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Phase II Environmental Site Assessment Investigation Report <br />206 Sutter Street, Stockton, California <br />Page 4 <br />4.2 GROUNDWATER <br />TPH-D was detected at concentrations of 17,000 milligrams per liter (µg/L) in DP-1, 260 µg/L in DP-4, <br />and 170 µg/L in DP-6. TPH-MO was detected at concentrations of 40,000 µg/L in DP-1 and 510 µg/L in <br />DP-7. TPH-G was detected at concentrations of 5,100 µg/L in DP-1 with lighter than water immiscible <br />sheen or product present and 110 µg/L in DP-4. <br />Detected VOCs by EPA Method 8021B includes benzene at 25 µg/L, toluene at 36 µg/L, ethylbenzene at <br />38 µg/L, m, p-xylene at 20 µg/L, 0-xylene at 1.9 µg/L, and xylenes at 22 µg/L in DP-1. VOCs were not <br />detected at or above their respective reporting limits in DP-7. <br />Detected VOCs by EPA Method 8062B includes benzene at 9.5 µg/L, ethylbenzene at 29 µg/L, xylenes at <br />17 µg/L, naphthalene at 24 µg/L, n-butyl benzene at 5.7 µg/L, 1,2,4-trimethylbenzene at 6.6 µg/L, 1,3,5- <br />trimethylbenzene at 10 µg/L, isopropyl benzene at 15 µg/L, 4-isopropyl toluene at 6.7 µg/L, n-propyl <br />benzene at 31 µg/L, and sec-butylbenzene at 3.1 µg/L in DP-1. DP-4 had concentrations of VOCs including <br />benzene at 1.3 µg/L, tert-butyl benzene at 0.58 µg/L, 1,2-dichroethane at 0.20 µg/L, and isopropyl benzene <br />at 0.51 µg/L. VOCs were not detected at or above their respective reporting limits in any of the other <br />collected groundwater samples. <br />VOC results were compared to the Maximum contaminant levels (MCLs) adopted by the California State <br />Water Resources Control Board (SWRCB), and naphthalene was compared to the California Division of <br />Water’s California Notification Level (CNL) of 17 µg/L. Benzene by both EPA methods was detected <br />above the MCL of 1.0 µg/L with the highest benzene concentration at 25 µg/L and Naphthalene was <br />detected above the CNL of 17 µg/L in the groundwater sample collected at DP-1. Benzene was detected <br />slightly above the MCL of 1.0 µg/L in the groundwater sample collected at DP-4. <br />Detected laboratory analytical results for the groundwater samples are included on Table B, Appendix D. <br />All soil and groundwater laboratory analytical reports and chain of custody forms are included in Appendix <br />E. <br />5.0 CONCLUSIONS <br />Condor conducted a Phase II ESA for the property located at 206 Sutter Street, Stockton, San Joaquin <br />County, California. The purpose of the work was to evaluate whether past use of the property had adversely <br />affected soil and/or groundwater beneath the Site. The evaluated property included one parcel designated <br />as Assessor Parcel Number (APN) 139-250-030. Based on review of historical documents the Site appears <br />to have had been occupied by a commercial fueling station in the southwestern portion of the Site from <br />approximately the 1930’s to the 1960’s which was replaced by The Ambassador Hotel in the late 1960s or <br />early 1970s. In 2016 the hotel was demolished. In February 2017, Condor conducted a project-wide <br />geotechnical engineering study for the Ten Space Development Project in downtown Stockton and <br />advanced two geotechnical borings on the Site. Boring B-3 was terminated at approximately 10 feet bgs <br />due to a concrete obstruction and B-4 observations included stained soil and a smell of gasoline starting at <br />approximately 30 feet down to the boring terminus at 50 feet bgs. <br />Groundwater depths within the Stockton area historically ranged from 80 to 100 feet bgs during the time <br />when shallow groundwater was utilized for public water supply until the early 1980s. Shallow groundwater <br />subsequently was not used for public supply and rebounded to shallower depths of approximately 20-30 <br />feet bgs beneath Stockton. Currently, the regional groundwater gradient is easterly due to the critically over- <br />drafted groundwater basin from agricultural irrigation to the east, which has created a large regional cone <br />of depression centered approximately 10 miles east of Stockton. This regional easterly gradient beneath <br />Stockton has been present since the 1980s. As a result, many Stockton releases that occurred prior to the