首页> 外文期刊>Journal of water resource and protection >Assessment of Saltwater Intrusion and Discharges to a Wetland with a 3D Transient Variable Density Flow Model: The Coastal Plane Oropesa-Torreblanca Aquifer, Spain
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Assessment of Saltwater Intrusion and Discharges to a Wetland with a 3D Transient Variable Density Flow Model: The Coastal Plane Oropesa-Torreblanca Aquifer, Spain

机译:利用3D瞬态可变密度流模型评估咸水对湿地的入侵和排放:西班牙沿海平面Oropesa-Torreblanca含水层

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摘要

The proper characterization of coastal aquifers requires modeling variable density flow effects. However, most models estimate processes as saline intrusion based on 2D models with constant density and are rarely calibrated to honor salinity measurements. These facts limit the model predictions reliability, affecting the estimated hydrodynamic parameters, external stresses, and other model outputs that can be critical for planning or management decisions. This paper describes the re-assessment of a coastal aquifer model (Oropesa-Torreblanca, eastern Spain) subjected to moderate-to-high saline intrusion with a transient 3D variable density flow model. Previous models were based on 2D low-resolution grids without variable density effects. The new model honors the observed trends of both piezometric and salinity data. Results show the importance of the variable density effects having on critical outputs as sea intrusion and the discharges to a local wetland of high environmental value. The widespread intrusion process and its current stabilization are confirmed but, compared to previous models, the annual average intrusion is 156% higher, discharge to the wetland increases 30%, and the inflows from neighboring formations increase 22%. The more accurate aquifer models, as well as the new discharges and intrusion estimations, are important contributions for future water and environmental planning decisions in the area.
机译:沿海含水层的正确表征需要对可变密度流效应进行建模。但是,大多数模型都基于恒定密度的2D模型将过程估计为盐水入侵,并且很少进行校准以符合盐度测量标准。这些事实限制了模型预测的可靠性,影响了估计的流体动力学参数,外部应力以及其他对计划或管理决策至关重要的模型输出。本文介绍了对瞬态3D变密度流模型进行中度至高度盐水入侵的沿海含水层模型(西班牙东部的奥罗佩萨-托雷布兰卡)的重新评估。先前的模型基于2D低分辨率网格,而没有可变的密度效应。新模型符合测压和盐度数据的观测趋势。结果表明,可变密度效应对关键输出(如海入侵)和向高环境价值的局部湿地的排放具有重要意义。确认了广泛的入侵过程及其当前的稳定性,但是与以前的模型相比,年平均入侵增加了156%,向湿地的排放量增加了30%,来自邻近地层的流入量增加了22%。更精确的含水层模型以及新的排放量和入侵估算,对于该地区未来的水和环境规划决策具有重要意义。

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