Effect of organic C on stable Fe isotope fractionation and isotope exchange kinetics between aqueous Fe(II) and ferrihydrite at neutral pH

Author:

Chanda PiyaliORCID,Zhou Zhe,Latta Drew E.ORCID,Scherer Michelle M.,Beard Brian L.,Johnson Clark M.

Funder

National Science Foundation

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference67 articles.

1. Dynamics of ferrihydrite-bound organic carbon during microbial Fe reduction;Adhikari;Geochim. Cosmochim. Acta,2017

2. Change in the magnetic properties of nanoferrihydrite with an increase in the volume of nanoparticles during low-temperature annealing;Balaev;Phys. Solid State,2016

3. User’s manual for WATEQ4F, with revised thermodynamic data base and test cases for calculating speciation of major, trace, and redox elements in natural waters;Ball;U.S. Geol. Surv. Water-Resour. Investig. Rep.,1991

4. Iron isotope fractionation between aqueous ferrous iron and goethite;Beard;Earth Planet. Sci. Lett.,2010

5. Application of Fe isotopes to tracing the geochemical and biological cycling of Fe;Beard;Chem. Geol.,2003

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