Susceptibility of soil organic carbon to priming after long-term CO2 fumigation is mediated by soil texture
journal contributionposted on 10.02.2021, 03:51 by Qiao XuQiao Xu, Jian JinJian Jin, Xiaojuan WangXiaojuan Wang, Roger ArmstrongRoger Armstrong, Caixian TangCaixian Tang
© 2018 Elsevier B.V. Elevated CO2 (eCO2) may enhance soil organic carbon (SOC) sequestration via greater input of photosynthetic carbon (C). However, greater rhizodeposits under eCO2 may stimulate microbial decomposition of native SOC. This study aimed to examine the status and stability of SOC in three Australian cropping soils after long-term CO2 enrichment. Samples (0–5 cm) of Chromosol, Vertosol and Calcarosol soils were collected from an 8-year Free-air CO2 Enrichment (SoilFACE) experiment and were used to examine SOC dynamics by physical fractionation and incubation with 13C-glucose. Compared to the ambient CO2 (aCO2) (390–400 μmol mol−1), 8 years of elevated CO2 (eCO2) (550 μmol mol−1) did not increase SOC concentration of all soils, but changed SOC distribution with 12% more C in coarse soil fractions and 5% less C in fine fractions. Elevated CO2 also enhanced the susceptibility of SOC to 13C-glucose-induced priming, but this effect was only significant in the coarse-textured Calcarosol topsoil. The eCO2 history increased labile C (coarse C fraction, +13%) and soil pH (+0.25 units), and decreased available N (−30%) in the Calcarosol, which stimulated microbial biomass C by 28%, leading to an enhanced priming effect. Despite with greater total primed C, the Chromosol that had the highest amount of native C, had lower primed C per unit of SOC when compared to the low-C Calcarosol. In conclusion, the effect of long-term eCO2 enrichment on soil C and N availability in cropping soils depended on soil type with the coarse-textured Calcarosol soil being more susceptible to substrate-induced decomposition of its SOC.
We thank Mahabubur Mollah for maintaining the FACE facility and the SoilFACE technical team (Mel Munn, Liana Warren, Russel Argall and Roger Perris) for managing the field experiment. The Australian SoilFACE is jointly funded by the Victorian State Department of Economic Development, Jobs, Transport and Resources and the University of Melbourne with funding from the Grains Research and Development Corporation (GRDC) and the Australian Government Department of Agriculture and Water Resources.
JournalScience of the Total Environment
Pagination9p. (p. 1112-1120)
Rights StatementThe Author reserves all moral rights over the deposited text and must be credited if any re-use occurs. Documents deposited in OPAL are the Open Access versions of outputs published elsewhere. Changes resulting from the publishing process may therefore not be reflected in this document. The final published version may be obtained via the publisher’s DOI. Please note that additional copyright and access restrictions may apply to the published version.
Science & TechnologyLife Sciences & BiomedicineEnvironmental SciencesEnvironmental Sciences & EcologyFree-air CO2 enrichment (FACE)C-13-glucosePhysical fractionationPriming effectSOC stabilityELEVATED ATMOSPHERIC CO2MICROBIAL BIOMASSTEMPERATURE INCREASEEXTRACTION METHODCROP RESIDUESDECOMPOSITIONNITROGENFORESTMATTERRHIZOSPHERE(13)C-glucoseFree-air CO(2) enrichment (FACE)