CO2 fluxes and carbon sequestration within eucalypt stands in Congo

Since October 2000, CO2 and water fluxes are measured within a young eucalypt stand in Congo. In this experiment, our main objective is to derive the net carbon ecosystem exchange (carbon sequestration) from continuous eddy flux measurements, and to compare these estimates to those obtained from 1) measurements of Net Primary Productivity (NPP) and soil heterotrophic respiration, and 2) measurements of carbon stocks (soil and biomass) and their variations over a chronosequence. Carbon stocks and soil respiration measurements were obtained over a chronosequence that includes 6 stands from 6 months up to 10 years within a 43000 ha massif of clonal eucalypt plantations established around Pointe Noire (4°S 12°E, Republic of Congo) over poor, sandy, and highly desaturated soils previously covered by littoral savannas. The Eddy correlation measurements were obtained from the top of a tower erected within the 3 year-old stand of the chronosequence. Soil CO2 efflux (monitored with a respiration chamber connected to a portable Li6200 infrared gas analyzer) exhibited strong seasonal variations, reflecting the seasonal changes in soil water content. Maximum values were obtained during the wet season, while minimum values were obtained in September-October at the end of the dry season (that lasts from June to October). Annual soil CO2 efflux was 11.8 t C/ha at Eddy correlation site, and 16.7 t C/ha at the 10 year old stand. At each site, good relationships were obtained between soil volumetric water content (measured from 0 to 6 cm from the surface) and soil respiration. The soil moisture effect on soil respiration was easily described by a 3 parameters equation. Rhizospheric and heterotrophic contributions to total soil CO2 efflux were estimated from comparison of soil CO2 efflux measured over trenched plots and soil CO2 fluxes measured over non-trenched plots: at the eddy correlation site (3 year-old stand), root respiration contributed to 26% of total annual CO2 efflux. First results obtained at other stands indicate that root contribution to total soil C02 efflux increases with stand age (e.g. around 57% at the 6 year-old stand), probably as a result of root biomass increase with stand age. Similar to soil CO2 efflux, NEE measured by eddy correlation exhibited strong seasonal variations with lowest NEE values (highest CO2 uptake) obtained during the wet season, when LAI and REW (relative extractable water) were maximum. At this time, minimum diurnal peaks of NEE were typically about -25 micromol m-2 s-1. By contrast, minimum peaks obtained at the end of the dry season were about - 12 micromol m-2 s-1. Monthly NEP ranged from -85.3 g C m-2 up to 29.8 g C m-2. This positive value (net carbon emission) has been observed at the transition between the dry and the wet season, and resulted from a faster increase of ecosystem respiration (estimated from nocturnal NEE measurements) than photosynthesis, after the first rains. Daily gross primary production (GPP) was found to be strongly correlated with daily actual evapo-transpiration (AET), resulting in water use efficiencies (WUE-GPP) of about 5.2 g DM/kg H2O. For the two-year period covered by eddy correlation measurements (October 2000 to October 2002), mean annual net C exchange (NEP) was -370 g C m-2/year. This corresponds to a net carbon uptake by the stands, but represents a small fraction of GPP (-1990 g C m-2/year), due to important carbon loss by ecosystem respiration (1620 g C m-2/year). Aboveground respiration, root respiration, and heterotrophic soil respiration represented 27% (438 g C m-2/year), 19% (307 g C m-2/year) and 54% (874 g C m-2/year) of ecosystem respiration, respectively. Over the same period NPP was -1203 g C m-2/year (-676 g C m-2/year for total tree biomass increment, and -527 g C m-2/year for fine root turnover and litter production). Summing NPP and heterotrophic respiration provides another estimates of NEP (-330 g C m-2/year), slightly lower to the one obtain

