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- W38933967 abstract "The processes of a conceptual hydrologic model of a freshwater wetland are reviewed in detail. The unique hydrologic characteristic of wetlands is their narrow range of water table fluctuation above and below the ground surface which is dependent upon regional climatic and topographic characteristics and local site characteristics (microtopography, soil, vegetation) that create the necessary water depths and durations of inundation. The dominant processes controlling the distribution of water include atmospheric circulation, precipitation, evapotranspiration, and surface and groundwater flows. Surface and groundwater flows involve different portions of the same water mass. This water mass can be subdivided into surface water and three groundwater components: an unsaturated zone above the water table, an unconfined saturated zone below the water table, and a confined saturated zone below an impermeable aquiclude. One or another of these subdivisions may not exist at some sites or at different times at the same site. Most hydrologic differences among the various types of wetlands and shallow water bodies are of degree rather than of kind." @default.
- W38933967 created "2016-06-24" @default.
- W38933967 creator A5030085334 @default.
- W38933967 date "1988-01-01" @default.
- W38933967 modified "2023-10-11" @default.
- W38933967 title "Hydrologic Processes for Models of Freshwater Wetlands" @default.
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- W38933967 doi "https://doi.org/10.1016/b978-0-444-42936-0.50007-9" @default.
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