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Abstract
Soil carbon dioxide (CO
2) evolution is a combined product of the metabolic activity of plant roots and both free-living and symbiotic heterotrophs. Soil CO
2 efflux (S
f) rates are the second largest carbon flux in the global carbon cycle and the largest terrestrial contributor of CO
2 (Raich and Schlesinger 1992). The components of S
f can be broken down into heterotrophic respiration (R
H) and autotropic root respiration (R
R). Quantifying S
f and understanding the contribution of R
H and R
R on intensively managed sites is fundamental to understanding the carbon cycle and implications for carbon sequestration (McElligott and others 2016).
Parent Publication
Citation
Anderson, Peter H.; Maier, Christopher A. 2020. Effects of fertilization and irrigation on components of soil carbon efflux and soil respiration in loblolly pine plantations. In: Bragg, Don C.; Koerth, Nancy E.; Holley, A. Gordon, eds. 2020. Proceedings of the 20th biennial southern silvicultural research conference. e–Gen. Tech. Rep. SRS–253. Asheville, NC: U.S. Department of Agriculture, Forest Service, Southern Research Station: 174-176.