Saved in:
Bibliographic Details
Main Authors: Nouvellon, Yann, Hamel, Olivier, Bonnefond, Jean-Marc, Roupsard, Olivier, Saint André, Laurent, Epron, Daniel, Irvine, Mark R., Berbigier, Paul, Jourdan, Christophe, Joffre, Richard, Thongo, Armel, Mouvondy, Welcome J., Mabiala, André, Deleporte, Philippe, Laclau, Jean-Paul, Bouillet, Jean-Pierre, Marien, Jean-Noël, Dauzat, Jean
Format: conference_item biblioteca
Language:eng
Published: CNES
Subjects:F61 - Physiologie végétale - Nutrition, P33 - Chimie et physique du sol, Eucalyptus, carbone, nutrition des plantes, photosynthèse, enrichissement en gaz carbonique, échange gazeux, écosystème, biomasse, respiration du sol, variation saisonnière, teneur en eau du sol, évapotranspiration, http://aims.fao.org/aos/agrovoc/c_2683, http://aims.fao.org/aos/agrovoc/c_1301, http://aims.fao.org/aos/agrovoc/c_16379, http://aims.fao.org/aos/agrovoc/c_5812, http://aims.fao.org/aos/agrovoc/c_35921, http://aims.fao.org/aos/agrovoc/c_11098, http://aims.fao.org/aos/agrovoc/c_2482, http://aims.fao.org/aos/agrovoc/c_926, http://aims.fao.org/aos/agrovoc/c_33553, http://aims.fao.org/aos/agrovoc/c_24894, http://aims.fao.org/aos/agrovoc/c_7208, http://aims.fao.org/aos/agrovoc/c_2741, http://aims.fao.org/aos/agrovoc/c_1811,
Online Access:http://agritrop.cirad.fr/513075/
Tags: Add Tag
No Tags, Be the first to tag this record!
id dig-cirad-fr-513075
record_format koha
institution CIRAD FR
collection DSpace
country Francia
countrycode FR
component Bibliográfico
access En linea
databasecode dig-cirad-fr
tag biblioteca
region Europa del Oeste
libraryname Biblioteca del CIRAD Francia
language eng
topic F61 - Physiologie végétale - Nutrition
P33 - Chimie et physique du sol
Eucalyptus
carbone
nutrition des plantes
photosynthèse
enrichissement en gaz carbonique
échange gazeux
écosystème
biomasse
respiration du sol
variation saisonnière
teneur en eau du sol
évapotranspiration
http://aims.fao.org/aos/agrovoc/c_2683
http://aims.fao.org/aos/agrovoc/c_1301
http://aims.fao.org/aos/agrovoc/c_16379
http://aims.fao.org/aos/agrovoc/c_5812
http://aims.fao.org/aos/agrovoc/c_35921
http://aims.fao.org/aos/agrovoc/c_11098
http://aims.fao.org/aos/agrovoc/c_2482
http://aims.fao.org/aos/agrovoc/c_926
http://aims.fao.org/aos/agrovoc/c_33553
http://aims.fao.org/aos/agrovoc/c_24894
http://aims.fao.org/aos/agrovoc/c_7208
http://aims.fao.org/aos/agrovoc/c_2741
http://aims.fao.org/aos/agrovoc/c_1811
F61 - Physiologie végétale - Nutrition
P33 - Chimie et physique du sol
Eucalyptus
carbone
nutrition des plantes
photosynthèse
enrichissement en gaz carbonique
échange gazeux
écosystème
biomasse
respiration du sol
variation saisonnière
teneur en eau du sol
évapotranspiration
http://aims.fao.org/aos/agrovoc/c_2683
http://aims.fao.org/aos/agrovoc/c_1301
http://aims.fao.org/aos/agrovoc/c_16379
http://aims.fao.org/aos/agrovoc/c_5812
http://aims.fao.org/aos/agrovoc/c_35921
http://aims.fao.org/aos/agrovoc/c_11098
http://aims.fao.org/aos/agrovoc/c_2482
http://aims.fao.org/aos/agrovoc/c_926
http://aims.fao.org/aos/agrovoc/c_33553
http://aims.fao.org/aos/agrovoc/c_24894
http://aims.fao.org/aos/agrovoc/c_7208
http://aims.fao.org/aos/agrovoc/c_2741
http://aims.fao.org/aos/agrovoc/c_1811
spellingShingle F61 - Physiologie végétale - Nutrition
