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FFnd <br /> ation test was done at the ground surface, which represents the soil-effluent interface of <br /> water mound osal system. As the soil became saturated, infiltration slow by <br /> ately a-half over a duration of the test. This is illustrated on the Infiltration Test <br /> ' Appendix !Test results indicate an infiltration rate comparable to the observedn r ouble ring infiltration test results are summarized below: <br /> TABLE 3 <br /> INFILTRATION TEST RESULTS <br /> INFILTRATION RATE IN <br /> CM/11R,CM/SEC,MINAN AND APPLICATION RATE IN GALLONS/FT'/DAY <br /> 12.24 cm/hr,0.0034 cm/sec, 12.5 min/in,0.757 gallons/ft /day <br /> Application Ram adapted from California State Water Resources Control Board Guidelines for the Design ofSeemge Systems and is based on the Pen Race. <br /> D. GROUNDWATER INFORMATION <br /> NLS§(2�, SS§ .1, NL 2.1. ,Groundwater depths and elevations throughout San Joaquin <br /> Coune lu ated on maps published by the County Flood Control and Water Conservation <br /> District. However, due to the high degree of variability in groundwater elevations in the Tracy <br /> area, groundwater lines of equal depth and equal elevation are not drawn for this area. The last <br /> map denoting lines of equal elevation for the Tracy area was published in 1992, and show the <br /> general groundwater flow to be in a northeasterly direction, toward the San Joaquin River. This is <br /> regarded as the generalized groundwater directional flow, primarily based on highly accurate <br /> groundwater studies at the Tracy Defense Depot. <br /> The referenced domestic well,which is approximately 250 feet from the proposed mound disposal <br /> area,was sounded with the standing water level measured at four feet. During the drilling of the <br /> 40-inch deep perc test boring, no capillary fringe water was encountered. <br /> A geotechnical investigation conducted by the firm Construction Testing and Engineering, Inc. <br /> measured the groundwater table to be at seven feet in October 2005 in the proposed locatio f the <br /> new Church building. This groundwater depth measurement occurred after irrigation season, o <br /> the potential may exist for the water table to rise higher during the irrigation ason. A wate table <br /> depth of seven feet would preclude the installation of a conventional, or semi-co do <br /> leachfield system. This is due to the required separation distance of five feet that must be <br /> maintained between the soil-effluent interface and the highest depth to the groundwater table. <br /> Unfortunately, no well log was found in EHD files for the referenced domestic well _o-underlying <br /> lithology could not be determined. In addition,the well had no electricity to it, save 1 water could <br /> not be sampled and tested to determine nitrate loading impacts from historical land uses, or to us <br /> in the nitrate loading calculations. <br /> 6 <br /> Chesney Consulting <br />