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Coupled effect of agricultural practices and climate on carbon storage in two contrasted permanent tropical pastures

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HAL Id: hal-02793133

https://hal.inrae.fr/hal-02793133

Submitted on 5 Jun 2020

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Coupled effect of agricultural practices and climate on carbon storage in two contrasted permanent tropical

pastures

Clement Stahl, Katja Klumpp, Robert Falcimagne, Catherine Picon-Cochard, P. Lecomte, Jean-François Soussana, Sébastien Fontaine, V. Blanfort

To cite this version:

Clement Stahl, Katja Klumpp, Robert Falcimagne, Catherine Picon-Cochard, P. Lecomte, et al.. Coupled effect of agricultural practices and climate on carbon storage in two contrasted permanent tropical pastures. Livestock, Climate Change & Food Security Conference, May 2014, Madrid„ Spain. 2014. �hal-02793133�

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y = -11.9x + 571.4 R² = 0.15 y = -5.9x + 361.0 R² = 0.18 0 50 100 150 200 250 300 350 400 450 500 0 5 10 15 20 25 30 y = 29.7x - 101.4 R² = 0.48 y = 10.7x - 44.8 R² = 0.31 0 50 100 150 200 250 300 350 400 450 500 0 5 10 15 20 25 30 intensive extensive y = 0.6x - 44.5 R² = 0.90 y = 0.4x + 118.6 R² = 0.28 0 50 100 150 200 250 300 350 400 450 500 0 100 200 300 400 500 y = 0.5x - 1.2 R² = 0.95 y = 0.3x + 7.1 R² = 0.77 0 50 100 150 200 250 300 350 400 450 500 0 100 200 300 400 500 600 intensive extensive Linéaire (extensive)

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ETVM Bio-Savane

Coupled effect of agricultural practices and climate

on carbon storage in two contrasted permanent

tropical pastures.

Clément Stahl

1-2 *

, Katja Klumpp

1

, Robert Falcimagne

1

, Catherine Picon-Cochard

1

, Lecomte

Philippe

3

, Jean-François Soussana

1

, Sébastien Fontaine

1

and Vincent Blanfort

1-3

(1) INRA, UR 874, Research Unit on permanent grasslands, 63100 Clermont Ferrand, France (2) CIRAD, UMR Selmet, Campus Agronomique, BP 709, 97387 Kourou Cedex French Guiana (3) CIRAD, UMR Selmet, Campus international de Baillarguet - TA C-112/ A 34398 Montpellier Cedex 5 * clement.stahl@ecofog.gf

 Investigate the drought effect on the carbon storage

in two contrasted agricultural management.

 Evaluate the specific consequences of the climatic

variability (i.e dry and wet season) on the GPP and

Reco.

AIMS

MATERIELS &

METHODS

 Intensity of dry season is different between dry and wet years

leading to a high inter- and intra-annual C storage variability in

relation to water condition.

 The old extensive pasture shows a higher net C storage but is

more affected to intermediate water conditions, between wet

and dry season, allowing the higher C storage in dry years.

 GPP and Reco are sensitive to SWC, but change their pattern in

dry and wet years

CONCLUSION

This study was conducted in two farms in French Guiana, South America (5°16’54”N, 52°54’44”W). Mean annual rainfall is 3041 mm and mean air temperature is around 25.7 °C. The study focused on a hilltop zone with clayey soils, classified as Ferralsols or Acrisols.

More than 15% of Amazon forest has been converted to pastures in last decades. Forests contain

more C than a pasture, however, only little information is available on the potential C

sequestration of those pastures in the long term and with respect to climatic variability. A better

insight on how climatic variability and agricultural management affects net carbon exchange (i.e.

NEE) of cattle pastures are, thus, important to increase C storage and to prevent from increasing

greenhouse gas emission.

We thank the farmers, who permit to samples their pastures. We thank also the great technician assistance of Cirad Guyane and Inra Clermont during this experimentation.

RESULTS

Since 2010, we measured C sink potential by eddy covariance technique of the two pastures.

Eddy covariance flux measurements followed European flux guidelines, and gaps and poor quality data were reconstructed using the gap-filling strategy of Reichstein et al. (2005).

The pastures were established in 1978 (old) and 2008 (young) after deforestation of native rainforest and were grazed rotationally by livestock at low and high stocking density. The vegetation in the pastures was dominated by Brachiaria humidicola.

•Young pasture “ETVM”, were grazed at high stocking density 4.4 LSU ha-1 yr-1 (intensive).

•Old pasture “Bio-Savane”, were grazed at low stocking density 1.4 LSU ha-1 yr-1 (extensive).

Cumu

l

NEE (gC

m

-2

d)

2011

2012

2013

t C ha

-1

an

-1

2011

2012

2013

intensive

-1.06

+0.20

-1.45

extensive

-1.76

-2.56

-1.57

Seasonal variation of net carbon storage (NEE) in the two pastures, show an

effect of the water conditions modulated by the management. Extensive

management allows a better net C storage for dry years, while during the wet

year grazing treatments perform in the same way.

.

Annual Net Ecosystem Exchange (NEE) in the two pastures

Seasonal variation of water conditions during the 3 years. 2012

was the driest year of our study, and 2013 was the wettest.

0 5 10 15 20 25 30 -300 -100 100 300 500 700 jan. 2011 mar. 2011 may. 2011 jul. 2011 sep. 2011 nov. 2011 jan. 2012 mar. 2012 may. 2012 jul. 2012 sep. 2012 nov. 2012 jan. 2013 mar. 2013 may. 2013 jul. 2013 sep. 2013 nov. 2013 SWC 10 cm SWC 30 cm 0 5 10 15 20 25 30 -300 -100 100 300 500 700 jan. 2011 mar. 2011 may. 2011 jul. 2011 sep. 2011 nov. 2011 jan. 2012 mar. 2012 may. 2012 jul. 2012 sep. 2012 nov. 2012 jan. 2013 mar. 2013 may. 2013 jul. 2013 sep. 2013 nov. 2013 SWC 10 cm SWC 30 cm

Precipi

tat

ion

-ET

(mm)

Soi

l wat

er

conte

nt

(m

3

m

-3

)

intensive

extensive

GPP (g C m -2 mon th -1 ) Rec o (gC m -2 mon th -1 ) SWC 30 cm (m-3 m-3) --- intensive --- extensive C sink C source GPP (gC m-2 month-1)

2012

2012

2013

2013

In dry years, GPP increases with soil water content (SWC) while in wet

years GPP declines with SWC.

The part of GPP respired (Reco) is similar for both treatments in dry

years, while a higher fraction of GPP is respired in wet years by the

intensive grazing, which may explain the lower NEE (less negative)

during these years.

Références

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