Soil Organic Carbon (SOC)
Benchmark Value
Scoring Curve
This curve shows how a field measurement for this indicator would score across all available benchmark forms in this context.
Evidence & Context
Wetter, more fertile sites on specific soil types (e.g., basalt-derived Ferrosols) with potentially longer fire return intervals or periods of fire exclusion might achieve higher SOC levels, possibly up to ~4.1%
Soil Organic Carbon (SOC) percentage in the 0-10 cm soil depth
This benchmark represents the maximum Soil Organic Carbon percentage observed in wetter, more fertile savanna sites on basalt-derived Ferrosol soils under conservation management in tropical monsoonal savannas.
Based on Koombooloomba State Forest site data showing higher SOC due to basalt parent material and fire exclusion.
Sources (1)
Davies, J. (2017). Carbon and water exchange in Australian tropical savannas. PhD Thesis, James Cook University.
View SourceSupporting Sources (2)
Additional references from the underlying research that informed this benchmark.
Chen, X., Hutley, L.B., Eamus, D., Beringer, J. (2003). Carbon balance of a tropical savanna of northern Australia. Oecologia, 137, 405-416.
View SourceBlunden et al. (2024). Fire regime impacts on soil microbes, soil organic carbon and ground cover in an Australian tropical savanna.
View Source