Heterogeneous oxygenation of wetland soils with increasing inundation: Redox potential, water depth, and preferential flow paths

Saturated wetland soils are typically depleted in oxygen due to rapid consumption by biological processes. Fine‐grained sediments limit the vertical flux of oxygenated surface water. In forested wetlands potential exists for advective transport along preferential flow pathways created by decomposing...

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Veröffentlicht in:	Hydrological processes 2020-03, Vol.34 (6), p.1350-1358
Hauptverfasser:	Lahiri, Chayan, Davidson, Gregg R.
Format:	Artikel
Sprache:	eng
Schlagworte:	advection Advective transport bald cypress Biological activity Consumption Electrode potentials Flooding Floodplains Flow paths Forested wetlands Groundwater Groundwater mining Groundwater table Growing season Hydraulic gradient inundation Lakes Locations (working) Mississippi River floodplain oxbow lake Oxidoreductions Oxygen Oxygen consumption Oxygenation Pore water Preferential flow Redox potential Rivers Saturated soils Sediments Soil Surface water surface‐groundwater interaction Transport Vertical flux Water depth Water table wetland soil Wetland soils Wetlands
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