A study of the hydro-mechanical behaviour of compacted crushed argillite

被引:37
|
作者
Tang, C. S. [1 ,2 ]
Tang, A. M. [1 ]
Cui, Y. J. [1 ,3 ]
Delage, P. [1 ]
Schroeder, C.
Shi, B. [2 ]
机构
[1] UR Navier CERMES, Ecole Ponts ParisTech, Paris, France
[2] Nanjing Univ, Sch Earth Sci & Engn, Nanjing, Peoples R China
[3] China Three Gorges Univ, Yichang 443002, Peoples R China
关键词
Compacted crushed argillite; Radioactive waste disposal; Swelling pressure; Microstructure; Grain size effect; Hydro-mechanical coupling; MECHANICAL-BEHAVIOR; WATER-RETENTION; BENTONITE; CLAY; SUCTION; VOLUME; SUSCEPTIBILITY; MIXTURE; SOILS; MODEL;
D O I
10.1016/j.enggeo.2011.01.004
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
The argillite extracted from Bure site (France) is proposed, after being crushed and compacted, as a possible sealing and backfill material in the French geological high-level radioactive waste disposal. In this study, the effects of the grain size distribution and the microstructure on the hydro-mechanical behaviour of the compacted crushed argillite have been investigated. The volume change properties were investigated by running one-dimensional compression tests under constant water content (2.4-2.8%) with loading-unloading cycles. Under various vertical stresses, water flooding tests were carried out under constant-volume condition. Depending on the vertical stress level, either swelling or collapse behaviour was observed in the sense that vertical stress increased or decreased upon flooding respectively. A clear effect of grain size distribution has been also identified: finer samples exhibit stiffer compression behaviour and higher swelling potential. To provide a microstructure insight into the macroscopic behaviour feature observed, both mercury intrusion porosimetry (MIP) and scanning electron microscopy (SEM) observations were performed, evidencing that: (i) at the same dry density, the size of inter-aggregate pores is larger for the coarser crushed material; (ii) mechanical compression only reduces the inter-aggregate porosity in the stress range considered; (iii) the micro-mechanisms governing the flooding under constant-volume condition include the swelling of the clay particles, the increase of the intra-aggregate pores and the collapse of the inter-aggregate pores. The results show a strong effect of the grain size distribution on the hydro-mechanical behaviour and thus the close link between the microstructure and the hydro-mechanical behaviour. (C) 2011 Elsevier B.V. All rights reserved.
引用
收藏
页码:93 / 103
页数:11
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