Articles | Volume 18, issue 6
https://doi.org/10.5194/bg-18-2063-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-18-2063-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Similar importance of edaphic and climatic factors for controlling soil organic carbon stocks of the world
College of Environmental and Resource Sciences, Zhejiang University,
Hangzhou, Zhejiang 310058, China
Raphael A. Viscarra-Rossel
Soil and Landscape Science, School of Molecular and Life Sciences,
Curtin University, Perth, WA 6845, Australia
Tian Qian
College of Environmental and Resource Sciences, Zhejiang University,
Hangzhou, Zhejiang 310058, China
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We characterised the chemical and mineral composition of soil organic carbon fractions with mid-infrared spectroscopy. We identified unique and shared features of the spectra of carbon fractions, and the interactions between their organic and mineral components. These interactions are key to the persistence of C in soils, and we propose that mid-infrared spectroscopy could help to infer stability of soil C.
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We performed Roth C simulations across Australia and assessed the response of soil carbon to changing inputs and future climate change using a consistent modelling framework. Site-specific initialisation of the C pools with measurements of the C fractions is essential for accurate simulations of soil organic C stocks and composition at a large scale. With further warming, Australian soils will become more vulnerable to C loss: natural environments > native grazing > cropping > modified grazing.
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Short summary
Using the data from 141 584 whole-soil profiles across the globe, we disentangled the relative importance of biotic, climatic and edaphic variables in controlling global SOC stocks. The results suggested that soil properties and climate contributed similarly to the explained global variance of SOC in four sequential soil layers down to 2 m. However, the most important individual controls are consistently soil-related, challenging current climate-driven framework of SOC dynamics.
Using the data from 141 584 whole-soil profiles across the globe, we disentangled the relative...
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