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A study on groundwater hydrochemistry in Khatra Block, Bankura district, West Bengal

机译:西孟加拉邦班库拉地区Khatra区块的地下水水化学研究

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A study was conducted to detect the hydrochemistry of groundwater in Khatra Block,Bankura district, West Bengal. For this, nineteen water samples from borewells during postmonsoon and premonsoon sessions each were collected. Analyses of these water samples were done to evaluate their hydrochemistry and usability for domestic and agricultural uses. Measurement of some parameters which include pH, TDS, and EC has been done in situ sample location points itself. For determining other parameters like cations (Ca~(2+), Mg~(2+), Fe~(2+), Na~+, K~+) and anions (C1~-, HCO_3~-, SO_4~(2-), F~-), samples were brought to the laboratory. For determining irrigation suitability of collected groundwater samples, parameters such as sodium adsorption ratio (SAR), soluble sodium percentage (SSP), residual sodium carbonate (RSC), magnesium adsorption ratio (MAR), Kelly's ratio (KR), permeability index (PI) and corrosivity ratio (CR)were calculated. The waters are found to belong to low salinity and sodium types when marked in the US Salinity Laboratory (1954) diagram and suggest good for agricultural uses. The hydrochemistry of the investigated area is normally good but varies from very hard to hard. In few localities of the investigated area, total hardness is identified as high, which suggest not to use the water for drinking purpose. In such places, the groundwater may be contaminated by interaction between rock and water along with agricultural drain out. The Piper plot shows marked domination of Ca~(2+)-Na~+-SO_4~(2-), mixed Ca~(2+)-Mg~(2+)-Na~+-HCO_3~- types. To determine the suitability of these groundwater samples for domestic purposes, Water Quality Index (WQI), Gibb's ratio for both cations and anions, and Chloro-Alkaline Indices (CAI) have been calculated along with plotting in Chadha's and Schoeller diagrams. It also indicates the preponderance of alkaline earth over alkalis and weak acids over strong acids. For utilizing the groundwater in domestic purposes, index of water quality was also determined. Water Quality Index values varied from 74.74 to 209.4 in postmonsoon, and 70 to 205 in premonsoon period which suggest the water good enough to use for domestic purposes.
机译:进行了一项研究,以检测西孟加拉邦班库拉区Khatra Block的地下水水化学。为此,在季风前后和季风前后各采集了19个井筒的水样。对这些水样进行了分析,以评估其水化学性质以及在家庭和农业用途中的可用性。包括pH,TDS和EC在内的一些参数的测量已在原位样品定位点本身完成。用于确定其他参数,例如阳离子(Ca〜(2 +),Mg〜(2 +),Fe〜(2 +),Na〜+,K〜+)和阴离子(C1〜-,HCO_3〜-,SO_4〜( 2-),F〜-),将样品带到实验室。为了确定收集的地下水样品的灌溉适宜性,需要使用诸如钠吸附率(SAR),可溶性钠百分比(SSP),残留碳酸钠(RSC),镁吸附率(MAR),凯利比(KR),渗透系数(PI)之类的参数)和腐蚀率(CR)的计算。当在美国盐度实验室(1954)图表中标记时,发现这些水属于低盐度和钠类型,表明对农业有用。被调查区域的水化学性质通常很好,但变化范围很大。在调查区域的少数地方,总硬度被确定为很高,这表明不要将水用于饮用。在这些地方,岩石和水之间的相互作用以及农业的排泄物可能会污染地下水。吹笛者图显示了Ca〜(2 +)-Na〜+ -SO_4〜(2-),Ca〜(2 +)-Mg〜(2 +)-Na〜+ -HCO_3〜-混合型的显着支配性。为了确定这些地下水样品是否适合家庭用途,已经计算了水质指数(WQI),阳离子和阴离子的吉布比以及氯碱指数(CAI),并在Chadha和Schoeller图中进行了绘制。它也表明碱土类比碱类占优势,弱酸类比强酸类占优势。为了将地下水用于家庭目的,还确定了水质指标。季风后的水质指数值在74.74至209.4之间,季风前的水质指数在70至205之间,这表明该水质足以用于家庭用水。

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