Results of miniature piezocone penetration tests (PCPT) on cohesive so
il specimens in a calibration chamber system are presented. The influe
nce of soil type, stress history, penetration boundary conditions, and
fitter locations on PCPT data are investigated. An increase in the st
rength of the soil around the cone penetrometer is observed when penet
ration is resumed after a dissipation test. The penetration depth requ
ired to attain a steady excess pore pressure value at the tip of the c
one is influenced by the overconsolidation ratio and the lateral stres
s coefficient. The empirical values of the cone factor and the pore pr
essure factor are found to be strongly influenced by the lateral stres
s and the plasticity index. The tip resistance measured during the min
iature quasi-static friction cone penetration tests (QCPT) are consist
ently lower than the values obtained from the PCPT. Interpretation of
the dissipation results to evaluate the radial coefficient of consolid
ation should be based on the initial dissipation values of the excess
pore pressure, and not the penetration pore pressure.