Performance of the bentonite barrier at temperatures beyond 100 °C:: A critical review

被引:131
作者
Wersin, P. [1 ]
Johnson, L. H. [1 ]
McKinley, I. G. [1 ]
机构
[1] Natl Cooperat Disposal Radioact Waste, Nagra, CH-5430 Wettingen, Switzerland
关键词
bentonite buffer; temperature effects; alteration; high-level waste repository;
D O I
10.1016/j.pce.2006.02.051
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Many current concepts for the engineered barriers of high-level waste repositories include a bentonite buffer or backfill which will be exposed to significantly raised temperatures for a period of decades to centuries. To assess its stability, available experimental and natural analogue data on thermally-exposed bentonite is reviewed. The two main alteration processes identified are cementation by precipitation of SiO2 and transformation of smectite to non-expandable illite layers. These may lead to reduced swelling and loss of plasticity as well as increased hydraulic conductivity and diffusivity. Relevant data for repository conditions from both laboratory and field studies is scarce, but nevertheless yields a fairly consistent picture. Thus, no significant changes of hydraulic and mechanical properties have been reported for bentonite materials exposed to temperatures of at least 120 degrees C under wet conditions. The data suggest significant cementation and perhaps also illitisation effects occur at 150 degrees C and beyond. Interestingly, natural analogue bentonite samples that showed substantial cementation and illitisation effects still displayed rather favourable hydraulic properties. Under dry conditions, bentonite is stable to higher temperatures - maybe as high as 350 degrees C. In order to verify the findings from this work and to get more reliable information at temperatures beyond 130 degrees C, a series of long-term experiments examining hydraulic, mechanical and mineralogical changes under realistic conditions would be useful. (C) 2006 Elsevier Ltd. All rights reserved.
引用
收藏
页码:780 / 788
页数:9
相关论文
共 75 条
[2]   Formation of grain-coating chlorite in sandstones.: Laboratory synthesized vs. natural occurrences [J].
Aagaard, P ;
Jahren, JS ;
Harstad, AO ;
Nilsen, O ;
Ramm, M .
CLAY MINERALS, 2000, 35 (01) :261-269
[3]  
AHN JH, 1986, CLAY CLAY MINER, V34, P165
[4]   CALCULATION OF K-DIFFUSIONAL RATES IN BENTONITE BEDS [J].
ALTANER, SP .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1989, 53 (04) :923-931
[5]  
[Anonymous], ORIGIN MINERALOGY CL
[6]  
[Anonymous], 1968, CLAY MINER
[7]   PILOT FIELD EXPERIMENT WITH CANISTER-EMBEDDING CLAY UNDER SIMULATED REPOSITORY CONDITIONS [J].
ATABEK, R ;
LAJUDIE, A ;
LECHELLE, J ;
PUSCH, R .
ENGINEERING GEOLOGY, 1990, 28 (3-4) :291-302
[8]  
BEL J, 2001, P ICEM 2001 OCT 1 4
[10]   LAYER-BY-LAYER MECHANISM OF SMECTITE ILLITIZATION AND APPLICATION TO A NEW RATE LAW [J].
BETHKE, CM ;
ALTANER, SP .
CLAYS AND CLAY MINERALS, 1986, 34 (02) :136-145