DFT Analysis of Fe(H2O)63+ and Fe(H2O)62+ Structure and Vibrations; Implications for Isotope Fractionation-Reference-Cited by-同舟云学术

DFT Analysis of Fe(H2O)63+ and Fe(H2O)62+ Structure and Vibrations; Implications for Isotope Fractionation

Published:2004-03-17 Issue:14 Volume:108 Page:2726-2732
ISSN:1089-5639
Container-title:The Journal of Physical Chemistry A
language:en
Short-container-title:J. Phys. Chem. A

Author:

Jarzȩcki A. A.¹,Anbar A. D.¹,Spiro T. G.¹

Affiliation:

1. Department of Chemistry and Center for Environmental Bioinorganic Chemistry, Princeton University, Princeton, New Jersey 08544, and Department of Earth and Environmental Sciences and Department of Chemistry, University of Rochester, Rochester, New York 14627

Publisher

American Chemical Society (ACS)

Subject

Physical and Theoretical Chemistry

Link

https://pubs.acs.org/doi/pdf/10.1021/jp036418b

Reference73 articles.

1. Stable Isotope Geochemistry

2. Nonbiological Fractionation of Iron Isotopes

3. Natural mass-dependent variations in the isotopic composition of molybdenum

4. Iron Isotope Biosignatures

5. Demonstration of significant abiotic iron isotope fractionation in nature

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