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ARCHIVED REPORTS XR0011190
Environmental Health - Public
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EHD Program Facility Records by Street Name
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DR MARTIN LUTHER KING JR
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701
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3500 - Local Oversight Program
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PR0544217
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ARCHIVED REPORTS XR0011190
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Entry Properties
Last modified
3/4/2019 11:44:38 PM
Creation date
3/4/2019 4:40:03 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0011190
RECORD_ID
PR0544217
PE
3526
FACILITY_ID
FA0002512
FACILITY_NAME
GSG GAS & MART
STREET_NUMBER
701
Direction
E
STREET_NAME
DR MARTIN LUTHER KING JR
STREET_TYPE
BLVD
City
STOCKTON
Zip
95206
APN
14734311
CURRENT_STATUS
02
SITE_LOCATION
701 E DR MARTIN LUTHER KING JR BLVD
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
Scanner
WNg
Tags
EHD - Public
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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 />
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