Surface layers on a borosilicate nuclear waste glass corroded in MgCl2 solution

被引:57
作者
Abdelouas, A
Crovisier, JL
Lutze, W
Grambow, B
Dran, JC
Muller, R
机构
[1] FORSCHUNGSZENTRUM KARLSRUHE,INE,D-76021 KARLSRUHE,GERMANY
[2] CTR GEOCHIM SURFACE,CNRS,F-67084 STRASBOURG,FRANCE
[3] UNIV NEW MEXICO,FARRIS ENGN CTR 151,ALBUQUERQUE,NM 87131
[4] CTR SPECTROMETRIE NUCL & SPECTROMETRIE MASSE,IN2P3,F-91405 ORSAY,FRANCE
关键词
D O I
10.1016/S0022-3115(96)00672-1
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Surface layers on the French borosilicate nuclear waste glass, R7T7, corroded in MgCl2 solution were studied to determine the composition, structure and stability of crystalline phases. The characteristics of the phases constituting the surface layer varied with the parameter S/V X t, the glass surface area (S) to solution volume (V) ratio, times time (t). At low S/V X t values (< 360 days/m; less than or equal to 36 d) the surface layer was thin and contained mainly iron hydroxide particles and hydrotalcite crystals. At an intermediate S/V X t value (2800 d/m; 5.5 y) the surface layer contained hydrotalcite- chlorite- and saponite-type phases. At the highest S/V X t value (10(7) d/m; 463 d) the major phases were saponite, powellite, barite and cerianite solid solutions. About 95% of the uranium and > 98% of the neodymium released from the glass were precipitated in the surface layer. In the 463 day experiment, 86% of the neodymium in the surface layer was in solid solution with powellite, the rest with saponite. Uranium was contained exclusively in saponite. High S/V ratios, typical of disposal conditions for vitrified high-level radioactive waste, favor retention of actinides in fairly insoluble corrosion products. Observation of similar corrosion products on natural glasses as on nuclear waste glasses lend support to the hypothesis that the host phases for actinides observed in the laboratory are stable over geological periods of time.
引用
收藏
页码:100 / 111
页数:12
相关论文
共 58 条
[1]  
ABDELOUAS A, 1993, CR ACAD SCI II, V317, P1333
[2]  
ABDELOUAS A, 1993, CR ACAD SCI II, V317, P1067
[3]  
ABDELOUAS A, 1996, THESIS U LOUIS PASTE
[4]  
ABDELOUAS A, 1995, EUR J MINERAL, V5, P526
[5]  
ABDELOUAS A, 1994, CLAYS CLAY MINER, V5, P526
[6]   SECONDARY PHASE FORMATION DURING NUCLEAR WASTE-GLASS DISSOLUTION [J].
ABRAJANO, TA ;
BATES, JK ;
WOODLAND, AB ;
BRADLEY, JP ;
BOURCIER, WL .
CLAYS AND CLAY MINERALS, 1990, 38 (05) :537-548
[7]  
ANDRIAMBOLOLONA Z, 1992, APPL GEOCHEM S, V1, P23
[8]  
BERGER G, 1987, EARTH PLANET SC LETT, V25, P385
[9]   THERMAL-BEHAVIOR OF HYDROTALCITE AND OF ANION-EXCHANGED FORMS OF HYDROTALCITE [J].
BRINDLEY, GW ;
KIKKAWA, S .
CLAYS AND CLAY MINERALS, 1980, 28 (02) :87-91
[10]  
BROWER E, 1971, BUR MINES MINER RESO, V116, P21