Forest soil carbon cycle under elevated CO2 - a case of increased throughput?

Lukac, M.; Lagomarsino, A.; Moscatelli, M. C.; De Angelis, P.; Cotrufo, M. F.; Godbold, D. L.

doi:10.1093/forestry/cpn041

Cited by 38Soil Carbon and Nitrogen DynamicsPlant responses to elevated CO2CO2 Sequestration and Geologic Interactions

Forest soil carbon cycle under elevated CO2 - a case of increased throughput?

Lukac, M., Lagomarsino, A., Moscatelli, M. C., De Angelis, P., Cotrufo, M. F., Godbold, D. L.·2009·Forestry

DOI 10.1093/forestry/cpn041

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Abstract

Forest soils account for a large part of the stable carbon pool held in terrestrial ecosystems. Future levels of atmospheric CO2 are likely to increase C input into the soils through increased above- and below-ground production of forests. This increased input will result in greater sequestration of C only if the additional C enters stable pools. In this review, we compare current observations from four large-scale Free Air FACE Enrichment (FACE) experiments on forest ecosystems (EuroFACE, Aspen-FACE, Duke FACE and ORNL-FACE) and consider their predictive power for long-term C sequestration. At all sites, FACE increased fine root biomass, and in most cases higher fine root turnover resulted in higher C input into soil via root necromass. However, at all sites, soil CO2 efflux also increased in excess of the increased root necromass inputs. A mass balance calculation suggests that a large part of the stimulation of soil CO2 efflux may be due to increased root respiration. Given the duration of these experiments compared with the life cycle of a forest and the complexity of processes involved, it is not yet possible to predict whether elevated CO2 will result in increased C storage in forest soil.

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The increase in root respiration under enhanced CO2 is generally valid for FACE experiments under older (12-16 %) and recently established (22-46 %) systems.
“Root respiration has also been found to increase in SRWC systems under enhanced atmospheric CO2 concentrations [130], which seems to be generally valid for FACE experiments under older (12–16 %) and recently established (22–46 %) systems [153].”
From Carbon Sequestration by Perennial Energy Crops: Is the Jury Still Out? (2015) · cites this paper as [153]

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Authors: Lukac, M., Lagomarsino, A., Moscatelli, M. C., De Angelis, P., Cotrufo, M. F., & Godbold, D. L.
Affiliations: Imperial College London (GB)
ORCID: Lagomarsino, A.
Moscatelli, M. C.
Cotrufo, M. F.
Godbold, D. L.
Venue: Forestry
Publisher: Oxford University Press (OUP)
Published: 2009-01-01
Volume: 82
Issue: 1
Pages: 75-86
ISSN: 0015-752X (ISSN-L)
1464-3626
DOI: 10.1093/forestry/cpn041
OpenAlex: W2152484232
Cited by: 38
References: 75
Citations by year: 2023: 1 · 2022: 1 · 2021: 1 · 2020: 4 · 2018: 1 · 2016: 3 · 2015: 7 · 2014: 3 · 2013: 3 · 2012: 5
FWCI: 4.57
Type: journal article
Language: en
Open access: closed
Locations: Forestry An International Journal of Forest Research (publishedVersion)
UnitusOpen (Tuscia University) (submittedVersion)
HighWire Press Open Archive (submittedVersion)
Funders: University of Wisconsin-Milwaukee
Topics: Life Sciences › Agricultural and Biological Sciences › Soil Science › Soil Carbon and Nitrogen Dynamics
Life Sciences › Agricultural and Biological Sciences › Plant Science › Plant responses to elevated CO2
Physical Sciences › Environmental Science › Environmental Engineering › CO2 Sequestration and Geologic Interactions
Keywords: elevated CO2, free-air CO2 enrichment, carbon sequestration, root necromass, fine root turnover, root respiration, soil CO2 efflux, mass balance, terrestrial carbon storage

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Forest soil carbon cycle under elevated CO2 - a case of increased throughput?

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