The Fuentetoba Spring, with a mean flow of 210 L s(-1), releases the discharge from an aquifer that comprises three hydraulically-connected synclines. The spring has a very irregular flow of between 8 L s(-1) and 3,400 L s(-1) due to the predominant water circulation that is non-Darcian turbulent flow as an underground torrent in the vadose zone, as well as through well-developed karstic conduits in the phreatic and epiphreatic zones, as attested to by speleological explorations. The long response times to recharge by the Fuentetoba karstic system, seen in the spring's hydrograph, are controlled by regional factors. Nevertheless, certain responses that have very long time lags under high water conditions might be governed in the final stretch of the flowpath by mechanisms of pressure or siphoning of the floodwave, and perhaps by constrictions or plugs of sediment in the conduits.
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机译：Fuentetoba弹簧的平均流量为210 L s（-1），释放出包含三个液压连接的同步斜度的含水层的排放物。由于主要的水循环是非达西湍流，如渗流区的地下洪流，以及通过水流，春季的水流非常不规则，介于8 L s（-1）和3,400 L s（-1）之间。潜水和上生带发育良好的岩溶导管，经岩石学探索证明。从春季水文图中可以看出，富恩特托巴岩溶系统对补给的响应时间长，受区域因素控制。但是，在高水位条件下某些具有很长时滞的响应可能会在流径的最终伸展过程中受到洪水波的压力或虹吸作用机制的控制，并且可能受到管道中沉积物的收缩或堵塞的影响。
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