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Mr Michaellafizrna <br /> a., page 3 <br /> rProposed Bench Testing for Oxidizer Injection acted soil remaining <br /> Despite the lack of groundwater plume migration and the limited volume of imp ears have remained <br /> groundwater over last four evalua e the potential for the <br /> bencath the site, contaminant concentrations <br /> We Propose <br /> relatively <br /> stable <br /> oxidizing zing sou onto agCce significantly rate the pace of cleanup <br /> injection of were <br /> vated in 1999 to a depth of 20 feet OnlHminor resignificant levels <br /> vels of <br /> Contaminated soils were exca les collected from the excavation <br /> re$ent in confirmation soil same sleeted at depths of 25 and 30 feet in monitoring een the depths of <br /> p resent in soil samples co <br /> TPHd were p acted soil does <br /> It is estimated that impacted soil remains beneath the, <br /> diameter of the area of imp able aids of <br /> 20 feet and approxirnately 35-40 feet below gra approximate 1Q0tion c <br /> ed Assuming ori average TPHd concentration of 2,004 ppa e <br /> not appear to exceed l5 feet These dimensions indicate that app is of soil samp <br /> soil m the saturated zone are impac Anal leas resul <br /> the mass of contaminant is about d area 0 pounds n through the site is <br /> ed area of residual soil contamination ti remaining beneath the <br /> summarized in Table 3 The estimated <br /> Figure 3 A cross sec <br /> floor of the 1999 remedial excavation is shown on Fig <br /> depicted on Figure <br /> otentialiy amendable to the Introduction l°of chemical <br /> Q f et�0 12 5 feet <br /> The impacted area appears to be p which is <br /> monitoring well MW3 The excavation was backfilled from a depth clay well <br /> throughpermeability Beneath this are five or mor bee n ecnative <br /> d iritoi monitoring <br /> with pea gravel <br /> of high peen An oxidizing solution could j <br /> underlain by poorly graded sand ea ravel within the farmer <br /> Presumably the greater part of the solution <br /> would <br /> ltwould then function as a reservoir, <br /> MW3 h permeability p contaminated soil and to <br /> excavation pit due to its hig p h the underlying Petroleum <br /> allowing the oxidizing solution to migrate vertically throng dioxide and water <br /> portion of the well screen The salutiobnon Quid react with the p <br /> siphon through the lower p hydrocarbons to car <br /> hydrocarbons sorbed to the soil, oxidizing the by Fenton's Reagent has <br /> as the oxidizing solution <br /> We propose to evaluate using Fentoe Rot gidu In government-sponsored studi e, the I-ants <br /> long been used in n s wastewater Reagent has been shown to be effective in oxidizing organic <br /> infection of Fento <br /> such as fuel hydrocarbons and chlorinated solvents e formation f hydroxyl radicals by <br /> -ton's Reagent oxidizers <br /> known <br /> Reagent consists of a solution of H2O2 <br /> Fe ent is one of strongest oxClassi known due tot en h of the solution is <br /> the catalysis of hydrogen peroxide The oxidizing strength <br /> typically in the form of FeSOa � This may be accomplished by <br /> catalyzed by ferrous iron, yp Hof approximately 3- rade Fe504) <br /> maximized when the treated water is at a p To control <br /> lfiiric acid (which is a common adulterant temper is between 70-1000 F <br /> the addition of su action e optimal temp eroxide and have water oil <br /> Temperature will rise ` th the necessary to stage the introduction of P <br /> temperature and pHs maybe <br /> the heat of reaction <br /> hand to dilute the reaction and q <br /> s the Potential to alter the valence of n (RWQCB) has <br /> The oxidizing strength of the reetallic Ions and <br /> agent has p Central Valley Regi <br /> halogens The Regional Water Quality Control Board, <br /> 6\C3A0UNDZE.\W00LSLY C"T\QMQ\2005\4QM2005 doc <br />