Laserfiche WebLink
in the Victor formation is unconfined. The groundwater monitoring wells sample <br /> water from the Victor formation. Most wells penetrate through the Victor <br /> formation into the underlying formations to obtain higher water quality and <br /> better flow characteristics. <br /> The Laguna formation of Pliocene age consists of stream laid sand and clay <br /> (3) . It contains discontinuous lenses of unconsolidated to semi-consolidated <br /> sand and silt with lesser amounts of clay and gravel . The boundary between <br /> the Victor and Laguna formation at the site is at approximately 150 ft. In <br /> the well drillers report log for the QAP plant wells included in the appendix, <br /> a clay layer approximately 100 ft thick is evident between 50 and 150 ft. <br /> Alternating layers of sand and clay below 150 ft are part of the Laguna <br /> formation. <br /> The Victor and Laguna formations constitute an upper aquifer system. The <br /> confining layer separating the upper aquifer from the lower Mehrten formation <br /> prevents hydraulic continuity between these systems. <br /> Groundwater Ouality Monitoring Program <br /> QAP installed three groundwater monitoring wells in August 1985 to comply with <br /> the Regional Board reporting program under Order 85-149. The monitoring wells <br /> terminate at approximately 90 ft. Free groundwater was encountered in each <br /> well at approximately 70 ft below existing ground surface. Monitoring well <br /> samples are analyzed quarterly. Resulting data is included in the appendix. <br /> Figure 2 shows the location of the three monitoring wells installed under <br /> Order 85-149. Water quality in the shallow groundwater samples obtained from <br /> the monitoring wells is characterized by a high nitrate content, indicating <br /> contamination from agricultural fertilizers. Table 1 shows average nitrate <br /> concentration and average conductivity data for the three monitoring wells. <br /> Table 1 <br /> WATER QUALITY PARAMETERS IN MONITORING WELLS <br /> Nitrate Conductivity <br /> Year m 1 (umhos/cm) <br /> 1985 69 1,070 <br /> 1986 89 1,010 <br /> 1987 74 1,100 <br /> 1988 71 1,060 <br /> In addition to the monitoring wells installed in 1985 a domestic well <br /> monitoring program was established at the request of Edward Steffani of the <br /> Stockton East Water District. Five domestic wells in the immediate vicinity <br /> of the plant are sampled and a Title 22 chemical analysis is performed every <br /> quarter. Well locations for the domestic well monitoring program are shown in <br /> Figure 4. <br /> 1-6 <br /> RP033-L <br />