Laserfiche WebLink
y <br /> a <br /> yuuc[a ES�Cp611TAN1$ <br /> 3.0 MONITORING RESULTS SUMMARY <br /> 3.1 GROUNDWATER PHYSICAL CHARACTERISTICS AND POTENTIOMETRIC <br /> SURFACE ELEVATIONS <br /> Table 3-1 presents a summaryof groundwater parameters, depths and elevations Since <br />' groundwater elevations were last taken on 15 November 1999, groundwater elevations have <br /> increased by an average of 0 82 feet <br /> I <br /> Table 3-1 <br /> Groundwater Parameter, Depth, and Elevation Data <br /> Top of <br /> Conduc- Casing Depth to 2 March 2000 <br /> Temp tivity Elevation (ft Water Water Elevation (ft <br /> Well °C) I pH I ( MHOS) I MSL ft) MSL) <br /> MW-2 219 618 1,530 NM 2706 NM <br /> MW-2A 205 464 1,260 1191 2705 -1514 <br /> MW-3A NM NM NM 1123 26 37 -1514 <br /> IMW-4 NM NM NM 13 46 27 86 -1440 <br /> MW-5 NM NM NM 12 83 2565 -12 82 <br />' MW-6 NM NM NM 1317 26 93 -13 76 <br />' MW-7 NM NM NM 1314 2860 -1546 <br /> MW-8 NM NM NM 13 76 NM NM <br />' <br /> Mm_WW__ 18 8 7 14 1,290 1226 2745 -15 19 <br /> =__j <br /> Note NM = Not Measured <br /> A potentiometric 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 horizontal groundwater gradient down the center of the trough was 0 002 ft/ft <br /> i <br /> LTR0JECrS\SAN10QWA11o9wvr WPD 4 <br /> I <br />