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d` �-' � 'rV' ,r. :,s;: - � "A'�.,f'"".u.^. .�.�s'sc�9� .'a�::'u`tl _._.� ;.1.. ...L^«.saxbei.w��`�„-•e._,_......:i....vy, ,Ym.,,r...,.r:..>.�- -.� <br /> �.k <br /> aye <br /> Mr. Glenn R. Dembroff <br /> L3ltramar Inc. <br /> April 9, 1991 <br /> Page 2 <br /> Fieldwork conducted at the site by Delta, including the activities outlined above, were performed in <br /> accordance with the field methods and procedures described in Enclosure A. <br /> Sitegite Information <br /> The site is currently operated as a retail Ultramar gasoline station. Ultramar purr:iased the site from <br /> Conoco Inc. in )uly 1990. The site is located in a rural agricultural area that is currently undergoing <br /> residential and commercial development. The flat-lying topography surrounding the site is between 30 _ <br /> and 35 feet above mean sea level. <br /> previous investigative activities have been performed at the site by the previous owner(Conoco Inc.) <br /> since 1985 resulting in the drilling and installation of a total off 33 vadose and/or ground water <br /> monitoring wells. All but one of the 33 well;(MW 20)is current] dry. <br /> The regional drought conditions <br /> that exist are partially responsible for lowering the ground water table below the monitoring well <br /> screens. <br /> Site Soils <br /> The soil borings for monitoring wells were advanced at the site on <br /> Three bruary 7 and 8,1991,to a depth <br /> F <br /> of re feet (MW-35 and MW 36)and 70 feet(MW-34)below the surface. The location of these borings <br /> is shown in Figure 2 and the soil boring logs are presented in Enclosure B. Sediments underlying the <br /> site consist predominantly of an interbedded sequence of sand,silty and clayey sand,and silty and sandy <br /> clay straturr.to a depth o€approximately 60 feet below the surface. In the Loring for monitoring well <br /> MW-34,a moist,unsaturated sandy clay and clayey sand layer was present between approximately 59 <br /> and 68 feet below the surface. These strata were underlain by a saturated sand stratum that was sampled <br /> at a maximum depth of 70 feet below the surface. <br /> Soil 5am'3ie Anal ses <br /> soil samples were obtained at 5-foot intervals and were screened for the presence of organic vapors <br /> using a photoionization detector(PID) as described in Enclosure A. PIIS results are recorded on the <br /> soil boring logs contained in Enclosure B. <br /> vapor <br /> ing <br /> Soil samples were selected for <br /> s made in the field, Onenso les sample was selectee!for altal s from <br /> position and physical observat on <br /> each boring. These samples were collected from a depth of approximately 45 feet 1-clow the surface. <br /> The samples were submitted to a California-certified laboratory and analyzed for tlae presence of total <br /> petroleum hydrocarbons (TPH)as gasoline,and benzene,toluene,etbylbenzene and xylenes(BTEX). <br /> A summary of the analytical results for soil samples collected in February 1991 is presented in Table 1. <br /> Copies of the sail sample laboratory reports are presented in Enclosure C. TPH as gasoline was not <br /> detected in the soil sample collected form boring MW-34 or boring MW-36. A TPH conccntrat-ton of <br /> 390 parts per million (ppm)was detected in the soil sample collected from boring MW-35. <br />