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首页> 外文期刊>Natural science >Interaction between karstic aquifers and allogenic rivers: The aquifer of the national park of the ephemeral river Lobos Canyon (Spain)
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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:短暂河洛伯斯峡谷(西班牙)国家公园的含水层

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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 hydrogenology methods tracer tests and measurements of flow into, out of and circulating within the karstic system. The method is designed to understand the hydrogeological behaviour of a river in sufficient detail, given a short study period. The methodology is applied to a karstic system in Spain, obtaining useful, quantitative results for a hydrological year, such as an estimate of the water balance, differentiation between autogenic and allogenic natural recharge, relationship and connection between the river and the aquifer, and measurements of infiltration capacity in watercourses under different hydrological 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。该方法包括常规的水文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。该方法旨在在较短的研究周期内足够详细地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,河流与含水层之间的关系和联系以及测量结果水文情况下河道入渗能力的变化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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