Laserfiche WebLink
31 August 2016 <br />AGE Project No. 96-0235 <br />Page 2 of 8 <br />Assessment of deep, dissolved MTBE, east of the former northern UST area has been <br />mostly completed. However, assessment of all dissolved petroleum east of the former <br />UST No. 3, southern area has not been completed and dissolved hydrocarbons are likely <br />migrating east to northeast of the southern UST area. <br />The CRWQCB has directed the limits of the dissolved plumes in the HU2 zone be defined <br />to determine if the remaining dissolved impact meets the criteria established in the Low- <br />Threat UST Case Closure Policy (LTCP), as a requirement for site closure. Based on <br />depth to groundwater measurements collected in 2016 at the site, first-encountered <br />groundwater in the area is approximately 15 feet bsg, while deeper groundwater is <br />significantly impacted between 40 and 60 feet bsg. The site groundwater monitoring well <br />network lacks wells to define the lateral extent of deeper dissolved petroleum <br />hydrocarbons and thus is an impediment to site closure. <br />2.1. REGIONAL GEOLOGIC/HYDROGEOLOGIC SETTING <br />The property is situated within the Great Valley Geomorphic Province of California; a <br />large, elongate, northwest trending, asymmetric structural trough. The Great Valley <br />Province has been filled with thick sequences of sediment ranging in age from Jurassic <br />to Recent, creating a nearly flat- lying alluvial plain that extends from the Tehachapi <br />Mountains in the south to the Klamath Mountains in the north. The California Coast Range <br />and the Sierra Nevada form the western and eastern boundaries of this province. Rocks <br />composing the basement complex of the province have not been completely defined but <br />are believed to be of metamorphic and igneous origin. The northern and southern portions <br />of the Great Valley Province have been designated the Sacramento and San Joaquin <br />Valleys, respectively. <br />The Modesto, Riverbank, and Turlock Lake Formations and overlying recent alluvium are <br />the principal source of domestic groundwater in the 13,500-square-mile San Joaquin <br />Valley Ground Water Basin (Basin 5-22). This basin is drained primarily by the San <br />Joaquin River. <br />3.0. SCOPE OF WORK <br />AGE proposes to advance three (3) direct push, soil probe borings to define the lateral <br />down-gradient extent of dissolved petroleum hydrocarbons to deep (HU2) groundwater <br />at the site and installation of a monitoring well for the collection of repeatable groundwater <br />samples proposed at well MW-29 in in Hydrogeologic Unit 3 (HU3). The soil borings are <br />proposed off-site in the City of Stockton Right-of-Way within the sidewalk area on the <br />west side of Harrison Street. <br />Advanced GeoEnvironmental Inc.