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Soil carbon and belowground carbon balance of a short-rotation coppice: assessments from three different approaches.

Identifieur interne : 001194 ( Main/Exploration ); précédent : 001193; suivant : 001195

Soil carbon and belowground carbon balance of a short-rotation coppice: assessments from three different approaches.

Auteurs : Gonzalo Berhongaray ; Melanie S. Verlinden ; Laura S. Broeckx ; Ivan A. Janssens ; Reinhart Ceulemans

Source :

RBID : pubmed:28261329

Abstract

Uncertainty in soil carbon (C) fluxes across different land-use transitions is an issue that needs to be addressed for the further deployment of perennial bioenergy crops. A large-scale short-rotation coppice (SRC) site with poplar (Populus) and willow (Salix) was established to examine the land-use transitions of arable and pasture to bioenergy. Soil C pools, output fluxes of soil CO 2, CH 4, dissolved organic carbon (DOC) and volatile organic compounds, as well as input fluxes from litter fall and from roots, were measured over a 4-year period, along with environmental parameters. Three approaches were used to estimate changes in the soil C. The largest C pool in the soil was the soil organic carbon (SOC) pool and increased after four years of SRC from 10.9 to 13.9 kg C m-2. The belowground woody biomass (coarse roots) represented the second largest C pool, followed by the fine roots (Fr). The annual leaf fall represented the largest C input to the soil, followed by weeds and Fr. After the first harvest, we observed a very large C input into the soil from high Fr mortality. The weed inputs decreased as trees grew older and bigger. Soil respiration averaged 568.9 g C m-2 yr-1. Leaching of DOC increased over the three years from 7.9 to 14.5 g C m-2. The pool-based approach indicated an increase of 3360 g C m-2 in the SOC pool over the 4-year period, which was high when compared with the -27 g C m-2 estimated by the flux-based approach and the -956 g C m-2 of the combined eddy-covariance + biometric approach. High uncertainties were associated to the pool-based approach. Our results suggest using the C flux approach for the assessment of the short-/medium-term SOC balance at our site, while SOC pool changes can only be used for long-term C balance assessments.

DOI: 10.1111/gcbb.12369
PubMed: 28261329
PubMed Central: PMC5310368


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<div type="abstract" xml:lang="en">Uncertainty in soil carbon (C) fluxes across different land-use transitions is an issue that needs to be addressed for the further deployment of perennial bioenergy crops. A large-scale short-rotation coppice (SRC) site with poplar (
<i>Populus</i>
) and willow (
<i>Salix</i>
) was established to examine the land-use transitions of arable and pasture to bioenergy. Soil C pools, output fluxes of soil CO
<sub>2</sub>
, CH
<sub>4</sub>
, dissolved organic carbon (DOC) and volatile organic compounds, as well as input fluxes from litter fall and from roots, were measured over a 4-year period, along with environmental parameters. Three approaches were used to estimate changes in the soil C. The largest C pool in the soil was the soil organic carbon (SOC) pool and increased after four years of SRC from 10.9 to 13.9 kg C m
<sup>-2</sup>
. The belowground woody biomass (coarse roots) represented the second largest C pool, followed by the fine roots (Fr). The annual leaf fall represented the largest C input to the soil, followed by weeds and Fr. After the first harvest, we observed a very large C input into the soil from high Fr mortality. The weed inputs decreased as trees grew older and bigger. Soil respiration averaged 568.9 g C m
<sup>-2</sup>
 yr
<sup>-1</sup>
. Leaching of DOC increased over the three years from 7.9 to 14.5 g C m
<sup>-2</sup>
. The pool-based approach indicated an increase of 3360 g C m
<sup>-2</sup>
in the SOC pool over the 4-year period, which was high when compared with the -27 g C m
<sup>-2</sup>
estimated by the flux-based approach and the -956 g C m
<sup>-2</sup>
of the combined eddy-covariance + biometric approach. High uncertainties were associated to the pool-based approach. Our results suggest using the C flux approach for the assessment of the short-/medium-term SOC balance at our site, while SOC pool changes can only be used for long-term C balance assessments.</div>
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<i>Populus</i>
) and willow (
<i>Salix</i>
) was established to examine the land-use transitions of arable and pasture to bioenergy. Soil C pools, output fluxes of soil CO
<sub>2</sub>
, CH
<sub>4</sub>
, dissolved organic carbon (DOC) and volatile organic compounds, as well as input fluxes from litter fall and from roots, were measured over a 4-year period, along with environmental parameters. Three approaches were used to estimate changes in the soil C. The largest C pool in the soil was the soil organic carbon (SOC) pool and increased after four years of SRC from 10.9 to 13.9 kg C m
<sup>-2</sup>
. The belowground woody biomass (coarse roots) represented the second largest C pool, followed by the fine roots (Fr). The annual leaf fall represented the largest C input to the soil, followed by weeds and Fr. After the first harvest, we observed a very large C input into the soil from high Fr mortality. The weed inputs decreased as trees grew older and bigger. Soil respiration averaged 568.9 g C m
<sup>-2</sup>
 yr
<sup>-1</sup>
. Leaching of DOC increased over the three years from 7.9 to 14.5 g C m
<sup>-2</sup>
. The pool-based approach indicated an increase of 3360 g C m
<sup>-2</sup>
in the SOC pool over the 4-year period, which was high when compared with the -27 g C m
<sup>-2</sup>
estimated by the flux-based approach and the -956 g C m
<sup>-2</sup>
of the combined eddy-covariance + biometric approach. High uncertainties were associated to the pool-based approach. Our results suggest using the C flux approach for the assessment of the short-/medium-term SOC balance at our site, while SOC pool changes can only be used for long-term C balance assessments.</AbstractText>
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<Citation>Ecology. 2009 Mar;90(3):598-611</Citation>
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