Hydrology and Watershed Management Program, Department of Engineering and Physics, Tarleton State University, BOX T-0390, Stephenville, TX 76402, United States.
J Environ Manage. 2010 Jul;91(7):1511-25. doi: 10.1016/j.jenvman.2010.02.023. Epub 2010 Mar 16.
Wetlands are one of the most important watershed microtopographic features that affect hydrologic processes (e.g., routing) and the fate and transport of constituents (e.g., sediment and nutrients). Efforts to conserve existing wetlands and/or to restore lost wetlands require that watershed-level effects of wetlands on water quantity and water quality be quantified. Because monitoring approaches are usually cost or logistics prohibitive at watershed scale, distributed watershed models such as the Soil and Water Assessment Tool (SWAT), enhanced by the hydrologic equivalent wetland (HEW) concept developed by Wang [Wang, X., Yang, W., Melesse, A.M., 2008. Using hydrologic equivalent wetland concept within SWAT to estimate streamflow in watersheds with numerous wetlands. Trans. ASABE 51 (1), 55-72.], can be a best resort. However, there is a serious lack of information about simulated effects using this kind of integrated modeling approach. The objective of this study was to use the HEW concept in SWAT to assess effects of wetland restoration within the Broughton's Creek watershed located in southwestern Manitoba, and of wetland conservation within the upper portion of the Otter Tail River watershed located in northwestern Minnesota. The results indicated that the HEW concept allows the nonlinear functional relations between watershed processes and wetland characteristics (e.g., size and morphology) to be accurately represented in the models. The loss of the first 10-20% of the wetlands in the Minnesota study area would drastically increase the peak discharge and loadings of sediment, total phosphorus (TP), and total nitrogen (TN). On the other hand, the justifiable reductions of the peak discharge and loadings of sediment, TP, and TN in the Manitoba study area may require that 50-80% of the lost wetlands be restored. Further, the comparison between the predicted restoration and conservation effects revealed that wetland conservation seems to deserve a higher priority while both wetland conservation and restoration may be equally important.
湿地是影响水文过程(如路径)和成分(如泥沙和养分)归宿和迁移的最重要的集水区微观地形特征之一。为了保护现有湿地和/或恢复已丧失的湿地,需要量化湿地对水量和水质的流域层面影响。由于监测方法在流域尺度上通常受到成本或物流的限制,因此可以采用分布式流域模型(如土壤和水评估工具(SWAT)),并结合 Wang [Wang, X., Yang, W., Melesse, A.M., 2008. Using hydrologic equivalent wetland concept within SWAT to estimate streamflow in watersheds with numerous wetlands. Trans. ASABE 51 (1), 55-72.] 开发的水文等效湿地(HEW)概念来增强模型,这是最佳选择。然而,这种综合建模方法的模拟效果信息严重缺乏。本研究的目的是在 SWAT 中使用 HEW 概念来评估位于曼尼托巴省西南部的布劳顿溪集水区内的湿地恢复以及明尼苏达州西北部的奥特尔泰尔河集水区上游内的湿地保护的影响。结果表明,HEW 概念允许准确地在模型中表示流域过程和湿地特征(如大小和形态)之间的非线性功能关系。在明尼苏达州研究区域内,丧失前 10-20%的湿地将大大增加泥沙、总磷(TP)和总氮(TN)的峰值流量和负荷。另一方面,在曼尼托巴省研究区域内,合理减少泥沙、TP 和 TN 的峰值流量和负荷可能需要恢复 50-80%的丧失湿地。此外,对预测的恢复和保护效果的比较表明,湿地保护似乎应该具有更高的优先级,而湿地保护和恢复可能同样重要。