E. Casella et Jf. Soussana, LONG-TERM EFFECTS OF CO2 ENRICHMENT AND TEMPERATURE INCREASE ON THE CARBON BALANCE OF A TEMPERATE GRASS SWARD, Journal of Experimental Botany, 48(311), 1997, pp. 1309-1321
Perennial ryegrass swards were grown in large containers on a soil, at
two N fertilizer supplies and were exposed during two years in highly
ventilated plastic tunnels to elevated (700 mu l l(-1) [CO2]) or ambi
ent atmospheric CO2 concentration at outdoor temperature and to a 3 de
grees C increase in air temperature in elevated CO2. The irrigation wa
s adjusted to obtain a soil water deficit during summer. The daily net
C assimilation was increased in elevated CO2 by 29 and 36% at the low
and high N supplies, respectively, Canopies grown in elevated CO2 for
14 to 27 months photosynthetized significantly less rapidly, in both
elevated and normal CO2 concentrations, than their counterparts develo
ped in ambient CO2, but the magnitude of this effect was small (-8% to
-13%). Elevated CO2 resulted in a large increase in the fructan conce
ntration in the pseudostems and laminae (+46% and +189%, respectively)
. In elevated CO2, the hexose and sucrose pool increased by 28% in the
laminae, whereas it did not vary significantly in the pseudo-stems, A
3 degrees C temperature increase in elevated CO2 did not affect signi
ficantly the average WSC concentrations in the pseudostems and laminae
, The elevated CO2 effects on the net C assimilation and on the noctur
nal shoot respiration were greater in summer than in spring. On averag
e, a 35% increase in the below-ground respiration was measured in elev
ated CO2. At the high N supply, a 3 degrees C increase in air temperat
ure led to a decline in the below-ground respiration due to a low soil
moisture, The below-ground carbon storage was increased by 32% and 96
% in elevated CO2 at the low and high N supplies, respectively, with n
o significant increased temperature effect. The role for the below-gro
und carbon storage of CO2-induced changes in the root fraction of the
grass and of temperature-induced changes in the moisture content of th
e soil are discussed.