| 
								       														0
<br />    														1 1 17 Lone Palm Avenue,Suite 201
<br />    			YA��							Modesto,California      1
<br />  																	209-579-222-2221
<br />     																Fax:209-579-2225
<br />      				A E 8 0 C I A T E 6  INC.
<br />       		On July 18, 2005, an ATC geologist supervised the advancement of cone penetration test (CPT) borings
<br />       		CPTI, CPT2, and CPT3 to depths of 137, 78, and 91 feet below ground surface (bgs), respectively.
<br />       		Groundwater samples were collected at a depth of 130 feet from CPTI; 70 feet from CPT2; and 87 feet
<br />       		from CPT3. Petroleum hydrocarbons were detected in the groundwater samples collected from CPTI and
<br />       		CPT3. In August 2005, ATC supervised the installation of four groundwater monitoring wells (JLM 16,
<br />       		JLM17, JLM18, and JLM19).  Petroleum hydrocarbons were not detected in groundwater samples
<br />       		collected from these wells. Shallow groundwater flow beneath the site generally flowed in a radial pattern
<br />       		towards JLM3 on August 30, 2005. Refer to ATC's Subsurface Investigation Report, dated November 7,
<br />       		2005, for additional information.
<br />       		In October and November of 2008, ATC supervised the installation of seven groundwater monitoring
<br />       		wells (JLM20 through JLM26). These wells were installed inside steel conductor casing to variable
<br />       		depths. Observations associated with JLM21 during development activities indicated that this well was
<br />       		compromised and needed to be replaced. Pursuant to a joint request from the San Joaquin County
<br />       		Environmental Health Department (SJCEHD) and the CRWQCB, ATC prepared the Well Desh•action
<br />       		and Installation Inside Existing Conductor Casing Workplan, dated December 8, 2008, describing
<br />       		proposed methodology to destroy the compromised well and replace it with another one at the same
<br />       		location. In electronic correspondence dated December 9, 2008, CRWQCB staff indicated the workplan
<br />       		would be approved and authorized scheduling the work. The CRWQCB approved the workplan in a letter
<br />       		dated December 10, 2008.  On December 10, 2008, an ATC geologist supervised the destruction of
<br />       		JLM21 and installation of replacement monitoring well JLM21. All of the monitoring wells (JLM3,
<br />       		JLM4, JLM5, and JLM12 through JLM26) were sampled on December 15, 2008, as part of the fourth
<br />       		quarter sampling event. Petroleum hydrocarbons were detected in groundwater samples collected from all
<br />       		of the wells except JLM15, JLM17, JLM18, JLM19, JLM24, and JLM25. Shallow groundwater flow
<br />       		beneath the site on December 15, 2008, generally flowed in a radial pattern towards JLM3. Intermediate
<br />       		and deep groundwater flow directions beneath the site on December 15, 2008, were to the southwest and
<br />       		northwest, respectively. Refer to ATC's Subsurface Investigation Report, dated February 13, 2009, for
<br />       		additional information.
<br />       		SUBSURFACE CONDITIONS
<br />       		Geology
<br />       		The  vadose  zone,  from  zero  to  approximately  22  feet  bgs,  generally  consists  of silty  sand  to
<br />       		approximately 10 feet bgs that is underlain by a laterally extensive clayey silttsihy clay layer extending to
<br />       		depths ranging from approximately 24 to 34 feet bgs. Interbedded layers of silts, sands, clays, and silty
<br />       		sands were encountered below the afore mentioned clay layer and extended to depths ranging from
<br />       		approximately 39 to 46 feet bgs, at which point a laterally extensive sandy layer was encountered. This
<br />       		sandy layer extended to approximately 55 feet bgs in the southern portion of the site and approximately
<br />       		62 feet bgs in the northeastern portion of the site and was underlain by interbedded silts, clays and sands
<br />       		to the depth explored for the intermediate depth wells(approximately 90 feet bgs).A clay layer extending
<br />       		from approximately 87.5 feet bgs to 115 feet bgs was encountered at JLM26 and was underlain by sandy
<br />       		silt to a depth of approximately 126 feet bgs. Sand was encountered to the terminal depth of 141 feet bgs
<br />       		at JLM26.
<br />       		Pilot Testing Workplan-J&L Market      									ATC Associates Inc.
<br />       		5:...\28589\Reports     										ATC Project No.54.28589.0001
<br />											2
<br />
								 |