P33 - Chimie et physique du sol
Eucalyptus
carbone
nutrition des plantes
photosynthèse
enrichissement en gaz carbonique
échange gazeux
écosystème
biomasse
respiration du sol
variation saisonnière
teneur en eau du sol
évapotranspiration
http://aims.fao.org/aos/agrovoc/c_2683
http://aims.fao.org/aos/agrovoc/c_1301
http://aims.fao.org/aos/agrovoc/c_16379
http://aims.fao.org/aos/agrovoc/c_5812
http://aims.fao.org/aos/agrovoc/c_35921
http://aims.fao.org/aos/agrovoc/c_11098
http://aims.fao.org/aos/agrovoc/c_2482
http://aims.fao.org/aos/agrovoc/c_926
http://aims.fao.org/aos/agrovoc/c_33553
http://aims.fao.org/aos/agrovoc/c_24894
http://aims.fao.org/aos/agrovoc/c_7208
http://aims.fao.org/aos/agrovoc/c_2741
http://aims.fao.org/aos/agrovoc/c_1811
F61 - Physiologie végétale - Nutrition
P33 - Chimie et physique du sol
Eucalyptus
carbone
nutrition des plantes
photosynthèse
enrichissement en gaz carbonique
échange gazeux
écosystème
biomasse
respiration du sol
variation saisonnière
teneur en eau du sol
évapotranspiration
http://aims.fao.org/aos/agrovoc/c_2683
http://aims.fao.org/aos/agrovoc/c_1301
http://aims.fao.org/aos/agrovoc/c_16379
http://aims.fao.org/aos/agrovoc/c_5812
http://aims.fao.org/aos/agrovoc/c_35921
http://aims.fao.org/aos/agrovoc/c_11098
http://aims.fao.org/aos/agrovoc/c_2482
http://aims.fao.org/aos/agrovoc/c_926
http://aims.fao.org/aos/agrovoc/c_33553
http://aims.fao.org/aos/agrovoc/c_24894
http://aims.fao.org/aos/agrovoc/c_7208
http://aims.fao.org/aos/agrovoc/c_2741
http://aims.fao.org/aos/agrovoc/c_1811
Nouvellon, Yann
Hamel, Olivier
Bonnefond, Jean-Marc
Roupsard, Olivier
Saint André, Laurent
Epron, Daniel
Irvine, Mark R.
Berbigier, Paul
Jourdan, Christophe
Joffre, Richard
Thongo, Armel
Mouvondy, Welcome J.
Mabiala, André
Deleporte, Philippe
Laclau, Jean-Paul
Bouillet, Jean-Pierre
Marien, Jean-Noël
Dauzat, Jean
CO2 fluxes and carbon sequestration within eucalypt stands in Congo
description Since October 2000, CO2 and water fluxes are measured within a young eucalypt stand in Congo. In this experiment, our main objective is to derive the net carbon ecosystem exchange (carbon sequestration) from continuous eddy flux measurements, and to compare these estimates to those obtained from 1) measurements of Net Primary Productivity (NPP) and soil heterotrophic respiration, and 2) measurements of carbon stocks (soil and biomass) and their variations over a chronosequence. Carbon stocks and soil respiration measurements were obtained over a chronosequence that includes 6 stands from 6 months up to 10 years within a 43000 ha massif of clonal eucalypt plantations established around Pointe Noire (4°S 12°E, Republic of Congo) over poor, sandy, and highly desaturated soils previously covered by littoral savannas. The Eddy correlation measurements were obtained from the top of a tower erected within the 3 year-old stand of the chronosequence. Soil CO2 efflux (monitored with a respiration chamber connected to a portable Li6200 infrared gas analyzer) exhibited strong seasonal variations, reflecting the seasonal changes in soil water content. Maximum values were obtained during the wet season, while minimum values were obtained in September-October at the end of the dry season (that lasts from June to October). Annual soil CO2 efflux was 11.8 t C/ha at Eddy correlation site, and 16.7 t C/ha at the 10 year old stand. At each site, good relationships were obtained between soil volumetric water content (measured from 0 to 6 cm from the surface) and soil respiration. The soil moisture effect on soil respiration was easily described by a 3 parameters equation. Rhizospheric and heterotrophic