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Hydrogeochemical Behaviour and Assessment of Groundwater Quality from WGAMG'0 Watershed, Chimur Taluka, Chandrapur District, Maharashtra

机译:马哈拉施特拉邦钱德拉布尔地区奇莫尔·塔卢卡WGAMG'0流域的水文地球化学行为和地下水质量评估

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The study area of WGAMG’0 watershed is bounded by longitudes 79°14’00” and 79°21’00” and Latitudes 20°31’00” and 20°36’00” N and covers 11 villages of Chimur Tehsil, Chandrapur District, Maharashtra. Fourteen dugwells were identified and fixed as observation wells to gather the information on pre-monsoon water level fluctuation, depth to hard rock, water bearing zone, average depth of wells, average diameter of wells and other related hydrogeological data. The collected groundwater samples having pH values 7.3 to 8.1 are dominantly alkaline. While the electrical conductivity values of the collected samples vary from 845-1132 μS/cm. The TDS values from deeper aquifers range from 596-724 mg/L and the total hardness ranges from 281-616 mg/L respectively. The anion chemistry of groundwater samples from the study area is dominated by HCO3, Cl, SO4 and NO3. The concentration values ranges from 325-566 mg/L, 12.3-34.1 mg/L, 6.3-56.1 mg/L and 75.4-258.3 mg/L respectively. The primary source of HCO3- is considered to be the dissolution of minerals like calcite and dolomite, where in addition to that the CO2 gas is also dissolved through the process of anoxic biodegradation of the organic matter in deeper aquifers. In the present area of investigation, 100% samples fall in the range of 500-1000 mg/L indicating that water samples are of freshwater in nature and permissible for drinking. The suitability of the groundwater for irrigation purpose has also been checked by estimating the following values: Sodium Adsorption Ratio (SAR), U.S. Salinity Laboratory diagram, Percent Sodium (% Na), Residual Sodium Carbonate (RSC), Soluble Sodium Percentage (SSP), Mg Ratio (MR), Corrosively Ratio (CR), Kelley’s Ratio (KR) and Permeability Index (PI). These parameters have brought the marginal utility for irrigation purpose.
机译:WGAMG'0流域的研究区域以经度79°14'00”和79°21'00”以及北纬20°31'00”和20°36'00”的边界为界,并覆盖了钱德拉普尔的Chimur Tehsil 11个村庄马哈拉施特拉邦区。确认并固定了14座挖坑井作为观测井,以收集有关季风前水位波动,硬岩深度,含水层,井的平均深度,井的平均直径和其他相关水文地质数据的信息。所收集的pH值为7.3至8.1的地下水样品主要为碱性。收集的样品的电导率值在845-1132μS/ cm之间变化。深层含水层的TDS值分别为596-724 mg / L和总硬度为281-616 mg / L。研究区域地下水样品的阴离子化学成分主要为HCO3,Cl,SO4和NO3。浓度范围分别为325-566 mg / L,12.3-34.1 mg / L,6.3-56.1 mg / L和75.4-258.3 mg / L。 HCO3-的主要来源被认为是溶解了方解石和白云石等矿物,此外,CO2气体还通过深层含水层中有机物的缺氧生物降解过程而溶解。在目前的研究领域,100%的样品含量在500-1000 mg / L范围内,这表明水样品本质上是淡水,可以饮用。还通过估算以下值来检查地下水是否适合灌溉目的:钠吸收率(SAR),美国盐度实验室图,钠百分比(%Na),残留碳酸钠(RSC),可溶性钠百分比(SSP) ,镁比(MR),腐蚀性比(CR),凯利比(KR)和渗透性指数(PI)。这些参数为灌溉目的带来了边际效用。

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