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+ 1 <br /> CALIFORNIA GEOPHYSICAL GROUP,IjNC„ , ,, <br /> P O Box 578341, Modesto, CA 95357 ''• ,I 91`' k "'`- Tel (209) 527-1247 <br /> September 23, 1998 P 46 Fax (209) 527-4810 <br /> Public Health Services <br /> San Joaquin County <br /> P O Box 388 <br /> Stockton, CA 95201 <br /> ATTN Ms Carol Oz <br /> RE Work Plan August 21, 1998 Addendum <br /> Darpetro, Inc USA Service Station <br /> 749 E Charter Way <br /> Stockton, CA <br /> Site No 1060 <br /> On September 16, 1998, 1 received a call from Ms Carol Oz requesting further information on the <br /> above referenced work plan She requested us to verify the radius of influence of the Vapor <br /> Extraction System and information of the Air Sparging equipment we plan to use <br /> On September 16, 1998, we measured the vacuum in each vapor extraction well by closing the <br /> vacuum to that well and keeping open the vacuum to all the other wells It was impossible to <br />. measure the vacuum in the monitoring wells because the depth to water was 34 3 feet and the <br /> highest slotted casing in any of the monitoring wells is 35 feet <br /> Well Closest Well Vacuum in Hg" <br /> (Feet) <br /> VW-1 22 230 <br /> VW-3 22 3 20 <br /> VW-4 23 250 <br /> VW-5 23 360 <br /> VW-6 26 010 <br /> We have prepared a graph (Fig 1) which plots the distance to the closest well vs the vacuum in <br /> each well The result is a line through two points which ends at 26 feet Therefore, the radius of <br /> influence is 26 feet Originally the radius was calculated to be about 38 feet, however, we were <br /> able to measure some of the monitoring wells at that time There were some abnormalities in the <br /> readings, since two wells were 22 feet distant and two wells were 23 feet distant from the nearest <br /> well This is possibly due to the geological units Some of the units are more porous than others <br /> and allow the vacuum to extend farther After the water table falls below 35 feet we will again <br /> check the vacuum pressures in the monitoring wells <br />