Relationship between groundwater levels and oxygen availability in fen peat soils

•Ground water levels cannot be directly translated into oxygen availability.•The hypoxic zone is of different extent above groundwater levels (GWL).•Full oxygen saturation never occurred in 20 cm soil depth, even at GWL of −80 cm.•The offset between groundwater level and oxygen availability is site...

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Veröffentlicht in:	Ecological engineering 2018-09, Vol.120, p.85-93
Hauptverfasser:	Dickopp, Jan, Lengerer, Andreas, Kazda, Marian
Format:	Artikel
Sprache:	eng
Schlagworte:	Aeration Anoxia Availability Depth Environmental restoration Fens Grassland management Grasslands Groundwater Groundwater levels Groundwater table Hydrology Hypoxia Hypoxic conditions Land use Organic matter Oxic conditions Oxygen Oxygen content Pasture Peat Peat soils Porosity Probability theory Regression analysis Restoration Rooting Rooting density Saturated soils Saturation Soil Soil conservation Soil depth Soil management Soil porosity Soil water Statistical analysis Water levels Water table Wetland management Wetland restoration Wetlands
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