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Interpretation of groundwater quality using principal component analysis from Anantapur district, Andhra Pradesh, India

机译:使用印度安得拉邦阿南塔普尔区主成分分析法解释地下水质量

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摘要

Groundwater samples from the Anantapur district, Andhra Pradesh, India, are analyzed for chemical constituents to identify the hydrogeochemical processes that control the groundwater quality. The groundwater is brackish and very hard, with an excess alkalinity, and is not fit for drinking and irrigation. Principal component analysis is made on the chemical variables, and the first two principal components are chosen, which account for 77.34% of the total variance in the data set. The first principal component is characterized by total dissolved solids, Na+, Cl–, , , pH and F– parameters, and the second principal component is represented by Ca2+, , Mg2+ and ions. These components are interpreted as controlled by the higher rate of evapotranspiration, topographic lows, poor drainage conditions, longer residence of water in the aquifer, ion exchange, irrigation return flow, heavy use of fertilizers, and sewage wastes, which are further supported by the scatter diagrams, ionic signatures, and mechanisms controlling the water chemistry diagrams. The principal component scores clearly explained the variations in the local and regional hydrogeochemical processes, broadly distinguished the geogenic sources from the anthropogenic ones, and easily helped to select the index wells for the long-term monitoring, which would reduce the cost of monitoring programs. The principal component analysis in the present study area is assisted to facilitate the determination of assemblages of groundwater quality results, which explain the genetic processes and points of origin of pollutants of residential and agricultural zones for mitigating the adverse effects caused by the inferior quality of water on the human health as well as on plant growth for sustainable development. Hence, the application of the principal component analysis can be used as a complementary tool in the hydrogeochemical analysis of any region and helps to plan appropriate management measures in time to control and improve the groundwater quality.
机译:分析来自印度安得拉邦安纳布尔(Anantapur)地区的地下水样品的化学成分,以识别控制地下水质量的 水文地球化学过程。 地下水微咸且非常坚硬,碱度过高, ,不适合饮用和灌溉。对化学变量进行主成分 分析,选择前两个 主要成分,占 总方差的77.34%。数据集。第一个主成分 的特征在于总溶解固体,Na + ,Cl – ,pH和F – 参数,第二个 主要成分由Ca 2 + ,Mg 2 + 和离子表示。这些成分被解释为受 较高的蒸散速率,地形低点,排水 条件差,水在含水层中滞留时间更长,离子交换, 灌溉回水,肥料的大量使用以及污水中的散布图,离子签名和控制水化学的机制进一步支持了这种情况。 图。主成分评分清楚地解释了局部和区域水文地球化学过程中的 变异, 广泛地区分了人为的 的成因,并且易于使用选择用于长期 监测的指标井,这将降低监测程序的成本。 本研究区域的主成分分析是 协助简化地下水 质量结果的确定,解释了居民和农业区污染物的遗传过程和成因点 >以减轻因劣质水对人类健康以及植物生长造成的不利影响,从而实现可持续发展。因此,主 成分分析的应用可以用作任何地区 水文地球化学分析的补充工具,并有助于规划适当的 管理及时采取措施控制和改善地下水 的质量。

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  • 来源
    《Environmental Geosciences》 |2006年第4期|239-259|共21页
  • 作者单位

    Department of Geology, Andhra University, Visakhapatnam 530 003, India srnandipati@rediffmail.com;

    Department of Geology, Andhra University, Visakhapatnam 530 003, India drjohndevadas@gmail.com;

    Department of Geology, Andhra University, Visakhapatnam 530 003, India kandula_svrao@yahoo.com;

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  • 入库时间 2022-08-17 23:35:08

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