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A 2-D, diffusion-based, wetland flow model
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DOI：10.1016/S0022-1694(96)03282-9.png)
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Abstract
En 中文
Surface water flow in wetlands occurs typically in a low gradient environment where topographic and flow resistance variations control the discharge distribution. it is within this fluid mechanical regime that the biochemical processes constituting wetland ecology take place. Presented herein are the basics of a mathematical model that takes advantage of the hydraulics typical of wetlands. The resulting model, in the form of a 2-D, non-linear diffusion equation, allows incorporation of spatial variations in Bow resistance and topography, The applicability of the model to one- and two-dimensional wetland type flow is demonstrated using two cases: a laboratory experiment and a wetland pond. Results illustrate the versatility of the formulation and the important influence of topography variations on flow depth and velocity variations. The use of a fixed rectangular calculation domain to simulate the flow pattern in wetlands with irregular wet boundaries is the most significant practical aspect of the WETFLOW model. Future research will concentrate on dealing with extreme heterogeneity in the elevation and Bow resistance distributions, through a combination of measurements and use of stochastic fractals to represent property distributions (Molt and Boman, 1993, Water Resour. Res., 29: 3769-3774). Experimental studies are needed to quantify the relationship of Bow resistance to different combinations of slope, water depth, and a suitable measure of vegetation density for a wetland ecosystem. (C) 1997 Elsevier Science B.V.
Keywords:
OVERLAND-FLOW
Journal
IF:
6.3
Papers:
2.3W
Citations:
9.8W
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