contributions to total soil CO2 efflux were estimated from comparison of soil CO2 efflux measured over trenched plots and soil CO2 fluxes measured over non-trenched plots: at the eddy correlation site (3 year-old stand), root respiration contributed to 26% of total annual CO2 efflux. First results obtained at other stands indicate that root contribution to total soil C02 efflux increases with stand age (e.g. around 57% at the 6 year-old stand), probably as a result of root biomass increase with stand age. Similar to soil CO2 efflux, NEE measured by eddy correlation exhibited strong seasonal variations with lowest NEE values (highest CO2 uptake) obtained during the wet season, when LAI and REW (relative extractable water) were maximum. At this time, minimum diurnal peaks of NEE were typically about -25 micromol m-2 s-1. By contrast, minimum peaks obtained at the end of the dry season were about - 12 micromol m-2 s-1. Monthly NEP ranged from -85.3 g C m-2 up to 29.8 g C m-2. This positive value (net carbon emission) has been observed at the transition between the dry and the wet season, and resulted from a faster increase of ecosystem respiration (estimated from nocturnal NEE measurements) than photosynthesis, after the first rains. Daily gross primary production (GPP) was found to be strongly correlated with daily actual evapo-transpiration (AET), resulting in water use efficiencies (WUE-GPP) of about 5.2 g DM/kg H2O. For the two-year period covered by eddy correlation measurements (October 2000 to October 2002), mean annual net C exchange (NEP) was -370 g C m-2/year. This corresponds to a net carbon uptake by the stands, but represents a small fraction of GPP (-1990 g C m-2/year), due to important carbon loss by ecosystem respiration (1620 g C m-2/year). Aboveground respiration, root respiration, and heterotrophic soil respiration represented 27% (438 g C m-2/year), 19% (307 g C m-2/year) and 54% (874 g C m-2/year) of ecosystem respiration, respectively. Over the same period NPP was -1203 g C m-2/year (-676 g C m-2/year for total tree biomass increment, and -527 g C m-2/year for fine root turnover and litter production). Summing NPP and heterotrophic respiration provides another estimates of NEP (-330 g C m-2/year), slightly lower to the one obtain
format conference_item
topic_facet F61 - Physiologie végétale - Nutrition
P33 - Chimie et physique du sol
Eucalyptus
carbone
nutrition des plantes
photosynthèse
enrichissement en gaz carbonique
échange gazeux
écosystème
biomasse
respiration du sol
variation saisonnière
teneur en eau du sol
évapotranspiration
http://aims.fao.org/aos/agrovoc/c_2683
http://aims.fao.org/aos/agrovoc/c_1301
http://aims.fao.org/aos/agrovoc/c_16379
http://aims.fao.org/aos/agrovoc/c_5812
http://aims.fao.org/aos/agrovoc/c_35921
http://aims.fao.org/aos/agrovoc/c_11098
http://aims.fao.org/aos/agrovoc/c_2482
http://aims.fao.org/aos/agrovoc/c_926
http://aims.fao.org/aos/agrovoc/c_33553
http://aims.fao.org/aos/agrovoc/c_24894
http://aims.fao.org/aos/agrovoc/c_7208
http://aims.fao.org/aos/agrovoc/c_2741
http://aims.fao.org/aos/agrovoc/c_1811
author Nouvellon, Yann
Hamel, Olivier
Bonnefond, Jean-Marc
Roupsard, Olivier
Saint André, Laurent
Epron, Daniel
Irvine, Mark R.
Berbigier, Paul
Jourdan, Christophe
Joffre, Richard
Thongo, Armel
Mouvondy, Welcome J.
Mabiala, André
Deleporte, Philippe
Laclau, Jean-Paul
Bouillet, Jean-Pierre
Marien, Jean-Noël
Dauzat, Jean
author_facet Nouvellon, Yann
Hamel, Olivier
Bonnefond, Jean-Marc
Roupsard, Olivier
Saint André, Laurent
Epron, Daniel
Irvine, Mark R.
Berbigier, Paul
Jourdan, Christophe
Joffre, Richard
Thongo, Armel
Mouvondy, Welcome J.
