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8 January 1993 <br /> (GeoAudit CV 45-49C5-1. 10) <br /> ' Page 4 of 7 <br /> ' TABLE 1 <br /> GROUNDWATER SAMPLE STABILIZATION PARAMETERS <br /> 24 November 1992 <br /> 1 WELL NO. GALLONS pH TEMP. (C) CONDUCT. <br /> MW-1 0 6.8 25. 6 1140 <br /> 2 7 .2 20. 6 1223 <br /> 4 7.6 20. 3 1246 <br /> 6 7.8 20. 3 1256 <br /> ' 8 7.8 19.7 1247 <br /> MW-2 0 7 .2 26. 1 1386 <br /> 2 6.8 20. 1 1183 <br /> 4 7.0 20. 3 1135 <br /> 10 7.2 19. 1 1132 <br /> 15 7. 3 18. 3 1128 <br /> ' MW-3 0 6.5 10. 1 1689 <br /> 2 6.8 16. 8 1863 <br /> 4 6.8 17.4 1838 <br /> 1 6 7 .0 18.8 1856 <br /> 8 7 . 1 18. 5 1865 <br /> ' 22 January 1993 <br /> MW-3* 0 6.9 62. 3 882 <br /> 1 6.5 64.7 741 <br /> 2 6.3 64. 6 729 <br /> 3 5.8 64.7 686 <br /> ' 4 5. 5 64.7 726 <br /> 5 5. 5 64. 5 710 <br /> 6 5. 5 64. 5 709 <br /> 7 5.4 64.2 695 <br /> * temperature (°F) <br /> ' FINDINGS <br /> The generalized stratigraphic sequence in the borings consisted of <br /> alternating layers of fine to medium-grained sands, silty clays, <br /> sandy clays and clayey sands. <br />