Laserfiche WebLink
III I„I , I <br /> I I V lu II II IIi IlPli I I Ih li II I, I` <br /> e0 I 11 I n' , 1 t IIII III ICI ' <br /> - x>• c a s - �— i 3 Y9w ins wx<ar`7�h{i�I�II''�*Il�hiw.�°-µr w ,w k „n u <br /> II <br /> i 1 I I I <br /> I <br /> . Project No S8080-06-03 <br /> February 16, 1996 <br /> �I { <br /> Page 3 1 11 <br /> 1 <br /> FINDINGS <br /> ' I <br /> Groundwater Elevations_ <br /> A review of the last reported groundwater level measurements performed in December ' <br /> 1995, indicates that groundwater levels have risen an average of 0 73 feet in the last four <br /> weeks to depths ranging from 50 94 to 53 47 feet below TOC The direction of groundwater + <br /> flow beneath the site on January 11, 1996 was to the south-southwest Groundwater <br /> elevation contours are depicted on Figure 2 <br /> Analy1ical Results <br /> A cumulative summary of groundwater analytical data is presented on Table II TPHg was <br /> detected in only MW-3 at a concentrations of 370 ug/L MTBE was detected in wells MW- <br /> 1, MW-2, MW-3 and MW-5 at concentrations of 920, 14, 110 and 670 ug/L, respectively �� <br /> Benzene was detectedZetectable <br /> ' wells MW-1, MW-3, MW-4 and MW-5 at concentrations flanging <br /> from 12 to 2 6 ug/L MTBE concentrations ranged from 35 ug/L (MW-3)'i6 <br /> 700 ug/L (MW-1) Hd was not detected in any of the wells sampled' Chemical I �t <br /> concentrations in groundwater are depicted on Figure 2 <br /> Imo^ <br /> TPHg, BTEX and MTBE were not detected in trip blank sample TB-1 and equipment blank i-�- <br /> sample EB-1 <br /> DISCUSSION JAI& <br /> R <br /> The concentrations of TPHg and benzene have decreased significantly in each well since <br /> December 1995 Concentrations of MTBE increased in three of the five wells sampled' <br /> The distribution of benzene and MTBE in groundwater beneath and upgradient (north) of I' <br /> the site continues to strongly suggest an upgradient offsite source for the groundwater ' <br /> impacts beneath the Togo's site � , <br /> I <br /> IiE;� i1 I <br /> I <br /> I , <br /> a <br /> I <br /> i 1 I V II 11 i <br /> Illi' h <br /> I I <br /> I' <br /> 1 <br />