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Comparison of ecosystem and soil CO2 efflux in a beech
(Fagus Sylvatica L.) forest
Jérome Ngao, Bernard Longdoz, André Granier
To cite this version:
Jérome Ngao, Bernard Longdoz, André Granier. Comparison of ecosystem and soil CO2 efflux in
a beech (Fagus Sylvatica L.) forest. International symposium : Forests soils under global and local
changes : from research to practice, Sep 2004, Bordeaux, France. 1 p., 2004. �hal-02828196�
COMPARISON OF ECOSYSTEM AND SOIL CO
COMPARISON OF ECOSYSTEM AND SOIL CO
2
2
EFFLUX
EFFLUX
IN A BEECH (
IN A BEECH (
Fagus
Fagus
Sylvatica
Sylvatica
L
L
.
.
) FOREST
) FOREST
J
J
.
.
NGAO,
NGAO,
B. LONGDOZ,
B. LONGDOZ,
A.
A.
GRANIER
GRANIER
UMR Ecologie Ecophysiologie Forestière, INRA Nancy, 54280 Champe
UMR Ecologie Ecophysiologie Forestière, INRA Nancy, 54280 Champenouxnoux
2.
2.
SITE
SITE
4.
4.
MAP OF FLUX MEASUREMENTS
MAP OF FLUX MEASUREMENTS
Soil COSoil CO22efflux (efflux (SSRR) : a major component of forest carbon balance) : a major component of forest carbon balance
Partitioning the ecosystem COPartitioning the ecosystem CO22efflux (efflux (RRecoeco).).
Eddy covariance (Eddy covariance (ECEC) technique for S) technique for SRRmeasurements instead of widely measurements instead of widely
used closed dynamic chamber (
used closed dynamic chamber (CDCCDC) technique typically limited by low ) technique typically limited by low turbulences in below
turbulences in below--canopy situations.canopy situations.
Difference between sampling areas SDifference between sampling areas SRRand Rand Recoeco measurements.measurements.
OverOver--or underestimations of Sor underestimations of SRRcontribution to Rcontribution to Recoeco..
Aim of the study : (i) To compare RAim of the study : (i) To compare Recoecoand Sand SRRfluxes measured at the Hesse fluxes measured at the Hesse
state forest (57, France). (ii) Determinism of R
state forest (57, France). (ii) Determinism of Recoecovariationsvariations
1. CONTEXT
1. CONTEXT
98.0
98.0
867
867
F
F
SOIL
SOIL
ECOSYSTEM
ECOSYSTEM
2003
2003
G
G
E
E
D
D
C
C
B
B
A
A
Global
Global
79.1
79.1
70.2
70.2
74.9
74.9
60.2
60.2
100.7
100.7
75.6
75.6
79.6
79.6
100.0
100.0
Comparison
Comparison
with R
with R
ecoeco(%)
(%)
700
700
621
621
662
662
532
532
890
890
668
668
704
704
884
884
CO
CO
22Efflux
Efflux
(g
(g
CC.m
.m
--22)
)
0 2 4 6 8 10 0 30 60 90 120 150 180 210 240 270 300 330 360 Day of year (2003) C O2 e ff lu x ( gC .m -2.d -1) Global Soil Respiration Ecosystem RespirationFig. 1
Fig. 1
0 1 2 3 4 5 6 7 0 60 120 180 240 300 360 420 480 540 600Day of year (since 2003)
S o il C O 2 e ff lu x ( g C .m -2.d -1) A B C D E F G
Fig. 2
Fig. 2
RRecoecomeasured continously with the EC method measured continously with the EC method (Photo 1). Averaged every 30 minutes.
(Photo 1). Averaged every 30 minutes.
SSRRmeasured with the CDC (Licor 6200 system, measured with the CDC (Licor 6200 system,
Photo 2) in 7 plots (from A to G, Map)
Photo 2) in 7 plots (from A to G, Map)
3.
3.
MEASUREMENT SYSTEMS
MEASUREMENT SYSTEMS
Photo 2 Photo 2 Photo 1 Photo 1 A A B B C C D D EE F F G G A A B B C C D D EE F F G G N E W S LAI 5 LAI 5--77 LAI 3 LAI 3--55 LAI 7 LAI 7--9.59.5 BOR BOR BO BO Bre Bre
Soil Type Hydromorphism Soil Type Hydromorphism
Measurements every 2 weeks. Within each plot, n=12.Measurements every 2 weeks. Within each plot, n=12.
Dominant Wind Direction
Dominant Wind Direction
LocationLocation: 48°40’, 7°05’E: 48°40’, 7°05’E
Mean annualMean annualrainfall :rainfall :820820mmmm
Mean annual temperatureMean annual temperature::9.2°9.2°CC
Soil TypeSoil Type: : Stagnic luvisolStagnic luvisol
SpeciesSpecies: 90% : 90% BeechBeech((F. sylvaticaF. sylvaticaL.)L.)
AgeAge: 35 : 35 yearsyears Mean LAIMean LAI: 7.3: 7.3
Hesse
Hesse
State Forest (Northeast France)
State Forest (Northeast France)
Nancy
Nancy HesseHesse N E W S
6. RESULTS
6. RESULTS
Tab. 1
Tab. 1
7. CONCLUSIONS
7. CONCLUSIONS
-
-
PERSPECTIVES
PERSPECTIVES
Significant discrepancies between global mean SSignificant discrepancies between global mean SRRand Rand Recoeco((Fig. 1Fig. 1).).
Significant differences between plots on seasonal SSignificant differences between plots on seasonal SRRflux evolution (flux evolution (Fig. 2Fig. 2) and annual CO) and annual CO22efflux efflux values (
values (Table 1Table 1): The contribution of S): The contribution of SRRto Rto Recoecomay change with wind direction.may change with wind direction.
Effect of LAI or soil type on SEffect of LAI or soil type on SRRdifferences?differences?
Wind direction during the RWind direction during the Recoecomeasurements (measurements (Fig. 3Fig. 3) highlights the potential CO) highlights the potential CO22sources:sources:
In progress
In progress
: Footprint analysis for determination of relative flux contrib: Footprint analysis for determination of relative flux contribution.ution.To compare RTo compare Recoecowith selected and weighted Swith selected and weighted SRRvalues from the footprint analysisvalues from the footprint analysis
Thanks to Bernard, Chef, Anne, Fanta.Thanks to Bernard, Chef, Anne, Fanta.
Work supported by the CarboEurope IP and the Work supported by the CarboEurope IP and the GIP
GIP--ECOFOR.ECOFOR.
0 0.06 0.12 0.18 0.24 0.3 0 30 60 90 120 150 180 210 240 270 300 330