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首页> 外文期刊>Hydrogeology journal >An innovative artificial recharge system to enhance groundwater storage in basaltic terrain: example from Maharashtra, India
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An innovative artificial recharge system to enhance groundwater storage in basaltic terrain: example from Maharashtra, India

机译:一种创新的人工补给系统,可增强玄武岩地区的地下水储量:印度马哈拉施特拉邦的实例

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摘要

The management of groundwater poses challenges in basaltic terrain as its availability is not uniform due to the absence of primary porosity. Indiscriminate excessive withdrawal from shallow as well as deep aquifers for meeting increased demand can be higher than natural recharge, causing imbalance in demand and supply and leading to a scarcity condition. An innovative artificial recharge system has been conceived and implemented to augment the groundwater sources at the villages of Saoli and Sastabad in Wardha district of Maharashtra, India. The scheme involves resectioning of a stream bed to achieve a reverse gradient, building a subsurface dam to arrest subsurface flow, and installation of recharge shafts to recharge the deeper aquifers. The paper focuses on analysis of hydrogeological parameters like porosity, specific yield and transmissivity, and on temporal groundwater status. Results indicate that after the construction of the artificial recharge system, a rise of 0.8-2.8 m was recorded in the pre- and post-monsoon groundwater levels in 12 dug wells in the study area; an increase in the yield was also noticed which solved the drinking water and irrigation problems. Spatial analysis was performed using a geographic information system to demarcate the area of influence of the recharge system due to increase in yields of the wells. The study demonstrates efficacy, technical viability and applicability of an innovative artificial recharge system constructed in an area of basaltic terrain prone to water scarcity.
机译:地下水的管理在玄武地形中提出了挑战,因为由于缺乏主要的孔隙度,地下水的可用性不统一。为满足增加的需求而从浅水层和深水层中滥砍滥伐可能高于自然补给,造成供需不平衡,并导致短缺。已经设计并实施了一种创新的人工补给系统,以增加印度马哈拉施特拉邦沃达地区Saoli和Sastabad村的地下水源。该方案包括切除河床以实现反向坡度,修建地下大坝以阻止地下水流,以及安装补给井以补给较深的含水层。本文着重分析水文地质参数,例如孔隙度,比产率和透射率,以及地下水的瞬时状态。结果表明,在建立人工补给系统之后,研究区的12口挖井的季风前后地下水位记录了0.8-2.8 m的上升;还注意到产量增加,从而解决了饮用水和灌溉问题。使用地理信息系统进行空间分析,以划定由于井产量增加而导致的补给系统影响范围。这项研究证明了一种创新的人工补给系统的有效性,技术可行性和适用性,该系统在易于缺水的玄武岩地带建造。

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