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are observed at <br /> er- <br /> and natural biodetank sites. <br /> plumehmigrat on will be most <br /> inhibiited <br /> ground fuel. tank <br /> by the gradual groundwater gradient. <br /> Y7aterWork recommends monitoring and sampling of the sites <br /> wells to confirm the groundwater gradient and the <br /> distribution of dis"olved contaminants. Frequently, <br /> st <br /> monitoring wells drecord d�illingheir ig est leveConfirmationin the rof <br /> ls <br /> sampling event, important since <br /> the results for well Pre :c a only benzene near the SAI,. <br /> the initial analysis reca:cded only <br /> orongoing uponithese resassessed. <br /> results, <br /> athneed <br /> d for remedial measures <br /> 5.0 REFERENCES <br /> Page, R.W. , 1986, Geology of the Fresh Groundwater Basthe <br /> in of <br /> Sectionntt Geological SurRestorealley California with <br /> vey professional 1401- <br /> S. <br /> C, 54p. <br /> 1 <br /> 6 <br />