Soil carbon and belowground carbon balance of a short-rotation coppice: assessments from three different approaches
- Autores
- Berhongaray, Gonzalo; Verlinden, Melanie S.; Broeckx, Laura S.; Janssens, Ivan A.; Ceulemans, Reinhart
- Año de publicación
- 2017
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- 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 CO2, CH4, 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.
Fil: Berhongaray, Gonzalo. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universiteit Antwerp; Bélgica
Fil: Verlinden, Melanie S.. Universiteit Antwerp; Bélgica
Fil: Broeckx, Laura S.. Universiteit Antwerp; Bélgica
Fil: Janssens, Ivan A.. Universiteit Antwerp; Bélgica
Fil: Ceulemans, Reinhart. Universiteit Antwerp; Bélgica - Materia
-
BIOENERGY
CARBON FLUXES
CARBON POOLS
LAND-USE CHANGE
POPLAR
POPULUS SP
SECOND-GENERATION BIOFUELS
SOIL ORGANIC CARBON - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
.jpg)
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/66104
Ver los metadatos del registro completo
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Soil carbon and belowground carbon balance of a short-rotation coppice: assessments from three different approachesBerhongaray, GonzaloVerlinden, Melanie S.Broeckx, Laura S.Janssens, Ivan A.Ceulemans, ReinhartBIOENERGYCARBON FLUXESCARBON POOLSLAND-USE CHANGEPOPLARPOPULUS SPSECOND-GENERATION BIOFUELSSOIL ORGANIC CARBONhttps://purl.org/becyt/ford/4.1https://purl.org/becyt/ford/4Uncertainty 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 CO2, CH4, 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.Fil: Berhongaray, Gonzalo. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universiteit Antwerp; BélgicaFil: Verlinden, Melanie S.. Universiteit Antwerp; BélgicaFil: Broeckx, Laura S.. Universiteit Antwerp; BélgicaFil: Janssens, Ivan A.. Universiteit Antwerp; BélgicaFil: Ceulemans, Reinhart. Universiteit Antwerp; BélgicaBlackwell Publishing Ltd2017-02info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/66104Berhongaray, Gonzalo; Verlinden, Melanie S.; Broeckx, Laura S.; Janssens, Ivan A.; Ceulemans, Reinhart; Soil carbon and belowground carbon balance of a short-rotation coppice: assessments from three different approaches; Blackwell Publishing Ltd; GCB Bioenergy; 9; 2; 2-2017; 299-3131757-1707CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1111/gcbb.12369info:eu-repo/semantics/altIdentifier/url/https://onlinelibrary.wiley.com/doi/full/10.1111/gcbb.12369info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2026-02-06T12:40:57Zoai:ri.conicet.gov.ar:11336/66104instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982026-02-06 12:40:57.686CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
| dc.title.none.fl_str_mv |
Soil carbon and belowground carbon balance of a short-rotation coppice: assessments from three different approaches |
| title |
Soil carbon and belowground carbon balance of a short-rotation coppice: assessments from three different approaches |
| spellingShingle |
Soil carbon and belowground carbon balance of a short-rotation coppice: assessments from three different approaches Berhongaray, Gonzalo BIOENERGY CARBON FLUXES CARBON POOLS LAND-USE CHANGE POPLAR POPULUS SP SECOND-GENERATION BIOFUELS SOIL ORGANIC CARBON |
| title_short |
Soil carbon and belowground carbon balance of a short-rotation coppice: assessments from three different approaches |
| title_full |
Soil carbon and belowground carbon balance of a short-rotation coppice: assessments from three different approaches |
| title_fullStr |
Soil carbon and belowground carbon balance of a short-rotation coppice: assessments from three different approaches |
| title_full_unstemmed |
Soil carbon and belowground carbon balance of a short-rotation coppice: assessments from three different approaches |
| title_sort |
Soil carbon and belowground carbon balance of a short-rotation coppice: assessments from three different approaches |
| dc.creator.none.fl_str_mv |
Berhongaray, Gonzalo Verlinden, Melanie S. Broeckx, Laura S. Janssens, Ivan A. Ceulemans, Reinhart |
| author |
Berhongaray, Gonzalo |
| author_facet |
Berhongaray, Gonzalo Verlinden, Melanie S. Broeckx, Laura S. Janssens, Ivan A. Ceulemans, Reinhart |
| author_role |
author |
| author2 |
Verlinden, Melanie S. Broeckx, Laura S. Janssens, Ivan A. Ceulemans, Reinhart |
| author2_role |
author author author author |
| dc.subject.none.fl_str_mv |
BIOENERGY CARBON FLUXES CARBON POOLS LAND-USE CHANGE POPLAR POPULUS SP SECOND-GENERATION BIOFUELS SOIL ORGANIC CARBON |
| topic |
BIOENERGY CARBON FLUXES CARBON POOLS LAND-USE CHANGE POPLAR POPULUS SP SECOND-GENERATION BIOFUELS SOIL ORGANIC CARBON |
| purl_subject.fl_str_mv |
https://purl.org/becyt/ford/4.1 https://purl.org/becyt/ford/4 |
| dc.description.none.fl_txt_mv |
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 CO2, CH4, 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. Fil: Berhongaray, Gonzalo. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universiteit Antwerp; Bélgica Fil: Verlinden, Melanie S.. Universiteit Antwerp; Bélgica Fil: Broeckx, Laura S.. Universiteit Antwerp; Bélgica Fil: Janssens, Ivan A.. Universiteit Antwerp; Bélgica Fil: Ceulemans, Reinhart. Universiteit Antwerp; Bélgica |
| description |
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 CO2, CH4, 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. |
| publishDate |
2017 |
| dc.date.none.fl_str_mv |
2017-02 |
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info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
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article |
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publishedVersion |
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http://hdl.handle.net/11336/66104 Berhongaray, Gonzalo; Verlinden, Melanie S.; Broeckx, Laura S.; Janssens, Ivan A.; Ceulemans, Reinhart; Soil carbon and belowground carbon balance of a short-rotation coppice: assessments from three different approaches; Blackwell Publishing Ltd; GCB Bioenergy; 9; 2; 2-2017; 299-313 1757-1707 CONICET Digital CONICET |
| url |
http://hdl.handle.net/11336/66104 |
| identifier_str_mv |
Berhongaray, Gonzalo; Verlinden, Melanie S.; Broeckx, Laura S.; Janssens, Ivan A.; Ceulemans, Reinhart; Soil carbon and belowground carbon balance of a short-rotation coppice: assessments from three different approaches; Blackwell Publishing Ltd; GCB Bioenergy; 9; 2; 2-2017; 299-313 1757-1707 CONICET Digital CONICET |
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eng |
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eng |
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Blackwell Publishing Ltd |
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