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Interaction between karstic aquifers and allogenic rivers: the aquifer of the national park of the ephemeral river Lobos Canyon (Spain)

机译:岩溶含水层和异源河流之间的相互作用:短暂河流国家公园的含水层Lobos Canyon(西班牙)

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摘要

A methodology is described for understanding the interaction of karstic aquifers with allogenic rivers, where little information is available. This methodology includes conventional hydrogen- ology methods tracer tests and measurements of flow into, out of and circulating within the karstic system. The method is designed to un- derstand the hydrogeological behaviour of a river in sufficient detail, given a short study pe- riod. The methodology is applied to a karstic system in Spain, obtaining useful, quantitative results for a hydrological year, such as an esti- mate of the water balance, differentiation be- tween autogenic and allogenic natural recharge, relationship and connection between the river and the aquifer, and measurements of infiltration capacity in watercourses under different hydro- logical situations. The paper deals with a useful example that could be applied to other rivers and aquifers where few data are available. It can be applied to aquifers under a natural regime and Mediterranean climate.
机译:描述了一种方法,用于了解岩溶含水层与异源河流之间的相互作用,而有关信息很少。这种方法学包括常规的氢气学方法,示踪剂测试以及对流入,流出和在岩溶系统中循环的流量的测量。在简短的研究期间内,该方法旨在充分了解河流的水文地质行为。该方法应用于西班牙的一个岩溶系统,获得了水文年的有用的定量结果,例如水平衡的估算,自生和异源自然补给之间的差异,河流与河流之间的关系和联系。含水层,以及在不同水文情况下水道入渗能力的测量。本文提供了一个有用的示例,该示例可以应用于其他几乎没有可用数据的河流和含水层。它可以应用于自然条件和地中海气候下的含水层。

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