Modes of occurrence of arsenic in high-arsenic coal by extended X-ray absorption fine structure spectroscopy
被引:24
作者:
Zhao, FH
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机构:
China Univ Min & Technol, Beijing 100083, Peoples R ChinaChina Univ Min & Technol, Beijing 100083, Peoples R China
Zhao, FH
[1
]
Ren, DY
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机构:China Univ Min & Technol, Beijing 100083, Peoples R China
Ren, DY
Zheng, BS
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机构:China Univ Min & Technol, Beijing 100083, Peoples R China
Zheng, BS
Hu, TD
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h-index: 0
机构:China Univ Min & Technol, Beijing 100083, Peoples R China
Hu, TD
Liu, T
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h-index: 0
机构:China Univ Min & Technol, Beijing 100083, Peoples R China
Liu, T
机构:
[1] China Univ Min & Technol, Beijing 100083, Peoples R China
[2] Chinese Acad Sci, Inst Geochem, Guiyang 550002, Peoples R China
[3] Chinese Acad Sci, Inst High Energy Phys, Beijing 100039, Peoples R China
来源:
CHINESE SCIENCE BULLETIN
|
1998年
/
43卷
/
19期
关键词:
high-arsenic coal;
modes of occurrence;
synchrotron radiation;
EXAFS spectroscopy;
D O I:
10.1007/BF02883414
中图分类号:
O [数理科学和化学];
P [天文学、地球科学];
Q [生物科学];
N [自然科学总论];
学科分类号:
07 ;
0710 ;
09 ;
摘要:
The concentration ranges of As and Sb in six Late Permian high-arsenic coals collected from Xingren and Xingyi, Guizhou Province are 94.1 mu g.g(-1)-3.2% and 8.1 mu g.g(-1)-120 mu g.g(-1), respectively. Based on the mineralogical analysis, no arsenic and arsenic-bearing minerals are detected in these samples and arsenic occurs in coal macerals. By extended X-ray absorption fine structure(EXAFS) spectroscopy, we have found that arsenic in these high-arsenic coal samples coordinates with oxygen; the coordination number of As with oxygen for these samples is 4 except one sample(H(9)) for which the coordination number of As is 3. Therefore, arsenic in these high-arsenic coals does not occur in sulfide minerals, but occurs in arsenate or arsenite phase, and the preponderance of As is in arsenate of As(5+).