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2900 - Site Mitigation Program
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PR0518922
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Entry Properties
Last modified
5/17/2019 2:19:45 PM
Creation date
5/17/2019 1:59:18 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
WORK PLANS
RECORD_ID
PR0518922
PE
2960
FACILITY_ID
FA0014223
FACILITY_NAME
HESS DUBOIS
STREET_NUMBER
348
Direction
W
STREET_NAME
HARDING
STREET_TYPE
WAY
City
STOCKTON
Zip
95203
CURRENT_STATUS
02
SITE_LOCATION
348 W HARDING WAY
P_LOCATION
01
QC Status
Approved
Scanner
AMeuangkhoth
Tags
EHD - Public
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21 March 2003 <br /> AGE-NC Project No. 95-0114 <br /> Page 4 of 11 <br /> 2.4. HYDROGEOLOGIC FLOW UNITS <br /> Based on the CPT results, AGE has developed a preliminary site hydrogeologic model comprised <br /> of seven informal zones,a vadose(unsaturated)zone and six hydrological units;the model presented <br /> is interpretational and will be modified as more data is collected.Hydrological units maybe defined <br /> as significant vertical intervals of sediments having significant lateral extent and having similar <br /> hydrologic characteristics (i.e. hydraulic conductivity, transmissivity, etc.) over its vertical and <br /> horizontal extent. A `flow unit' may be defined as a hydrologic unit and is characterized by <br /> significantly greater hydraulic conductivity values than overlying and underlying units. A flow unit <br /> is capable of serving as a preferred migration route, and could potentially allow migration of large <br /> contaminant masses over great distances. <br /> The seven hydrologic units are as follows (depths are approximate and can vary by several feet <br /> across the site): <br /> Vadose Zone-Extending from surface grade to 25 feet bsg. The vadose zone is predominantly fine <br /> grained material from surface grade to 20 feet bsg,with a clay occurring between 20 feet and 40 to <br /> 50 feet bsg across portions of the site. <br /> Hydrological Units 1, 3 and 5 (HU1, HU3 and HU5) are clay layers characterized by low pore <br /> pressure. HU1 is located at the top of the current saturated zone (25 feet bsg) and extends to 40 to <br /> 50 feet bsg. HU3 and HU5 are located at depths of approximately 60 and 80 feet bsg,respectively, <br /> and vary in thickness between 1 and 10 feet. <br /> Hydrological Units 2,4 and 6(HU2,HU4 and HU6)are composed dominantly of interbedded silts <br /> and clays,with minor layers of silty sand,sand and cemented sand.These intervals are characterized <br /> by pore pressure variations from low to high pressure,with no laterally consistent pressure patterns. <br /> In general, the lower dynamic pore pressures are associated with clay- and sand-rich intervals, <br /> whereas higher pressures are mainly associated with clayey silts and "stiff fine-grained" intervals <br /> below 100 feet bsg. Significant and continuos sand are present at approximately 70 feet, 110 feet bsg <br /> and 120 feet bsg, and below that depth on-site. <br /> 3.0. SCOPE OF WORK <br /> AGE proposes to advance four soil borings using hollow-stem auger techniques for installation of <br /> `multi-level' ground water monitoring wells, and advance fifteen soil borings for collection of soil <br /> gas samples. The scope of work will include the following tasks: <br /> • Permitting and pre-field work activities; <br /> Advanced GeoEnviron mental,Inc. <br />
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