Deformation behaviour of clay under repeated one-dimensional unloading–reloading

Author:

Suddeepong Apichat1,Chai Jinchun1,Shen Shuilong2,Carter John3

Affiliation:

1. Department of Civil Engineering and Architecture, Saga University, 1 Honjo machi, Saga City, Saga 840-8502, Japan.

2. Department of Civil Engineering and State Key Laboratory of Ocean Engineering, Shanghai Jiao Tong University, Shanghai 200240, China.

3. Faculty of Engineering and Built Environment, The University of Newcastle, NSW 2308, Australia.

Abstract

The deformation of clayey soil under repeated cycles of unloading and reloading has been investigated in oedometer tests using both undisturbed and reconstituted Ariake clay samples. The test results indicate that even for repeated unloading–reloading in the overconsolidated stress range, the deformation of the soil sample is not purely elastic and there is an accumulation of permanent deformation. Based on the test results, a model has been proposed for predicting unloading–reloading-induced deformation. The proposed model has been used to simulate the behaviour of a clayey soil deposit in the Saga Plain, Japan, in response to groundwater fluctuation. Good agreement between the simulation and the field measurements indicates that the proposed model can be used to predict land subsidence induced by groundwater fluctuations.

Publisher

Canadian Science Publishing

Subject

Civil and Structural Engineering,Geotechnical Engineering and Engineering Geology

Reference11 articles.

1. ASTM. 2006. Standard practice for classification of soils for engineering purposes (Unified Soil Classification System). ASTM standard D2487. American Society for Testing and Materials, West Conshohocken, Pa.

2. An Improved Model of Soil Response to Load, Unload and Re-Load Cycles in an Oedometer

3. Carter, J.P., Booker, J.R., and Wroth, C.P. 1982. A critical state model for cyclic loading. In Soil mechanics - transient and cyclic loads. Chapter 9. Edited by G.N. Pande and O.C. Zienkiewicz. John Wiley and Sons, London, pp. 219–252.

4. Land subsidence due to groundwater drawdown in Shanghai

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