Articles | Volume 11, issue 1
https://doi.org/10.5194/soil-11-35-2025
https://doi.org/10.5194/soil-11-35-2025
Original research article
 | 
16 Jan 2025
Original research article |  | 16 Jan 2025

Comprehensive increase in CO2 release by drying–rewetting cycles among Japanese forests and pastureland soils and exploring predictors of increasing magnitude

Yuri Suzuki, Syuntaro Hiradate, Jun Koarashi, Mariko Atarashi-Andoh, Takumi Yomogida, Yuki Kanda, and Hirohiko Nagano

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Cited articles

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Asano, M. and Wagai, R.: Evidence of aggregate hierarchy at micro- to submicron scales in an allophanic Andisol, Geoderma, 216, 62–74, https://doi.org/10.1016/j.geoderma.2013.10.005, 2014. a, b, c, d
Barnard, R. L., Blazewicz, S. J., and Firestone, M. K.: Rewetting of soil: Revisiting the origin of soil CO2 emissions, Soil Biol. Biochem., 147, 107819, https://doi.org/10.1016/j.soilbio.2020.107819, 2020. a, b
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Short summary
We incubated 10 Japanese soils to study CO2 release under drying–rewetting cycles (DWCs). CO2 release was increased by DWCs among all soils, showing soil-by-soil variations in CO2 release increase magnitude. The organo-Al complex was the primary predictor for the increase magnitude, suggesting vulnerability of carbon protection by reactive minerals against DWCs. Microbial biomass decrease by DWCs was also suggested, although its link with the CO2 release increase is still unclear.
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