Research Article

Modified Liu-Carter Compression Model for Natural Clays with Various Initial Water Contents

Table 1

Details of soil samples and model parameters.

Soils (g⋅cm−3) (%)/ (kPa)Reference

Singapore clay2.74841.590.692180.500.54Low et al. [8]
Gulf of Guinea clay2.651183.281.05981.170.55Hattab et al. [17]
Lianyungang clay2.73531.791.24690.610.60Deng et al. [18]
Jangyu clay2.71602.351.45600.970.44Chung et al. [19]
Undisturbed Ariake clay 2.661274.301.27381.150.30Liu and Hong [20]
Disturbed Ariake clay2.661274.301.27291.270.26Liu and Hong [20]
Shanghai clay2.70451.150.941600.310.24Li et al. [21]
Batiscan clay2.67432.131.851171.151.05Leroueil et al. [22]
Wenzhou clay Bian [23]
 5 m2.70 651.911.05610.600.53
 7.5 m2.73 701.941.01580.520.41
 10 m2.71 691.901.02800.580.53
 12.5 m2.71 732.011.02920.740.56
 15 m2.70 761.840.901000.530.85
 17.5 m2.71 741.730.871480.540.42
 20 m2.71651.600.911380.550.57
 22.5 m2.73671.420.781560.370.79