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boring were prepared on each of the four proposed parcels. Each test boring was pre-saturated <br /> the day before perc testing, In addition to pre-saturation, the shallow test borings were scarified <br /> to open smeared soil surfaces within the hardpan stratum caused by the drilling process. There <br /> was no standing water in any of the test borings after the 24-hr pre-saturation period, except the <br /> shallow test borings on parcels 3 and 4. <br /> As indicated on the attached FIELD PERCOLATION TESTING REPORTS, the shallow perc <br /> rate for parcel 2 was the only shallow test to have acceptable percolation. All four deep perc <br /> tests passed with relatively rapid rates. These deep perc rates illustrate the larger porosity of the <br /> underlying sand and gravel strata. The perc test results are summarized below for each of the <br /> four proposed parcels: <br /> PERCOLATION TEST RESULTS <br /> PARCEL No SHALLOW t42")PERC RATE IN MIN/INCH PARCEL No DEEP(25')PERC RATE IN MINANCH <br /> Parcel 1 75 min/in (Failed) Parcel 1 42 min/in <br /> Parcel 2 21,4 min/in Parcel 2 6,$ min/in <br /> Parcel 3 0 min/in (Failed) Parcel 3 4.6 min/in <br /> Parcel 4 0 min/in (Failed) Parcel 4 12 min/in <br /> III. NITRATE LOADING STUDY RESULTS <br /> A. GROUNDWATER INFORMATION <br /> 1. GROUNDWATER GRADIENT, VELOCITY AND ANALYSES <br /> The static water level under the center of the project is located approximately 120 ft below grade <br /> according to the 1999 Lines ofEquol Depth Map published by the San Joaquin County Flood <br /> Control District. The 1999 Lines of Equal Elevation map illustrate the groundwater to be <br /> approximately -30 ft MSL. Additional data was obtained from the attached 2000 Groundwater <br /> Contour and Monitoring Well Location Map for the Harney Landfill. This report indicates the <br /> groundwater elevation to be approximately -20 ft MSL. The 1992 Lines of'Equal Elevation map <br /> illustrates the groundwater to be -40 ft MSL. Therefore, the static groundwater level appears to <br /> have risen 20 feet in the past nine years. <br /> Groundwater directional flow is in a south-southeasterly direction according to the Groundwater <br /> Contour map. From this map, it appears the gradient is to the south near Harney Lane, and then <br /> changes to a southeasterly direction at the south end of the Landfill. <br /> 4 <br />