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ARCHIVED REPORTS XR0004909
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2900 - Site Mitigation Program
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PR0536618
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ARCHIVED REPORTS XR0004909
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Last modified
3/4/2019 12:30:17 PM
Creation date
3/4/2019 10:22:54 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0004909
RECORD_ID
PR0536618
PE
2960
FACILITY_ID
FA0021026
FACILITY_NAME
STOCKTON CHARTER WAY COMMON PLUME
STREET_NUMBER
440
Direction
W
STREET_NAME
CHARTER
STREET_TYPE
WAY
City
STOCKTON
Zip
95206
APN
16503003
CURRENT_STATUS
01
SITE_LOCATION
440 W CHARTER WAY
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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WNg
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EHD - Public
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EGG <br /> 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 piezometric pressure <br /> • Phreatic Surface <br /> • In situ horizontal coefficient of consolidation (ch) <br /> • In situ horizontal coefficient of permability (kh) <br /> In order to correctly interpret the equilibrium piezometric pressure and/or the <br /> phreatic 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 /> commonly referred to as tioO, the point at which 100% of the excess pore <br /> pressure has dissipated <br /> Interpretation of either 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 /> 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 /> nominally consolidated soils, can be equally applied to overconsolidated 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 soils being tested are taken into consideration <br /> (Danziger 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 /> . Pore pressure dissipation data is presented in graphical ford in Appendix PPDT <br />
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