Suchergebnisse

The file associated with this record is under embargo until 12 months after publication, in accordance with the publisher's self-archiving policy. The full text may be available through the publisher links provided above. ; Peatlands are globally important areas for carbon preservation; although covering only 3% of global land area, they store 30% of total soil carbon. Lowland peat soils can also be very productive for agriculture, but their cultivation requires drainage as most crops are intolerant of root-zone anoxia. This leads to the creation of oxic conditions in which organic matter becomes vulnerable to mineralisation. Given the demand for high quality agricultural land, 40% of the UK's peatlands have been drained for agricultural use. In this study we present the outcomes of a controlled environment experiment conducted on agricultural fen peat to examine possible trade-offs between celery growth (an economically important crop on the agricultural peatlands of eastern England) and emissions of greenhouse gases (carbon dioxide (CO2) and methane (CH4)) at different temperatures (ambient and ambient +5 °C), water table levels (-30 cm, and -50 cm below the surface), and fertiliser use. Raising the water table from -50 cm to -30 cm depressed yields of celery, and at the same time decreased the entire ecosystem CO2 loss by 31%. A 5 °C temperature increase enhanced ecosystem emissions of CO2 by 25% and increased celery dry shoot weight by 23% while not affecting the shoot fresh weight. Fertiliser addition increased both celery yields and soil respiration by 22%. Methane emissions were generally very low and not significantly different from zero. Our results suggest that increasing the water table can lower emissions of greenhouse gases and reduce the rate of peat wastage, but reduces the productivity of celery. If possible, the water table should be raised to -30 cm before and after cultivation, and only decreased during the growing season, as this would reduce the overall greenhouse gas emissions and peat loss, potentially not affecting the production of vegetable crops. ; This research would not be possible without the assistance of Martin Hammond and his son, Alexander Hammond, from Rosedene Farm. We thank them for their help and for allowing us to take soil samples from the farm. Funding for this project was provided by the Grantham Centre for Sustainable Futures. This project has received funding from the European Union's Horizon 2020 research and innovation program under grant agreement No. 727890, and NERC UAMS Grant (NE/P002552/1) to Donatella Zona. Jonathan Leake (NE/M017044/1), Susan Page and Joerg Kaduk (NE/P014097/1) acknowledge funding support from the NERC Soil Security Programme. Steven Banwart (NE/N007514/2) acknowledges funding from the NERC UK-China critical zone science programme on soil and water resources. ; Peer-reviewed ; Post-print