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Former Beacon Station No 12 574 June 7,2005 <br /> Stockton California Results of Additional Groundwater Assessment <br /> • Quarterly groundwater monitoring data from the first quarter 2005 indicate the highest <br /> concentrations of TPHg in monitoring well MW-12 Seasonal fluctuation of TPHg and <br /> benzene and the relationship to the groundwater level for monitoring wells MW-3 through <br /> MW-17, air sparge well AS-1, and vapor wells VW-1 and VW-4 are shown on concentration <br /> versus time graphs I through 34 <br /> The distribution of TPHg in groundwater is delineated to the north and east by monitoring <br /> wells MW-4 and MW-8 Delineation to the west and south of the dispenser island area is <br /> not indicated by current data However, concentrations of TPHg in groundwater decrease by <br /> 2 to 3 magnitudes from the dispenser island area to monitoring wells MW-10 to the west and <br /> MW-9 to the south Concentrations of TPHg in groundwater samples collected in the first <br /> quarter 2005 from the monitoring wells MW-7 and MW-9 indicate that the impacted <br /> groundwater extends to approximately the south property line The distribution of benzene <br /> in groundwater, as shown on Figure 8, is delineated to the north by MW-4, to the east by <br /> MW-8, to the south by MW-11 and to the west by MW-I0 <br /> Fate and Transport of Petroleum Hydrocarbons in Soil and Groundwater <br /> Petroleum hydrocarbons possibly released from UST systems enter vadose zone soils <br /> Petroleum hydrocarbons released to vadose zone soils migrate generally downward, under <br /> the force of gravity A portion of the hydrocarbons released in the vadose zone adsorb onto <br /> soil particles and contribute to relatively stationary, secondary soil sources Fine-grained <br /> soils, which are predominant at the site (see Figures 3 and 4), tend to decrease migration <br /> rates and, when laterally discontinuous and interbedded, may introduce a lateral component <br /> to the downward migration <br /> Petroleum hydrocarbons that migrate downward to the capillary fringe and water table tend <br /> to dissolve in the groundwater and migrate by advection generally south-southeastward with <br /> the groundwater although generally at a lower rate Physical dispersion and molecular <br /> diffusion act on the dissolved hydrocarbon constituents to dilute concentrations and tend to <br /> Addtn1GWassmnt <br /> Project No 1474 15 9 HORIZON ENVIRONMENTAL INC. <br />