Mabiala, André
Deleporte, Philippe
Laclau, Jean-Paul
Bouillet, Jean-Pierre
Marien, Jean-Noël
Dauzat, Jean
author_sort Nouvellon, Yann
title CO2 fluxes and carbon sequestration within eucalypt stands in Congo
title_short CO2 fluxes and carbon sequestration within eucalypt stands in Congo
title_full CO2 fluxes and carbon sequestration within eucalypt stands in Congo
title_fullStr CO2 fluxes and carbon sequestration within eucalypt stands in Congo
title_full_unstemmed CO2 fluxes and carbon sequestration within eucalypt stands in Congo
title_sort co2 fluxes and carbon sequestration within eucalypt stands in congo
publisher CNES
url http://agritrop.cirad.fr/513075/
work_keys_str_mv AT nouvellonyann co2fluxesandcarbonsequestrationwithineucalyptstandsincongo
AT hamelolivier co2fluxesandcarbonsequestrationwithineucalyptstandsincongo
AT bonnefondjeanmarc co2fluxesandcarbonsequestrationwithineucalyptstandsincongo
AT roupsardolivier co2fluxesandcarbonsequestrationwithineucalyptstandsincongo
AT saintandrelaurent co2fluxesandcarbonsequestrationwithineucalyptstandsincongo
AT eprondaniel co2fluxesandcarbonsequestrationwithineucalyptstandsincongo
AT irvinemarkr co2fluxesandcarbonsequestrationwithineucalyptstandsincongo
AT berbigierpaul co2fluxesandcarbonsequestrationwithineucalyptstandsincongo
AT jourdanchristophe co2fluxesandcarbonsequestrationwithineucalyptstandsincongo
AT joffrerichard co2fluxesandcarbonsequestrationwithineucalyptstandsincongo
AT thongoarmel co2fluxesandcarbonsequestrationwithineucalyptstandsincongo
AT mouvondywelcomej co2fluxesandcarbonsequestrationwithineucalyptstandsincongo
AT mabialaandre co2fluxesandcarbonsequestrationwithineucalyptstandsincongo
AT deleportephilippe co2fluxesandcarbonsequestrationwithineucalyptstandsincongo
AT laclaujeanpaul co2fluxesandcarbonsequestrationwithineucalyptstandsincongo
AT bouilletjeanpierre co2fluxesandcarbonsequestrationwithineucalyptstandsincongo
AT marienjeannoel co2fluxesandcarbonsequestrationwithineucalyptstandsincongo
AT dauzatjean co2fluxesandcarbonsequestrationwithineucalyptstandsincongo
_version_ 1792495513174540288
spelling dig-cirad-fr-5130752024-01-28T11:16:21Z http://agritrop.cirad.fr/513075/ http://agritrop.cirad.fr/513075/ CO2 fluxes and carbon sequestration within eucalypt stands in Congo. Nouvellon Yann, Hamel Olivier, Bonnefond Jean-Marc, Roupsard Olivier, Saint André Laurent, Epron Daniel, Irvine Mark R., Berbigier Paul, Jourdan Christophe, Joffre Richard, Thongo Armel, Mouvondy Welcome J., Mabiala André, Deleporte Philippe, Laclau Jean-Paul, Bouillet Jean-Pierre, Marien Jean-Noël, Dauzat Jean. 2002. In : Regards croisés sur les changements globaux, Arles, 25-29 novembre 2002 : résumés des présentations de la session par affichage. INRA, CNES, CNFCG, CNRS-INSU. Paris : CNES, 2 p. Regards croisés sur les changements globaux, Arles, France, 25 Novembre 2002/29 Novembre 2002. CO2 fluxes and carbon sequestration within eucalypt stands in Congo Nouvellon, Yann Hamel, Olivier Bonnefond, Jean-Marc Roupsard, Olivier Saint André, Laurent Epron, Daniel Irvine, Mark R. Berbigier, Paul Jourdan, Christophe Joffre, Richard Thongo, Armel Mouvondy, Welcome J. Mabiala, André Deleporte, Philippe Laclau, Jean-Paul Bouillet, Jean-Pierre Marien, Jean-Noël Dauzat, Jean eng 2002 CNES Regards croisés sur les changements globaux, Arles, 25-29 novembre 2002 : résumés des présentations de la session par affichage F61 - Physiologie végétale - Nutrition P33 - Chimie et physique du sol Eucalyptus carbone nutrition des plantes photosynthèse enrichissement en gaz carbonique échange gazeux écosystème biomasse respiration du sol variation saisonnière teneur en eau du sol évapotranspiration http://aims.fao.org/aos/agrovoc/c_2683 http://aims.fao.org/aos/agrovoc/c_1301 http://aims.fao.org/aos/agrovoc/c_16379 http://aims.fao.org/aos/agrovoc/c_5812 http://aims.fao.org/aos/agrovoc/c_35921 http://aims.fao.org/aos/agrovoc/c_11098 http://aims.fao.org/aos/agrovoc/c_2482 http://aims.fao.org/aos/agrovoc/c_926 http://aims.fao.org/aos/agrovoc/c_33553 http://aims.fao.org/aos/agrovoc/c_24894 http://aims.fao.org/aos/agrovoc/c_7208 http://aims.fao.org/aos/agrovoc/c_2741 Congo http://aims.fao.org/aos/agrovoc/c_1811 