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首页> 外文期刊>Journal of water resource and protection >Estimation of Groundwater Recharge Using GIS Method: A Case Study of Makotopong Village-Polokwane, South Africa
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Estimation of Groundwater Recharge Using GIS Method: A Case Study of Makotopong Village-Polokwane, South Africa

机译:使用GIS方法估算地下水充电 - 以南非大厦 - 莫克瓦尔村的案例研究

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South Africa is a relatively dry country, with most rural areas experiencing high demand for water supply. Groundwater is one of the best alternative sources that can be used to augment the demand. However, this cannot sus-tainably be achieved unless accurate prediction of recharge to the groundwater aquifer is done. The objective of the study was to accurately estimate the groundwater recharge using ArcGIS method with a view of ensuring adequate groundwater for water supply exploitation. The study was conducted in Makotopong village in Polokwane. Data used in the study were sourced from diverse governmental agencies. Borehole logs were obtained from National Groundwater Archives. Geological and hydrogeological data were obtained from Council for Geoscience. All captured data were analysed to show the rainfall variations and estimation of groundwater recharge in different years. Groundwater recharge was estimated using ArcGIS 10.5. The simulated annual groundwater recharge varied from 0 mm to 51 mm with a mean recharge value of 12.04 mm/yr. The estimation of groundwater recharge using GIS methods resulted in a mean recharge value of 12.04 mm/year which shows a close comparison with previous studies conducted using Chlorine Mass Balance (CMB) and Water-Table Fluctuation (WTF). This implies that GIS is a potential tool that can be used to estimate groundwater recharge. It is recommended that GIS Method of estimating recharge be used in designing optimal sustainable groundwater supply systems.
机译:南非是一个相对干旱的国家,拥有大多数农村地区,遭受良好的供水需求。地下水是可用于增强需求的最佳替代来源之一。然而,除非进行准确地预测地下水含水层的准确预测,否则这不能达到可疑地实现。该研究的目的是准确估计使用ArcGIS方法的地下水补给,以确保供水剥削的适当地下水。该研究在波洛瓦的Makotopong Village进行。该研究中使用的数据来自不同的政府机构。钻孔原木是从国家地下水档案馆获得的。从地球科学理事会获得地质和水文地质数据。分析了所有捕获的数据以显示不同年份地下水补给的降雨变化和估算。使用ArcGIS 10.5估计地下水补给。模拟的年地下水补给压力从0毫米到51毫米,平均充电值为12.04 mm / yr。使用GIS方法估计地下水再充电导致平均补给值12.04mm /级,其显示与使用氯质量平衡(CMB)和水表波动(WTF)进行的先前研究进行了紧密的比较。这意味着GIS是一种潜在的工具,可用于估计地下水充电。建议在设计最佳的可持续地下水供应系统时使用估算补给的GIS方法。

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