超采含水层垂直渗漏的空间分析:德克萨斯州Hueco bolson含水层,1956-1995

Alfonso Nuñez, Hugo A. Loáiciga
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引用次数: 0

摘要

向埃尔帕索(美国)-华雷斯城(墨西哥)地区提供淡水的地下蓄水层正在以比它们通过自然或人工补给补充自己的速度更快的速度枯竭。这种含水层超采的状况导致研究区下伏的Hueco bolson含水层水位下降,有水质恶化的危险。对未来水需求的预测表明,埃尔帕索-华雷斯河谷的地下水供应可能无法持续到2030年以后。建立了埃尔帕索-华雷斯河谷下Hueco bolson含水层的稳态三层模型,以表征垂直泄漏,这是研究区域地下水开采影响的一个指标。在将含水层动力学概念定义为空间过程的基础上,利用地理信息系统对水文地质变量进行制图和处理,计算了1956 - 1995年Hueco bolson含水层垂直渗漏的空间格局及其变化规律。空间水文学方法为含水层渗漏变化检测提供了一种重要的管理手段。©1999 John Wiley &儿子,Inc。
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Spatial analysis of vertical leakage in overdrafted aquifers: The Hueco bolson aquifer, Texas, 1956–1995

The ground-water aquifers that supply the El Paso (United States)–Ciudad Juarez (Mexico) region with fresh water are being depleted faster than they can replenish themselves through natural or induced recharge. This condition of aquifer overdraft has produced water level declines in the Hueco bolson aquifer underlying the study area and threatens water quality deterioration. Projections of future water demand indicate that ground-water supplies in the El Paso–Juarez Valley may not be sustainable beyond the year 2030. A steady-state, three-layer model of the Hueco bolson aquifer underlying the El Paso–Juarez Valley was developed to characterize vertical leakage, an indicator of ground-water extraction impacts in the study area. Based on the conceptualization of aquifer dynamics as a spatial process, a geographic information system was implemented to map and process hydrologic and geologic variables, thus allowing the calculation of the spatial pattern of vertical leakage in the Hueco bolson aquifer and how it changed in the period between 1956 and 1995. The spatial hydrologic method developed for change detection of aquifer leakage provides an important management tool in overdrafted aquifers. © 1999 John Wiley & Sons, Inc.

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