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Environmental geochemistry and quality assessment of surface and subsurface water of Mahi River basin, western India

机译:印度西部Mahi流域的环境地球化学和地表水和地下水的质量评估

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The hydrogeochemical study of surface and subsurface water of Mahi River basin was undertaken to assess the major ion chemistry, solute acquisition processes and water quality in relation to domestic and irrigation uses. The analytical results show the mildly acidic to alkaline nature of water and dominance of Na~+ and Ca~(2+) in cationic and HCO_3~- and Cl~- in anionic composition. In general, alkaline-earth elements (Ca~(2+) + Mg~(2+)) exceed alkalis (Na~+ + K~+) and weak acids (HCO_3~-) dominate over strong acids (SO_4~(2+) + Cl~) in majority of the surface and groundwater samples. Ca~(2+)-Mg~(2+)-HCO_3~- is the dominant hydrochemical facies both in surface and groundwater of the area. The weathering of rock-forming minerals mainly controlled the solute acquisition process with secondary contribution from marine and anthropogenic sources. The higher concentration of sodium and dissolved silica, high equivalent ratios of (Na~+ + K~+/ TZ~+), (Na~+ + K~+/Cl~-) and low ratio of (Ca~(2+) + Mg~(2+))/ (Na~+ + K~+) suggest that the chemical composition of the water is largely controlled by silicate weathering with limited contribution from carbonate weathering and marine and anthropogenic sources. Kaolinite is the possible mineral that is in equilibrium with the water, implying that the chemistry of river water favors kaolinite formation. Assessment of water samples for drinking purposes suggests that the majority of the water samples are suitable for drinking. At some sites concentrations of TDS, TH, F~-, NO_3~- and Fe are exceeding the desirable limit of drinking. However, these parameters are well within the maximum permissible limit except for some cases. To assess the suitability for irrigation, parameters like SAR, RSC and %Na were calculated. In general, both surface and groundwater is of good to suitable category for irrigation uses except at some sites where high values of salinity, %Na and RSC restrict its uses.
机译:进行了Mahi流域地表和地下水的水文地球化学研究,以评估与家庭和灌溉用途相关的主要离子化学,溶质获取过程和水质。分析结果表明,水呈弱酸性至碱性,阳离子组成中Na〜+和Ca〜(2+)占优势,阴离子组成中HCO_3〜-和Cl〜-占优势。通常,碱土金属元素(Ca〜(2+)+ Mg〜(2+))超过碱金属(Na〜+ + K〜+),而弱酸(HCO_3〜-)则比强酸(SO_4〜(2 +)+ Cl〜)在大多数地表和地下水样品中。 Ca〜(2 +)-Mg〜(2 +)-HCO_3〜-是该地区地表水和地下水中主要的水化学相。成岩矿物的风化主要控制了溶质的获取过程,而海洋和人为源的贡献则是次要的。钠和溶解二氧化硅的浓度较高,(Na〜+ + K〜+ / TZ〜+),(Na〜+ + K〜+ / Cl〜-)的当量比高,(Ca〜(2+ )+ Mg〜(2 +))/(Na〜+ + K〜+)表明水的化学成分主要受硅酸盐风化作用控制,碳酸盐化风化作用以及海洋和人为来源的贡献有限。高岭石是可能与水保持平衡的矿物,这意味着河水的化学性质有利于高岭石的形成。对用于饮用目的的水样本的评估表明,大多数水样本都适合饮用。在某些场所,TDS,TH,F〜,NO_3〜和Fe的浓度超过了理想的饮用极限。但是,除某些情况外,这些参数都在最大允许极限内。为了评估灌溉的适用性,计算了SAR,RSC和%Na等参数。一般而言,地表水和地下水都适合用于灌溉用途,但在某些盐度,%Na和RSC值较高的地区除外。

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