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Supplemental Investigation Report <br /> BP Oil Site No 11193 <br /> C A M B R I A Stockton, California <br /> October 13, 2000 <br /> Fate and Transport Modeling Fate and transport modeling was performed to evaluate the potential <br /> for BTEX and MTBE migration to the Caltrans well The AT123D model modified for input of <br /> source concentrations rather than a mass loading was used The primary assumptions of the model <br /> include (1) the aquifer thickness is homogeneous, isotropic, and comprised of a single, horizontal <br /> layer of uniform thickness, and (2) the hydraulic gradient is uniform and constant within the model <br /> domain <br /> Input parameters were estimated from the previous hydraulic testing, groundwater monitoring and <br /> other available data These parameters are presented in Appendix H and summarized on the tables <br /> below <br /> Table A— Model Input Parameters <br /> Parameter Value Comment <br /> Hydraulic conductivity 0 39 meters per day Site maximum from hydraulic testing <br /> Hydraulic gradient 0 007 northeastward July 14, 2000 monitoring event with <br /> extended well network <br /> Effective porosity 030 Typical of silty sand <br /> Bulk density 17 grams per milliliter T real of silty sand <br /> Fraction of organic carbon 00005 Analytical results from boring C13-4 <br /> Constituent Concentration Benzene 0 084 mg/1 Maximum reported during <br /> Toluene 0 002 mg/l July 14, 2000 monitoring event <br /> Ethylbenzene 0 015 mg/1 <br /> Xylenes 0 018 mg/l <br /> MTBE 250 mg/l <br /> The release of BTEX and MTBE was simulated in the model by introducing a steady concentration <br /> over a fixed time interval and source area A source duration of 5 years was used based on the interval <br /> between the initial reports of MTBE in 1993 and tank replacement in 1998 The source area was <br /> assumed to encompass the entire UST complex with dimensions of 1 meter thick by 10 meters long <br /> by 10 meters wide The model simulated migration over 100 years, calculated dispersivity values and <br /> assumed no degradation of these constituents <br /> 12 <br />