Laserfiche WebLink
1 <br /> NNLIGEAS OESCiEi5 CG6AuR3 <br /> J <br /> . 3.0 MONITORING RESULTS SUMMARY <br />' 3.1 <br /> GROUNDWATER PHYSICAL_CHARACTERISTICS AND POTENTIOMETRIC <br /> tSURFACE ELEVATIONS <br /> Table 3-1 presents a summary of groundwater parameters, depths and elevations Since <br /> tgroundwater elevations were last taken on 17 March 1998, groundwater elevations have <br /> increased by an average of 2.12 feet. These were the highest groundwater elevations measured <br /> since sampling began. <br />' Table 3-1 <br /> Groundwater Parameter, Depth, and Elevation Data <br />' Top of 18 June <br /> Conduc- Casing Depth to 1998 Water <br />' Temp hvity Elevation (ft Water Elevation (ft <br /> Well (°C) pH (WHOS) MSL} (ft) MSL} <br /> MW-2 NM NM NM NM 2858 NM <br /> MW-2A 243 707 1,200 11 91 2902 -17 11 <br /> MW-3A 252 704 1,400 1123 2847 -1724 <br /> MW-4 262 779 1,450 1346 29 12 -1566 <br /> I MW-5 26 3 690 1,080 1283 2703 -1420 <br /> MW-6 247 696 1,340 1317 2839 -1522 <br /> MW-7 228 690 1,300 13 14 3002 -16 88 <br /> MW-8 NM NM NM 13 76 3043 -1667 <br /> IMW-9 239 715 1,400 12 26 2822 -1596 <br /> Note NM = Not Measured <br /> I <br /> A potentiometnc contour map developed from the water level data is presented on Figure 3-1 <br /> As in previous sampling rounds groundwater flow is generally toward the north-northeast within <br /> a trough. The average horizontal groundwater gradient down the center of the trough was <br /> 0 0009 ft/ft. <br /> L TR0IECr&SAN)0QUiSAUBA_96]UN 5 my 1996 <br />