氟在土壤中的富集与淋滤
Fluoride Enrichment and Leaching in the Soil:A Review
查看参考文献61篇
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文摘
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土壤中的氟处于淋失和富集两种地球化学作用过程的平衡之中.淋失过程占优势的条件下,在干旱半干旱地区内的特定区域形成地带性的高氟地面水和地下水,这是饮水型地方性氟中毒发生的物质基础.在氟的富集占优势的条件下,湿润气候地区将形成富氟土壤,并与其它条件结合则产生燃煤型地方性氟中毒.在决定风化壳中氟平衡状态的诸因素中,粘土矿物对氟的吸附与解吸附性质是最关键的因素 |
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其他语种文摘
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Fluoride is in the geochemical balance of enrichment and leaching in the soils. Under the conditions of the leaching process being dominant, high-fluoride surface water and groundwater form in the arid and semi-arid areas, and drinking water type endemic fluorosis forms. Under the conditions of the enrichment being the dominant process, fluorine-rich soil forms in humid climatic regions, and combined with other conditions coal-combustion type endemic fluorosis forms. Fluoride adsorption and desorption on clay minerals is the most critical factor in the various factors affecting the equilibrium of fluorine in weathering crust |
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来源
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矿物学报
,2010,30(4):496-500 【核心库】
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关键词
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氟
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土壤
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粘土矿物
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吸附
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解吸附
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地址
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1.
中国科学院地球化学研究所, 环境地球化学国家重点实验室, 贵州, 贵阳, 550002
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贵州省人民医院, 贵州, 贵阳, 550002
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语种
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中文 |
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文献类型
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研究性论文 |
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ISSN
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1000-4734 |
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学科
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地质学;环境科学基础理论 |
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基金
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贵州省项目
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贵州省"十一五"社会发展科技项目
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科技部国际合作重大项目
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文献收藏号
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CSCD:4097448
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