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a <br /> Ground water samples were collected from all borings and tested for purgeable <br /> hydrocarbons (EPA method 602) and gasoline (using GC/FID). Ground water analytical <br /> data is given In Table 2. The perched ground water also displays low concentrations of <br /> gasoline and benzene, and slightly higher levels of toluene, xylene, and ethyls benzene. i <br /> The highest levels of gasoline and ethyls benzene are in boring#3, benzene and toluene <br /> Is in boring #o. and xylene Is in boring #1. <br /> Contours of gasolfi-,c In water and soil are shown In Plate 2 and benzene in water in Plate <br /> 3. For tie most part, the various components have a similar NE-SW elongated <br /> disiribudon pattern, with water contamination being a little more widespread then soil. <br /> Xylene in the water h<<s the widest distribution. Cross sections (Figures S, 4 & 5) <br /> through the study area show the vertical and lateral distribution of contamination and <br /> how they correlate with the analytical data. <br /> State allowable limits for the various volatile organic compounds (VOC) detected by lab <br /> r analyses during this study are listed in Table 3. Three of the five compounds detected are <br /> above the action level set by the state for drinking water or waters with potential <br /> i.� domestic use. Even though this shallow water is not used for domestic purposes,the <br /> county may require remedial action because of the close proximity of a city well. <br /> Surface water eventually percolates down to deeper depths and may be incorporated into s <br /> drinking water aquifers. <br /> Conclusions <br /> The conclusions of this study are briefly listed below. <br /> 1) There Is a bimodal distribution of the stratigraphy of the site: sand dominates the <br /> upper 7 to 9 feet, while clay dominates below that horizon. <br /> 2) The top 3 to 4 feet predominantly contain fill material (sand, silt, clay, & gravel) <br /> w plus debris like wood, metal, and cement. <br /> 3) The first ground water occurs at the shallow depth of 12.5 to 13 feet. <br /> 4) Due to artificial recharge of the ground water from leakage of the irrigation pipes <br /> located on the north side of the property, this shallow ground water flows to the <br /> south (regional gradient is to the north) and is in abundant supply. <br /> 5) Soil contamination is very low and is restricted to a shallow depth (about 10 to 15 <br /> feet) in the area around the previous tank location (<5 feet thick & <50 feet radius). <br /> Microbial degradation will continue to reduce the contamination level and remove <br /> the hydrocarbons from the environment. <br /> 6) Ground water contamination is present at very low levels and is restricted to a thin <br /> sandy unit about 2 t 3 feet thick (from about 12 to 15 feet in depth). This perched <br /> water table is underlain by a fairly impervious clay unit (aquitard) that will <br /> __.---.____.___greatly_.retard-vertical-migration-of-both-ground-water-and-the-contaminants.–As-with----------=----:- - —=— <br /> soil contamination, the already low contamination levels are steadily decreasing <br /> through the microbial degradation process. <br /> ;J <br /> t3 <br />