4.6 Article

Impacts of litter decay on organic leachate composition and reactivity

Journal

BIOGEOCHEMISTRY
Volume 154, Issue 1, Pages 99-117

Publisher

SPRINGER
DOI: 10.1007/s10533-021-00799-3

Keywords

Dissolved organic matter; Litter leaching; Reactivity; Decomposition; FT-ICR MS; Boreal; DOM; DOC

Funding

  1. Formas [239-2014-698]
  2. Royal Physiography Society Lund
  3. Helmholtz Association
  4. Krycklan via SITES
  5. Aforsk

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Decomposition of litter produces dissolved organic matter (DOM) that significantly impacts soil carbon sequestration. Different litter sources exhibit varying chemical properties and degradability, influencing the dynamics of DOM and carbon sequestration in soil. In-depth molecular analyses of litter-derived DOM provide insights into the complex interactions within soil systems.
Litter decomposition produces labile and recalcitrant forms of dissolved organic matter (DOM) that significantly affect soil carbon (C) sequestration. Chemical analysis of this DOM can provide important knowledge for understanding soil DOM dynamics, but detailed molecular analyses on litter derived DOM are scarce. Here we use ultrahigh resolution mass spectrometry (FT-ICR MS) to characterize the molecular composition of DOM from fresh and progressively decomposed litter samples. We compared high reactive (HR) and low reactive (LR) litter sources with regard to changes in the chemistry and bioavailability of leachates throughout the early phase of litter decay. We show that litter reactivity is a driver of chemical changes in the leached DOM of litter species. Birch, alder and Vaccinium (i.e. HR) litter initially produced more DOM with a higher lability than that of spruce, pine and wood (i.e. LR) litter. Labile oxidized phenolic compounds were abundant in leachates produced during the initial HR litter decay stages, indicating litter lignin degradation. However, the similarity in chemistry between HR and LR leachates increased during the litter decay process as highly leachable structures in HR litter were depleted. In contrast, chemistry of leachates from LR litter changed little during the litter decay process. The oxygenated phenolic compounds from HR litter were driving the lability of HR leachates and the changes in relative abundance of molecules during DOM incubation. This appeared to result in the creation of stable aliphatic secondary microbial compounds. In LR leachates, lability was driven by labile aliphatic compounds, while more resistant phenolic compounds were associated with recalcitrance. These results show how DOM dynamics follow different paths depending on litter reactivity, which has important implications for soil biogeochemistry and C sequestration.

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