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Supplementary Site Assessment Report <br /> Former Mobil Bulk Plant 04-343 <br /> April 26, 1996 <br /> ' • Groundwater elevation has remained relatively constant at approximately 20 feet above <br /> mean sea level [NGVD-1929]; approximately 11 fbg. The gradient is generally to the north <br /> ' at 0.01 foot-per-foot. <br /> • During the past three quarters, no benzene has been detected in any well above Title 22 <br /> ' of the California Code of Regulations maximum concentration limit (MCL) for drinking <br /> water (1 ppb). Dissolved-phase TPH-G has been detected only in AW-3, at concentrations <br /> less than 100 ppb. Low to moderate concentrations of TPH-D have been detected in AW-1 <br /> ' through AW-5, and AW-12 during the past three quarters (Table 2)_ <br /> • The results of the background groundwater analysis are summarized in Table 3 and <br /> ' discussed below in Section 5.2.1 <br /> 5.2 BIOREMEDIATION PARAMETER STUDY <br /> ' The purpose of this study is to evaluate the feasibility of enhancing biodegradation radation of <br /> hydrocarbon-affected soil and groundwater using an oxygen-releasing compound. Hydrocarbon- <br /> degrading microorganisms are widespread in the environment and occur in fresh and salt water, <br /> soil, and groundwater. Bacteria are the most numerous and biochemically active group. There <br /> exist hundreds of known hydrocarbon-degrading bacteria. Bacteria require a carbon source for <br /> ' cell growth and an oxygen source to sustain metabolic functions required for growth. Nutrients, <br /> including nitrogen and phosphorous are also required for cell growth. Bacteria that use organic <br /> ' compounds such as petroleum as their source of carbon are heterotrophic, and those that use <br /> oxygen are aerobic (EPA, 1995). <br /> Hydrocarbon degradation is essentially an oxidation-reduction reaction where the hydrocarbon <br /> ' is oxidized (donates electrons) and an electron acceptor (e.g. oxygen) is reduced (accepts <br /> electrons). There are a number of different compounds that can act as electron acceptors <br /> ' including oxygen, nitrate, iron oxides [Fe(OH)3], and sulfate. Dissolved oxygen (DO) is the <br /> most thermodynamically favored electron acceptor used in the biodegradation of petroleum <br /> hydrocarbons, and it also is the food source for the enzyme that can initiate the metabolism of <br /> ' hydrocarbon (Young, 1984). Under the right chemical conditions, the introduction of oxygen <br /> to hydrocarbon-affected groundwater can stimulate the growth of indigenous microbes and <br /> accelerate their metabolism of petroleum hydrocarbons. Metabolism of soil hydrocarbons present <br /> 1 below the static groundwater level may also benefit from the oxygen enhancement process and <br /> result in hydrocarbon concentration reduction. This process is dependent on various factors in <br /> addition to the electron acceptors described above, including the presence of an appropriate <br /> microbial population, nutrients, and pH. <br /> On August 16, 1995, additional groundwater samples were collected from Monitoring Wells <br /> AW-3 and AW-9 as part of the study. A summary of these background water analyses is <br /> presented in Table 3. These wells were selected in order to compare groundwater within a <br />;, 5 <br />