Since October 2000, CO2 and water fluxes are measured within a young eucalypt stand in Congo. In this experiment, our main objective is to derive the net carbon ecosystem exchange (carbon sequestration) from continuous eddy flux measurements, and to compare these estimates to those obtained from 1) measurements of Net Primary Productivity (NPP) and soil heterotrophic respiration, and 2) measurements of carbon stocks (soil and biomass) and their variations over a chronosequence. Carbon stocks and soil respiration measurements were obtained over a chronosequence that includes 6 stands from 6 months up to 10 years within a 43000 ha massif of clonal eucalypt plantations established around Pointe Noire (4°S 12°E, Republic of Congo) over poor, sandy, and highly desaturated soils previously covered by littoral savannas. The Eddy correlation measurements were obtained from the top of a tower erected within the 3 year-old stand of the chronosequence. Soil CO2 efflux (monitored with a respiration chamber connected to a portable Li6200 infrared gas analyzer) exhibited strong seasonal variations, reflecting the seasonal changes in soil water content. Maximum values were obtained during the wet season, while minimum values were obtained in September-October at the end of the dry season (that lasts from June to October). Annual soil CO2 efflux was 11.8 t C/ha at Eddy correlation site, and 16.7 t C/ha at the 10 year old stand. At each site, good relationships were obtained between soil volumetric water content (measured from 0 to 6 cm from the surface) and soil respiration. The soil moisture effect on soil respiration was easily described by a 3 parameters equation. Rhizospheric and heterotrophic contributions to total soil CO2 efflux were estimated from comparison of soil CO2 efflux measured over trenched plots and soil CO2 fluxes measured over non-trenched plots: at the eddy correlation site (3 year-old stand), root respiration contributed to 26% of total annual CO2 efflux. First results obtained at other stands indicate that root contribution to total soil C02 efflux increases with stand age (e.g. around 57% at the 6 year-old stand), probably as a result of root biomass increase with stand age. Similar to soil CO2 efflux, NEE measured by eddy correlation exhibited strong seasonal variations with lowest NEE values (highest CO2 uptake) obtained during the wet season, when LAI and REW (relative extractable water) were maximum. At this time, minimum diurnal peaks of NEE were typically about -25 micromol m-2 s-1. By contrast, minimum peaks obtained at the end of the dry season were about - 12 micromol m-2 s-1. Monthly NEP ranged from -85.3 g C m-2 up to 29.8 g C m-2. This positive value (net carbon emission) has been observed at the transition between the dry and the wet season, and resulted from a faster increase of ecosystem respiration (estimated from nocturnal NEE measurements) than photosynthesis, after the first rains. Daily gross primary production (GPP) was found to be strongly correlated with daily actual evapo-transpiration (AET), resulting in water use efficiencies (WUE-GPP) of about 5.2 g DM/kg H2O. For the two-year period covered by eddy correlation measurements (October 2000 to October 2002), mean annual net C exchange (NEP) was -370 g C m-2/year. This corresponds to a net carbon uptake by the stands, but represents a small fraction of GPP (-1990 g C m-2/year), due to important carbon loss by ecosystem respiration (1620 g C m-2/year). Aboveground respiration, root respiration, and heterotrophic soil respiration represented 27% (438 g C m-2/year), 19% (307 g C m-2/year) and 54% (874 g C m-2/year) of ecosystem respiration, respectively. Over the same period NPP was -1203 g C m-2/year (-676 g C m-2/year for total tree biomass increment, and -527 g C m-2/year for fine root turnover and litter production). Summing NPP and heterotrophic respiration provides another estimates of NEP (-330 g C m-2/year), slightly lower to the one obtain conference_item info:eu-repo/semantics/conferenceObject Conference info:eu-repo/semantics/closedAccess http://catalogue-bibliotheques.cirad.fr/cgi-bin/koha/opac-detail.pl?biblionumber=176102