New experimental developments for in situ XAFS studies of chemical reactions under hydrothermal conditions

被引:33
作者
Hoffmann, MM [1 ]
Darab, JG [1 ]
Heald, SM [1 ]
Yonker, CR [1 ]
Fulton, JL [1 ]
机构
[1] Pacific NW Natl Lab, Environm & Hlth Sci Div, Richland, WA 99352 USA
关键词
X-ray absorption fine structure spectroscopy (XAFS); hydrothermal solutions; sodium tungstate; nickel bromide; quartz;
D O I
10.1016/S0009-2541(99)00202-8
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
New experimental developments for in situ X-ray absorption fine structure spectroscopy (XAFS) studies of hydrothermal systems are described. Improvements in materials of construction and the design of spectroscopic cells have allowed application of XAFS as a powerful method to derive the molecular structures of reacting species. Two different spectroscopic cells are described that are suitable for in situ XAFS studies of aqueous solutions under hydrothermal conditions. One cell consists of a titanium alloy body with a corrosion-resistant platinum-iridium insert and diamond windows for X-ray transmission. Using this cell, XAFS spectra were acquired on aqueous tungstate solutions up to 400 degrees C. The results demonstrate how XAFS can be used to study the speciation of isopolytungstates and their equilibria at high temperatures. Results from model calculations using the FEFF ab initio code are used to explain the observed spectral changes with changes in pH and temperature. The second XAFS cell consists of a simple fused-silica capillary having a 180 mu m inner diameter. High-quality spectra of a 0.2 molal nickel bromide solution were collected in these small capillaries demonstrating the feasibility of the approach to the study of a wide range of geochemical systems. Further, the XAFS spectra show that the nickel bromide solution irreversibly reacts with the fused-silica capillary at 425 degrees C. Based upon these observations, a potential use of the fused-silica capillary is suggested for in situ studies of silicate formation, or, in general, for studies of chemical interactions of hydrothermal brine solutions with quartz. (C) 2000 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:89 / 103
页数:15
相关论文
共 43 条
[1]  
BAI S, IN PRESS J PHYSICA A
[2]  
Bassett WA, 1998, GEOPH MONOG SERIES, V101, P507
[3]   RAMAN-SPECTROSCOPIC AND ELECTROCHEMICAL STUDY OF POLYMERIZATION OF TUNGSTEN (VI) IN A HYDROTHERMAL SOLUTION UP TO 1 KBAR AND 200-DEGREES-C [J].
BILAL, BA ;
HAUFE, P ;
MOLLER, P .
PHYSICA B & C, 1986, 139 (1-3) :721-724
[4]  
BROWN GE, 1988, REV MINERAL, V18, P431
[5]   THE ENTHALPY OF DILUTION OF AQUEOUS SODIUM-CHLORIDE TO 673-K USING A NEW HEAT-FLOW AND LIQUID-FLOW MICROCALORIMETER - EXCESS THERMODYNAMIC PROPERTIES AND THEIR PRESSURE COEFFICIENTS [J].
BUSEY, RH ;
HOLMES, HF ;
MESMER, RE .
JOURNAL OF CHEMICAL THERMODYNAMICS, 1984, 16 (04) :343-372
[6]  
COLLINGS M, 1998, MINERALOGICAL MAG A, V62, P345
[7]  
COTTON FA, 1980, ADV INORG CHEM, P844
[8]  
CYVIN SJ, 1968, MOL VIBRATIONS MEAT, P71
[9]   Chemistry of technetium and rhenium species during low-level radioactive waste vitrification [J].
Darab, JG ;
Smith, PA .
CHEMISTRY OF MATERIALS, 1996, 8 (05) :1004-1021
[10]  
EVANS HT, 1971, PERSPECTIVES STRUCTU, P35