Processes controlling DOC in pore water during simulated drought cycles in six different UK peats
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  • 作者:J. M. Clark (123) j.m.clark@reading.ac.uk
    A. Heinemeyer (4)
    P. Martin (56)
    S. H. Bottrell (2)
  • 关键词:Dissolved organic carbon – ; DOC – ; Sulphate – ; Drought – ; Episodic acidification – ; Peat – ; Climate change
  • 刊名:Biogeochemistry
  • 出版年:2012
  • 出版时间:July 2012
  • 年:2012
  • 卷:109
  • 期:1-3
  • 页码:253-270
  • 全文大小:876.1 KB
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  • 作者单位:1. Soil Research Centre, Department of Geography and Environmental Science, School of Human and Environmental Sciences, University of Reading, Whiteknights, PO Box 233, Reading, RG6 6DW UK2. School of Earth and Environment and School of Geography, University of Leeds, Woodhouse Lane, Leeds, LS2 9JT UK3. Grantham Institute for Climate Change Fellow, Civil and Environmental Engineering, Imperial College London, South Kensington, London, SW7 2AZ UK4. Stockholm Environment Institute at the Environment Department and Centre for Terrestrial Carbon Dynamics (York-Centre), University of York, Heslington, York, YO10 5DD UK5. Department of Biology, University of York, Heslington, York, YO10 5DD UK6. National Oceanography Centre, Southampton, European Way, Southampton, SO14 3ZH UK
  • 刊物类别:Earth and Environmental Science
  • 刊物主题:Earth sciences
    Geochemistry
    Biochemistry
    Soil Science and Conservation
    Terrestrial Pollution
  • 出版者:Springer Netherlands
  • ISSN:1573-515X
文摘
The effect of episodic drought on dissolved organic carbon (DOC) dynamics in peatlands has been the subject of considerable debate, as decomposition and DOC production is thought to increase under aerobic conditions, yet decreased DOC concentrations have been observed during drought periods. Decreased DOC solubility due to drought-induced acidification driven by sulphur (S) redox reactions has been proposed as a causal mechanism; however evidence is based on a limited number of studies carried out at a few sites. To test this hypothesis on a range of different peats, we carried out controlled drought simulation experiments on peat cores collected from six sites across Great Britain. Our data show a concurrent increase in sulphate (SO4) and a decrease in DOC across all sites during simulated water table draw-down, although the magnitude of the relationship between SO4 and DOC differed between sites. Instead, we found a consistent relationship across all sites between DOC decrease and acidification measured by the pore water acid neutralising capacity (ANC). ANC provided a more consistent measure of drought-induced acidification than SO4 alone because it accounts for differences in base cation and acid anions concentrations between sites. Rewetting resulted in rapid DOC increases without a concurrent increase in soil respiration, suggesting DOC changes were primarily controlled by soil acidity not soil biota. These results highlight the need for an integrated analysis of hydrologically driven chemical and biological processes in peatlands to improve our understanding and ability to predict the interaction between atmospheric pollution and changing climatic conditions from plot to regional and global scales.
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