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一种模拟湿地与地下水相互作用以预测开发影响的简单方法。

A Simple Method for Simulating Groundwater Interactions with Fens to Forecast Development Effects.

机构信息

U.S. Geological Survey, Upper Midwest Water Science Center, University of Wisconsin-Milwaukee, Lapham Hall, Room 338, 3209 North Maryland Avenue, Milwaukee, WI, 53211 Survey.

The Nature Conservancy, Mukwonago River Watershed Office, East Troy, WI, 53120-1836.

出版信息

Ground Water. 2020 Jul;58(4):524-534. doi: 10.1111/gwat.12931. Epub 2019 Aug 20.

Abstract

Protection of fens-wetlands dependent on groundwater discharge-requires characterization of groundwater sources and stresses. Because instrumentation and numerical modeling of fens is labor intensive, easy-to-apply methods that model fen distribution and their vulnerability to development are desirable. Here we demonstrate that fen areas can be simulated using existing steady-state MODFLOW models when the unsaturated zone flow (UZF) package is included. In cells where the water table is near land surface, the UZF package calculates a head difference and scaled conductance at these "seepage drain" cells to generate average rates of vertical seepage to the land. This formulation, which represents an alternative to blanketing the MODFLOW domain with drains, requires very little input from the user because unsaturated flow-routing is inactive and results are primarily driven by easily obtained topographic information. Like the drain approach, it has the advantage that the distribution of seepage areas is not predetermined by the modeler, but rather emerges from simulated heads. Beyond the drain approach, it takes account of intracell land surface variation to explicitly quantify multiple surficial flows corresponding to infiltration, rejected recharge, recharge and land-surface seepage. Application of the method to a basin in southeastern Wisconsin demonstrates how it can be used as a decision-support tool to first, reproduce fen distribution and, second, forecast drawdown and reduced seepage at fens in response to shallow pumping.

摘要

保护湿地依赖于地下水的排放,这需要对地下水的来源和压力进行特征描述。由于湿地的仪器仪表和数值建模工作非常繁重,因此需要易于应用的方法来模拟湿地的分布及其对开发的脆弱性。在这里,我们展示了当包含非饱和带流(UZF)包时,可以使用现有的稳态 MODFLOW 模型来模拟湿地区域。在地下水位接近地面的单元格中,UZF 包会计算这些“渗流排水”单元格中的水头差和缩放电导,以生成垂直渗流到地面的平均速率。这种替代方法,代表了在 MODFLOW 区域内覆盖排水的替代方案,只需要用户提供很少的输入,因为非饱和流路由是不活跃的,结果主要由易于获得的地形信息驱动。与排水方法一样,它具有优势,即渗流区域的分布不是由建模者预先确定的,而是由模拟的水头确定的。除了排水方法之外,它还考虑了单元格内地面表面的变化,以明确量化与入渗、拒绝补给、补给和地表渗流相对应的多个地表流。该方法在威斯康星州东南部的一个流域中的应用表明,它可以用作决策支持工具,首先是再现湿地的分布,其次是预测浅层抽水对湿地的水位下降和渗流减少。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b7ee/7383665/7b53c3547d81/GWAT-58-524-g001.jpg

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