Simulation of Natural Iron Oxide Alteration in Soil: Conversion of Synthetic Ferrihydrite to Hematite Without Artificial Dopants, Observed With Magnetic Methods-Reference-Cited by-同舟云学术

Simulation of Natural Iron Oxide Alteration in Soil: Conversion of Synthetic Ferrihydrite to Hematite Without Artificial Dopants, Observed With Magnetic Methods

Published:2020-07 Issue:7 Volume:21 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Bilardello Dario¹^ORCID,Banerjee Subir K.¹,Volk Michael W. R.²^ORCID,Soltis Jennifer A.³^ORCID,Penn R. Lee³^ORCID

Affiliation:

1. Institute for Rock Magnetism University of Minnesota Minneapolis MN USA

2. Department of Earth and Planetary Sciences Harvard University Cambridge MA USA

3. Department of Chemistry University of Minnesota Minneapolis MN USA

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GC009037

Reference86 articles.

1. Variations in relative abundances of goethite and hematite in Bengal Fan sediments: Climatic vs. diagenetic signals

2. Identification and paleoclimatic significance of magnetite nanoparticles in soils

3. Aggregation-Based Crystal Growth and Microstructure Development in Natural Iron Oxyhydroxide Biomineralization Products

4. Evidence for a simple pathway to maghemite in Earth and Mars soils

5. Hydromaghemite, an intermediate in the hydrothermal transformation of 2-line ferrihydrite into hematite

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