Advanced

DOC leaching from a coniferous forest floor: modeling a manipulation experiment

Tipping, E; Fröberg, M; Berggren, D; Mulder, J and Bergkvist, Bo LU (2005) In Journal of Plant Nutrition and Soil Science/Zeitschrift für Pflanzenernahrung und Bodenkunde 168(3). p.316-324
Abstract
The DyDOC model simulates the C dynamics of forest soils, including the production and transport of dissolved organic matter (DOM), on the basis of soil hydrology, metabolic processes, and sorption reactions. The model recognizes three main pools of soil C: litter, substrate (an intermediate transformation product), and humic substances. The model was used to simulate the behavior of C in the 0 horizon of soil under a Norway spruce stand at Asa, Sweden, that had been subjected to experimental manipulations (addition and removal) of above-ground litter inputs and to removal of the Oi and Oe layers. Initially, the model was calibrated using results for the control plots and was able to reproduce the observed total soil C pool and C-14... (More)
The DyDOC model simulates the C dynamics of forest soils, including the production and transport of dissolved organic matter (DOM), on the basis of soil hydrology, metabolic processes, and sorption reactions. The model recognizes three main pools of soil C: litter, substrate (an intermediate transformation product), and humic substances. The model was used to simulate the behavior of C in the 0 horizon of soil under a Norway spruce stand at Asa, Sweden, that had been subjected to experimental manipulations (addition and removal) of above-ground litter inputs and to removal of the Oi and Oe layers. Initially, the model was calibrated using results for the control plots and was able to reproduce the observed total soil C pool and C-14 content, DOC flux and DO C-14 content, and the pool of litter C, together with the assumed content of C in humic substances (20% of the total soil C), and the assumed distribution of DOC between hydrophilic and hydrophobic fractions. The constant describing DOC exchange between micro- and macropores was estimated from short-term variations in DOC concentration. When the calibrated model was used to predict the effects of litter and soil manipulations, it underestimated the additional DOC export (up to 33%) caused by litter addition, and underestimated the 22% reduction in DOC export caused by litter withdrawal. Therefore, an additional metabolic process, the direct conversion of litter to DOC, was added to the model. The addition of this process permitted reasonably accurate simulation of the results of the manipulation experiments, without affecting the goodness-of-fit in the model calibration. The results suggest that, under normal conditions, DOC exported from the Asa forest floor is a mixture of compounds derived from soil C pools with a range of residence times. Approximately equal amounts come from the litter pool (turnover time 4.6 yr), the substrate pool (26 yr), and the humic-substances pool (36 yr). (Less)
Please use this url to cite or link to this publication:
author
organization
publishing date
type
Contribution to journal
publication status
published
subject
in
Journal of Plant Nutrition and Soil Science/Zeitschrift für Pflanzenernahrung und Bodenkunde
volume
168
issue
3
pages
316 - 324
publisher
John Wiley & Sons
external identifiers
  • wos:000230044800003
  • scopus:20444499061
ISSN
1436-8730
DOI
10.1002/jpln.200421645
language
English
LU publication?
yes
id
0b180ee0-5a67-474e-8d94-6cb5ef67834c (old id 147085)
date added to LUP
2007-07-03 09:46:01
date last changed
2017-08-27 03:52:08
@article{0b180ee0-5a67-474e-8d94-6cb5ef67834c,
  abstract     = {The DyDOC model simulates the C dynamics of forest soils, including the production and transport of dissolved organic matter (DOM), on the basis of soil hydrology, metabolic processes, and sorption reactions. The model recognizes three main pools of soil C: litter, substrate (an intermediate transformation product), and humic substances. The model was used to simulate the behavior of C in the 0 horizon of soil under a Norway spruce stand at Asa, Sweden, that had been subjected to experimental manipulations (addition and removal) of above-ground litter inputs and to removal of the Oi and Oe layers. Initially, the model was calibrated using results for the control plots and was able to reproduce the observed total soil C pool and C-14 content, DOC flux and DO C-14 content, and the pool of litter C, together with the assumed content of C in humic substances (20% of the total soil C), and the assumed distribution of DOC between hydrophilic and hydrophobic fractions. The constant describing DOC exchange between micro- and macropores was estimated from short-term variations in DOC concentration. When the calibrated model was used to predict the effects of litter and soil manipulations, it underestimated the additional DOC export (up to 33%) caused by litter addition, and underestimated the 22% reduction in DOC export caused by litter withdrawal. Therefore, an additional metabolic process, the direct conversion of litter to DOC, was added to the model. The addition of this process permitted reasonably accurate simulation of the results of the manipulation experiments, without affecting the goodness-of-fit in the model calibration. The results suggest that, under normal conditions, DOC exported from the Asa forest floor is a mixture of compounds derived from soil C pools with a range of residence times. Approximately equal amounts come from the litter pool (turnover time 4.6 yr), the substrate pool (26 yr), and the humic-substances pool (36 yr).},
  author       = {Tipping, E and Fröberg, M and Berggren, D and Mulder, J and Bergkvist, Bo},
  issn         = {1436-8730},
  language     = {eng},
  number       = {3},
  pages        = {316--324},
  publisher    = {John Wiley & Sons},
  series       = {Journal of Plant Nutrition and Soil Science/Zeitschrift für Pflanzenernahrung und Bodenkunde},
  title        = {DOC leaching from a coniferous forest floor: modeling a manipulation experiment},
  url          = {http://dx.doi.org/10.1002/jpln.200421645},
  volume       = {168},
  year         = {2005},
}