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r. KLEINFELDER <br /> L <br /> Based on our findings, the subsurface soils encountered consisted predominately of fine-grained <br /> Lsilty sand to a depth of about 8'/2 feet below the existing ground surface, underlain by low- to S <br /> moderately-plastic sandy silt to a depth of about 12 feet. These soils were further underlain by <br /> moderately-plastic sandy clay to the maximum depth explored. Groundwater was not <br /> Lencountered in the test boring. Detailed descriptions of the subsurface conditions encountered <br /> during our field investigation are presented on the Log of Boring presented on Plate 5. <br /> LThe Soil Survey of San Joaquin County, California published by the U.S. Department of <br /> Agriculture, Soil Conservation Service (1992) refers to the near-surface soils within the project S <br /> area as belonging to the Veritas soil series (map symbol 266). These soils are described as <br /> Lhaving "moderate" percolation characteristics for septic tank absorption fields. The soils are <br /> listed to have an available water capacity of 0.12 to 0.15 inches/inch, a pH ranging from 7.4 to <br /> 8.4, and an organic content of 1 to 2 percent. <br /> 1 <br /> V <br /> 6. PERCOLATION TESTING G t <br /> z <br /> L Three 6-inch diameter percolation holes were drilled using solid-stem auger. The approximate <br /> test locations and approximate dimensions from a reference point are presented on Plate 1. The <br /> Lholes were drilled and prepared between 7 and 8 am on May 10, 2004 in accordance with <br /> SJCEHD criteria. Approximately 2 inches of fine gravel were placed at the bottom of each test 3 <br /> hole. The holes were then pre-soaked with a minimum of 12 inches of water at least 24 hours <br /> L <br /> prior to performing the test. The holes were originally presoaked on May 10, 2004 soon after <br /> drilling. The percolation tests were started at about 9:00 am under sunny and warm weather on <br /> May 11, 2004, in accordance with accepted guidelines using clear potable water. The <br /> Lapproximate depth below existing site grade of each percolation test is shown on the following <br /> table. The holes had scored sides and no significant loose material at the bottom. No standing <br /> ,_4 <br /> water from presoaking remained in any of the test holes at the time of testing. From a fixed <br /> L <br /> reference point, a marked location on the side of PVC pipe inserted into the hole, the drop in <br /> water level was measured in approximately 30-minute intervals for four hours, refilling as <br /> necessary to maintain the prescribed amount of water over the gravel (SJCEHD Procedure #2). <br /> LUnder the observation of a representative from the SJCEHD, the last 30-minute reading of the <br /> four-hour period was recorded and used to calculate the percolation rate in minutes per inch. <br /> The estimated percolation rates are summarized below. A copy of our field percolation test <br /> 6. results signed by a representative from SJCEHD is attached. Details of each test can be found on S <br /> the field percolation test sheets. 1' <br /> r. Test Number Performed Depth (feet) Percolation Rate (min./inch) <br /> P-1 3.4 8.1 <br /> P-2 3.4 4.9 <br /> 6. P-3 3.4 2.1 <br /> L <br /> L44419.G01/ST04R785 June 8,2004 <br /> ©2004 Kleinfelder,Inc. Page 3 of 6 <br /> L <br />