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y <br /> t e zonal ;Fater Quality. control <br /> µ- method has been accepted by he = 9 ,t other <br /> Board for samp3ing <br /> and che:�ical analyses of soils <br /> locations in San Joaquin County• <br /> 5 foot intervals, beginning at <br /> wSoil samples -„ere collected at inserted <br /> 5 ft, y sampler <br /> 5 feet, through a depi;h of ° with ale Upon retrieval, <br /> filling tool removal• <br /> hydraulically after dr - gist for <br /> SSB field geolo <br /> soil samples were described Y an for chemical <br /> lithology and color. prior to sannle submission with a model <br /> x-a res soil Samples <br /> were screened <br /> and physical analyse r res�nce <br /> nd photoionizatio^ detector (PID) to determineCalibrated <br /> IM., _ the PID <br /> of volatile organic compounds (VOCs) . Fere the: <br /> as per manufacturer ' s 3irections. Subsanples <br /> laboratory analyses, <br /> appropriate intervals for <br /> submitted at 15E field geologists and <br /> based on recommerdatians of the ss field <br /> F3 general concordance with Anheuser- usch <br /> t. representative. <br /> r.;•.,....� ground <br /> water monitor well, as <br /> x, The borehole was completed as a <br /> described scribed in Table 4_3 , :he 95 ft <br /> shown in <br /> Figure 4-2, th o= 76 ft with <br /> borehole was backfilled through a dep Decisions to <br /> (� prior to monitor well completion• <br /> bentonite P an attempt to , <br /> screen discrete intervals 'Fere based on <br /> rater bear <br /> strata at an in <br /> ( intercept presumed prior to <br /> coincident with highest FID detector readings-five well plus <br /> was developed aY purg g <br /> �f sampling, the well periodically <br /> fluid volumes. oevelopment :rater was <br /> drilling end drummed <br /> and electrical conductivity, , <br /> �b monitored for pH Qnding analytical results. <br /> onsite far ultimate disposal p <br /> jcoliected immediately after <br /> A ground water ample was as well as <br /> this sample, <br /> upon collection, ice- <br /> development. <br /> s, were stored on <br /> previously collected soil sample the water and soil samples <br /> Following completion of sampling, Sacramento, <br /> the field g <br /> eologist <br /> t7 were delivered by to Anlab, <br /> t <br /> q-3 <br /> VIA <br />