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首页> 外文期刊>Environmental Monitoring and Assessment >Groundwater hydro-geochemistry, quality, microbiology and human health risk assessment in semi-arid area of Rajasthan, India: a chemometric approach
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Groundwater hydro-geochemistry, quality, microbiology and human health risk assessment in semi-arid area of Rajasthan, India: a chemometric approach

机译:印度拉贾斯坦邦半干旱地区的地下水 - 地球化学,品质,微生物学和人体健康风险评估:化学计量方法

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The present investigation focused on groundwater hydro-geochemistry of Alsisar block of Jhunjhunu district, India, aims on evaluating the quality of groundwater for drinking and irrigation purposes and assessing the human health risk from ingestion of groundwater. The groundwater of Alsisar block is neutral to alkaline, brackish and very hard in nature. Total dissolved solids, total hardness, Na+, Mg2+, HCO3-, F- and NO3- in majority of the groundwater samples were exceeding the World Health Organization and Bureau of Indian Standards recommended limits. The drinking water quality index ranged from 111.53 to 492.84. None of the sample belonged to excellent and good categories of drinking water quality. Fluoride varied from 0.018 to 4.176 mg L-1, and nitrate varied from 0.34 to 520.66 mg L-1 in groundwater. The non-carcinogenic risk assessment for children, men and women owing to ingestion of fluoride and nitrate-enriched groundwater indicates human health risks in the entire study area. Irrigation with groundwater of Alsisar block is liable to cause salinity and magnesium hazard to agricultural crops grown in the area. Source apportionment using principal component analysis suggests the geogenic origin of fluoride and anthropogenic origin of nitrate. Na+-Mg2+-Cl- followed by Na+-Mg2+-HCO3- are the predominant hydrochemical facies in the groundwater of Alsisar block. Silicate rock weathering, ion exchange and evaporation are the predominating processes governing ionic concentrations in the groundwater. Biochemical and molecular tests demonstrated the presence of Brevibacillus borstelensis strain DSM 6347 16s rRNA and Bacillus paramycoides strain MCCC 1A04098 16s rRNA in the groundwater of the area.
机译:目前的调查专注于印度九羽地区三星块地下水地球化学,旨在评估地下水的饮酒和灌溉用途,并评估从地下水摄入的人类健康风险。秃鹰块的地下水是中性到碱性,咸水,非常难以本质上。总溶解的固体,总硬度,Na +,Mg2 +,HCO3,F-和No3的大多数地下水样本都超过了世界卫生组织和印度标准局的推荐限额。饮用水质量指数从111.53到492.84。没有一个样本属于优秀和良好的饮用水质量。氟化物在0.018至4.176mg L-1中变化,硝酸盐在地下水中的0.34至520.66mg L-1变化。由于摄入氟化物和硝酸盐富含地下水的儿童,男性和女性的非致癌风险评估表明了整个研究区域的人类健康风险。与秃鹰块的地下水灌溉是易于引起该地区种植的农业作物的盐度和镁危害。使用主成分分析的源分配表明氟化物和人为硝酸盐的造环血管突。 Na + -mg2 + -cl-之后是Na + -mg2 + -HCO3-是Alsisar块地下水中的主要水化学相。硅酸盐岩石风化,离子交换和蒸发是治疗地下水中的离子浓度的占优势过程。生物化学和分子试验证明了Brevibacillus Borstelensis菌株DSM 6347 16S rRNA和芽孢杆菌副型菌株MCCC 1A04098 16S RRNA在该区域的地下水中。

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