Effects of elevated [CO2] on forest growth and carbon storage: a modellinganalysis of the consequences of changes in litter quality/quantity and root exudation
Re. Mcmurtrie et al., Effects of elevated [CO2] on forest growth and carbon storage: a modellinganalysis of the consequences of changes in litter quality/quantity and root exudation, PLANT SOIL, 224(1), 2000, pp. 135-152
Many researchers have proposed that the stimulus of plant growth under elev
ated [CO2] observed in short-term experiments will be moderated in the long
er term by a reduction in soil nitrogen (N) availability linked to decrease
d litter quality and/or increased litter production. However, these negativ
e feedbacks may be offset to some extent by a stimulus in N fixation linked
to increased root exudation. The aim of this modelling study is to examine
how changes in litter quality/quantity and root exudation - if they occur
- will affect the CO2 responses of net primary productivity and ecosystem c
arbon (C) storage on different timescales. We apply a model of C and N cycl
ing in forest ecosystems (G'DAY) to stands of Norway spruce (Picea abies, L
. Cast) growing at a N-limited experimental site at Flakaliden, Sweden, and
draw the following conclusions: (1) in the absence of changes in litter qu
ality and root exudation, the short-term CO2 stimulus of litter quantity le
ads to only a minimal CO2 stimulus of productivity or C storage in the medi
um term (approximate to 20 years) and long term (approximate to 200 years),
because of constraints on soil N availability; (2) increasing plant nitrog
en use efficiency (via a decrease in the N:C ratio of new litter) makes lit
tle impact on these results; (3) a significant CO2 response in the medium t
erm requires a substantial decrease in the N:C ratio of older litter, when
it is approaching stabilisation as soil organic matter, although the long-t
erm CO2 response remains small; and (4) an increase in N fixation leads to
a small effect on productivity in the short term, but a very large effect o
n both productivity and C storage in the long term. These results suggest t
hat soil N constraints on the long-term CO2-fertilisation effect can be ove
rcome to a significant extent only by increases in N acquisition, although
only modest increases may be required.