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GIS and SBF for estimating groundwater recharge of a mountainous basin in the Wu River watershed, Taiwan

机译:GIS和SBF估算台湾吴江流域山区盆地的地下水补给

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The temporal and spatial distributions of precipitation are extremely uneven; so, careful management of water resources in Taiwan is crucial. The long-term overexploitation of groundwater resources poses a challenge to water resource management in Taiwan. However, assessing groundwater resources in mountainous basins is challenging due to limited information. In this study, a geographic information system (GIS) and stable base-flow (SBF) techniques were used to assess the characteristics of groundwater recharge considering the Wu River watershed in central Taiwan as a study area. First, a GIS approach was used to integrate five contributing factors: lithology, land cover/land use, lineaments, drainage, and slope. The weights of factors contributing to the groundwater recharge were obtained from aerial photos, geological maps, a land use database, and field verification. Second, the SBF was used to estimate the groundwater recharge in a mountainous basin scale. The concept of the SBF technique was to separate the base-flow from the total streamflow discharge in order to obtain a measure of groundwater recharge. The SBF technique has the advantage of integrating groundwater recharge across an entire basin without complex hydro-geologic modelling and detailed knowledge of the soil characteristics. In this study, our approach for estimating recharge provides not only an estimate of how much water becomes groundwater, but also explains the characteristics of a potential groundwater recharge zone.
机译:降水的时空分布极为不均匀。因此,认真管理台湾的水资源至关重要。长期过度开采地下水资源对台湾的水资源管理提出了挑战。但是,由于信息有限,评估山区流域的地下水资源具有挑战性。在这项研究中,以台湾中部的吴河流域为研究区域,利用地理信息系统(GIS)和稳定基流(SBF)技术评估了地下水的补给特性。首先,使用GIS方法整合了五个影响因素:岩性,土地覆盖/土地利用,线条,排水和坡度。可从航拍照片,地质图,土地利用数据库和现场核查中获得有助于地下水补给的因素的权重。其次,利用SBF估算山区盆地规模的地下水补给量。 SBF技术的概念是将基本流量与总流量流量分开,以获得对地下水补给的度量。 SBF技术的优势在于,无需复杂的水文地质建模和对土壤特性的详细了解,即可将整个流域的地下水补给量综合起来。在这项研究中,我们的补给量估算方法不仅提供了对地下水中多少水的估算,而且还解释了潜在的补水区的特征。

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