Role of nuclear volume in driving equilibrium stable isotope fractionation of mercury, thallium, and other very heavy elements
By E. Schauble. 2007
452 citations recorded by the source corpus.
Subfields: Geochemistry and Petrology, Health, Toxicology and Mutagenesis, Inorganic Chemistry
View Paper: https://www.semanticscholar.org/paper/7d7ab863f1a9fc4c980a7485875655acb2bb5022
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In Geochemistry and Petrology
In Health, Toxicology and Mutagenesis
In Inorganic Chemistry
Citations in the corpus
- Low-temperature isotopic fractionation of uranium (2007, background): “These isotopic shifts have been attributed to nuclear field shift effects (Nomura et al., 1996), whereby heavy isotope enrichment is predicted to occur in the reducedU(IV)-bearing species with respect to the oxidized U(VI)-bearing species (Schauble, 2007).”
- A review of global environmental mercury processes in response to human and natural perturbations: Changes of emissions, climate, and land use (2018, background): “Largest odd-MIF signatures are associated with MIE by photochemical reactions, whereas odd-MIF associated with NVF (identifiable by a different D199Hg/D201Hg ratio) is relatively small.”
- Natural variations in uranium isotope ratios of uranium ore concentrates: Understanding the 238U/235U fractionation mechanism (2010, background): “Equilibrium nuclear-volume isotopic fractionation factors should scale as 1/T, rather than 1/T (Schauble 2007), and given the precision of this study, it is possible some of the scatter in the low-temperature deposits can be explained by variable temperatures of deposition.”