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首页> 外文期刊>Environmental Management >Hydrogeochemical Assessment of Groundwater for Drinking and Agricultural Use: A Case Study of Rural Areas of Alwar, Rajasthan
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Hydrogeochemical Assessment of Groundwater for Drinking and Agricultural Use: A Case Study of Rural Areas of Alwar, Rajasthan

机译:水下饮水和农业用途的水文地球化学评估 - 以阿尔瓦斯,拉贾斯坦邦农村地区为例

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摘要

Groundwater contributes substantially to the development of arid and semi-arid regions around the globe. The present study integrates groundwater quality and its suitability for drinking and irrigation around Alwar city of Rajasthan state, where agriculture is the major land use. The application for drinking was assessed by comparing the observed value with prescribed standards of WHO. Groundwater was found suitable for drinking at most of the locations. The suitability of groundwater for irrigation was determined by calculating ion-based ratios and comparing them against the suggested ratios and indices for agricultural quality. Suitability for irrigation was assessed against electrical conductivity (EC), percentage sodium (%Na), residual Na_2CO_3 (RSC), per cent soluble sodium (SSP), sodium adsorption ratio (SAR), Mg hazard and permeability index (PI) etc., and the quality was compromised for EC, %Na and Mg Hz. Since the soil was sandy, the groundwater was found suitable for irrigation over long-term use, with the only problem of magnesium hazard. Based on the different ratios of anions and cations, silicate weathering was observed to be regulating groundwater chemistry, and the groundwater belonged to mixed CaMgCl and CaHCO_3~- type based on Piper's classification and relative abundance of ions. Further, meteoric genesis classification showed that the groundwater in the study region had direct base exchange and shallow meteoric water percolation. Presence of kaolinite and quartz minerals in soil confirmed that silicate weathering is the major process controlling groundwater chemistry.
机译:地下水大幅促进了全球干旱和半干旱地区的发展。本研究综述了地下水质量及其饮酒和灌溉的适用性,围绕阿尔瓦斯坦邦的阿尔瓦斯城市饮酒和灌溉,农业是主要的土地利用。通过将观察到的值与卫生组织的规定标准进行比较来评估饮酒申请。发现地下水适合在大多数地区饮用。通过计算基于离子的比率并将其与农业质量的建议比率和指标进行比较来确定地下水进行灌溉的适用性。根据电导率(EC),百分比(%NA),残余NA_2CO_3(RSC),百分比可溶性钠(SSP),钠吸附比(SAR),MG危险和渗透率指数(PI)等进行灌溉的适用性。 ,质量因EC,%NA和MG Hz受到损害。由于土壤是含沙的,发现地下水适用于长期使用的灌溉,少量造成的含镁。基于阴离子和阳离子的不同比率,观察到硅酸盐风化为调节地下水化学,基于吹笛者的分类和离子的相对丰度,地下水属于混合CAMGCL和CAHCO_3〜型。此外,迁移成因分类表明,研究区的地下水具有直接的基础交换和浅气流渗透。土壤中高岭石和石英矿物质的存在证实,硅酸盐风化是控制地下水化学的主要过程。

著录项

  • 来源
    《Environmental Management》 |2021年第3期|513-521|共9页
  • 作者单位

    Department of Environmental Engineering Delhi Technological University Delhi 110042 India;

    Department of Environmental Engineering Delhi Technological University Delhi 110042 India;

    Department of Environmental Engineering Delhi Technological University Delhi 110042 India;

    Department of Environmental Engineering Delhi Technological University Delhi 110042 India;

    Department of Environmental Engineering Delhi Technological University Delhi 110042 India;

    Department of Geological Engineering Canakkale Onsekiz Mart UEniversity Canakkale Turkey;

    Department of Environmental Engineering Delhi Technological University Delhi 110042 India;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Siliserh Lake; Groundwater; Irrigation; Silicate weathering; FTIR;

    机译:Simerh Lake;地下水;灌溉;硅酸盐风化;FTIR.;

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