doi:10.1023/B:BIOG.0000031054.19158.7c
Biogeochemistry
69 (3): 379-403, July 2004
Copyright © 2004 Kluwer Academic
Publishers
All rights reserved
Effects
of elevated CO2 on nutrient cycling in a sweetgum plantation
D. W. Johnson
Environmental and Resource Sciences, University of Nevada-Reno, Reno, Nevada 89557 USA(e-mail: dwj@cabnr.unr.edu; phone: +1-775-784-4511;
fax: +1-775-784-4789))
W. Cheng
Department of Environmental Studies, University of
California-Santa Cruz, Santa Cruz, California 95064 USA
J. D. Joslin
Belowground Forest Research Oak Ridge, Tennessee 37830 USA
R. J. Norby
Environmental Sciences Division, Oak Ridge National Laboratory,
Oak Ridge, Tennessee 37830 USA
N. T. Edwards
Environmental Sciences Division, Oak Ridge National Laboratory,
Oak Ridge, Tennessee 37830 USA
D. E. Todd
Environmental Sciences Division, Oak Ridge National Laboratory,
Oak Ridge, Tennessee 37830 USA
Abstract
The
effects of elevated CO2 on nutrient cycling and selected belowground
processes in the closed-canopy sweetgum plantation were assessed as part of a free-air CO2 enrichment (FACE) experiment at Oak Ridge, Tennessee. We hypothesized
that nitrogen (N) constraints to growth response to elevated CO2
would be mitigated primarily by reduced tissue concentrations (resulting in
increased biomass production per unit uptake) rather than increased uptake.
Conversely, we hypothesized that the constraints of other nutrients to growth
response to elevated CO2 would be mitigated primarily by increased
uptake because of adequate soil supplies. The first hypothesis was not
supported: although elevated CO2 caused reduced foliar N
concentrations, it also resulted in increased uptake and requirement of N,
primarily because of greater root turnover. The additional N uptake with
elevated CO2 constituted between 10 and 40% of the estimated soil
mineralizeable N pool. The second hypothesis was largely supported: elevated CO2
had no significant effects on tissue concentrations of P, K, Ca, or Mg and
caused significantly increased uptake and requirement of K, Ca, and Mg. Soil
exchangeable pools of these nutrients are large and should pose no constraint
to continued growth responses. Elevated CO2 also caused increased
microbial biomass, reduced N leaching and increased P leaching from O horizons
(measured by resin lysimeters), reduced soil solution NH4+, SO42-, and Ca2+
concentrations, and increased soil solution pH. There were no statistically
significant treatment effects on soil nutrient availability as measured by
resin capsules, resin stakes, or in situ
incubations. Despite significantly lower litterfall N concentrations in the
elevated CO2 treatment, there were no significant treatment effects
on translocation or forest floor biomass or nutrient contents. There were also
no significant treatment effects on the rate of decomposition of fine roots. In
general, the effects of elevated CO2 on nutrient cycling in this
study were not large; future constraints on growth responses imposed by N
limitations will depend on changes in N demand, atmospheric N deposition, and
soil mineralization rates.
Keywords
Carbon
dioxide, Forest, Nutrients, Uptake, Nutrient cycling
Article ID: 5150932