Department of Civil Engineering, University of Texas at El Paso, El Paso, TX.
Earth Systems Modeling Branch, U.S. Geological Survey, Mounds View, MN.
Ground Water. 2023 May-Jun;61(3):421-430. doi: 10.1111/gwat.13254. Epub 2022 Sep 27.
Groundwater inundation due to sea level rise can affect island and coastal freshwater resources by exposing water tables to direct, continuous evaporation. Numerical simulations of groundwater inundation effects on coastal and island aquifers have been limited by an inability to simulate solute transport and variable density flow between the aquifer and lakes formed by groundwater inundation. Consequently, we contributed to the development of a new tool, the Lake Transport Package, for MODFLOW 6 that can calculate solute concentrations within lakes and allows for variable density flow between lakes and aquifers. Here we use groundwater inundation as an example application to showcase the functionality of the Lake Transport Package and the advantages of using this tool over past methods of representing groundwater inundation. We developed hypothetical island simulations based on hydrogeological characteristics of the Bahamas. Multiple sea level rise and lake evaporation rates were simulated to evaluate the effects of groundwater inundation on freshwater lens size for different climates. The results demonstrate the ability of the Lake Transport Package to calculate the solute concentration of the lake for transient simulations, including hypersaline concentrations. Higher sea level rise and greater lake evaporation rates lead to a greater loss of the freshwater lens and higher lake salinity. The formation of a lake and corresponding expansion due to groundwater inundation increases the loss of freshwater by 6-36%, depending on the lake evaporation rate. These simulations validate the performance and demonstrate usefulness of the Lake Transport Package as a tool in representing groundwater inundation.
由于海平面上升导致的地下水浸没会通过将地下水位暴露于直接、持续的蒸发中来影响岛屿和沿海淡水资源。由于无法模拟地下水浸没对沿海和岛屿含水层的溶质运移和可变密度流的影响,对地下水浸没影响的数值模拟一直受到限制。因此,我们为 MODFLOW 6 开发了一个新的工具,即湖泊输运包,用于计算湖泊内的溶质浓度,并允许湖泊和含水层之间的可变密度流。在这里,我们将地下水浸没作为一个示例应用,展示湖泊输运包的功能以及使用该工具相对于过去代表地下水浸没的方法的优势。我们根据巴哈马的水文地质特征开发了假设的岛屿模拟。模拟了多种海平面上升和湖泊蒸发率,以评估不同气候条件下地下水浸没对淡水透镜体大小的影响。结果表明,湖泊输运包能够计算瞬态模拟中的湖泊溶质浓度,包括高盐浓度。更高的海平面上升和更大的湖泊蒸发率会导致淡水透镜体更大的损失和更高的湖泊盐度。由于地下水浸没形成的湖泊及其相应的扩张会导致淡水损失增加 6-36%,具体取决于湖泊蒸发率。这些模拟验证了湖泊输运包的性能,并展示了其作为代表地下水浸没的工具的有用性。