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岩石中氟的赋存状态研究
引用本文:徐立荣,雒昆利. 岩石中氟的赋存状态研究[J]. 环境化学, 2008, 27(1): 91-95
作者姓名:徐立荣  雒昆利
作者单位:济南大学城市发展学院,济南,250002;中国科学院地理科学与资源研究所,北京,100101
基金项目:国家科技攻关计划 , 山东省重点学科水文学与水资源基金 , 山东省教育厅资助项目
摘    要:使用逐级化学提取方法对岩石中氟的赋存状态进行了研究.结果表明:岩石中氟主要与K和Al呈显著相关,高氟岩石中氟与P呈显著正相关,氟主要以氟磷灰石的形式存在;经逐级提取后残渣中的氟与Ca呈显著负相关关系,碳酸盐岩和磷块岩中的氟主要以水溶态和碳酸盐结合态等易溶形式存在;而硅质岩、黑色页岩、硅质碳板岩和碳质板岩中的氟主要存在于难溶矿物中.

关 键 词:  岩石  赋存状态  逐级化学提取.
收稿时间:2007-05-17
修稿时间:2007-05-17

STUDIES ON MODE OF OCCURRENCE OF FLUORINE IN ROCKS
XU Li-rong,LUO Kun-li. STUDIES ON MODE OF OCCURRENCE OF FLUORINE IN ROCKS[J]. Environmental Chemistry, 2008, 27(1): 91-95
Authors:XU Li-rong  LUO Kun-li
Abstract:Sequential extraction experiments were used to determine the mode of occurrence of fluorine in rocks in this paper.The results show that F correlates positively with K and Al in rocks,and there is also significant positive correlation between F and P in rocks with high F content,in which F is likely to occur as fluorapatite.Negative correlation is found between F and Ca in leached residues.Our data suggest that F occurs as water-soluble compounds and carbonates-associated in carbonate rocks and phosphorite rocks.However,in siliceous rocks,black shale and carbonaceous slate,F mainly occurs in stable compounds which are not dissolved in our solvents.
Keywords:fluorine  rock  mode of occurrence  sequential extraction experiments.
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