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首页> 外文期刊>Environmental earth sciences >Mechanism of fluoride enrichment in groundwater of hard rock aquifers in Medak, Telangana State, South India
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Mechanism of fluoride enrichment in groundwater of hard rock aquifers in Medak, Telangana State, South India

机译:印度南部特兰甘纳邦Medak硬岩含水层地下水中氟的富集机理

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摘要

A total of 194 groundwater samples were collected from wells in hard rock aquifers of the Medak district, South India, to assess the distribution of fluoride in groundwater and to determine whether this chemical constituent was likely to be causing adverse health effects on groundwater user in the region. The study revealed that the fluoride concentration in groundwater ranged between 0.2 and 7.4 mg/L with an average concentration of 2.7 mg/L. About 57% of groundwater tested has fluoride concentrations more than the maximum permissible limit of 1.5 mg/L. The highest concentrations of fluoride were measured in groundwater in the north-eastern part of the Medak region especially in the Siddipeta, Chinnakodur, Nanganoor and Dubhaka regions. The areas are underlain by granites which contain fluoride-bearing minerals like apatite and biotite. Due to water-rock interactions, the fluoride has become enriched in groundwater due to the weathering and leaching of fluoride-bearing minerals. The pH and bicarbonate concentrations of the groundwater are varied from 6.6 to 8.8 and 18 to 527 mg/L, respectively. High fluoride concentration in the groundwater of the study area is observed when pH and the bicarbonate concentration are high. Data plotted in Gibbs diagram show that all groundwater samples fall under rock weathering dominance group with a trend towards the evaporation dominance category. An assessment of the chemical composition of groundwater reveals that most of the groundwater samples have compositions of Ca2+ -Mg2+ -Cl- > Ca2+ -Na+ -HCO3(-) > Ca (2+) -HCO3 (-) > Na+ -HCO3-. This suggests that the characteristics of the groundwater flow regime, long residence time and the extent of groundwater interaction with rocks are the major factors that influence the concentration of fluoride. It is advised not to utilize the groundwater for drinking purpose in the areas delineated, and they should depend on alternate safe source.
机译:从南印度Medak区硬岩含水层的水井中总共收集了194个地下水样品,以评估地下水中氟化物的分布,并确定该化学成分是否可能对印度洋地下水使用者造成不利的健康影响。区域。研究表明,地下水中的氟化物浓度在0.2至7.4 mg / L之间,平均浓度为2.7 mg / L。测试的地下水中约有57%的氟化物浓度超过最大允许限值1.5 mg / L。在Medak地区东北部,尤其是Siddipeta,Chinnakodur,Nanganoor和Dubhaka地区的地下水中,氟化物的最高浓度被测出。这些地区被花岗岩所覆盖,这些花岗岩中含有磷矿和黑云母等含氟矿物。由于水与岩石的相互作用,氟化物由于含氟矿物的风化和浸出而富集在地下水中。地下水的pH值和碳酸氢盐浓度分别为6.6至8.8和18至527 mg / L。当pH和碳酸氢盐浓度较高时,研究区域的地下水中氟化物浓度较高。吉布斯图中绘制的数据表明,所有地下水样本都属于岩石风化主导类,并且具有蒸发主导类的趋势。对地下水化学成分的评估表明,大多数地下水样品的成分为Ca2 + -Mg2 + -Cl-> Ca2 + -Na + -HCO3(-)> Ca(2+)-HCO3(-)> Na + -HCO3-。这表明地下水流态的特征,较长的停留时间以及地下水与岩石的相互作用程度是影响氟化物浓度的主要因素。建议不要在划定的区域内将地下水用于饮用,它们应依靠替代的安全水源。

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