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I <br /> TEMA VAC <br /> Nutrients <br /> G a Both organic and inorganic nutrients must be available to support bio-activity in soil and <br /> groundwater. Petroleum hydrocarbons and carbon dioxide are examples of organic nutrients. <br /> Analytical data from the fourth quarter sampling event indicates the presence of petroleum <br /> hydrocarbons in all but three of the monitoring wells. Fourth quarter 1996 analytical data are <br /> summarized on Appendix A. Microorganisms that derive their carbon source and energy for <br /> synthesis from organic carbon are called Chemoheterotrphs. <br /> Analytical data indicate detectable concentrations of several inorganic chemicals that serve as <br /> yt g <br /> nutrients that promote bio-activity (summarized on Table 1). These include Oxygen, Nitrates, <br /> ortho phosphate (the soluble form of phosphorous), and ferrous iron (Balser, p 101). Oxygen, <br /> nitrate and ortho phosphate are considered to be the most important inorganic nutrients to <br /> support bio-activity. Ferrous iron is also a required nutrient, but to a lessor extent. <br /> Microorganisms break down organic compounds (carbon and energy source) by a complex <br /> oxidation-reduction series of reactions. The process involves the oxidation of organic compounds <br /> 3 coupled with the terminal reduction of inorganic compounds (Baker, p 16). Under aerobic <br /> a conditions, oxygen is the preferential terminal reduction acceptor (McAllister, p 162). However, <br /> as DO is depleted (anaerobic conditions) from groundwater, nitrate and sulfate become the <br /> preferential terminal reduction acceptors. Anaerobic biodegradation has been found to be less <br /> efficient and therefore slower than aerobic biodegradation(McAllister, p 163). <br /> f Table 2 shows the generalized relationship of benzene to nutrient availability if bio-activityis <br /> occurring in groundwater <br /> TABLE 2 <br /> Benzene Oxygen Nitrates Ferrous Tran Sulfates <br /> high low low high low <br /> low high high low high <br /> FINDINGS and CONCLUSIONS <br /> Utility Survey <br /> Available data indicate that the storm drain is the deepest of the subsurface facilities, <br /> approximately S feet below Country Club Boulevard. The trunk that runs along Franklin appears <br /> { <br /> to be shallower. Gradient of the storm drain is to the south. <br /> The sanitary sewer appears to be shallower than the storm drain piping at Country Club, but <br /> becomes deeper going north. Gradient of the sanitary sewer is to the north, along Franklin Ave. <br /> Project 30-0212 <br /> r April 17, 1997 <br /> 4 <br />