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Comparison of analysis results to regulatory benchmarks <br /> The California EPA Maximum Contaminant Levels (CA MCLs) represent the water quality objectives at <br /> this site Groundwater constituent levels did not exceed any CA MCLs (Table 1) (CA Code of <br /> Regulations, 2003) Environmental Screening Levels (ESLs) set by the San Francisco Bay California <br /> Regional Water Quality Control Board (CRWQCB) were compared with groundwater constituent <br /> concentrations when a CA MCL was not available (CRWQCB, 2004) The ESLs serve as screening <br /> values and represent a conservative substitute when no CA MCL exists For constituents that did not <br /> have a CA MCL, groundwater levels at the site did not exceed ESLs (Table 1) In particular, no <br /> chromium was found in the groundwater For a few constituents, the method detection limits exceeded <br /> the CA MCL or ESL values (Table 1) Complete analysis results are reported in the laboratory data <br /> sheets (Attachment B) <br /> Metal levels measured in aquifer sediments were compared with the ESL values appropriate for deep <br /> soils (> 3 m bgs) in a current or potential drinking water aquifer with residential sod usage None of <br /> the metals detected in the sediments exceeded the corresponding ESLs (Table 2) Chromium total soil <br /> concentrations fell below total sal ESL and Cr(Ill) ESL values, but exceeded the ESL value for Cr(VI) <br /> a <br /> Because chromium mobilization during ozone treatment is of special concern at this site it is <br /> useful <br /> compare the chromium levels in aquifer sediments to levels reported in the literature for similar soil <br /> types Chromium levels well above literature values could signal some unusual geochemistry or an <br /> anthropogenic input The chromium content of natural minerals and sods varies widely with the type <br /> and nature of the rocks or sediments The lowest natural chromium levels are generally found in <br /> granites (1 —26 mg/kg), carbonates (1 — 16 mg/kg) and sandy sediments (16— 36 mg/kg) In general, <br /> the highest chromium content tends to be associated with the finest grain size sods (Alloway 1990, <br /> Richard 1991) From boring logs, sediments retrieved from MW-913 consist primarily of well graded <br /> coarse to medium sand with 20%fine gray sands (55 ft) and well graded silty sand transitioning to silty <br /> clay (60 ft) The sample was homogenized before analysis so constituents from both soil textures <br />' should-be present -The-total chromium level measured in the sediments from MW-9R, 16 mg/kg, is <br /> consistent with the lower chromium levels previously reported in sandy sediments The presence of <br /> finer sediments in MW-9R at 60 ft bgs did not elevate levels in the combined sample out of the normal <br /> range for sandy sediments, such as those found in MW-9R at 55 ft bgs <br /> Possible Chromium Mobilization During Ozone Treatment <br /> Mobilization of redox sensitive metals into <br /> the groundwater has been reported as a general <br /> consequence of in-s,tu oxidation treatments (Cnmi, 2003, USEPA, 2002) The California Regional <br /> Water Quality Control Board has expressed particular concern with possible chromium mobilization <br /> during ozone treatment, and chromium mobilization has been reported as a consequence of <br /> ' permanganate sod treatment-(Cnmi,-2003) This-evaluation-will-thus-focus-on-how-ozone treatment - - <br /> C\Documents and <br />' Settings%crlohnson\DesktopVUnccaJ\GeochemEval_D 2 November 2004 <br /> cc doc <br />