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soils that are weakly to strongly cemented. The soil survey indicates that for septic tank <br /> absorption fields, the slow permeability can be overcome by increasing the size of the <br /> absorption field, backfilling trenches with coarse material, and installing long absorption <br /> lines. <br /> Additional information provided by the USDA-Soil Conservation Service <br /> (Appendix B) indicates that Stockton clay from this area has a very high cation exchange <br /> capacity (CEC) varying from 45 to 60b meq/100g. The significance of the CEC to adsorb <br /> ammonia-nitrogen will be discussed later in Section 6.0. <br /> 3.2 REGIONAL HYDROGEOLOGY <br /> Information on the regional hydrology was obtained from the Department of Water <br /> Resources (DWR) and from local well drillers. Maps maintained by the DWR Central <br /> District Office indicate that the depth to water in wells in the area varies seasonally and <br /> has been historically increasing (i.e., the water table has been dropping). The water level <br /> in the fall is approximately 10 feet lower than the level in the spring. The reported depth <br /> to water in the Spring of 1993 was 75 feet, and the reported direction of flow was to the <br /> southeast. <br /> First groundwater in the vicinity of the property is encountered at approximately <br /> 90 feet bgs. Standing water in completed wells is approximately 80 feet bgs. A second <br /> aquifer is encountered at approximately 120 to 130 feet bgs. The DWR considers both <br /> these aquifers to be in hydraulic communication. Older residential wells in the area may <br /> be completed in either the shallow or intermediate aquifer (less than 130 feet bgs). <br /> Newer residential wells must have the borehole sealed to 100 feet bgs and so are <br /> generally completed to deeper aquifers. <br /> Water in the upper aquifer is of good quality, but the water has higher salt levels <br /> than are found in deeper aquifers. The agricultural chemical dibromochloropropane <br /> (DBCP) is often present in the upper aquifer in areas that have been utilized for growing <br /> grapes. <br /> a <br /> 3.3 GROUNDWATER CHARACTERISTICS <br /> i <br /> The DWR periodically samples wells in San Joaquin County for nitrates and other <br /> parameters. Data from 1969 to 1993 for the three wells closest to the property were <br /> reviewed at the DWR central District. None of the wells had nitrates above the drinking <br /> SAC 125.12 3 <br /> DAMES &MOORE <br />