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Title: Characterizing the Atmospheric Mn Cycle and Its Impact on Terrestrial Biogeochemistry

Journal Article · · Global Biogeochemical Cycles
DOI:https://doi.org/10.1029/2023GB007967· OSTI ID:2329558
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  1. Department of Earth and Atmospheric Sciences Cornell University Ithaca NY USA, Now at Nicholas School of the Environment Duke University Durham NC USA
  2. Department of Earth and Atmospheric Sciences Cornell University Ithaca NY USA
  3. La Follette School of Public Affairs University of Wisconsin Madison WI USA
  4. Biological and Environmental Engineering Cornell University Ithaca NY USA
  5. School of Integrative Plant Sciences Cornell University Ithaca NY USA
  6. Department of Ecology and Evolutionary Biology Cornell University Ithaca NY USA
  7. Department of Ecology and Evolutionary Biology Yale University New Haven CT USA
  8. Dip. Scienze della Terra e del Mare University of Palermo Palermo Italy
  9. Instituto de Fisica Universidade de Sao Paulo Sao Paulo Brazil
  10. Saw Science Invercargill New Zealand
  11. Izana Atmospheric Research Centre AEMET Joint Research Unit to CSIC “Climate and Composition of the Atmosphere” Santa Cruz de Tenerife Spain
  12. School of Geography, Earth and Environmental Sciences University of Birmingham Birmingham UK
  13. Department of Civil &, Environmental Engineering Texas A&,M University College Station TX USA
  14. Institute of Marine Sciences University of California Santa Cruz CA USA
  15. Earth &, Planetary Sciences Department University of California Santa Cruz CA USA
  16. Australian Nuclear Science and Technology Organisation Lucas Heights NSW Australia
  17. Rosenstiel School of Marine and Atmospheric Science University of Miami Miami FL USA
  18. Comisión Nacional de Energía Atómica Universidad de Buenos Aires Buenos Aires Argentina
  19. Instituto de Biodiversidad y Medioambiente BIOMA Universidad de Navarra Pamplona España
  20. Finnish Meteorological Institute Helsinki Finland
  21. Cooperative Institute for Research in the Atmosphere Colorado State University Fort Collins CO USA
  22. School of Geography, Earth and Environmental Sciences University of Birmingham Birmingham UK, Department of Environmental Sciences Faculty of Meteorology Environment and Arid Land Agriculture King Abdulaziz University Jeddah Saudi Arabia
  23. Department of Chemical and Biomolecular Engineering Clarkson University Potsdam NY USA
  24. Swiss Federal Laboratories for Materials Science and Technology (EMPA) Duebendorf Switzerland
  25. Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems South China Botanical Garden Chinese Academy of Sciences Guangzhou China
  26. Geography Institute Pontificia Universidad Católica de Chile Santiago Chile, Center for Climate and Resilience Research University of Chile Santiago Chile
  27. Department of Chemistry Ghent University Gent Belgium
  28. Energy, Environmental and Chemical Engineering Washington University St. Louis MO USA
  29. Izana Atmospheric Research Centre AEMET Joint Research Unit to CSIC “Climate and Composition of the Atmosphere” Santa Cruz de Tenerife Spain, CIMEL Electronique Paris France
  30. Izana Atmospheric Research Centre AEMET Joint Research Unit to CSIC “Climate and Composition of the Atmosphere” Santa Cruz de Tenerife Spain, Instituto de Productos Naturales y Agrobiología IPNA CSIC La Laguna Spain

Abstract The role of manganese (Mn) in ecosystem carbon (C) biogeochemical cycling is gaining increasing attention. While soil Mn is mainly derived from bedrock, atmospheric deposition could be a major source of Mn to surface soils, with implications for soil C cycling. However, quantification of the atmospheric Mn cycle, which comprises emissions from natural (desert dust, sea salts, volcanoes, primary biogenic particles, and wildfires) and anthropogenic sources (e.g., industrialization and land‐use change due to agriculture), transport, and deposition, remains uncertain. Here, we use compiled emission data sets for each identified source to model and quantify the atmospheric Mn cycle by combining an atmospheric model and in situ atmospheric concentration measurements. We estimated global emissions of atmospheric Mn in aerosols (<10 μm in aerodynamic diameter) to be 1,400 Gg Mn year −1 . Approximately 31% of the emissions come from anthropogenic sources. Deposition of the anthropogenic Mn shortened Mn “pseudo” turnover times in 1‐m‐thick surface soils (ranging from 1,000 to over 10,000,000 years) by 1–2 orders of magnitude in industrialized regions. Such anthropogenic Mn inputs boosted the Mn‐to‐N ratio of the atmospheric deposition in non‐desert dominated regions (between 5 × 10 −5 and 0.02) across industrialized areas, but that was still lower than soil Mn‐to‐N ratio by 1–3 orders of magnitude. Correlation analysis revealed a negative relationship between Mn deposition and topsoil C density across temperate and (sub)tropical forests, consisting with atmospheric Mn deposition enhancing carbon respiration as seen in in situ biogeochemical studies.

Sponsoring Organization:
USDOE
Grant/Contract Number:
DE‐SC0021302
OSTI ID:
2329558
Journal Information:
Global Biogeochemical Cycles, Journal Name: Global Biogeochemical Cycles Vol. 38 Journal Issue: 4; ISSN 0886-6236
Publisher:
American Geophysical Union (AGU)Copyright Statement
Country of Publication:
United States
Language:
English

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