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' Mr Ronald Rowe <br /> November'), 1998 <br /> Page 3 <br />' Department of Health Services for the analysis of hazardous materials Certification Number <br /> 1346) Samples were analyzed for total petroleum hydrocarbons as gasoline (TPH-G) and <br /> benzene, toluene, ethylbenzene, and xylenes (BTEX) using EPA Method 5030/8015 and 8015 <br /> Modified, and oxygenates using EPA Method 8260B The analytical reports for the <br /> tHydroPunchTM groundwater sampling are included in Attachment C <br /> Groundwater Monitoring Well Constructions. All boreholes were constructed with 2-inch <br />' diameter Schedule 40 polyvinyl chlonde (PVC) blank casing and 0 020-inch slotted casing <br /> Table I summarizes the well construction details <br />' Groundwater Monitoring Well Development, Sampling, and Surveying The newly <br /> constructed wells were developed on August 14, 1998 by Wayne Drilling, Inc (California C-57 <br /> License Number 718139) of Lincoln, California and supervised by a BC field technician After <br />' development, each well was sampled by the BC field technician and the samples were submitted <br /> to Acculabs, Inc The development and decontamination water was transported to an on site <br /> evaporation pond The analytical reports for the well sampling are included in Attachment C <br /> Development and sampling notes are included as Attachment D <br /> Top-of-Casing and groundwater surface elevations, and horizontal locations of each <br /> groundwater monitoring well (MW-1 through MW-4) were surveyed by Tom Morrow, <br /> Incorporated of West Sacramento, California A copy of the survey site map by Tom Morrow, <br /> Incorporated is included as Attachment E <br />' Results <br /> The following summarizes the results of the investigation <br />' Local Geology and Hydrogeology. Results from previous site investigations conducted by <br /> Leeward Consultants, are consistent with this investigation The subsurface stratigraphy is <br />' interbedded silts, sandy silts, silty sands, and sand Bedding contacts are commonly gradational <br /> However, there are a few sharp contacts that usually separate an overlying sand from a finer <br />' gramed soil Grain size analyses of three samples collected in MW-2 correspond with the <br /> lithological descriptions given for the same interval Cross section A-A' is shown on Figure 2 <br /> and Figure 3 shows the lithogic cross section of A-A' <br />' Groundwater was encountered during drilling at 69 to 73 feet bgs Depth to water measured in <br /> the wells on September 16, 1998 ranged from 68 51 to 68 87 feet bgs (Table 2) Measured static <br />' water levels in the wells were higher than the depth of groundwater during drilling which may <br /> indicate semi-confined or confined groundwater conditions Groundwater flow direction <br /> beneath the facility vanes due to a very flat gradient <br />' <br /> Use or disclastrre of data continued on this sheet is subject to the restriction specified at the beginning of this <br /> document <br /> BCSACO111600011627 11WELLMTXOC <br />