Dl. Randlett et al., ELEVATED ATMOSPHERIC CARBON-DIOXIDE AND LEAF-LITTER CHEMISTRY - INFLUENCES ON MICROBIAL RESPIRATION AND NET NITROGEN MINERALIZATION, Soil Science Society of America journal, 60(5), 1996, pp. 1571-1577
Elevated atmospheric CO2 has the potential to influence rates of C and
N cycling in terrestrial ecosystems by altering plant litter chemistr
y and slowing rates of organic matter decomposition, We tested the hyp
othesis that the chemistry of leaf litter produced at elevated CO2 wou
ld slow C and N transformations in soil. Soils were amended with Popul
us leaf litter produced under two levels of atmospheric CO2 (ambient a
nd twice-ambient) and soil N availability (low and high). Kinetic para
meters for microbial respiration and net N mineralization were determi
ned on soil with and without litter during a 32-wk lab incubation, Pro
duct accumulation curves for CO2-C and inorganic N were fit to a first
order rate equation [y = A(1 - e(-kt))] using nonlinear regression an
alyses, Although CO2 treatment affected soluble sugar concentration in
leaf litter (ambient = 120 g kg(-1), elevated = 130 g kg(-1)), it did
not affect starch concentration or C/N ratio, Microbial respiration,
microbial biomass, and leaf litter C/N ratio were affected by soil N a
vailability but not by atmospheric CO2, Net N mineralization was a lin
ear function of time and was not significantly different for leaves gr
own at ambient (50 mg N kg(-1)) and elevated CO2 (35 mg N kg(-1)). Con
sequently, we found no evidence for the hypothesis that leaf litter pr
oduced at elevated atmospheric CO2 will dampen the rates of C and N cy
cling in soil.