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- W4220772709 abstract "<p>This study considers how the stoichiometry and energy content of organic matter reservoirs and fluxes through and from a peatland enable the carbon fluxes and storage within a peatland to be constrained. The study considers the elemental composition of the above- and below-ground biomass, litter, the peat profile, dissolved and particulate organic matter within a blanket bog in northern England for which only the C budget had been measured. The study shows, based only the elemental composition and calculation of oxidation and energy contents, that:</p><ul><li>DOC in first-order streams is significantly more oxidised than that in peat pore water but that there is no significant difference in organic carbon oxidation state down the peat profile.</li> <li>The approach predicts the occurrence and speciation of N uptake and release in the peatland with N used and recycled.</li> </ul><ul><li>The relatively high oxidation state of DOC in stream water means that acts as an end point for reaction.</li> <li>Methanogenesis does not develop in deep peat as it requires too much energy to form.</li> <li>Sulphate reduction did result in the formation of deep peat but in this catchment this was inadequate to account for the rate of peat formation.</li> </ul><p>The formation of deep peat in this catchment could only be achieved if the DOM in the peat pore water was acting as an electron acceptor and energy source; however, it is unclear as to the flux of DOM up or down the peat profile.</p>" @default.
- W4220772709 created "2022-04-03" @default.
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- W4220772709 date "2022-03-27" @default.
- W4220772709 modified "2023-09-27" @default.
- W4220772709 title "Constraining the carbon budget of peat ecosystems: application of stoichiometry and enthalpy balances." @default.
- W4220772709 doi "https://doi.org/10.5194/egusphere-egu22-1658" @default.
- W4220772709 hasPublicationYear "2022" @default.
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