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' Aquifer Testing Work Plan • <br /> Formerrth GroBroadway <br /> Facility <br /> 1905 North Broadway Avenue - <br /> ' Stockton,California <br /> Sierra-Pacific Project No. 94-055.05 <br /> ' Yellowish-brown silty sand(SM)was intercepted from about 52 to 65 bgs,and clayey-sand(SC)from <br /> about 65 to 70 bgs. The clayey-sand sequence is underlain by a thin layer of reddish-brown clay (CL). <br /> ' The documented presence of fertilizer and pesticide compounds at 70 feet bgs indicates that these clayey <br /> ' stratigraphic units are laterally discontinuous and thus incapable of stopping possible downward <br /> migration of surface waters containing elevated levels of pesticide or fertilizer compounds. <br /> ' 3.2 Ground Water <br /> ' The facility lies within the confines of the lower San Joaquin River drainage. The terrain is flat, and <br /> surface waters generally flow westward. Most surface runoff in the east Stockton area ultimately reaches <br /> the San Joaquin River during periods ofheavy precipitation. The northwest-oriented Stockton Diverting <br /> Canal lies approximately 500 feet northeast of the facility. The unlined diversion canal is a major <br /> ' ground-water recharge area. Water levels measured at the subject site have risen as much as 30 feet <br /> since 1993 due to ground water infiltration along the Stockton Diverting Canal. <br /> The site has four monitoring wells. Six other monitoring wells, located west of the subject site, are <br /> ' included in the monitoring well array. The well array has been monitored quarterly since May 1993. <br /> Ground water moves laterally within discontinuous sandy formations. Discontinuous beds (layers) of <br /> ' clayey sediment tend to restrict vertical(downward)migration of ground water. <br /> ' 3.3 Surface Water <br /> The facility lies within the lower San Joaquin River watershed. The nearest body of surface water to the <br /> ' site is the unlined Stockton Diverting Canal. The Stockton Diverting Canal has flowed continuously <br /> since early 1995. Surface water flowing northwest in the canal either percolates to the uppermost <br /> saturated zone or continues to flow to the lower San Joaquin River near the Port of Stockton. Levees <br /> which confine the Stockton Diverting Canal are well above the level of the PureGro Stockton facility. <br /> ' Storm water runoff from the site can not enter the canal. The City of Stockton maintains a network of <br /> ditches and storm drains which ultimately discharge into the San Joaquin River. Shallow drainage <br /> ' ditches are present along the west boundary of the facility on both sides of Report Avenue. <br /> SIERRA-PACIFIC GROUP 4 <br />