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—I I I, SIN4� <br /> ti, 1:,•i• E: iiti (; H01, t�ct [: ltr.souitct:s , lr �: . <br /> STERN i: :_ Ul.( GIr, ittisou8Ct: 5 , INC. <br /> "Mel IV <br /> J,FUW411,3April l7)o APR 13 1950 <br /> ENVIRONMENTAL HEASN <br /> OEM,. <br /> PFRMff15ERtP'r° <br /> ,.. <br /> GROUNDWATER PLOW <br /> 3 Fipre 3 is the potentiometric stnfncc rasp of the Shallow goundwn[cr,hasca on depth-[o-watec <br /> mea,ureme„ts mkca on 19 December 1989. Water-clevation data are tabulated is "able 2. <br /> Hydr0Srrjphs showing gruundarter fluctuations over time are included as AtWchu-cut B. T~atimattd <br /> ® grotw4water flow was to the east ar a gradient of about 0-55a. <br /> ,t <br /> C�oncentra:ions of 1'Pl and aromatic hydrexarbons In groundwater spItar E,.)have remained <br /> the sa[ae when wrnp2sed to previous samples except for well AtW-5. TPP and aromatic h orarbons <br /> haw ii;creuW spprcuamatcly an t rder of maotude for well MWS,siece the suppling in Uplembcr <br /> 1989,rettuuing tc.the concemiratious reported for the March 1.9V sampling <br /> M <br /> We app;eciste lhs oppom[nity to py'ovide j¢•a;c*c ,and envircmmeatal <br /> rnn:ultzug services t <br /> Chevron and tnut this report meets your attds. If yuu liavc—Y questions-P1=6call u at(415)ac7- <br /> ® 7595. <br /> Sincerely, <br /> ,%,=We Gcol 'c Itnsource,Inc, <br /> otnas J. <br /> Prolyd <br /> 17 <br /> . !� INLlMAUNP <br />