The results of a 3-yr study on the effects of elevated CO2 on soil N and P,
soil pCO(2), and calculated CO2 efflux in a fire-regenerated Florida scrub
oak ecosystem are summarized. We hypothesized that elevated CO2 would caus
e (i) increases in soil pCO(2) and soil respiration and (ii) reduced levels
of soil-available N and P. The effects of elevated CO2 on soil N availabil
ity differed according to the method used. Results of resin lysimeter colle
ctions and anion exchange membrane tests in the field showed reduced NO3- i
n soils in Years 1 and 3. On the other hand, re-analysis of homogenized, bu
ried soil bags after 1 yr suggested a relative increase in N availability (
lower C to N ratio) under elevated CO2. In the case of P, the buried bags a
nd membranes suggested a negative effect of CO2 on P during the first year;
this faded over time, however, as P availability declined overall, probabl
y in response to P uptake. Elevated CO2 had no effect on soil pCO(2) or cal
culated soil respiration at any time, further suggesting that plant rather
than microbial uptake was the primary factor responsible for the observed c
hanges in N and P availability with elevated CO2.