首页> 外文OA文献 >Development of a tool for managing groundwater resources in semi-arid hard rock regions: application to a rural watershed in South India
【2h】

Development of a tool for managing groundwater resources in semi-arid hard rock regions: application to a rural watershed in South India

机译:开发管理半干旱硬岩地区地下水资源的工具:应用于印度南部的农村流域

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

摘要

Until recently, aquifers located in hard rock formations (granite, gneiss, schist) were considered as a highly heterogeneous media, and no adequate methodology for groundwater management was available. Recent research studies have shown that when hard rocks are exposed to regional and deep-weathering processes and when the geology is relatively homogenous, a typical hard rock aquifer is made of two main superimposed hydrogeological layers each characterized by quite homogeneous specific hydrodynamic properties: namely the saprolite and the fissured layers. Therefore, for these cases, hard rock aquifers can be considered as a multi-layered system. Based on these works, an operational decision support tool (DST-GW ) designed for the management of groundwater resources in hard rock area under variable agro-climatic conditions has been developed. The tool focuses on the impact of changing cropping pattern, artificial recharge and rainfall conditions on groundwater levels at the scale of small watersheds (10 to about 100 km2 in case well-developed weathering profile). DST-GW is based on the groundwater balance and the 'water table fluctuation method', which are well-adapted methods in hard rock and semiarid contexts. Based on field data from an overexploited South Indian watershed (58 km2), the model allows calibrating, at watershed scale, the variation in specific yield of the aquifer with depth, as well as the rainfall-aquifer recharge relationship. Seasonal basin-scale piezometric levels are computed with an average deviation of ?0?56 m compared to measurements from 2001 to 2005. The model shows that, if no measure is taken, the water table depletion will induce the drying-up of most of the exploited borewells by the year 2012. Scenarios of mitigation measures elaborated with the tool show that change in cropping patterns could rapidly reverse the tendency and lead to a sustainable management of the resource. This work presents the developed tool and particularly the hydraulic model involved in and its application to a case study. However, the purpose tool is applicable at watershed scale but not design for the groundwater management of a very small area or for a single borewell.
机译:直到最近,位于坚硬岩层(花岗岩,片麻岩,片岩)中的含水层仍被认为是一种高度非均质的介质,还没有足够的地下水管理方法。最近的研究表明,当硬岩暴露于区域和深层的风化过程中并且地质条件相对均匀时,典型的硬岩含水层是由两个主要的叠加水文地质层组成的,每个层的特征是相当均匀的比流体动力学特性:腐泥土和裂隙层。因此,对于这些情况,硬岩含水层可以被视为多层系统。在这些工作的基础上,开发了一种用于在变化的农业气候条件下管理硬岩地区地下水资源的操作决策支持工具(DST-GW)。该工具侧重于在小流域范围内(如果天气状况良好,则为10至约100 km2)改变种植方式,人工补给和降雨条件对地下水位的影响。 DST-GW是基于地下水平衡和“地下水位波动法”的,它们是在硬岩石和半干旱环境中的适应性强的方法。基于来自过度开发的南印度流域(58 km2)的现场数据,该模型可以在流域范围内校准含水层单位产量随深度的变化以及降雨-含水层补给关系。与2001年至2005年的测量值相比,季节性流域尺度测压水位的平均偏差为?0?56 m。该模型显示,如果不采取任何措施,地下水位的枯竭将导致大部分水的枯竭。到2012年,该井将被开采。利用该工具制定的缓解措施方案表明,种植方式的变化可以迅速扭转这一趋势,并导致对资源的可持续管理。这项工作介绍了开发的工具,特别是涉及的液压模型及其在案例研究中的应用。但是,该目标工具适用于分水岭规模,但不适用于很小面积或单个钻孔的地下水管理。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
代理获取

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号