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ARCHIVED REPORTS XR0001518
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3500 - Local Oversight Program
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PR0544465
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ARCHIVED REPORTS XR0001518
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Last modified
5/16/2019 1:34:15 PM
Creation date
5/16/2019 1:06:50 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0001518
RECORD_ID
PR0544465
PE
3528
FACILITY_ID
FA0005837
FACILITY_NAME
STEFANOS GASOLINE*
STREET_NUMBER
1419
Direction
E
STREET_NAME
CHARTER
STREET_TYPE
WAY
City
STOCKTON
Zip
95205
APN
15137016
CURRENT_STATUS
02
SITE_LOCATION
1419 E CHARTER WAY
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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EHD - Public
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May 5, 2000 Ramage Environmental <br /> Stefono's Gas Site <br /> Stockton, CA <br /> The CPT holes were grouted using our support rig The grouting procedure consists of <br /> using a retraction grout collar which permits grouting of the holes as the CPT and sampling <br /> rods are retracted <br /> 3 0 CONE PENETRATION TEST DATA & INTERPRETATION <br /> The cone penetration test data is presented in graphical form in the attached Appendix <br /> Penetration depths are referenced to existing ground surface This data includes CPT <br /> logs of measured soil parameters and a computer tabulation of interpreted soil types along <br /> with additional geotechnical parameters and pore pressure dissipation data <br /> The stratigraphic interpretation is based on relationships between cone bearing (Qc), <br /> sleeve friction (Fs), and penetration pore pressure (Ut) The friction ratio (Rf), which is <br /> sleeve friction divided by cone bearing, is a calculated parameter that is used to infer soil <br /> 4P behavior type Generally, cohesive soils (clays) have high friction ratios, low cone bearing <br /> and generate large excess pore water pressures Cohesionless soils (sands) have lower <br /> friction ratios, high cone bearing and generate little in the way of excess pore water <br /> pressures <br /> The interpretation of soils encountered on this project was carried out using recent <br /> correlations developed by Robertson et al, 1990. It should be noted that it is not always <br /> possible to clearly identify a soil type based on Qc, Fs and Ut In these situations, <br /> experience and judgment and an assessment of the pore pressure dissipation data should <br /> be used to infer the soil behavior type The soil classification chart used to interpret soil <br /> types based on Qc and Rf is provided in the Appendix <br /> We hope the information presented is sufficient for your purposes If you have any <br /> questions, please do not hesitate to contact our office at (925) 313-5800 <br /> Sincerely, <br /> Tim J Boyd <br /> Operations Manager— CPT Division <br /> i <br />
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