Department of Physical, Chemical and Natural Systems, University Pablo de Olavide, Utrera Rd. Km 1, 41013 Seville, Spain.
Water Environ Res. 2013 Jul;85(7):632-42. doi: 10.2175/106143013x13698672321508.
Andalusia's lowland countryside has a network of small geographically isolated playa lakes scattered across an area of 9000 km2 whose watersheds are mostly occupied by clayey rocks. The hydrological model proposed by the authors seeks to find equilibrium among usefulness, simplicity, and applicability to isolated playas in a semiarid context elsewhere. Based in such model, the authors have used monthly climatic data, water stage measurements, and the basin morphometry of a particular case (Los Jarales playa lake) to calibrate the soil water budget in the catchment and the water inputs from the watershed (runoff plus groundwater flow) at different scales, from monthly to daily. After the hydrologic model was calibrated, the authors implemented simulations with the goal of reproducing the past hydrological dynamics and forecasting water regime changes that would be caused by a modification of the wetland morphometry.
安达卢西亚低地乡村有一个由地理上小而孤立的潟湖组成的网络,分布在 9000 平方公里的区域内,其流域主要被粘土层岩石占据。作者提出的水文模型旨在在半干旱地区找到孤立潟湖的实用性、简单性和适用性之间的平衡。基于该模型,作者使用了每月的气候数据、水位测量值以及特定案例(洛斯贾拉雷斯潟湖)的流域形态测量值,以校准集水区的土壤水分预算和来自流域的水分输入(径流加地下水流动),从每月到每日不等。水文模型校准后,作者进行了模拟,目的是再现过去的水文动态,并预测由于湿地形态的改变而导致的水情变化。