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' Site Background Information K & S Gas & Grocery <br /> Page 5 of 5 <br /> low pore pressures,however, a pore pressure dissipation test conducted at CPT-4 suggests that the <br /> hydraulic conductivity is low in this sand interval (between 2X10'5 and 4X10"' centimeters per <br /> second cm/s) <br />' Hydrogeologic Unit 3 (HU3) - HU3 extends from 85 feet to between 95 feet and 100 feet bsg, it <br /> consists of predominantly fine-grained material, except for two thin cemented sand lenses (each <br /> approximately 1 foot thick) at the western edge of the survey area This zone is characterized by <br />' variable pore pressures,though moderate to high pore pressures are evident in more clayey intervals, <br /> and low pore pressures in stiffer fine-grained intervals <br /> Hydrogeologic Unit 4 (HU4)- HU4 extends from 95 feet to 100 feet to approximately 120 feet bsg <br /> and consists of approximately 10 feet of fine-grained sediment overlying approximately 10 feet of <br />' sand, the lower half of the sand interval is gravelly sand HU4 is characterized by very low to low <br /> pore pressure <br /> 1 Hydrogeologic Unit 5 (HU5) - This unit extends from approximately 120 feet to approximately <br /> 135 feet bsg It is a predominantly fine-grained interval, silts and a 2-foot thick sand lense in the <br /> western half of the survey area transition to silty clay in the eastern half The lateral variation in soil <br />' types is reflected in the pore pressures, which tend to be dominantly low in the western half and <br /> moderate to high in the eastern half of the area <br />' Hydrogeologic Unit 6 (HU6) - This unit extends from approximately 135 feet to 150 feet bsg and <br /> interval consists predominantly of sand and gravelly sand, and is characterized by very low to low <br />' pore pressure <br /> Hydrogeologic Unit 7(HU7)-Beginning at 150 feet bsg,HU7 is evidenced as a black clay recovered <br /> at total depth in wells MW-8 and MW-9 <br /> 1 <br />' REFERENCES <br /> Maxey, G B , 1964, Hydrostratigraphic units Journal of Hydrology, v 2, pp 124-129 <br /> tRobertson,P K , Campanella,R G ,Gillespie,D and Greig,J , 1986, Use of piezometer cone data <br /> Proceedings of the ASCE Specialty Conference in Situ 86, Use of In Situ Tests in <br />' Geotechnical Engineering, Blacksburg,p 1263-1280 <br /> Sanders, L L , 1998,A manual of field hydrogeology, Prentice-Hall, Inc ,New Jersey, 381 p <br /> 1 <br /> Advanced GeoEnvironmental,Inc <br />