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ARTESIAN I NVIKONMENTAL CONSULT ; j[CR',-' �1 ' AL H�E+LALTH <br />' 93 JUL 19 P14 2. 23 <br /> Date July 15, 1993 <br /> , y <br /> Quarterly Groundwater Monitoring <br />' Sampled May 14, 1993 <br /> 1045 W Charter Way <br /> Stockton, California <br />' Project No 040-001-08 <br /> Prepared for <br />' Mr Dante John Nomelhru <br /> Nomelhm Construction Company <br /> P O Box 1528 <br />' Stockton, California 95201 <br />' This report presents the results of the quarterly groundwater monitoring well <br /> sampling,performed on May 14, 1993 by Artesian Environmental Consultants <br /> (Artesian) at the subject site(Figures 1 and 2) The site history is summarized in <br /> Appendix A <br /> SITE DESCRIPTION <br /> The site is located at 1045 West Charter Way,in Stockton, California A site location <br /> map is presented in Figure 1 A map showing the site structure and boring locations <br />' is presented in Figure 2 The property is located in an industrial area <br /> GROUNDWATER SAMPLING <br />' On May 14, 1993,Artesian staff measured depth to water for sixgroundwater <br /> monitoring wells designated MW-1 through MW-6 Monitor wells MW-3, MW-4, <br />' MW-5 and MW-6 were purged and sampled according to a revised schedule approved <br /> by Ms Lunda Turkatte of the San Joaquin County of Environmental Health All <br /> groundwater samples were collected according to the Artesian standard operating <br /> procedures (SOP) for groundwater sampling included in Appendix B Free product <br /> measurements were made with an oil-water interface probe <br /> All purged water was temporarily stored in DOT 17-H, 55-gallon containers pending <br /> analytical results The groundwater samples were shipped under chain-of-custody to <br /> Chromalab, Inc of San Ramon, California, a state-certified laboratory <br /> GROUNDWATER FLOW <br /> Figure 3 shows the potentiomet is surface of shallow groundwater based on depth-to- <br /> water measurements taken on May 14, 1993 The estimated groundwater gradient <br /> and flow direction was 0 010 vertical feet per horizontal foot <br /> to the east-northeast for the May 14, 1993 sampling event Groundwater-elevation <br /> Idata ale presented in Table 1 q <br /> C <br /> a ��,v <br />