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1 � 1 <br /> ., as <br /> kn KLEINFELDER <br /> FIELD EXPLORATIONS AND TESTING <br /> The subsurface conditions at the site were explored on February 26, 2002, by drilling one boring <br /> to a depth of approximately 10 feet below existing grade. The boring was drilled using a Simco <br /> 2400 truck-mounted drill rig equipped with 4-inch O.D. solid-stem auger. During the same time <br /> period, percolation borings were drilled to depths of about 3.5 and 4.0 feet below site grade. The <br /> location of the percolation tests is approximately 100 feet west of a private well on the project 2� <br /> site. The approximate percolation test locations are presented as P-1 and P-2 on the attached p <br /> plate. 0 <br /> Based on our findings, the subsurface soils encountered consisted of brown to gray/brown sandy , <br /> clays with gravel to a depth of about 2 feet below site grade, underlain by brown sandy clay to a <br /> depth of about 4 feet. These soils were underlain by light brown sandy clays to a depth of about ur s LPK G <br /> 8 feet, followed by sandy silts to the depth explored. <br /> The percolation tests were performed on—Marc1L6.,2 0�2, in accordance with accepted guidelines $� 91 <br /> using clear potable water. The procedure calls for first placing about 2 inches of fine gravel at <br /> the bottom of the bore hole. The hole is then pre-soaked with water at least 24 hours prior to <br /> performing the test. The test is performed by first adding about 6 inches of water per 3 foot of <br /> percolation test depth above the gravel to the hole. From a fixed reference point, the drop in <br /> water level is measured in approximately 30-minute intervals for four hours, refilling as <br /> necessary to maintain the prescribed amount of water over the gravel. Under the observation of <br /> a sanitarian from the San Joaquin County Public Health Services, Environmental Health Division <br /> (SJCPHS/EHD), the last 30-minute reading of the four hour period is recorded and used to <br /> calculate the percolation rate in minutes per inch. The estimated percolation rates are <br /> summarized below. A copy of our field percolation test results signed by a representative from <br /> SJCPHS/EHD is attached. <br /> if itt, E NIC6l`atlon`Rate min./inch <br /> ,fie b P-1 3.5 63 ' y <br /> P-2 4.0 17 .U-Z) <br /> Following our percolation testing, a staff engineer with our firm obtained a sample of <br /> groundwater using clean procedures from a spigot ne eon-site wel The well was located <br /> approximately 200 feet north of that parcel's southeast corner. The same day, the water sample <br /> was submitted to Sequoia Analytical using chain-of-custody procedures for DBCP and nitrate <br /> testing. The results of our tests and a copy of the chain-of-custody are attached. <br /> NITRATE LOADING CALCULATIONS <br /> Per SJCPHS/EHD requirements, the following summarizes our nitrate loading calculations for <br /> the proposed leach field. The State drinking water standard for nitrate is 45 milligrams per liter <br /> (NOO and 10 mg/1 as Nitrogen (N) in groundwater. In our evaluation of nitrate loading, we have <br /> used the Hantzsche mass balance equation (source: Predicting Ground-Water Niirate-Nitrogen <br /> 12573/2002R320 April 16,2002 <br /> ©2002 Kleinfelder,Inc. Page 2 of 4 <br />