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KLEINFELDE R <br /> ................ <br /> ............. <br /> ... . .. .................. X <br /> . . ........................... .... <br /> ------ . ........ <br /> ------------ <br /> ..... . . ....................... <br /> .. .. ...... .. .. ...... <br /> .................................... <br /> .......... <br /> ..................................... ... <br /> ............................... W <br /> .. ............ <br /> .. ...... . ................ <br /> . ............ <br /> Chromium VI .042 - .05 .05# <br /> Selenium .012 0.01 <br /> Primary MCL for Total Chromium <br /> MW-1 is upgradient of the identified landfill zones and therefore, it appears that the observed <br /> concentrations may be background for the site. Selenium was not detected in the downgradient <br /> wells. Hexavalent chromium was detected in one downgradient well, MW-4, at concentrations <br /> of.03 to .039 mg/l. <br /> Of the 11 metals..consistently detected in ground water at the site, only one was reported at <br /> concentrations exceeding the established second= MCL. This metal, manganese, was <br /> reported at concentrations ranging from non-detect (detection limit equals .01 mg/1) in MW-4 <br /> to 0.12 mg/l in MW-3. The secondary MCL for manganese, which is largely based on <br /> objectionable taste.or odor rather than health criteria, is .05 mg/l. It is common for shallow <br /> ground water in the San Joaquin valley to .contain manganese at concentrations exceeding <br /> 05 mg/l. The analytical results are summarized on Table 5-7. <br /> 5.3.2.3 General Minerals <br /> Ground water samples were analyzed for major cations (calcium, sodium, potassium, <br /> magnesium, and iron) and anions (bicarbonate, carbonate, chloride, sulfate, and nitrate) during <br /> the summer of 1989 and the winter of 1990. The results of these analyses are presented on <br /> Table 5-8. <br /> To assess the relative abundance of major ions and anions, the analytical results were <br /> converted from mg/l to meq/1. The relative percentages were then graphed on Stiff diagrams <br /> (see 1990 SWAT). From this information, it appears that the cations in ground water at the <br /> site are fairly consistent across the facility. However, the anions present in the ground water <br /> CR14-92-12 Page 18 of 39 24-220109-1709 <br /> Copyright 1992 Kleipfelder, Inc. <br />