�What is soil carbon? �A synopsis of properties and factors affecting carbon storage, turnover, and persistence within soils
March 2023
Yoko Slowey, Ben Kocar and Mark Chappell
US Army Engineer Research and Development Center (ERDC)
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DISCOVER | DEVELOP | DELIVER
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Soils – Integral to Resilient Environments
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Ecosystem services of soils:
https://www.noaa.gov/education/resource-collections/climate/carbon-cycle
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Soil - The Largest Terrestrial Carbon Pool
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Play a critical role in regulating atmospheric CO2
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Soil Organic Matter
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Role of Soil Organic Matter on Soil Quality
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Organic Matter Composition
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Biomass
(living)
Detritus
(dead, identifiable)
Humus (non-identifiable)
Nonhumic Material
(proteins, carbohydrates, etc.)
Humin: insoluble in acid or base; highly condensed, high MW, OM
Humic Acids: soluble in base, but insoluble in acid; medium MW (300,000 da)
Fulvic Acids:soluble in acid and base; low MW (<50,000 da)
Soil Organic Matter Compositions (Mostly “Traditional” View)
Humic Material
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Soil Organic Matter Composition (“Emergent” View)
- Need to understand carbon flows rather than carbon stocks
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Soil Carbon Cycling
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Soil carbon
Carbon Inputs
Carbon Outputs
Vast Majority is Plant Tissue, also some Animal Tissue
Decomposition and oxidation of Soil Organic Matter (SOM) and evolution of CO2 (Microbially-driven)
Surficial Detritus, Root Mass
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Soil Carbon Cycling
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Soil carbon
Carbon Inputs
Carbon Outputs
Vast Majority is Plant Tissue, also some Animal Tissue
Decomposition and oxidation of Soil Organic Matter (SOM) and evolution of CO2 (Microbially-driven)
Surficial Detritus, Root Mass
Soil Carbon Cycling is Bounded and Governed by Ecosystem Properties
- Biota
- Climate
- Parent Material
- Topography
- Time
Ecosystem-Dependent Carbon Fluxes Control Soil Carbon Stocks
“Natural” Soil Carbon Equilibrium
Soil Carbon “Saturation”
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Soil Carbon Stabilization Mechanisms
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SOC
oxidation
chemical
protection
biochemical
protection
physical
protection
Redox
(O2 availability)
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Factors that Promote SOC Stabilization & Accumulation
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Impact of tilling on SOC
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File Name
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File Name
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Torn et al., Nature 1997
Substrate age (kyr)
Carbon (Kg m-2)
∆14C (‰)
Poorly crystalline Al+Fe (Kg m-2)
Highest C content
Five Soil Forming Factors:
Constant: Climate, Biota, Topography, Parent Material
Variable: Time (age of parent material)
Case Study: Hawaiian Archipelago as a Model System
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Summary
Yoko Slowey, PhD (Yoko.M.Slowey@erdc.dren.mil)
Ben Kocar, PhD, CPSS (Benjamin.D.Kocar@erdc.dren.mil)
Mark Chappell, PhD (Mark.A.Chappell@erdc.dren.mil)
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https://www.noaa.gov/education/resource-collections/climate/carbon-cycle
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Questions?
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