Characterization of porosity in sulfide ore minerals: A USANS/SANS study
-
Fang Xia
, Jing Zhao , Barbara E. Etschmann , Joël Brugger , Christopher J. Garvey , Christine Rehm , Hartmut Lemmel , Jan Ilavsky , Young-Soo Han and Allan Pring
Abstract
Porosity plays a key role in the formation and alteration of sulfide ore minerals, yet our knowledge of the nature and formation of the residual pores is very limited. Herein, we report the application of ultra-small-angle neutron scattering and small-angle neutron scattering (USANS/SANS) to assess the porosity in five natural sulfide minerals (violarite, marcasite, pyrite, chalcopyrite, and bornite) possibly formed by hydrothermal mineral replacement reactions and two synthetic sulfide minerals (violarite and marcasite) prepared experimentally by mimicking natural hydrothermal conditions. USANS/ SANS data showed very different pore size distributions for these minerals. Natural violarite and marcasite tend to possess less pores in the small size range (<100 nm) compared with their synthetic counterparts. This phenomenon is consistent with a higher degree of pore healing or diagenetic compaction experienced by the natural violarite and marcasite. Surprisingly, nanometer-sized (<20 nm) pores were revealed for a natural pyrite cube from La Rioga, Spain, and the sample has a pore volume fraction of ~7.7%. Both chalcopyrite and bornite from the massive sulfide assemblage of the Olympic Dam deposit in Roxby Downs, South Australia, were found to be porous with a similar pore volume fraction (~15%), but chalcopyrite tends to have a higher proportion of nanometer-size pores centered at ~4 nm while bornite tends to have a broader pore size distribution. The specific surface area is generally low for these minerals ranging from 0.94 to 6.28 m2/g, and the surfaces are generally rough as surface fractal behavior was observed for all these minerals. This investigation has demonstrated that USANS/SANS is a very useful tool for analyzing porosity in ore minerals. We believe that with this quantified porosity information a deeper understanding of the complex fluid flow behavior within the porous minerals can be expected.
© 2014 by Walter de Gruyter Berlin/Boston
Articles in the same Issue
- Highlights and Breakthroughs Merrillite and apatite as recorders of planetary magmatic processes
- Highlights and Breakthroughs Comparing clays from Mars and Earth: Implications for martian habitability
- Data-driven abductive discovery in mineralogy
- Thermal expansion of fluorapatite-hydroxylapatite crystalline solutions
- Synthesis and structure of carbonated barium and lead fluorapatites: Effect of cation size on A-type carbonate substitution
- Optical absorption spectroscopy study of the causes for color variations in natural Fe-bearing gahnite: Insights from iron valency and site distribution data
- Si-magnetite nano-precipitates in silician magnetite from banded iron formation: Z-contrast imaging and ab initio study
- Ordering kinetics in synthetic Mg(Al,Fe3+)2O4 spinels: Quantitative elucidation of the whole Al-Mg-Fe partitioning, rate constants, activation energies
- Experimental study of phlogopite reaction rim formation on olivine in phonolite melts: Kinetics, reaction rates, and residence times
- Etch-pit size, dissolution rate, and time in the experimental dissolution of olivine: Implications for estimating olivine lifetime at the surface of Mars
- Ferrian saponite from the Santa Monica Mountains (California, U.S.A., Earth): Characterization as an analog for clay minerals on Mars with application to Yellowknife Bay in Gale Crater
- A large spectral survey of small lunar craters: Implications for the composition of the lunar mantle
- In-situ characterization of oxalic acid breakdown at elevated P and T: Implications for organic C-O-H fluid sources in petrologic experiments
- Slawsonite-celsian-hyalophane assemblage from a picrite sill (Prague Basin, Czech Republic)
- Determining hematite content from NUV/Vis/NIR spectra: Limits of detection
- The role of water in generation of group II kimberlite magmas: Constraints from multiple saturation experiments
- Quantum mechanical modeling of hydrolysis and H2O-exchange in Mg-, Ca-, and Nisilicate clusters: Implications for dissolution mechanisms of olivine minerals
- Redox-driven exsolution of iron-titanium oxides in magnetite in Miller Range (MIL) 03346 nakhlite: Evidence for post crystallization oxidation in the nakhlite cumulate pile?
