Consolidation characteristics of clay, which are compressibility, permeability and consolidation velocity etc., are conventionally represented by relationships between the “arithmetic scaled” volume ratio
f or void ratio
e and the logarithmic scaled effective stress
p, coefficient of permeability
k and coefficient of consolidation
cv etc. However, some previous works have suggested that a relation of volume ratio
f and effective stress
p in double logarithmic scale (log
f-log
p) is able to express compressibility of clay more reasonably than the one in single logarithmic scale (
f-log
p). At the exordium of this paper, the rationale of representation of consolidation characteristics of clay including
k and
cv by “logarithmic
f” than “arithmetic
f” was derived from a revisional study on them. Next, experimental results of a series of centrifuge consolidation test for the very soft clay (dredged clay) were examined. Then their results were numerically simulated for two cases of using “logarithmic
f” or “arithmetic
f”. As a consequence, consolidation curves experimentally obtained were correctly represented by the numerical simulation with “logarithmic
f”. Moreover, it was found that more stable and faster calculation is enabled by applying “logarithmic
f” instead of “arithmetic
f” to the expansion of the consolidation equation.
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