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3.2 Description of the mass transport properties of the soils underlying the site with respect <br /> to the nitrate and/or any other constituent of concern identified for the project site: The <br /> results from the percolation test prepared by Joel Montano of Dillon& Murphy have determined <br /> that the site is permeable to a maximum depth of exploration of 42 inches. The soil type allows <br /> for infiltration of water through the top soils. The infiltration rate will limit the natural treatment <br /> of the sites soils as they drain from the surface layers. <br /> The soil survey by US Department of Agriculture (USDA) indicates that the site is composed of <br /> Hollenbeck silty clay. The Hollenbeck silty clay is composed of 10 inches of silty clay, followed <br /> by 27 inches of clay, followed by 5 inches of silty clay loam, and followed by 18 inches of <br /> cemented soil. <br /> 4.0 GROUNDWATER ANALYSIS <br /> 4.1 Description of the depth to groundwater, seasonal fluctuations of groundwater depth, <br /> directional flow and gradient: Description of depth to groundwater, seasonal fluctuations of <br /> groundwater,directional flow and gradient are referred to in Section 4 of the Soil Suitability Report <br /> prepared by Dillon&Murphy that is attached in the Appendix. <br /> 4.2 Description/discussion of any existing and/or potential groundwater <br /> contamination issues in the general location of the site: Description of existing or potential <br /> groundwater contamination issues in the general location of the site are referred to in Section 4.2 <br /> of the Soil Suitability Report prepared by Dillon& Murphy (See Appendix). <br /> 4.3 Description of the current use of groundwater at the site and of the future expected use <br /> of groundwater as related to the proposed development project: <br /> Based on the most recent results from San Joaquin County's "Flood Control and Water <br /> Conservation District" report on groundwater from Fall of 2017, the estimated depth to <br /> groundwater was determined to be 110 feet below the surface. This was verified with the <br /> California Department of Water Resource's Water Data Library. The results of the historic depth <br /> to ground water show that the relative depth has not changed drastically throughout the years. It <br /> fluctuates minimally on a yearly basis. The proposed improvements will not have a negative effect <br /> on the current depth to ground water as the proposed usage is less than that of agriculture. See <br /> appendix for the site's depth groundwater tables and diagrams. <br /> 5.0 SOURCES AND CALCULATED IMPACT OF NITRATE TO <br /> GROUNDWATER <br /> 5.1 Description of all current off-site sources of nitrate to soil and groundwater in the general <br /> up gradient area and the contribution of nitrate load from these sources to the project site: <br /> Current off-site source of nitrate to soil and groundwater in the general up gradient area and the <br /> contribution of nitrate loads are agriculture and neighboring sites with septic systems with minimal <br /> to no current impact to the site. The site does have an existing module office, a welding shop and <br /> building for storing farming equipment which were accounted for when determining the capacity <br /> for the proposed improvements. The neighboring sites do not pose a significant impact to nitrate <br /> 2 <br />