Soil Carbon Saturation - Do Soils Have a Carbon Storage Limit, and If So, What Controls It?

Soil Carbon Saturation - Do Soils Have a Carbon Storage Limit, and If So, What Controls It?

AGU via YouTube Direct link

Intro

1 of 19

1 of 19

Intro

Class Central Classrooms beta

YouTube playlists curated by Class Central.

Classroom Contents

Soil Carbon Saturation - Do Soils Have a Carbon Storage Limit, and If So, What Controls It?

Automatically move to the next video in the Classroom when playback concludes

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

Never Stop Learning.

Get personalized course recommendations, track subjects and courses with reminders, and more.

Someone learning on their laptop while sitting on the floor.