Abstract
The reactions of Au3+ with green rust, stibnite, pyrite, and chalcopyrite were investigated in the laboratory and the size of the gold clusters formed was measured using extended X-ray absorption fine structure (EXAFS) spectroscopy, scanning electron microscopy (SEM), and transmission electron microscopy (TEM). The individual clusters produced were between approximately 29 Å and 77 Å in diameter and may occur individually or as composite clusters from hundreds to thousands of angstroms in size. This work shows that it is possible to form “invisible” gold through reduction of Au3+ by green rust phases and the surfaces of sulfide minerals.
© 2015 by Walter de Gruyter Berlin/Boston
Articles in the same Issue
- TEM study of mullite growth after muscovite breakdown
- The reduction of aqueous Au3+ by sulfide minerals and green rust phases
- Manganoan kinoshitalite in Mn-rich marble and skarn from Virginia
- Expandability of anchizonal illite and chlorite: Significance for crystallinity development in the transition from diagenesis to metamorphism
- X-ray absorption spectroscopy of silicates for in situ, sub-micrometer mineral identification
- Radiation damage in zircon
- Neutron and temperature-resolved synchrotron X-ray powder diffraction study of akaganéite
- Li-rich zincostaurolite and its decompression-related breakdown products in a diaspore-bearing metabauxite from East Samos (Greece): An EMP and SIMS study
- Olivine from planetary basalts: Chemical signatures that indicate planetary parentage and those that record igneous setting and process
- Observations on the relationship between crystallographic orientation and biasing in apatite fission-track measurements
- Borocookeite, a new member of the chlorite group from the Malkhan gem tourmaline deposit, Central Transbaikalia, Russia
- New thermochemical evidence on the stability of dickite vs. kaolinite
- Thermodynamics of Fe oxides: Part I. Entropy at standard temperature and pressure and heat capacity of goethite (α-FeOOH), lepidocrocite (γ-FeOOH), and maghemite (γ-Fe2O3)
- Thermodynamics of Fe oxides: Part II. Enthalpies of formation and relative stability of goethite (α-FeOOH), lepidocrocite (γ-FeOOH), and maghemite (γ-Fe2O3)
- An in situ neutron diffraction study of cation disordering in synthetic qandilite Mg2TiO4 at high temperatures
- Peristeritic plagioclase in North Sea hydrocarbon reservoir rocks: Implications for diagenesis, provenance and stratigraphic correlation
- Incorporation of Ni into natural goethite: An investigation by X-ray absorption spectroscopy
- Characterization of an early metamorphic stage through inclusions in zircon of a diamondiferous quartzofeldspathic rock from the Erzgebirge, Germany
- Gersdorffite (NiAsS) chemical state properties and reactivity toward air and aerated, distilled water
- The concentration and speciation of hydrogen in feldspars using FTIR and 1H MAS NMR spectroscopy
- The significance of mineral inclusions in large diamonds from Yakutia, Russia
- Letters. Evidence from surface phonons for the (2 × 1) reconstruction of the (101̄4) surface of calcite from computer simulation
- Transformation of SiO2 to the amorphous state by shearing at high pressure
Articles in the same Issue
- TEM study of mullite growth after muscovite breakdown
- The reduction of aqueous Au3+ by sulfide minerals and green rust phases
- Manganoan kinoshitalite in Mn-rich marble and skarn from Virginia
- Expandability of anchizonal illite and chlorite: Significance for crystallinity development in the transition from diagenesis to metamorphism
- X-ray absorption spectroscopy of silicates for in situ, sub-micrometer mineral identification
- Radiation damage in zircon
- Neutron and temperature-resolved synchrotron X-ray powder diffraction study of akaganéite
- Li-rich zincostaurolite and its decompression-related breakdown products in a diaspore-bearing metabauxite from East Samos (Greece): An EMP and SIMS study
- Olivine from planetary basalts: Chemical signatures that indicate planetary parentage and those that record igneous setting and process
- Observations on the relationship between crystallographic orientation and biasing in apatite fission-track measurements
- Borocookeite, a new member of the chlorite group from the Malkhan gem tourmaline deposit, Central Transbaikalia, Russia
- New thermochemical evidence on the stability of dickite vs. kaolinite
- Thermodynamics of Fe oxides: Part I. Entropy at standard temperature and pressure and heat capacity of goethite (α-FeOOH), lepidocrocite (γ-FeOOH), and maghemite (γ-Fe2O3)
- Thermodynamics of Fe oxides: Part II. Enthalpies of formation and relative stability of goethite (α-FeOOH), lepidocrocite (γ-FeOOH), and maghemite (γ-Fe2O3)
- An in situ neutron diffraction study of cation disordering in synthetic qandilite Mg2TiO4 at high temperatures
- Peristeritic plagioclase in North Sea hydrocarbon reservoir rocks: Implications for diagenesis, provenance and stratigraphic correlation
- Incorporation of Ni into natural goethite: An investigation by X-ray absorption spectroscopy
- Characterization of an early metamorphic stage through inclusions in zircon of a diamondiferous quartzofeldspathic rock from the Erzgebirge, Germany
- Gersdorffite (NiAsS) chemical state properties and reactivity toward air and aerated, distilled water
- The concentration and speciation of hydrogen in feldspars using FTIR and 1H MAS NMR spectroscopy
- The significance of mineral inclusions in large diamonds from Yakutia, Russia
- Letters. Evidence from surface phonons for the (2 × 1) reconstruction of the (101̄4) surface of calcite from computer simulation
- Transformation of SiO2 to the amorphous state by shearing at high pressure