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C-loading in African Dark Earths: Specific Surface Area
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Classroom Contents
Soil Carbon Saturation - Do Soils Have a Carbon Storage Limit, and If So, What Controls It?
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- 1 Intro
- 2 Soil carbon storage and losses on a global-scale
- 3 What is mineral-associated and why is it important?
- 4 Soil carbon storage: a balance between inputs and outputs
- 5 What is soil carbon saturation?
- 6 Biotic vs. mineralogical controls
- 7 Mineralogical controls across soils
- 8 Mineralogical capacity in practice
- 9 Estimating mineralogical capacity: a historical perspective
- 10 Relationship between MOC and clay + silt content
- 11 Global synthesis of mineral-associated
- 12 Under-saturation with management and soil depth
- 13 Temperature controls and vulnerability of MOC
- 14 Global mineral-associated carbon and mineralogical saturation
- 15 Why is the mineralogical capacity relevant?
- 16 Management implications and challenges
- 17 Take-away messages
- 18 C-loading in African Dark Earths: Specific Surface Area
- 19 Carbon Loading (C-loading)
