakota coal potentiometric surface. Monthly water level data <br /> including hydrographs for all monitor well sites are contained in Appendix 7-1. <br /> Ground water in the Dakota coal is under artesian conditions with a general downward <br /> vertical head, but there are areas with upward vertically recharging head pressures. Mean <br /> artesian heads in the lower Dakota coal range from 18 feet at Monitor Well GW-N14 and 42 <br /> feet at Monitor Well GW-N29. The average artesian head for the lower Dakota coal is 34 <br /> feet. Water levels in the Dakota coal display seasonal variability that coincides with <br /> the irrigation season and operation of the ditch irrigation system. The maximum seasonal <br /> water level fluctuation observed in Monitor Well GW-N4 is about 3.0 feet due to its <br /> location in the valley bottom. The Nucla East wells display seasonal variability from 2.8 <br /> feet at Monitor Well GW-N17P1 to 14.6 feet at Monitor Well GW-N20. Shallowing occurs from <br /> April to September and there appears to be little lag between when the irrigation season <br /> starts and the shallowing of the static water levels occurs. There are no discernible <br /> water level responses to precipitation, nor can any affect from mining be observed at any <br /> of the Dakota coal monitor wells at the Nucla or Nucla East mining area. <br /> Underburden Water Levels. Twelve monitor wells have been installed to monitor water <br /> levels in the underburden aquifer system. Six of those monitor wells (GW-N1, GW-N1P1, <br /> GW-N3, GW-N5, GW-N6 and GW-N11) are located in and proximate to the Nucla Mine site. The <br /> remaining six monitor wells (GW-N13, GW-N16, GW-N16P1, GW-N192 GW-N33 and GW-N34) are <br /> located proximate to the Nucla East mining area. Exhibits 7-1 and 7-4 show the <br /> 7-8 Revised 04/11/88 <br />