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
[41]  
Meunier A., 2004, ILLITE
[42]   Hydrothermal reactivity of K-smectite at 300°C and 100 bar:: dissolution-crystallization process and non-expandable dehydrated smectite formation [J].
Mosser-Ruck, R ;
Cathelineau, M ;
Baronnet, A ;
Trouiller, A .
CLAY MINERALS, 1999, 34 (02) :275-290
[43]   INVESTIGATION OF KINNEKULLE K-BENTONITE AIMED AT ASSESSING THE LONG-TERM STABILITY OF BENTONITES UNDER REPOSITORY CONDITIONS [J].
MULLERVONMOOS, M ;
KAHR, G ;
BUCHER, F ;
MADSEN, FT .
ENGINEERING GEOLOGY, 1990, 28 (3-4) :269-280
[44]   THE CONVERSION OF SMECTITE TO ILLITE DURING DIAGENESIS - EVIDENCE FROM SOME ILLITIC CLAYS FROM BENTONITES AND SANDSTONES [J].
NADEAU, PH ;
WILSON, MJ ;
MCHARDY, WJ ;
TAIT, JM .
MINERALOGICAL MAGAZINE, 1985, 49 (352) :393-400
[45]  
*NAGR, 1985, 850109 NGB NAGR GEW
[46]  
Nagra, 2002, Nagra Technical Report NTB 02-05
[47]  
NIRAS, 2001, 200106E ONDRAFNIRAS
[48]  
NUMO, 2004, TR0403 NUMO
[49]   Thermodynamic modeling and sensitivity analysis of porewater chemistry in compacted bentonite [J].
Ochs, M ;
Lothenbach, B ;
Shibata, M ;
Yui, M .
PHYSICS AND CHEMISTRY OF THE EARTH, 2004, 29 (01) :129-136
[50]  
Oscarson D.W., 1989, APPL CLAY SCI, V4, P279