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Estimating shallow groundwater availability in small catchments using streamflow recession and instream flow requirements of rivers in South Africa

机译:利用南非河流的河流径流衰退和河川流量估算来估算小流域的浅层地下水利用率

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Groundwater is an important resource for multiple uses in South Africa. Hence, setting limits to its sustainable abstraction while assuring basic human needs is required. Due to prevalent data scarcity related to groundwater replenishment, which is the traditional basis for estimating groundwater availability, the present article presents a novel method for determining allocatable groundwater in quaternary (fourth order) catchments through information on streamflow. Using established methodologies for assessing baseflow, recession flow, and instream ecological flow requirement, the methodology develops a combined stepwise methodology to determine annual available groundwater storage volume using linear reservoir theory, essentially linking low flows proportionally to upstream groundwater storages. The approach was trialled for twenty-one perennial and relatively undisturbed catchments with long-term and reliable streamflow records. Using, the Desktop Reserve Model, instream flow requirements necessary to meet the present ecological state of the streams were determined, and baseflows in excess of these flows were converted into a conservative estimates of allocatable groundwater storages on an annual basis. Results show that groundwater development potential exists in fourteen of the catchments, with upper limits to allocatable groundwater volumes (including present uses) ranging from 0.02 to 3.54 x 10(6) m(3) a(-1) (0.10-11.83 mm a(-1)) per catchment. With a secured availability of these volume 75% of the years, variability between years is assumed to be manageable. A significant (R-2 = 0.88) correlation between baseflow index and the drainage time scale for the catchments underscores the physical basis of the methodology and also enables the reduction of the procedure by one step, omitting recession flow analysis. The method serves as an important complementary tool for the assessment of the groundwater part of the Reserve and the Groundwater Resource Directed Measures in South Africa and could be adapted and applied elsewhere. (C) 2016 The Authors. Published by Elsevier B.V.
机译:地下水是南非多种用途的重要资源。因此,需要在确保人类基本需求的同时,限制其可持续性抽象。由于与地下水补给有关的普遍数据稀缺,这是估算地下水可利用性的传统基础,因此,本文提出了一种新颖的方法,可通过有关水流的信息确定四元(四级)流域的可分配地下水。使用已建立的评估基础流量,后退流量和河内生态流量需求的方法,该方法开发了一种组合的逐步方法,使用线性水库理论确定了年可用地下水存储量,基本上将低流量与上游地下水存储成比例地联系起来。该方法已在具有长期可靠流量记录的21个常年和相对不受干扰的流域进行了试验。使用Desktop Reserve模型,确定了满足河流当前生态状况所需的河流内流量需求,并将超过这些流量的基础流量每年转换为可分配地下水储量的保守估计。结果表明,在十四个流域中存在地下水开发潜力,可分配地下水量(包括当前用途)的上限范围为0.02至3.54 x 10(6)m(3)a(-1)(0.10-11.83 mm a (-1))。有了这些年份的75%的安全可用性,可以认为年份之间的差异是可控的。流域底流指数与排水时间尺度之间的显着相关性(R-2 = 0.88)突显了该方法的物理基础,并且使该程序减少了一步,而无需进行经济衰退流量分析。该方法是评估保护区地下水部分和南非地下水资源指示措施的重要补充工具,可以在其他地方进行调整和应用。 (C)2016作者。由Elsevier B.V.发布

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