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ARCHIVED REPORTS XR0011078
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3500 - Local Oversight Program
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PR0544222
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ARCHIVED REPORTS XR0011078
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Entry Properties
Last modified
3/5/2019 5:09:56 PM
Creation date
3/5/2019 1:55:03 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0011078
RECORD_ID
PR0544222
PE
3528
FACILITY_ID
FA0005976
FACILITY_NAME
TIRE & WHEEL MASTERS
STREET_NUMBER
814
Direction
E
STREET_NAME
CHARTER
STREET_TYPE
WAY
City
STOCKTON
Zip
95206
APN
16718101
CURRENT_STATUS
02
SITE_LOCATION
814 E CHARTER WAY
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
Scanner
WNg
Tags
EHD - Public
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Page 8 <br /> Gco(agtcal reckxus rxG <br /> Site Conceptual Modet Report <br /> Project No 724 2 <br /> May 2,2006 <br /> ' units) extending to 23 feet bgs A thin, 0 5 foot thick sand to clayey sand unit is <br /> present at 24 feet bgs that is underlain by more fine grained units Silty sands, sandy <br /> silts or silts are present from 24— 27 feet bgs A thin, 1 foot thick sand to clayey sand <br /> ' unit is present at 27 feet bgs that is underlain by two feet of sandy units The <br /> remainder of the borehole encountered more fine grained units from 29 to 55 6 feet <br /> A soil sample from 37 feet bgs was identified as an olive, slightly moist, axed plastic <br /> ' clayey silt by the field geologist This data correlates well to the CPT log that shows <br /> the interval as a clayey silt to silty clay <br /> ' • CPT-2 The CPT log shows primarily fine grained units extending to the total depth <br /> of 67 feet bgs The log shows clays or silty clays to 8 feet bgs, then silty sand to <br /> sandy silt layers to 11 feet bgs This is underlain by fine grained units extending to 25 <br /> feet bgs A 0 5 foot thin sand to clayey sand unit was identified at 26 feet bgs, and <br /> again at 66 feet bgs The remainder of the borehole encountered more fine grained <br /> units from 26 to 67 feet bgs Soil samples from 35 feet bgs were identified as an <br /> olive, moist to wet, sandy clay with very fine sand grains by the field geologist This <br /> transitioned downward to an olive, moist, soft, clayey silt This data correlates fairly <br /> to the CPT log that shows the interval as clay <br /> ' • CPT-3 The CPT log shows primarily fine grained units extending to the total depth <br /> of 61 feet bgs Fine grained units are present from the surface to 26 feet bgs Two <br /> feet of silty sand to sandy silts are noted at 26 to 28 feet bgs and these are underlain <br /> by a very thin (<0 5 feet thick) sand to clayey sand layer The remainder of the <br /> borehole encountered more fine grained units from 28 to 61 feet bgs A soil sample <br /> ' from 35 feet bgs was identified as a brown, moist, firm silt by the field geologist The <br /> CPT log shows this depth to be silty clay to clay <br /> ' o CPT-4 The CPT log shows primarily fine grained units extending to the total depth <br /> of 82 feet bgs Fine grained units are present from the surface to 37 feet bgs Two <br /> feet of sand/silty sand to sandy silts are noted from 37 to 39 feet bgs The remainder <br /> ' of the borehole encountered more fine grained units from 39-to 82 feet bgs A soil <br /> sample from 38 5 - 40 feet bgs (with 12" recovery in tubes) was identified as a fine to <br /> coarse, dark grey, moist sand by the field geologist The CPT log shows this interval <br /> ' to be transitioning from the sandy units noted at 37 feet to clayey units at 40 feet <br /> Note The cross sections were developed using data gathered by different individuals <br /> utilizing different methodologies Therefore, they need to be looked at as one of several <br /> possible interpretations of actual site conditions ) <br /> ' GTI has completed cross sections depicting our interpretation of the subsurface- see Figure 3 <br /> for section locations Figure 4 Cross Section A — A' illustrates the geology trending from <br /> the northwest to the east of the site The diagram indicates that more sands are present below <br /> 65 feet bgs on site and below 50 feet bgs in the off-site location of MW-1091209 GTI's <br /> interpretation of the geology has shown sand units at 25 and 50 feet bgs as laterally <br /> continuous These units were not uniformly identified in the original boring logs for wells <br />
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