- Energetics of lanthanide-doped calcium phosphate apatite
- Thermal conductivity of molten and glassy NaAlSi3O8, CaMgSi2O6, and Mg2SiO4 by non-equilibrium molecular dynamics at elevated temperature and pressure
- Energetics of heterometal substitution in ε-Keggin [MO4Al12(OH)24(OH2)12]6/7/8+ ions
- Ab initio calculations of elastic constants of plagioclase feldspars
- Diagenetic formation of interlayer-deficient fluorophlogopite as a clay mineral in Early Cambrian phosphorite (Lesser Himalaya, India): The trioctahedral analog of illite
- Natural sepiolite: Enthalpies of dehydration, dehydroxylation, and formation derived from thermochemical studies
- A new interpretation of decomposition products of serpentine under shock compression
- model for calculating the viscosity of natural iron-bearing silicate melts over a wide range of temperatures, pressures, oxygen fugacites, and compositions
- The replacement of chalcopyrite by bornite under hydrothermal conditions
- Characterization of porosity in sulfide ore minerals: A USANS/SANS study
- Synthesis of a quenchable high-pressure form of magnetite (h-Fe3O4) with composition Fel(Fe2+0.75Mg0.26)Fe2(Fe3+ 0.70Cr0.15Al0.11Si0.04)2O4
- High-pressure elasticity of sodium majorite garnet, Na2MgSi5O12
- Armstrongite from Khan Bogdo (Mongolia): Crystal structure determination and implications for zeolite-like cation exchange properties
- Steinhardtite, a new body-centered-cubic allotropic form of aluminum from the Khatyrka CV3 carbonaceous chondrite
- New Mineral Names
- Book Review
Articles in the same Issue
- Highlights and Breakthroughs Merrillite and apatite as recorders of planetary magmatic processes
- Highlights and Breakthroughs Comparing clays from Mars and Earth: Implications for martian habitability
- Data-driven abductive discovery in mineralogy
- Thermal expansion of fluorapatite-hydroxylapatite crystalline solutions
- Synthesis and structure of carbonated barium and lead fluorapatites: Effect of cation size on A-type carbonate substitution
- Optical absorption spectroscopy study of the causes for color variations in natural Fe-bearing gahnite: Insights from iron valency and site distribution data
- Si-magnetite nano-precipitates in silician magnetite from banded iron formation: Z-contrast imaging and ab initio study
- Ordering kinetics in synthetic Mg(Al,Fe3+)2O4 spinels: Quantitative elucidation of the whole Al-Mg-Fe partitioning, rate constants, activation energies
- Experimental study of phlogopite reaction rim formation on olivine in phonolite melts: Kinetics, reaction rates, and residence times
- Etch-pit size, dissolution rate, and time in the experimental dissolution of olivine: Implications for estimating olivine lifetime at the surface of Mars
- Ferrian saponite from the Santa Monica Mountains (California, U.S.A., Earth): Characterization as an analog for clay minerals on Mars with application to Yellowknife Bay in Gale Crater
- A large spectral survey of small lunar craters: Implications for the composition of the lunar mantle
- In-situ characterization of oxalic acid breakdown at elevated P and T: Implications for organic C-O-H fluid sources in petrologic experiments
- Slawsonite-celsian-hyalophane assemblage from a picrite sill (Prague Basin, Czech Republic)
- Determining hematite content from NUV/Vis/NIR spectra: Limits of detection
- The role of water in generation of group II kimberlite magmas: Constraints from multiple saturation experiments
- Quantum mechanical modeling of hydrolysis and H2O-exchange in Mg-, Ca-, and Nisilicate clusters: Implications for dissolution mechanisms of olivine minerals
- Redox-driven exsolution of iron-titanium oxides in magnetite in Miller Range (MIL) 03346 nakhlite: Evidence for post crystallization oxidation in the nakhlite cumulate pile?
- Energetics of lanthanide-doped calcium phosphate apatite
- Thermal conductivity of molten and glassy NaAlSi3O8, CaMgSi2O6, and Mg2SiO4 by non-equilibrium molecular dynamics at elevated temperature and pressure
- Energetics of heterometal substitution in ε-Keggin [MO4Al12(OH)24(OH2)12]6/7/8+ ions
- Ab initio calculations of elastic constants of plagioclase feldspars
- Diagenetic formation of interlayer-deficient fluorophlogopite as a clay mineral in Early Cambrian phosphorite (Lesser Himalaya, India): The trioctahedral analog of illite
- Natural sepiolite: Enthalpies of dehydration, dehydroxylation, and formation derived from thermochemical studies
- A new interpretation of decomposition products of serpentine under shock compression
- model for calculating the viscosity of natural iron-bearing silicate melts over a wide range of temperatures, pressures, oxygen fugacites, and compositions
- The replacement of chalcopyrite by bornite under hydrothermal conditions
- Characterization of porosity in sulfide ore minerals: A USANS/SANS study
- Synthesis of a quenchable high-pressure form of magnetite (h-Fe3O4) with composition Fel(Fe2+0.75Mg0.26)Fe2(Fe3+ 0.70Cr0.15Al0.11Si0.04)2O4
- High-pressure elasticity of sodium majorite garnet, Na2MgSi5O12
- Armstrongite from Khan Bogdo (Mongolia): Crystal structure determination and implications for zeolite-like cation exchange properties
- Steinhardtite, a new body-centered-cubic allotropic form of aluminum from the Khatyrka CV3 carbonaceous chondrite
- New Mineral Names
- Book Review