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Quantifying the impacts of rainwater harvesting in a case study catchment; the Arvari River, Rajasthan, India

机译:量化雨水收获在案例研究流域的影响;阿瓦里河,拉贾斯坦邦,印度

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Rainwater Harvesting (RWH) is the collection and storage of runoff for the primary purpose of groundwater recharge in arid and semi-arid regions of India. In India investment in RWH for groundwater recharge is increasing. However despite this, very little is known on the catchment hydrological impacts of RWH. Although RWH is a small-scale operation, when implemented across a catchment, the impact on groundwater and river flow could be significant. However, there is currently no study that has comprehensively quantified this impact. This paper proposes a method to explore the effects of RWH in a case study catchment of the 500km~2 ungauged Arvari River Basin in Rajasthan, India where 366 RWH structures have been built since 1985. Difficulties associated with working in semi-arid regions, such as this catchment, include the high spatial and temporal variability of climate, particularly rainfall, and landscape conditions and data scarcity. Detailed field studies of local scale effects of RWH and recharge under a number of structures were studied during the monsoon of 2007 in the catchment. Discharge over anicuts on the river was also monitored and water level rise in wells. These results will be extended to the catchment scale using a conceptual catchment water balance model that captures the main hydrological processes. Water moves through the catchment in a series of linked storages for each landuse, where the upper and lower catchments are separate domains. The groundwater system consists of an unconfined alluvial aquifer over a confined hard rock aquifer. This will allow different scenarios of land use and levels of RWH to be explored to quantify the hydrological impact on the catchment.
机译:雨水收获(RWH)是径流的收集和储存,用于印度干旱和半干旱地区地下水充电的主要目的。在印度投资RWH为地下水充电正在增加。然而,尽管如此,对RWH的流域水文影响很少。虽然RWH是一个小规模的操作,但是在集水区实现时,对地下水和河流的影响可能是显着的。但是,目前没有研究完全量化这种影响。本文提出了一种探讨RWH在拉贾斯坦邦的500km〜2个未凝固的Arvari河流域的案例研究集水效果的方法,其中1985年自1985年以来建立了366 rwh结构。与半干旱地区工作有关的困难作为这种流域,包括气候的高空间和时间变异,特别是降雨,以及景观条件和数据稀缺。在集水区内的2007年季风期间,研究了RWH对局部规模效应并在许多结构下给予补给的详细领域研究。还监测了河上的排泄物,并监测水位升高。这些结果将使用捕获主要水文过程的概念性集水平衡模型来扩展到集水区规量表。水在每次土地使用的一系列连接存储中移动流量,其中上层和下部集水区是单独的畴。地下水系统包括一个不包含狭窄的硬岩含水层的冲积含水层。这将允许探索不同程度的土地利用和RWH水平,以量化对集水区的水文影响。

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