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Anthropogenic and Inherent Effects on Soil Organic Carbon across the U.S

Author

Listed:
  • Márcio R. Nunes

    (USDA-Agricultural Research Service (USDA-ARS), National Laboratory for Agriculture and the Environment, University Boulevard, Ames, IA 50011–3611, USA)

  • Harold M. van Es

    (Section of Soil and Crop Sciences, School of Integrative Plant Science, Cornell University, Ithaca, NY 14853, USA)

  • Kristen S. Veum

    (USDA-ARS, Cropping Systems and Water Quality Research Unit, 269 Agricultural Engineering Bldg., University of Missouri, Columbia, MO 65211, USA)

  • Joseph P. Amsili

    (Section of Soil and Crop Sciences, School of Integrative Plant Science, Cornell University, Ithaca, NY 14853, USA)

  • Douglas L. Karlen

    (USDA-ARS, DL Karlen Consulting LLC, 487 Ashland Ave., St. Pual, MN 55102, USA)

Abstract

Soil organic carbon (SOC) influences several soil functions, making it one of the most important soil health indicators. Its quantity is determined by anthropogenic and inherent factors that must be understood to improve SOC management and interpretation. Topsoil (≤15 cm) SOC response to tillage depth and intensity, cover crops, stover removal, manure addition, and various cropping systems was assessed using 7610 observations from eight U.S. regions. Overall, including cover crops, reducing tillage depth and intensity increased SOC. The positive effects of cover crops were more noticeable in South Central, Northwest, and Midwest regions. Removing high rates (>65%) of crop residue decreased SOC in Midwestern and Southeastern soils. Depending on region, applying manure increased SOC by 21 to 41%, compared to non-manured soils. Diversified cropping systems (e.g., those utilizing small mixed vegetables, perennials, or dairy-based systems) had the highest topsoil SOC content, while more intensive annual row crops and large-scale single vegetable production systems, had the lowest. Among inherent factors, SOC increased as precipitation increased, but decreased as mean annual temperature increased. Texture influenced SOC, showing higher values in fine-texture than coarse-texture soils. Finally, this assessment confirmed that SOC can be a sensitive soil health indicator for evaluating conservation practices.

Suggested Citation

  • Márcio R. Nunes & Harold M. van Es & Kristen S. Veum & Joseph P. Amsili & Douglas L. Karlen, 2020. "Anthropogenic and Inherent Effects on Soil Organic Carbon across the U.S," Sustainability, MDPI, vol. 12(14), pages 1-19, July.
  • Handle: RePEc:gam:jsusta:v:12:y:2020:i:14:p:5695-:d:384896
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    References listed on IDEAS

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    1. Michael W. I. Schmidt & Margaret S. Torn & Samuel Abiven & Thorsten Dittmar & Georg Guggenberger & Ivan A. Janssens & Markus Kleber & Ingrid Kögel-Knabner & Johannes Lehmann & David A. C. Manning & Pa, 2011. "Persistence of soil organic matter as an ecosystem property," Nature, Nature, vol. 478(7367), pages 49-56, October.
    2. Margaret S. Torn & Susan E. Trumbore & Oliver A. Chadwick & Peter M. Vitousek & David M. Hendricks, 1997. "Mineral control of soil organic carbon storage and turnover," Nature, Nature, vol. 389(6647), pages 170-173, September.
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    2. Hafiz Muhammad Rashad Javeed & Mazhar Ali & Nitasha Kanwal & Iftikhar Ahmad & Aftab Jamal & Rafi Qamar & Ali Zakir & Hina Andaleeb & Raheela Jabeen & Emanuele Radicetti & Roberto Mancinelli, 2023. "Nitrogen Mineralization in Texturally Contrasting Soils Subjected to Different Organic Amendments under Semi-Arid Climates," Land, MDPI, vol. 12(5), pages 1-17, April.

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