Cited by 163Soil Carbon and Nitrogen DynamicsPasture and Agricultural SystemsSoil erosion and sediment transport

Land use effects on soil carbon fractions in the southeastern United States. I. Management-intensive versus extensive grazing

Conant, Richard T., Six, Johan, Paustian, Keith·2003·Biology and Fertility of Soils

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Crossref · 10.1007/s00374-003-0652-z

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2 of 2 references verified0 citation errors · 0 not checkable

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  • The scientific literature is mixed on SOC responses to rotational grazing: some studies show positive responses, many show no significant difference, and a few suggest a slight negative response.

    “The scientific literature is decidedly mixed with some studies showing positive SOC responses to rotational grazing (e.g. [56], [57]), many showing no significant difference (e.g. [28], [29]) and a few suggesting a slight negative SOC response (e.g. [27], [58]).”
  • Adaptive multi-paddock grazing can improve animal and forage productivity and potentially sequester more soil organic carbon than continuous grazing.

    “By managing for more optimal forage growth and recovery, adaptive multi-paddock (AMP) grazing can improve animal and forage productivity, potentially sequestering more soil organic carbon (SOC) than continuous grazing.”
  • Our estimated sequestration rate (3.59 Mg C ha-1 yr-1) is considerably greater than the mean C sequestration rate of 0.41 Mg C ha-1 yr-1 for 'management intensive grazing' in the Southeastern U.S. cited by Conant et al. (2003).

    “Our estimated sequestration rate (3.59 Mg C ha -1 yr -1 ) is considerably greater than the mean C sequestration rate of 0.41 Mg C ha -1 yr -1 for”
  • Teague et al. (2016) estimated that AMP grazing could induce SOC sequestration rates 10 times greater than the commonly used default value of 0.41 Mg C ha-1 yr-1 proposed by Conant et al. (2003).

    “For instance, Teague et al. (2016) estimated that AMP grazing could induce SOC sequestration rates 10 times greater than the commonly used default value of 0.41 Mg C ha -1 yr -1 proposed by Conant et al. (2003).”
  • Because soils further from C saturation accumulate C faster than soils near saturation, and because our estimated soil C sequestration rate is much greater than 0.41 Mg C ha-1 yr-1, we expect continued sequestration, likely to diminish over time.

    “However, because soils that are further from C saturation will accumulate C faster than soils near saturation, and because our estimated soil C sequestration rate is much greater than the 0.41 Mg C ha -1 yr -1 indicated by Conant et al. (2003), we expect continued sequestration, likely to diminish over time (Minasny et al., 2017;Stewart et al., 2007).”

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Authors
Conant, R. T., Six, J., & Paustian, K.
Affiliations
  • Colorado State University (US)
  • University of California, Davis (US)
Corresponding author
Conant, Richard T.
Venue
Biology and Fertility of Soils
Published
2003-10-01
Volume
38
Issue
6
Pages
386-392
ISSN
  • 0178-2762 (ISSN-L)
  • 1432-0789
OpenAlex
W2006956383
Cited by
163
References
2
Citations by year
2026: 3 · 2025: 7 · 2024: 11 · 2023: 15 · 2022: 11 · 2021: 5 · 2020: 8 · 2019: 5 · 2018: 12 · 2017: 5 · 2016: 9 · 2015: 10 · 2014: 6 · 2013: 6 · 2012: 12
FWCI
6.56
Type
journal article
Language
en
Open access
closed
Locations
  • Biology and Fertility of Soils (publishedVersion)
  • QUT ePrints (Queensland University of Technology) (submittedVersion)
Funders
  • U.S. Department of Energy
  • Virginia Polytechnic Institute and State University
Topics
  • Life Sciences › Agricultural and Biological Sciences › Soil Science › Soil Carbon and Nitrogen Dynamics
  • Life Sciences › Agricultural and Biological Sciences › Forestry › Pasture and Agricultural Systems
  • Life Sciences › Agricultural and Biological Sciences › Soil Science › Soil erosion and sediment transport
Keywords
soil organic carbon, soil carbon fractions, management-intensive grazing, extensive grazing, particulate organic matter, mineral-associated organic carbon, soil nitrogen, carbon sequestration, grazing management, grassland management, soil C:N ratio, clay and silt content

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