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Groundwater fluoride enrichment in an active rift setting: Central Kenya Rift case study

机译:活跃裂谷环境中的地下水氟化物富集:肯尼亚中部裂谷案例研究

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摘要

Groundwater is used extensively in the Central Kenya Rift for domestic and agricultural demands. In these active rift settings groundwater can exhibit high fluoride levels. In order to address water security and reduce human exposure to high fluoride in drinking water, knowledge of the source and geochemical processes of enrichment are required. A study was therefore carried out within the Naivasha catchment (Kenya) to understand the genesis, enrichment and seasonal variations of fluoride in the groundwater. Rocks, rain, surface and groundwater sources were sampled for hydrogeochemical and isotopic investigations, the data was statistically and geospatially analyzed. Water sources have variable fluoride concentrations between 0.02-75 mg/L. 73% exceed the health limit (1.5 mg/L) in both dry and wet seasons. F~- concentrations in rivers are lower (0.2-9.2 mg/L) than groundwater (0.09 to 43.6 mg/L) while saline lake waters have the highest concentrations (0.27-75 mg/L). The higher values are confined to elevations below 2000 masl. Oxygen (δ~(18)O) and hydrogen (δD) isotopic values range from - 62 to + 5.8‰ and - 31.3 to + 33.3‰, respectively, they are also highly variable in the rift floor where they attain maximum values. Fluoride base levels in the precursor vitreous volcanic rocks are higher (between 3750-6000 ppm) in minerals such as cordierite and muscovite while secondary minerals like illite and kaolinite have lower remnant fluoride (< 1000 ppm). Thus, geochemical F~- enrichment in regional groundwater is mainly due to a) rock alteration, i.e. through long residence times and natural discharge and/or enhanced leakages of deep seated geothermal water reservoirs, b) secondary concentration fortification of natural reservoirs through evaporation, through reduced recharge and/or enhanced abstraction and c) through additional enrichment of fluoride after volcanic emissions. The findings are useful to help improve water management in Naivasha as well as similar active rift setting environments.
机译:肯尼亚中部裂谷广泛使用地下水以满足家庭和农业需求。在这些活跃的裂谷环境中,地下水中氟化物含量较高。为了解决水的安全问题并减少人类接触饮用水中的高氟化物,需要了解浓缩的来源和地球化学过程。因此,在奈瓦沙流域(肯尼亚)内进行了一项研究,以了解地下水中氟化物的成因,富集和季节性变化。对岩石,雨水,地表水和地下水进行了采样,以进行水文地球化学和同位素研究,并对数据进行了统计和地理空间分析。水中的氟化物浓度在0.02-75 mg / L之间。在干燥和潮湿的季节中,超过健康限值(1.5 mg / L)的73%。河流中的F-浓度低于地下水(0.09至43.6 mg / L)(0.2-9.2 mg / L),而盐湖水的浓度最高(0.27-75 mg / L)。较高的值被限制在2000 masl以下的海拔高度。氧(δ〜(18)O)和氢(δD)同位素值分别在-62至+ 5.8‰和-31.3至+ 33.3‰范围内,并且在裂谷层达到最大值时也高度可变。堇青石和白云母等矿物中玻璃质前火山岩中的氟化物碱含量较高(在3750-6000 ppm之间),而伊利石和高岭石等次生矿物中的残留氟化物含量较低(<1000 ppm)。因此,区域地下水中的地球化学富集主要是由于a)岩石蚀变,即长时滞和自然排放和/或深层地热水储集层渗漏增加,b)自然储集层通过蒸发的二次浓缩强化,通过减少补给和/或增加提取,以及c)通过在火山释放后进一步富集氟化物。这些发现对于帮助改善奈瓦沙以及类似的活跃裂谷环境中的水管理非常有用。

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  • 来源
    《The Science of the Total Environment》 |2016年第1期|641-653|共13页
  • 作者单位

    Department of Geology, University of Nairobi, P.O Box 30197, Nairobi, Kenya;

    Geoforschungs Zentrum, Telegrafenberg, 14473 Potsdam, Germany;

    Department of Geology, University of Nairobi, P.O Box 30197, Nairobi, Kenya;

    Department of Geology, University of Nairobi, P.O Box 30197, Nairobi, Kenya;

    Senckenberg Biodiversity and Climate Research Centre, Senckenberganlage 25, 60325 Frankfurt, Germany,Institut fuer Geowissenschaften, Goethe Universitaet Frankfurt, Altenhoeferallee 1, 60438 Frankfurt, Germany;

    UFZ-Helmholtz-Centre for Environmental Research, Department of Hydrogeology, Permoserstr. 15, 04318 Leipzig, Germany;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Fluoride; Chloride; Isotopes; Water-rock interaction; Groundwater; Central Kenya Rift;

    机译:氟化物;氯化物;同位素;水岩相互作用;地下水;肯尼亚中部裂谷;

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