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1 <br /> gasolinc OvN1acnatcs addItncs weic detected It nr above tilt, lahoiatory reported detection limits in any of the <br /> surface ctiate: sa:riplcs <br /> • On Mateh 2() 1999 ( ondoi conducted tirstuartct 1999 groEandwatc,r and surface water monitorml= at Herman <br /> q L <br /> & Helen s Matrria I aboiatory anaktical results of the groundwater samples collected during the first quarter <br /> 1999 monitoring cvcnt were p,enerally consistent with Historical quarterly groundwater analvocal data <br /> (Jroundwalc: cic4atroii nrcasurcmcnts cc7ilected at the site on March '16 1999 indicated that the aveiagc depth to <br /> grotrndwatel �tias ippiokiinately > 5 feet below the ninnitor well and surface water station inLasuring points Fhis <br /> average rfcpth to eater !s 0 1 feet gteatei than the avcragt depth to water measured on Deccmbcr 30 1998 <br /> Groundwater elc:v,rtroli tontntns for March ''6 1999 indicated that the groundwater gradient at the site was <br /> gLI1Lrally uinststcnt with the historical groundwater giadicnt <br />' I aboraton, analytical lcsttlts Of tl1c Surface water samples collected during the first quarter, 1999 monitoring <br /> cvcnt were gcncrally consistent with historical surface water analytical data for B11-:X and TPP-() M FBE <br />' however was detected for the first tirric in the sample collected from IDCW (2 2 µg/1) MTBE was detected in <br /> samples DDN and DDS at significantly higher concentrations during the first quarter, 1999, monitoring event <br /> (980 and 3,500 µg/l respectively) than In prior monitoring events Additionally, TAML was detected for the <br />' first time in samples DDN and DDS <br /> On June 30 1999, ( ondor conducted second quarter, 1999, groundwater and surface water monitoring at Herman <br />' & Helen's Mar ma I aboratory analytical results of the groundwater samples collected during the second quarter, <br /> 1999 monitoring event were generally consistent with historical quarterly groundwater analytical data <br /> Groundwater elevation measurements collected at the site on June 30, 1999 indicated that the average depth to <br /> • groundwater was approximately 6 2 feet below the monitor well and surface water station measuring points Phis <br /> average depth to water is 0 7 feet greater than the average depth to water measured on March 26 1999 <br /> Groundwater LILvation contours for June 30, 1999, indicated that the groundwater gradient at the, sate IS generally <br /> consistent with the historical groundwater gradient <br /> Laboratory analytical results of the surface water samples collected during the second quarter, 1999 monitoring <br /> event were generally consistent with historical sur face water analytical data MTBL was dctected for the second. <br /> time In the sample collected from IDCW (1 4 �tg/l) MTBE was detected in samples DDN and DDS at <br /> significantly l[nvcl cunccntiationti during the second quarter 1999 monitoting event (5 4 and 1 8 µg/l, <br /> respectively) than in the first quarter 1999 monitoring event Additionally FAME was not dLtectcd in any of <br /> the suitatre watts sample du:mg the second quarter, 1999 monitoring event <br /> On September 23 1999 ( ondor conducted third quarter, 1999 groundwater and surface water monitoring at <br /> Berman & Helen s Marina Laboratory analytical results of the groundwater samples collected dui Ing the third <br /> quarter 1999 monitoring event were generally consistent with historical quarterly groundwater analytical data <br /> However benzene and total xylenes were detected for the first time in the gioundwatei sample collected from <br /> MW-3 <br /> IGroundwater elevation measurements collected at the site on September 23 1999, Indicated that the average <br /> depth to "Iaundksatci was approximately 6 5 feet belo�N the monitor well and surface water ;tatlon measuring <br /> points This average depth to water is 0 3 feet greater than the average depth to water measured on June 30, <br /> 1999 Gioundwatei elevation contours for September 23, 1999, indicated that the groundwater giadient at the <br /> site was generally consistent with the historical groundwater gradient <br /> The laboratory analytical surface water sample data for the third quarter, 1999, monitoring event were generally <br /> I representative of historical data, with the exception of the first quarter, 1999, data During the fust quarter, 1999, <br /> I <br />