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✓ On March 5, 1000 hours, percolation testing commenced for the two borings. There was no <br /> standing water in the test borings after the soak period. The initial volume of water did not seep <br /> away in the first 30 minutes at the start of the percolation tests for the test borings. <br /> Consequently,Percolation Test Procedure#2 was used in which perc readings for the two <br /> borings were taken over a four-hour test period to ensure maximum soil saturation under"worst- <br /> case scenario" conditions. The two perc tests exhibited identical and mediocre percolation rates <br /> for both parcels. The last half hour of the tests was witnessed by Michael Escotto of the San <br /> Joaquin County Environmental Health Department. <br /> The following chart summarizes and illustrates the parcel number,proposed acreage and perc test results: <br /> PROPOSED PARCEL PROPOSED ACREAGE PE ST RESULTS <br /> Parcel 1 7.89 Acres 35.7 min/in @-4d inches depth <br /> Parcel 2 5.00 Acres 5.7 min/in @ inches depth <br /> LOCAL GROUNDWATER AND SURFACE WATER INFORMATION <br /> The 1999 Lines of Equal Elevation Map published by the San Joaquin County Flood Control <br /> illustrates the groundwater elevation and the directional flow. It appears, and is generally <br /> accepted, that the groundwater is flowing in a north-northwest direction toward the San Joaquin <br /> River; however, at the intersection of Small Road and French Camp Road, the groundwater flow <br /> appears to be in a northeast direction. The 1999 Lines of Equal Depth Map illustrate the <br /> groundwater depth to be 27 feet below ground surface. <br /> A Well Driller's Log for a domestic well on South Small Road, directly to the southwest was <br /> available to illustrate the underlying soil lithology. Interestingly, the well log shows clay from 5 <br /> feet to 57 feet below grade. Consequently,perched water table conditions probably do not exist <br /> at higher elevations than the existing water table. From the 57400t depth on down to the well <br /> depth of 160 feet,there are intervening strata of sand and clay. <br /> Considering that the soil was saturated from this winter's heavy rainfall and pre-saturation, there is <br /> an extremely remote possibility of the surfacing of effluent from inundated conditions caused by <br /> flooding. The porosity of the subsurface soils as evidenced from the percolation test results should <br /> allow for adequate drainage. The subject property is not subject to the 100-year flood. <br /> It will be a reglement of EHD to install a 200-foot snout seal due to the proximity of the property <br /> to-the-Sharpe Army Depot. A water sample was obtained from a hose bibb 75 f .t w of h . <br /> domestic well and tested for nitrate and the agrichemicals DBCP/EDB. The nitrate water sample <br /> was placed in a plastic bottle and the DBCP/EDB sample was placed in a VOA with preservative. <br /> Both samples were placed in a cooled ice chest and subsequently delivered to A&L Labs in <br /> Modesto under the attached Chain of Custody. A low nitrate concentration of 11 ppm was <br /> determined in the well water and DBCP/EDB was non-detect. The depth of the sampled domestic <br /> well is unknown. <br /> Page -3- <br /> Chesney Consulting <br />