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Comparison of the transformation of organic matter flux through a raised bog and a blanket bog

Glatzel, Stephan; Worrall, Fred; Boothroyd, Ian M.; Heckman, Katherine

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Authors

Stephan Glatzel

Ian M. Boothroyd

Katherine Heckman



Abstract

This study has proposed that organic matter transfer and transformation into and through a peatland is dominated by preferential loss of carbohydrates and the retention of lignin-like molecules. Here we used elemental analysis and thermogravimetric analysis to analyse the biomass, litter, peat soil profile, particulate organic matter, and dissolved organic matter fluxes sampled from a continental raised bog in comparison a maritime blanket bog. The macromolecular composition and thermodynamic analysis showed that in the raised bog there had been little or no transformation of the organic matter and the accumulation was rapid with comparatively little transformation with only 13% loss of cellulose by 1 m depth compared to 92% removal of cellulosic material in the blanket bog. The lack of transformation is reflected in a difference in long term carbon accumulation rates between raised and blanket bog sites. We propose that raised bogs, with their lack of a stream outfall, have high stable water tables that mean the pore water become thermodynamically closed and reactions cease higher in the peat profile than in a blanket bog where sloping sites mean a frequent flushing of pore water and discharge of water leading to fluctuating water tables, flushing of reaction products and pore spaces remaining open.

Citation

Glatzel, S., Worrall, F., Boothroyd, I. M., & Heckman, K. (2024). Comparison of the transformation of organic matter flux through a raised bog and a blanket bog. Biogeochemistry, 167(4), 443-459. https://doi.org/10.1007/s10533-023-01093-0

Journal Article Type Article
Acceptance Date Oct 8, 2023
Online Publication Date Nov 10, 2023
Publication Date Apr 1, 2024
Deposit Date Jan 9, 2024
Publicly Available Date Jan 9, 2024
Journal Biogeochemistry
Print ISSN 0168-2563
Electronic ISSN 1573-515X
Publisher Springer
Peer Reviewed Peer Reviewed
Volume 167
Issue 4
Pages 443-459
DOI https://doi.org/10.1007/s10533-023-01093-0
Keywords Long term accumulation, Equilibrium, Thermodynamics, Closed system, Dissolved organic carbon, Carbon budget
Public URL https://durham-repository.worktribe.com/output/2117478

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Copyright Statement
This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.





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