Institute of Environmental Assessment and Water Research (IDAEA), CSIC, c/Jordi Girona 18-26, 08034 Barcelona, Spain; Associated Unit Hydrogeology Group UPC CSIC, Barcelona, Spain.
Institute of Environmental Assessment and Water Research (IDAEA), CSIC, c/Jordi Girona 18-26, 08034 Barcelona, Spain; Associated Unit Hydrogeology Group UPC CSIC, Barcelona, Spain.
Sci Total Environ. 2017 Aug 15;592:391-402. doi: 10.1016/j.scitotenv.2017.03.118. Epub 2017 Mar 18.
Groundwater management in urban areas requires a detailed knowledge of the hydrogeological system as well as the adequate tools for predicting the amount of groundwater and water quality evolution. In that context, a key difference between urban and natural areas lies in recharge evaluation. A large number of studies have been published since the 1990s that evaluate recharge in urban areas, with no specific methodology. Most of these methods show that there are generally higher rates of recharge in urban settings than in natural settings. Methods such as mixing ratios or groundwater modeling can be used to better estimate the relative importance of different sources of recharge and may prove to be a good tool for total recharge evaluation. However, accurate evaluation of this input is difficult. The objective is to present a methodology to help overcome those difficulties, and which will allow us to quantify the variability in space and time of the recharge into aquifers in urban areas. Recharge calculations have been initially performed by defining and applying some analytical equations, and validation has been assessed based on groundwater flow and solute transport modeling. This methodology is applicable to complex systems by considering temporal variability of all water sources. This allows managers of urban groundwater to evaluate the relative contribution of different recharge sources at a city scale by considering quantity and quality factors. The methodology is applied to the assessment of recharge sources in the Barcelona city aquifers.
城市地区的地下水管理需要详细了解水文地质系统以及预测地下水量和水质演变的适当工具。在这种情况下,城市地区和自然地区之间的一个关键区别在于补给评估。自 20 世纪 90 年代以来,已经发表了大量评估城市地区补给的研究,但没有特定的方法。这些方法大多表明,城市地区的补给率通常高于自然地区。可以使用混合比或地下水建模等方法来更好地估计不同补给源的相对重要性,并且可能被证明是评估总补给的有效工具。然而,准确评估这一输入是困难的。本研究的目的是提出一种方法来帮助克服这些困难,并量化城市含水层补给的时空变异性。补给计算最初是通过定义和应用一些分析方程来进行的,并基于地下水流动和溶质运移模型进行了验证。该方法通过考虑所有水源的时间变异性,适用于复杂系统。这使城市地下水管理者能够通过考虑数量和质量因素来评估城市尺度上不同补给源的相对贡献。该方法应用于评估巴塞罗那城市含水层的补给源。