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FIELD DOCUMENTS
Environmental Health - Public
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2900 - Site Mitigation Program
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PR0505722
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Last modified
1/30/2020 11:29:04 AM
Creation date
1/30/2020 9:56:36 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
FIELD DOCUMENTS
RECORD_ID
PR0505722
PE
2951
FACILITY_ID
FA0006961
FACILITY_NAME
KJAX
STREET_NUMBER
5451
Direction
E
STREET_NAME
HARDING
STREET_TYPE
WAY
City
STOCKTON
Zip
95202
APN
10122041
CURRENT_STATUS
02
SITE_LOCATION
5451 E HARDING WAY
P_LOCATION
99
P_DISTRICT
002
QC Status
Approved
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EHD - Public
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Woodward-Clyde <br /> V <br /> "The large, asymmetrical, northwestward-trending trough of the Sacramento Valley is the <br /> principal structure controlling the occurrence and movement of groundwater in the area. <br /> Along the flanks of the valley, which are the flanks of the trough, deposits generally are <br /> much thinner than those underlying either the topographic axis of the valley or the more <br /> westerly structural axis of the trough. In general, most of the confinement of groundwater <br /> occurs near the axis of the valley as a result of more extensive confining beds deposited <br /> there. Because the flanks of the valley are higher than its axis, recharge from tributary <br /> rivers and streams, as well as from irrigation return, has caused heads in the groundwater <br /> along the flanks to be higher than those along the axis, so that, overall, groundwater moves <br /> from the flanks toward the axis and thence south and westward toward the delta area and <br /> V <br /> points of ultimate discharge. Since development, some groundwater moves toward large <br /> pumping depressions in various parts of the valley." <br /> V <br /> Typically wells constructed in south-central Sacramento Valley are screened within the <br /> �- coarser sediments of flood-basin deposits which are under unconfined storage conditions. <br /> Groundwater flow in the Central Valley is strongly influenced by the numerous clay and silty <br /> lenses that are present in the aquifer system. Lithologic studies show that the aquifer system <br /> contains many isolated lenses of sand, silt, and clay. The fine-grained lenses, although <br /> limited in lateral extent, constitute more than 50 percent of the system and have an aggregate <br /> u <br /> thickness of as much as several thousand feet. Most recent studies show that the Central <br /> Valley aquifer system is a single heterogeneous system supported by the presence of <br /> V <br /> numerous fine-grained lenses and the hydraulic response of the system to pumping (USGS, <br /> 1991). <br /> V <br /> 1.4 PROJECT OBJECTIVE <br /> V <br /> The purpose of this work was to characterize the lateral and vertical extent of diesel <br /> contaminated soil in the vicinity of the former UST at the KJAX site. This included the <br /> advancement of soil borings and collection of soil samples and one groundwater sample. <br /> The activities were conducted in accordance with Chapter 6.7, Division 20 of the Health and <br /> V <br /> Safety Code and the California Underground Storage Tank Regulations (Subchapter 16 of <br /> Title 23 of the California Code of Regulations). These regulations prescribe the activities <br /> required to investigate and cleanup contaminated soil and groundwater resulting from UST <br /> V <br /> 8054/FEMA/KIAXPMR.M/8-24-95 SAC 1-4 <br /> V <br />
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