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Title: The response of global carbon storage in soils and net ecosystem production to changes in climate and atmospheric CO[sub 2]

Conference · · Bulletin of the Ecological Society of America; (United States)
OSTI ID:7265973
; ;  [1]
  1. Oak Ridge National Laboratory, TN (United States)

Globally, soils contain two or three times as much carbon as living biomass. The amount of carbon in soil is determined by two biotic processes - productivity of terrestrial vegetation and decomposition of organic matter. Decomposition processes have strong physical and biological controlling factors. A modified version of the Rothamsted Turnover model was used to evaluate response of soil carbon, globally, to changes in atmospheric CO[sub 2] and climate. Using information on climate and soil texture, computing soil moisture and organic matter inputs, we employed the model at a grid scale of 0.5[degrees] latitude and longitude. With no change in climate, increased litter inputs due to a doubling of atmospheric CO[sub 2] resulted in increases of 11-22% in soil carbon depending on the choice of CO[sub 2] response function. Using current CO[sub 2] concentration, changes in climate from a set of five atmospheric GCMs yield 5-10% decreases in soil carbon despite general increases in litter inputs. Soil carbon increases 6-18% as a result of combined climate and atmospheric CO[sub 2] changes. Our models project changes in total terrestrial ecosystem carbon of 13-24% as a result of the potential global changes. We present maps of these altered global carbon distributions.

OSTI ID:
7265973
Report Number(s):
CONF-940894-; CODEN: BECLAG
Journal Information:
Bulletin of the Ecological Society of America; (United States), Vol. 75:2; Conference: Annual Ecological Society of America (ESA) meeting: science and public policy, Knoxville, TN (United States), 7-11 Aug 1994; ISSN 0012-9623
Country of Publication:
United States
Language:
English