Description
In the context of reducing greenhouse gas (GHG) emissions to combat climate change, rewetting of peatlands is of particular importance. High groundwater levels covering organic matter in the soil prevent its oxidation to CO2. The amount of water needed to allow the rewetting of peatlands can be determined in lysimeter studies.
The evapotranspiration in fens depends essentially on the groundwater table, the vegetation (transpirational active biomass) and the saturation deficit of the atmosphere. After rewetting, these factors can lead to an evapotranspiration of 1000 l m-2 a-1 and even 2000 l m-2 a-1 in dry years depending on the vegetation. In a long term experiment over 20 years, the lysimeters planted with Phragmites australis showed the highest evapotranspiration rates, followed by those covered with Carex species. Evaluation of these results for a large, flooded, rewetted fen area in the Havelländisches Luch in the federal state of Brandenburg, Germany, with Phragmites confirmed the high values of evapotranspiration measured at the groundwater lysimeter station of ZALF in Paulinenaue
DOI
https://doi.org/10.13023/0zcr-6a59
Citation
Pesch, M.; Hoysagk, J.; Eulenstein, F.; and Behrendt, A., "Evapotranspiration of Rewetted and Drained Fen Soils With Grass – Long Term Lysimeter Studies" (2023). IGC Proceedings (1993-2023). 39.
https://uknowledge.uky.edu/igc/XXV_IGC_2023/Utilization/39
Included in
Agricultural Science Commons, Agronomy and Crop Sciences Commons, Plant Biology Commons, Plant Pathology Commons, Soil Science Commons, Weed Science Commons
Evapotranspiration of Rewetted and Drained Fen Soils With Grass – Long Term Lysimeter Studies
In the context of reducing greenhouse gas (GHG) emissions to combat climate change, rewetting of peatlands is of particular importance. High groundwater levels covering organic matter in the soil prevent its oxidation to CO2. The amount of water needed to allow the rewetting of peatlands can be determined in lysimeter studies.
The evapotranspiration in fens depends essentially on the groundwater table, the vegetation (transpirational active biomass) and the saturation deficit of the atmosphere. After rewetting, these factors can lead to an evapotranspiration of 1000 l m-2 a-1 and even 2000 l m-2 a-1 in dry years depending on the vegetation. In a long term experiment over 20 years, the lysimeters planted with Phragmites australis showed the highest evapotranspiration rates, followed by those covered with Carex species. Evaluation of these results for a large, flooded, rewetted fen area in the Havelländisches Luch in the federal state of Brandenburg, Germany, with Phragmites confirmed the high values of evapotranspiration measured at the groundwater lysimeter station of ZALF in Paulinenaue
