The objective of this investigation was to quantify the differences in
soil carbon stores after exposure of birch seedlings (Betula pendula
Roth.) over one growing season to ambient and elevated carbon dioxide
concentrations. One-year-old seedlings of birch were transplanted to p
ots containing 'C-4 soil' derived from beneath a maize crop, and place
d in ambient (350 mu L L-1) and elevated (600 mu L L-1) plots in a fre
e-air carbon dioxide enrichment (FACE) experiment. After 186 days the
plants and soils were destructively sampled, and analysed for differen
ces in root and stem biomass, total plant tissue and soil C contents a
nd delta(13)C values. The trees showed a significant increase (+50%) i
n root biomass, but stem and leaf biomasses were not significantly aff
ected by treatment. C isotope analyses of leaves and fine roots showed
that the isotopic signal from the ambient and elevated CO2 supply was
sufficiently distinct from that of the 'C-4 soil' to enable quantific
ation of net root C input to the soil under both ambient and elevated
CO2. After 186 days, the pots under ambient conditions contained 3.5 g
of C as intact root material, and had gained an additional 0.6 g C ad
ded to the soil through root exudation/turnover; comparable figures fo
r the pots under elevated CO2 were 5.9 g C and 1.5 g C, respectively.
These data confirm the importance of soils as an enhanced sink for C u
nder elevated atmospheric CO2 concentrations. We propose the use of 'C
-4 soils' in elevated CO2 experiments as an important technique for th
e quantification of root net C inputs under both ambient and elevated
CO2 treatments.