Metal stable isotope signatures as tracers in environmental geochemistry
JG Wiederhold - Environmental science & technology, 2015 - ACS Publications
The biogeochemical cycling of metals in natural systems is often accompanied by stable
isotope fractionation which can now be measured due to recent analytical advances. In …
isotope fractionation which can now be measured due to recent analytical advances. In …
Iron isotope systematics
Iron Isotope Systematics | Reviews in Mineralogy and Geochemistry | GeoScienceWorld
Skip to Main Content GeoScienceWorld GeoScienceWorld Close Journals Books GeoRef …
Skip to Main Content GeoScienceWorld GeoScienceWorld Close Journals Books GeoRef …
First-principles estimates of equilibrium magnesium isotope fractionation in silicate, oxide, carbonate and hexaaquamagnesium (2+) crystals
EA Schauble - Geochimica et Cosmochimica Acta, 2011 - Elsevier
Equilibrium mass-dependent magnesium isotope fractionation factors are estimated for a
range of crystalline compounds including oxides, silicates, carbonates, and salts containing …
range of crystalline compounds including oxides, silicates, carbonates, and salts containing …
High-temperature equilibrium isotope fractionation of non-traditional stable isotopes: Experiments, theory, and applications
High-temperature partitioning of the stable isotopes of rock-forming elements like Mg, Si, Fe,
Ni and others are useful new tools in geochemistry and cosmochemistry. Understanding the …
Ni and others are useful new tools in geochemistry and cosmochemistry. Understanding the …
The effect of bonding environment on iron isotope fractionation between minerals at high temperature
PA Sossi, HSC O'Neill - Geochimica et Cosmochimica Acta, 2017 - Elsevier
Central to understanding the processes that drive stable isotope fractionation in nature is
their quantification under controlled experimental conditions. The polyvalent element iron …
their quantification under controlled experimental conditions. The polyvalent element iron …
Isotopic fractionation of Mg2+ (aq), Ca2+ (aq), and Fe2+ (aq) with carbonate minerals
Density-functional electronic structure calculations are used to compute the equilibrium
constants for 26Mg/24Mg and 44Ca/40Ca isotope exchange between carbonate minerals …
constants for 26Mg/24Mg and 44Ca/40Ca isotope exchange between carbonate minerals …
Iron isotope fractionation between aqueous ferrous iron and goethite
The equilibrium Fe isotope fractionation factor between aqueous Fe (II) and goethite has
been experimentally measured to be− 1.05±0.08‰ in 56Fe/54Fe (2σ) at 22° C, using the …
been experimentally measured to be− 1.05±0.08‰ in 56Fe/54Fe (2σ) at 22° C, using the …
Iron isotope systematics in planetary reservoirs
Iron is the only polyvalent major element, and controls reduction–oxidation (redox) reactions
in a host of geologic processes and reservoirs, from the mineral-to planetary-scale, on Earth …
in a host of geologic processes and reservoirs, from the mineral-to planetary-scale, on Earth …
Iron and carbon isotope evidence for microbial iron respiration throughout the Archean
PR Craddock, N Dauphas - Earth and Planetary Science Letters, 2011 - Elsevier
Banded Iron-Formations (BIFs) are voluminous chemical sediments that are rich in iron-
oxide, carbonate and silica and whose occurrence is unique to the Precambrian. Their …
oxide, carbonate and silica and whose occurrence is unique to the Precambrian. Their …
First-principles calculations of equilibrium Mg isotope fractionations between garnet, clinopyroxene, orthopyroxene, and olivine: Implications for Mg isotope …
Equilibrium fractionation factors of Mg isotopes at high temperature and pressure are
investigated for pyrope, majorite, clinopyroxene, orthopyroxene, and olivine using density …
investigated for pyrope, majorite, clinopyroxene, orthopyroxene, and olivine using density …