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Evaluation of distributed recharge in an upland semi-arid karst system : the West Bank Mountain Aquifer, Middle East

机译:高原半干旱岩溶系统分布式补给评价:中东西岸山地含水层

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摘要

Assessment of recharge in a structurally complex upland karst limestone aquifer situated in a semi-arid environment is difficult. Resort to surrogate indicators such as measurement of spring outflow and borehole discharge, is a common alternative, and attempts to apply conventional soil moisture deficit analysis may not adequately account for the intermittent spate conditions that arise in such environments. A modelling approach has been made using the West Bank Mountain Aquifer system in the Middle East as a trial. The model uses object oriented software which allows various objects to be switched on and off. Each of the main recharge processes identified in the West Bank is incorporated. The model allows either conventional soil moisture deficit analysis calculations or wetting threshold calculations to be made as appropriate, and accommodates both direct recharge and secondary recharge. Daily time steps enable recharge and runoff routing to be calculated for each node. Model runs have enabled a series of simulations for each of the three aquifer basins in the West Bank and for the whole of the West Bank. These provide recharge estimates comparable to those prepared by earlier workers by conventional means. The model is adaptable and has been successfully used in other environments. ud
机译:评估半干旱环境中结构复杂的山地喀斯特石灰岩含水层中的补给非常困难。求助于替代指标,例如弹簧流出量和钻孔流量的测量,是一种常见的替代方法,尝试进行常规土壤水分亏缺分析可能无法充分考虑此类环境中间歇性的潮涌情况。已经使用中东的西岸山含水层系统进行了建模。该模型使用面向对象的软件,该软件允许打开和关闭各种对象。西岸确定的每个主要充值程序均已纳入。该模型允许根据需要进行常规的土壤水分亏缺分析计算或湿润阈值计算,并且可以容纳直接补给和二次补给。通过每日时间步长,可以为每个节点计算补给和径流路线。通过模型运行,可以对西岸的三个含水层盆地中的每一个以及整个西岸的区域进行一系列的模拟。这些提供的补给估算值可与早期工人通过常规方式估算的补给估算值相媲美。该模型具有适应性,并已在其他环境中成功使用。 ud

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