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- W2027597641 abstract "The Miller Woods wetland system contains over 150 individual minerotrophic fens. The fens are established in progradational beach complex of relict beach ridges and parabolic dunes and are in hydraulic connection with Lake Michigan. Large scale flow in the wetland system is horizontal to the northwest. The position of a ground-water divide which forms the southern hydrologic boundary does not coincide with geographical boundaries of the system and migrates in time and space. The position of the divide is not solely a function of topography, but is dependent on an interplay among evapotranspirative demands, antecedent soil moisture, and recent recharge. Small-scale, local flow systems develop and dissipate on variable temporal scales along the margins of individual wetlands in response to evapotranspirative demands by wetland vegetation and other climatic influences." @default.
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- W2027597641 date "1993-01-01" @default.
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- W2027597641 title "The nature of a dynamic water table in a system of non-tidal, freshwater coastal wetlands" @default.
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- W2027597641 doi "https://doi.org/10.1016/0022-1694(93)90046-c" @default.
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