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[3] PROPOSED DEVELOPMENT OF THE SUBJECT SITE <br /> As referenced, it is proposed to divide a 53 acre parcel into a 51 acre Designated Remainder and a <br /> 2 acre Parcel 1. It is our understanding there is to be no development or improvements made to the <br /> Designated Remainder and no future development of Parcel 1. Any related septic system structures <br /> and the domestic well must comply with published "distance" requirements. <br /> [4] SOIL PROFILE AND PERCOLATION TESTING <br /> The predominate soil type from grade to 3 ft is a clay soil with a high organic matter content. The <br /> soil type changes to a light brown, silty clay at four feet. A hardpan layer was not encountered in <br /> the drilling procedures. The well logs illustrate there are intermittent clay layers between grade and <br /> the depth to drinking water aquifers. <br /> The perc test boring was set at four feet below existing grade to illustrate the depth effluent <br /> percolation or the "wetting front" that will occur in native soil. From the perc test results, it was <br /> determined this four foot depth produces acceptable percolation rates. <br /> Our percolation tests were conducted according to San Joaquin County Department of <br /> Environmental Health regulations. The Field Test Data Sheets can be found in the Appendix. The <br /> perc test was conducted on January 14, 1999 in the location specified on the Tentative Map. <br /> However,after this date, it was decided to change the lot line to the south of the hay shed. Although <br /> the perc test was not officially conducted on Parcel 1, it is our opinion there would not be significant <br /> soil changes in the short distance from the north side of the shed to Parcel 1. Secondly, there are no <br /> plans to build another structure on Parcel 1, where it would be prudent to conduct the test. <br /> Although the indigenous soil are clay, the comparatively fast perc rate obtained can be attributed <br /> primarily to the alfalfa roots at the perc test depth. Also the clay soil was moist which can promote <br /> faster perc rates. <br /> [5] LOCAL GROUNDWATER AND SURFACE WATER INFORMATION <br /> The groundwater,or the zone of saturation is located at approximately 8 ft below grade. There was <br /> no evidence of a perched water table condition during our perc boring procedures. The property is <br /> subject to the 100 yr flood zone A25 (Elevation 20)per flood insurance rate map, community panel <br /> No. 060299 0570 B, dated July 4, 1988. <br /> vaffey Ag P pearck <br />