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ARCHIVED REPORTS XR0001107
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3500 - Local Oversight Program
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PR0544231
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ARCHIVED REPORTS XR0001107
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Last modified
3/6/2019 4:47:21 PM
Creation date
3/6/2019 2:09:30 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0001107
RECORD_ID
PR0544231
PE
3526
FACILITY_ID
FA0023968
FACILITY_NAME
NOMELLINI CONSTRUCTION CO
STREET_NUMBER
1045
Direction
W
STREET_NAME
CHARTER
STREET_TYPE
WAY
City
STOCKTON
Zip
95206
APN
16323040
CURRENT_STATUS
02
SITE_LOCATION
1045 W CHARTER WAY
P_LOCATION
01
QC Status
Approved
Scanner
WNg
Tags
EHD - Public
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EGG pore Pressure Dissipation Tests <br /> (PPDT) <br /> Pore Pressure Dissipation Tests (PPDT s) conducted at various intervals <br />' measured hydrostatic water pressures and determined the approximate depth of <br /> the ground water table A PPDT is conducted when the cone is halted at specific <br /> intervals determined by the field representative The variation of the penetration <br />' pore pressure (u) with time is measured behind the tip of the cone and recorded <br /> by a computer system <br /> Pore pressure dissipation data can be interpreted to provide estimates of <br />' • Equilibrium p€ezometr€c pressure <br /> Y Phreat€c Surface <br /> O In situ horizontal coefficient of consolidation (ch) <br />' O In situ horizontal coefficient of permability (kh) <br />' In order to correctly interpret the equilibrium piezometric pressure and/or the <br /> phreat€c surface, the pore pressure must be monitored until such time as there is <br /> no variation in pore pressure with time (refer to Figure PPD) This time is <br /> l <br /> commonly referred to as t100, the pont at which 100% of the excess pore <br /> ie pressure has dissipated <br /> Interpretation of ether ch and kh from dissipation results can be most easily <br /> achieved using either of two analytical approaches cavity-expansion theory or <br />' the strain-path approach Comparisons of the available solutions and results <br /> from field studies suggest that the cavity-expansion method of Torstensson <br /> (1977) and the strain-path approaches of Levadous (1980) and Teh (1987) all <br />' <br /> provide similar predications of consolidation parameters from CPTU dissipation <br /> data (Gillespie 1981, Kabir and Lutenegger 1990, Robertson et al (1991) <br /> Robertson et al. (1991) have shown that these methods, although developed for <br />' normally consolidated soils, can be equally applied to overconsol€dated soils <br /> Furthermore, comparisons of field and laboratory data indicate that the trends in <br /> the measured (laboratory) and predicated (CPTU) data are consistent provided <br />' the micro fabric and nature of the sols being tested are taken into consideration <br /> (Danz€ger 1990, Robertson et al 1991) <br /> A complete reference on pore pressure dissipation tests is presented by <br /> Robertson et al 1991 <br /> A summary of the pore pressure dissipation tests is summarized in Table 1 <br /> sPore pressure dissipation data is presented in graphical form in Appendix PPDT <br /> I <br />
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