Mapping the distribution and magnitude of soil inorganic and organic carbon stocks across Australia

• Soil inorganic carbon (SIC) maps were generated using a two-step mixture model. • SIC content accumulates at lower soil depths. • In the top 1 m, SIC carbon stock is approximately half of soil organic carbon (SOC). • In the 1–2 m depth range, SIC carbon stock is nearly three times larger than SOC. Understanding the presence and dynamics of soil inorganic carbon (SIC) is essential, given its role as a significant sink for atmospheric carbon within the global carbon cycle. In arid and semi-arid regions such as Australia, soils may contain a higher proportion of SIC compared to soil organic carbon (SOC). However, the relative magnitudes of SIC and SOC in these areas remain unclear. This study resolves this uncertainty by estimating Australia’s total soil carbon stocks, with a particular focus on the inorganic carbon fraction. The SIC content was predicted using a two-step quantile regression forests mixture model of classification and regression for six depth intervals: 0–5 cm, 5–15 cm, 15–30 cm, 30–60 cm 60–100 cm, and 100–200 cm at 90 m × 90 m resolution. Equivalent SOC maps were derived from our previous study. The SIC models utilised a compilation of environmental covariates and inorganic carbon content related data from pH (n = 41,590), effervescence (n = 15,105) and calcium carbonate measurements (n = 5,776). Both the classification model (kappa = 0.533) and regression model (R 2 = 0.468) for SIC achieved fair accuracy. The elevated concentration of SIC is consistent with the distribution of calcareous soils, and mainly accumulates in the lower depth. Our estimates indicate that the total carbon stock in Australian soils (0–2 m) is 78.9 Pg, with 44 % comprised of SIC. In the upper 1 m depth, carbon stock from SIC is half that of SOC (17.57 Pg vs. 37.75 Pg); however, in the lower depth interval of 1–2 m, SIC is three times larger than SOC (17.48 Pg vs. 6.13 Pg). In the arid and semi-arid regions of Australia, the amount of SIC stock (34.1 Pg C) is slightly larger than that of SOC stock (29.82 Pg C). This study provides a baseline measure of soil as a carbon sink in the forms of organic carbon and inorganic carbon within Australia.

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Publication Details

Journal
Geoderma
Published
2025-03-08
DOI
https://doi.org/10.1016/j.geoderma.2025.117239
Citations
4
Primary Topic
Soil Geostatistics and Mapping
Type
article
Field-Weighted Citation Impact
3.20
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article

Mapping the distribution and magnitude of soil inorganic and organic carbon stocks across Australia

Budiman Minasny, Mercedes Román Dobarco, Wartini Ng, José Padarian et al.
4 citations
Geoderma
Soil Geostatistics and Mapping
3.20
article

Mapping the distribution and magnitude of soil inorganic and organic carbon stocks across Australia

Budiman Minasny, Mercedes Román Dobarco, Wartini Ng, José Padarian, Alex B. McBratney
article en
4 citations

Abstract

• Soil inorganic carbon (SIC) maps were generated using a two-step mixture model. • SIC content accumulates at lower soil depths. • In the top 1 m, SIC carbon stock is approximately half of soil organic carbon (SOC). • In the 1–2 m depth range, SIC carbon stock is nearly three times larger than SOC. Understanding the presence and dynamics of soil inorganic carbon (SIC) is essential, given its role as a significant sink for atmospheric carbon within the global carbon cycle. In arid and semi-arid regions such as Australia, soils may contain a higher proportion of SIC compared to soil organic carbon (SOC). However, the relative magnitudes of SIC and SOC in these areas remain unclear. This study resolves this uncertainty by estimating Australia’s total soil carbon stocks, with a particular focus on the inorganic carbon fraction. The SIC content was predicted using a two-step quantile regression forests mixture model of classification and regression for six depth intervals: 0–5 cm, 5–15 cm, 15–30 cm, 30–60 cm 60–100 cm, and 100–200 cm at 90 m × 90 m resolution. Equivalent SOC maps were derived from our previous study. The SIC models utilised a compilation of environmental covariates and inorganic carbon content related data from pH (n = 41,590), effervescence (n = 15,105) and calcium carbonate measurements (n = 5,776). Both the classification model (kappa = 0.533) and regression model (R 2 = 0.468) for SIC achieved fair accuracy. The elevated concentration of SIC is consistent with the distribution of calcareous soils, and mainly accumulates in the lower depth. Our estimates indicate that the total carbon stock in Australian soils (0–2 m) is 78.9 Pg, with 44 % comprised of SIC. In the upper 1 m depth, carbon stock from SIC is half that of SOC (17.57 Pg vs. 37.75 Pg); however, in the lower depth interval of 1–2 m, SIC is three times larger than SOC (17.48 Pg vs. 6.13 Pg). In the arid and semi-arid regions of Australia, the amount of SIC stock (34.1 Pg C) is slightly larger than that of SOC stock (29.82 Pg C). This study provides a baseline measure of soil as a carbon sink in the forms of organic carbon and inorganic carbon within Australia.

GeodermaVol. 456
The University of Sydney (AU), UNSW Sydney (AU), Basque Centre for Climate Change (ES), Sydney Institute of Marine Science (AU)
Openalex Percentile: Top 10%
Soil Geostatistics and Mapping
3.20
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