Theoretical Constraints on Fe Reduction Rates in Upland Soils as a Function of Hydroclimatic Conditions-Reference-Cited by-同舟云学术

Theoretical Constraints on Fe Reduction Rates in Upland Soils as a Function of Hydroclimatic Conditions

Published:2020-12 Issue:12 Volume:125 Page:
ISSN:2169-8953
Container-title:Journal of Geophysical Research: Biogeosciences
language:en
Short-container-title:J. Geophys. Res. Biogeosci.

Author:

Calabrese Salvatore¹^ORCID,Barcellos Diego²^ORCID,Thompson Aaron³^ORCID,Porporato Amilcare⁴^ORCID

Affiliation:

1. Department of Biological and Agricultural Engineering Texas A&M University College Station TX USA

2. Escola Superior de Agricultura “Luiz de Queiroz” University of São Paulo Piracicaba Brazil

3. Department of Crop and Soil Sciences University of Georgia Athens GA USA

4. Department of Civil and Environmental Engineering and Princeton Environmental Institute Princeton University Princeton NJ USA

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Atmospheric Science,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020JG005894

Reference94 articles.

1. Barcellos D.(2018).Biogeochemical cycling of iron and carbon in humid (sub) tropical forest soils under fluctuating redox conditions(Ph.D. Thesis) University of Georgia.

2. Faster redox fluctuations can lead to higher iron reduction rates in humid forest soils

3. Hot Spots and Hot Moments of Soil Moisture Explain Fluctuations in Iron and Carbon Cycling in a Humid Tropical Forest Soil

4. Redox Fluctuations Control the Coupled Cycling of Iron and Carbon in Tropical Forest Soils

5. Reduction and immobilization of hexavalent chromium by microbially reduced Fe-bearing clay minerals

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