Skip to main content

Lund University Publications

LUND UNIVERSITY LIBRARIES

Impacts of litter decay on organic leachate composition and reactivity

Hensgens, Geert LU ; Lechtenfeld, Oliver J. ; Guillemette, François ; Laudon, Hjalmar and Berggren, Martin LU (2021) In Biogeochemistry 154(1). p.99-117
Abstract

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... (More)

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.

(Less)
Please use this url to cite or link to this publication:
author
; ; ; and
organization
publishing date
type
Contribution to journal
publication status
published
subject
keywords
Boreal, Decomposition, Dissolved organic matter, DOC, DOM, FT-ICR MS, Litter leaching, Reactivity
in
Biogeochemistry
volume
154
issue
1
pages
19 pages
publisher
Springer
external identifiers
  • scopus:85105448818
ISSN
0168-2563
DOI
10.1007/s10533-021-00799-3
language
English
LU publication?
yes
id
d9dd9a95-fded-45a8-9f1b-9d8d7706944e
date added to LUP
2021-06-07 14:47:11
date last changed
2022-04-27 02:14:33
@article{d9dd9a95-fded-45a8-9f1b-9d8d7706944e,
  abstract     = {{<p>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.</p>}},
  author       = {{Hensgens, Geert and Lechtenfeld, Oliver J. and Guillemette, François and Laudon, Hjalmar and Berggren, Martin}},
  issn         = {{0168-2563}},
  keywords     = {{Boreal; Decomposition; Dissolved organic matter; DOC; DOM; FT-ICR MS; Litter leaching; Reactivity}},
  language     = {{eng}},
  month        = {{05}},
  number       = {{1}},
  pages        = {{99--117}},
  publisher    = {{Springer}},
  series       = {{Biogeochemistry}},
  title        = {{Impacts of litter decay on organic leachate composition and reactivity}},
  url          = {{http://dx.doi.org/10.1007/s10533-021-00799-3}},
  doi          = {{10.1007/s10533-021-00799-3}},
  volume       = {{154}},
  year         = {{2021}},
}