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z <br /> 1 INTRODUCTION <br /> Geomatrix Consultants (Geomatrix) conducted an in-situ biodegradation investigation at <br /> the 230 Industrial Avenue site (the Site) in October 20051. The in-situ push-pull tests <br /> (PPTs) were completed in wells M-1A and M-113, which are located in the proposed <br /> treatment zone at the Former Nestle Facility (Figure A.2-1). Geomatrix completed these <br /> tests to evaluate in-situ carbohydrate utilization rates and assess potential changes in <br /> aquifer conditions due to carbohydrate addition. <br /> A single-well PPT consists of two phases, (1) the injection ("push") phase and (2) the <br /> extraction ("pull") phase. During the injection phase, a test solution consisting of water, <br /> a reactive solute, and a conservative tracer, is injected into the aquifer surrounding the <br /> test well. After the injection, the solution is allowed to remain in the aquifer pore space <br /> near the well for approximately 24 hours to react with solid and dissolved-phase <br /> constituents (referred to as the lag time). The extraction phase is then initiated following <br /> this 24 hour period. During the extraction phase, water is periodically extracted from the <br /> test well and sampled to obtain concentrations of the reactive solute, tracer, and other <br /> target constituents in groundwater. <br /> 1.1 Background Information <br /> In-situ treatment was proposed to the California Regional Water Quality Control Board <br /> (RWQCB), Central Valley Region in the July 12, 2005 Final Work Plan for Initial Testing <br /> and Characterization Program, and in the subsequent November 28, 2005 addendum. <br /> These documents were subsequently approved by the RWQCB. The objectives of the in <br /> situ treatment were two-fold: (1) identify an area for implementing the potential in-situ <br /> bioremediation (ISB) remedy; and, (2) collect preliminary data to facilitate the design of <br /> an ISB pilot test program at the Site <br /> The addition of a carbohydrate solution to groundwater containing chlorinated volatile <br /> organic compounds (VOCs) is an effective in situ remedial approach at many sites. This <br /> approach stimulates native microbial populations and promotes the reduction of <br /> chlorinated VOCs by dehalo-respiration2 s, a. Carbohydrate is both an energy source <br /> and a carbon source that may increase the growth and viability of a variety of different <br /> groups of subsurface microorganisms when added to the groundwater system. <br /> Carbohydrate is fermented by subsurface microorganisms, producing final end-products <br /> including methane and inorganic carbon (as carbon dioxide or bicarbonate). <br /> Intermediate fermentation products are produced, including organic acids and hydrogen. <br /> The intermediate fermentation products are used by subsurface microbes to reduce solid <br /> and dissolved mineral constituents and other relatively oxidized species (called electron <br /> acceptors). <br /> Examples of naturally occurring and anthropogenic electron acceptors in aquifer <br /> systems include oxygen, nitrate, sulfate, ferric iron (Fe III), manganese (Mn IV), and <br /> carbon dioxide. These electron acceptors can be reduced by adding carbohydrate to <br /> groundwater. VOCs, including trichloroethylene (TCE), cis-1,2-dichloroethylene (cis-1,2- <br /> DCE), and vinyl chloride (VC) can also function as electron acceptors, and the reduction <br /> of these compounds can be enhanced microbiologically by adding carbohydrate to the <br /> aqueous system. The microbiologically-mediated reduction of these electron acceptors <br /> is called respiration, and microbes utilize the energy gained from these oxidation- <br /> reduction (redox) reactions. The redox processes that occur as a result of carbohydrate <br /> addition can be monitored by analyzing the oxidized and reduced species of electron <br /> acceptors in groundwater. <br />