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Quality Assessment of Groundwater with Special Emphasis on Irrigation and Domestic Suitability in Suri I & II Blocks, Birbhum District, West Bengal, India

机译:印度西孟加拉邦Birbhum区Suri I和II区块的地下水质量评估,重点是灌溉和家庭适宜性

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The hydrochemical study of groundwater samples was carried out from the Suri I and II blocks of Birbhum district, West Bengal (latitudes 23.76° N – 23.99°N and longitudes 87.42°E - 87.64°E) with an objective of understanding the suitability of local groundwater quality for irrigation and domestic purposes. For this study groundwater samples were collected from 26 (twenty six) locations during the post monsoon and pre monsoon sessions spanning over 2012 and 2013. Groundwater samples were analyzed for their physical and chemical properties using standard laboratory methods. From the analyzed data, some parameters like SAR, SSP, RSC, MAR, PI and KR have been calculated for each water sample to identify the irrigational suitability. Accordingly, the groundwater has been found to be well to moderately suitable for irrigation. In the post monsoon session exceptionally high RSC values for around 80% samples indicate an alkaline hazard to the soil. The ion balance histogram for post monsoon indicates undesirable ion balance values according to fresh water standards whereas in pre monsoon, the samples show good ion balance in water. The Piper’s trilinear diagram used to determine water type suitable for consumption indicates groundwater in the study is of bicarbonate type (fresh type) in both and pre monsoon with exception of a couple of sulfate type samples during pre monsoon. Water Quality Index results depict 90% of water samples are suitable for drinking during post monsoon whereas in pre monsoon that tally comes down 60% rendering 40% samples unsuitable for drinking. Gibb’s diagrams prepared for the post monsoon and pre monsoon sessions indicate that the overall hydrogeochemistry of the study area is dominated by rock – water interaction processes.
机译:地下水样品的水化学研究是从西孟加拉邦Birbhum区的Suri I和II区块(北纬23.76°– 23.99°N,东经87.42°E-87.64°E)进行的,目的是了解当地的适用性用于灌溉和家庭目的的地下水质量。在本研究中,在2012年和2013年的季风后和季风前期间从26个(二十六个)地点收集了地下水样品。使用标准实验室方法分析了地下水样品的理化特性。从分析的数据中,已为每个水样计算了一些参数,如SAR,SSP,RSC,MAR,PI和KR,以确定灌溉的适用性。因此,已经发现地下水非常适合中等灌溉。在季风后时段,大约80%的样品的RSC值异常高,表明对土壤有碱危害。季风后的离子平衡直方图表示根据淡水标准的不良离子平衡值,而季风前的样品在水中显示出良好的离子平衡。用于确定适合消耗水类型的Piper的三线性图表明,研究中的地下水均为季风前后的碳酸氢盐类型(淡水),季风期间有几个硫酸盐类样品除外。水质指数的结果显示90%的水样本适合在季风后饮用,而季风前的总数下降60%,使40%的样本不适合饮用。吉布为季风后和季风前阶段准备的图表表明,研究区的整体水文地球化学主要由岩水相互作用过程主导。

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