Drained creep of undisturbed cohesive marine sediments

Authors

W. M. Tian
A. J. Silva, University of Rhode Island
G. E. Veyera, University of Rhode Island
M. H. Sadd, University of Rhode Island

Document Type

Article

Date of Original Version

1-1-1994

Abstract

Time-dependent deformations can be represented by a power law equation. The creep strain rate can be represented by an equation similar to that suggested earlier by other researchers. Ageing effects were evidenced in triaxial specimens by the increase of shear strength with both test duration and stress level. -from Authors

Publication Title, e.g., Journal

Canadian Geotechnical Journal

Volume

31

Issue

6

Citation/Publisher Attribution

Tian, W. M., A. J. Silva, G. E. Veyera, and M. H. Sadd. "Drained creep of undisturbed cohesive marine sediments." Canadian Geotechnical Journal 31, 6 (1994): 841-855. doi: 10.1139/t94-101.