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首页> 外文期刊>Environmental Geochemistry and Health >Geochemical provenance and spatial distribution of fluoride in groundwater of Mayo Tsanaga River Basin, Far North Region, Cameroon: implications for incidence of fluorosis and optimal consumption dose
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Geochemical provenance and spatial distribution of fluoride in groundwater of Mayo Tsanaga River Basin, Far North Region, Cameroon: implications for incidence of fluorosis and optimal consumption dose

机译:喀麦隆远北地区梅奥扎那加河流域地下水中氟化物的地球化学来源和空间分布:对氟中毒发生率和最佳消费剂量的影响

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摘要

The 500,000 inhabitants of Mayo Tsanaga River Basin are vulnerable to a "silent" fluorosis from groundwater consumption. For the first time, the groundwater is investigated for the purpose of identifying the provenance of fluoride and estimating an optimal dose of fluoride in the study area. Based on the fluoride content of groundwater, fluorine and major oxides abundances in rocks from the study area, mean annual atmospheric temperature, and on-site diagnosis of fluorosis in children, the following results and conclusions are obtained: Fluoride concentration in groundwater ranges from 0.19 to 15.2 mg/l. Samples with fluoride content of <1.5 mg/l show Ca-HCO_3rnsignatures, while those with fluoride >1.5 mg/l show a tendency towards Na-HCO_3 type. Fluor-apatite and micas in the granites were identified as the main provenance of fluoride in the groundwater through water-rock interactions in an alkaline medium. The optimal fluoride dose in drinking water of the study area should be 0.7 mg/l, and could be adjusted downward to a level of 0.6 mg/l due to the high consumption rate of groundwater, especially during drier periods.
机译:玛雅扎纳加河流域的50万居民很容易受到地下水消耗造成的“无声”氟中毒。首次对地下水进行了研究,目的是确定氟化物的来源并估算研究区域中氟化物的最佳剂量。根据研究区域岩石中的氟化物含量,岩石中的氟和主要氧化物含量,年平均气温以及对儿童氟中毒的现场诊断,得出以下结果和结论:地下水中的氟浓度范围为0.19至15.2 mg / l。氟化物含量<1.5 mg / l的样品表现出Ca-HCO_3特征,而氟化物含量> 1.5 mg / l的样品表现出Na-HCO_3类型的趋势。花岗岩中的氟磷灰石和云母通过碱性介质中的水-岩相互作用被确定为地下水中氟化物的主要来源。研究区域饮用水中的最佳氟化物剂量应为0.7 mg / l,并​​且由于地下水的高消耗率(尤其是在干旱时期),可以将其下调至0.6 mg / l的水平。

著录项

  • 来源
    《Environmental Geochemistry and Health》 |2010年第2期|147-163|共17页
  • 作者单位

    Department of Environmental Biology and Chemistry,Graduate School of Science and Engineering, University of Toyama, Gofuku 3190, Toyama 930-8555, Japan Center for Hydrological Research, Institute of Mining and Geological Research (IRGM), Box 4110,Yaounde, Cameroon;

    Department of Environmental Biology and Chemistry,Graduate School of Science and Engineering, University of Toyama, Gofuku 3190, Toyama 930-8555, Japan;

    Department of Geology and Environmental Science,University of Buea, Buea, Cameroon;

    Department of Geology and Environmental Science,University of Buea, Buea, Cameroon;

    Department of Geology and Mineral Science,University of Ilorin, PMB 1515, Ilorin, Nigeria;

    Laboratory of Geodynamics, Graduate School of Science and Engineering, University of Toyama, Gofuku 3190,Toyama 930-8555, Japan;

    Global Water Partnership, Yaounde, Cameroon;

    Provincial Delegation of Public Health,Far North Region, Box 620, Maroua, Cameroon;

    Provincial Hospital Maroua, Box 57, Maroua, Cameroon;

    Department of Environmental Biology and Chemistry,Graduate School of Science and Engineering, University of Toyama, Gofuku 3190, Toyama 930-8555, Japan;

    Department of Environmental Biology and Chemistry,Graduate School of Science and Engineering, University of Toyama, Gofuku 3190, Toyama 930-8555, Japan;

  • 收录信息 美国《科学引文索引》(SCI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    groundwater; fluoride provenance; optimal dose; fluorosis; mayo tsanaga river basin;

    机译:地下水;氟化物来源最佳剂量氟中毒梅加沙永河流域;

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