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Delineation of groundwater development potential zones in parts of marginal Ganga Alluvial Plain in South Bihar, Eastern India

机译:描绘印度东部比哈尔邦边缘恒河冲积平原部分地区的地下水开发潜力区

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摘要

A part of the Gangetic Alluvial Plain covering 2,228 km~2, in the state of Bihar, is studied for demarcating groundwater development potential zones. The area is mainly agrarian and experiencing intensive groundwater draft to the tune of 0.12 million cubic metre per square kilometres per year from the Quaternary marginal alluvial deposits, unconformably overlain northerly sloping Precambrian bedrock. Multiparametric data on groundwater comprising water level, hydraulic gradient (pre- and post-monsoon), aquifer thickness, permeability, suitability of groundwater for drinking and irrigation and groundwater resources vs. draft are spatially analysed and integrated on a Geographical Information System platform to generate thematic layers. By integrat-rning these layers, three zones have been delineated based on groundwater development potential. It is inferred that about 48% of the area covering northern part has high development potential, while medium and low development potential category covers 41 % of the area. Further increase in groundwater extraction is not recommended for an area of 173 km~2, affected by over-exploitation. The replenishable groundwater resource available for further extraction has been estimated. The development potential enhances towards north with increase in thickness of sediments. Local deviations are due to variation of-(1) cummulative thickness of aquifers, (2) deeper water level resulting from localised heavy groundwater extraction and (3) aquifer permeability.
机译:在比哈尔邦,研究了恒河冲积平原的一部分,覆盖了2228 km〜2,用于划定地下水的潜在开发区。该地区主要是农业区,每年从第四纪边缘冲积沉积物到地面的抽水量高达每平方公里12万立方米,不均匀地覆盖了北坡的前寒武纪基岩。对地下水的多参数数据进行空间分析,并在地理信息系统平台上进行整合,包括水位,水力梯度(季风前后),含水层厚度,渗透性,地下水对饮用水和灌溉的适用性以及地下水资源与吃水的关系。主题层。通过整合这些层,已根据地下水开发潜力划定了三个区域。据推测,北部地区约有48%的地区具有较高的发展潜力,而中低发展潜力类别则占该地区的41%。在过度开采的影响下,建议不要在173 km〜2的区域进一步增加地下水开采量。已估计可用于进一步开采的可补充地下水资源。随着沉积物厚度的增加,向北的发展潜力增强。局部偏差是由于以下因素引起的:(1)含水层的累积厚度;(2)局部重地下水抽取导致的更深水位;以及(3)含水层的渗透性。

著录项

  • 来源
    《Environmental Monitoring and Assessment》 |2010年第4期|179-191|共13页
  • 作者单位

    Department of Applied Geology, Indian School of Mines, Dhanbad 826004, India Central Ground Water Board, Ministry of Water Resources, Patna 800001, India;

    rnDepartment of Applied Geology, Indian School of Mines, Dhanbad 826004, India;

    rnCentral Ground Water Board, Ministry of Water Resources, Bangalore 560 102, 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

    ganga alluvial plain; GIS; replenishable resource; groundwater management; Bihar;

    机译:恒河冲积平原;地理信息系统可补充资源;地下水管理;比哈尔;

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