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

• Published in: Biogeochemistry 2024-04, Vol.167 (4), p.443-459
• Main Authors: Glatzel, Stephan, Worrall, Fred, Boothroyd, Ian M., Heckman, Katherine
• Format: Article
• Language: English
• Subjects: Accumulation; Biogeochemistry; Biogeosciences; Bogs; Carbohydrates; Carbon dioxide; Cellulose; Dissolved organic matter; Earth and Environmental Science; Earth science; Earth Sciences; Ecosystems; Environmental Chemistry; Flushing; Flushing (water); Fourier transforms; Groundwater table; Life Sciences; Lignin; Net losses; Organic soils; Particulate organic matter; Peat; Peat soils; Peatlands; Pore water; Reaction products; Respiration; Sloping sites; Soil profiles; Soil properties; Spectrum analysis; Thermogravimetric analysis; Water discharge; Water table
• ISSN: 1573-515X; 0168-2563; 1573-515X
• DOI: 10.1007/s10533-023-01093-0

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.