A simple estimation of heterotrophic respiration can be obtained analytically as the y-intercept of the linear regression between soil-surface CO2 efflux and root biomass. In the present study, a development of this indirect methodology is presented by taking into consideration both the temporal variation and the spatial heterogeneity of heterotrophic respiration. For this purpose, soil CO2 efflux, soil carbon content and main stand characteristics were estimated in seven evergreen forest ecosystems along an elevation gradient ranging from 250 to 1740 m. For each site and for each sampling date the measured soil CO2 efflux (RS) was predicted with the model RS = a x SC + b x RD±e, where SC is soil carbon content per unit area to a depth of 30 cm and RD is the root density of the 2–5 mm root class. Regressions with statistically significant a and b coefficients allowed the indirect separation of the two components of soil CO2 efflux. Considering that the different sampling dates were characterized by different soil temperature, it was possible to investigate the temporal and thermal dependency of autotrophic and heterotrophic respiration. It was estimated that annual autotrophic respiration accounts for 16–58% of total soil CO2 efflux in the seven different evergreen ecosystems. In addition, our observations show a decrease of annual autotrophic respiration at increasing availability of soil nitrogen.

Rodeghiero, M.; Cescatti, A. (2006). Indirect partitioning of soil respiration in a series of evergreen forest ecosystems. PLANT AND SOIL, 284 (1): 7-22. doi: 10.1007/s11104-005-5109-8 handle: http://hdl.handle.net/10449/20592

Indirect partitioning of soil respiration in a series of evergreen forest ecosystems

Rodeghiero, Mirco;
2006-01-01

Abstract

A simple estimation of heterotrophic respiration can be obtained analytically as the y-intercept of the linear regression between soil-surface CO2 efflux and root biomass. In the present study, a development of this indirect methodology is presented by taking into consideration both the temporal variation and the spatial heterogeneity of heterotrophic respiration. For this purpose, soil CO2 efflux, soil carbon content and main stand characteristics were estimated in seven evergreen forest ecosystems along an elevation gradient ranging from 250 to 1740 m. For each site and for each sampling date the measured soil CO2 efflux (RS) was predicted with the model RS = a x SC + b x RD±e, where SC is soil carbon content per unit area to a depth of 30 cm and RD is the root density of the 2–5 mm root class. Regressions with statistically significant a and b coefficients allowed the indirect separation of the two components of soil CO2 efflux. Considering that the different sampling dates were characterized by different soil temperature, it was possible to investigate the temporal and thermal dependency of autotrophic and heterotrophic respiration. It was estimated that annual autotrophic respiration accounts for 16–58% of total soil CO2 efflux in the seven different evergreen ecosystems. In addition, our observations show a decrease of annual autotrophic respiration at increasing availability of soil nitrogen.
Autotrophic respiration
Evergreen forests
Heterotrophic respiration
Soil CO2 partitioning
Soil respiration
2006
Rodeghiero, M.; Cescatti, A. (2006). Indirect partitioning of soil respiration in a series of evergreen forest ecosystems. PLANT AND SOIL, 284 (1): 7-22. doi: 10.1007/s11104-005-5109-8 handle: http://hdl.handle.net/10449/20592
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