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i <br /> i <br /> . Site Background Information <br /> I AGE-NC Protect No 97-0326 <br /> Page 5 of 5 <br /> tto low pore pressures, however, a pore-pressure dissipation test conducted at CPT-4 suggests that <br /> the hydraulic conductivity is low in this sand interval (between 2x 10-5 and 4x 10"' centimeters per <br />' second) <br /> Hydrogeologic Unit 3 (HU3) extends from 85 feet to between 95 and 100 feet bsg, it is <br /> predominantly fine grained except for two thin cemented sand lenses (each approximately 1 foot <br /> thick) at the western edge of the survey area This zone is characterized by variable pore pressures, <br /> apparently moderate to high pore pressures in more clayey intervals and low pore pressures in stiffer <br />' fine-grained Intervals <br /> Hydrogeologic Unit 4 (HU4) extends from between 95 and 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 /> Hydrogeologic Unit 5 (HU5) extends from approximately 120 to approximately 135 feet bsg It is <br /> a predominantly fine-grained interval, silts, and a 2-foot thick sand lense in the western half of the <br />' survey area transitions to silty clay in the eastern half The lateral variation in soil types is reflected <br /> in the pore pressures, which tend to be dominantly low in the western half and moderate to high in <br /> the eastern half of the area <br />' <br /> Hydrogeologic Unit 6 HU6 extends from approximately 135 feet to 150 feet bsg This interval <br /> { ) pp <br /> consists dominantly of sand and gravelly sand and is characterized by very low to low pore pressure <br /> 1 <br /> Hydrogeologic Unit 7 (HU7), 150 feet bsg, is a black clay recovered at total depth in wells MW-8 <br />' and MW-9 <br />' REFERENCES <br /> Maxey, G B , 1964, Hydrostratigraphic units Journal of Hydrology, v 2, pp 124-129 <br /> Robertson,P K , Campanella,R G , Gillespie,D and Greig,J , 1986, Use ofpiezometer cone data <br /> Proceedings of the ASCE Specialty Conference in Situ 86, Use of In Situ Tests to <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 GeoEnvuonmental,Inc <br /> 1 <br />