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首页> 外文期刊>Environmental Geology >Assessment of groundwater quality for drinking and irrigation purposes: a case study of Peddavanka watershed, Anantapur District, Andhra Pradesh, India
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Assessment of groundwater quality for drinking and irrigation purposes: a case study of Peddavanka watershed, Anantapur District, Andhra Pradesh, India

机译:用于饮用水和灌溉目的的地下水质量评估:以印度安得拉邦阿南塔普尔地区Peddavanka流域为例

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In India, the quantity and quality of water available for irrigation is variable from place to place. Assessment of water quality has been carried out to determine the sources of dissolved ions in ground-water. Quality of groundwater in a 398 km~2 Peddavanka watershed of a semi-arid region of south India is evaluated for its suitability for drinking and irrigation purposes. The middle Proterozoic Cuddapah Supergroup and Kurnool Group of rocks underlie most of the watershed. The main lithologic units consist chiefly of quartzite, limestone, and shale. Seventy-six water samples were collected from open-wells and bore-holes. Water samples were collected representative of the post-monsoon (winter) and pre-monsoon (summer). The quality assessment is made through the estimation of Ca~(2+), Mg~(2+), Na~ +, K~+, Cl~-, SO_4~(2-), CO_3~(2-), HCO_3~-, total hardness as CaCO_3, TDS, EC, and pH. Based on these analyses, parameters like sodium adsorption ratio, % sodium, residual sodium carbonate, non-carbonate hardness, potential salinity, Kelley's ratio, magnesium ratio, index of base exchange and permeability index were calculated. According to Gibbs' ratio samples in both seasons fall in the rock dominance field. The overall quality of waters in the study area in post-monsoon season is high for all constituents ruling out pollution from extraneous sources.
机译:在印度,可用于灌溉的水的数量和质量因地而异。已经对水质进行了评估,以确定地下水中溶解离子的来源。对印度南部半干旱地区Peddavanka流域398 km〜2的地下水质量进行了评估,以评估其是否适合饮用和灌溉。分水岭的大部分位于中元古代Cuddapah超群和Kurnool群岩石之间。主要的岩性单元主要由石英岩,石灰岩和页岩组成。从裸眼井和钻孔中收集了76个水样。收集代表季风后(冬季)和季风前(夏季)的水样。通过评估Ca〜(2 +),Mg〜(2 +),Na〜+,K〜+,Cl〜-,SO_4〜(2-),CO_3〜(2-),HCO_3进行质量评估〜-,总硬度为CaCO_3,TDS,EC和pH。在这些分析的基础上,计算出钠吸附率,钠百分比,残留碳酸钠,非碳酸盐硬度,潜在盐度,凯利比,镁比,碱交换指数和渗透率指数等参数。根据吉布斯的比率,两个季节的样本都属于岩石优势领域。季风后季节研究区域的水质总体较高,所有成分均排除了外来污染。

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