Abstract
The rheological behavior of soil mass is usually not governed simply by a single process of creep and stress relaxation. Here, a Mesri stress-strain-time relation function (Mesri., G. etc. 1981) is applied to describe the coupled effect of creep and stress relaxation of soft clay. Numerical results are compared with those obtained from data acquired from coupled creep-stress relaxation tests of clay samples. The results of the study are satisfactory. Some relevant factors influencing the coupled effect are also discussed.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
References
Mesri. G., Febres-Cordero. E., Shields, D. R., & Castro, A. (1981) Shear stress-strain-time behaviour of clays, Geotechnique, 31(4):537–552.
Liu Xiong (1994) An Introduction to Rheology of Rocks, Publishers of Geology, Beijing (In Chinese)
Zhu Changqi and Guo Jianyang (1990) A further understanding of the rheological characteristics of clay and the new method of determining the long-term strength of clay. Geomechanics, 11(2): 15–22 (In Chinese)
Xiong Junmin and Li Zuoqin (1993) Tests on coupled creep-relaxation of clay. Geomechanics, 14(4): 17–24 (In Chinese).
Author information
Authors and Affiliations
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 1999 Kluwer Academic Publishers
About this paper
Cite this paper
Li, J., Sun, J. (1999). Coupled Effect of Creep and Stress Relaxation of Soft Clay. In: Wang, R. (eds) IUTAM Symposium on Rheology of Bodies with Defects. Solid Mechanics and its Applications, vol 64. Springer, Dordrecht. https://doi.org/10.1007/0-306-46937-5_19
Download citation
DOI: https://doi.org/10.1007/0-306-46937-5_19
Publisher Name: Springer, Dordrecht
Print ISBN: 978-0-7923-5297-6
Online ISBN: 978-0-306-46937-4
eBook Packages: Springer Book Archive