In this paper, triaxial test results on overconsolidated cohesive soil with various preconsolidation pressures and overconsolidation ratios are shown which were carried out under drained or undrained condition. From these results,
e-log
p relationships at both peak and residual states and
q-
p relationships are presented. An expression on failure strength of overconsolidated cohesive soil is given which is obtained from the assumption that Hvorslev's failure criterion of soil is valid and the slope of
e-log
p relationship at wet side is different from the one at dry side. The validity of this idea is verified by the author's and other researchers' experimental results. Finally the relationship between the coefficients used in the present theory and the plasticity index is discussed.
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