Non-bridging oxygen and high-coordinated aluminum in metaluminous and peraluminous calcium and potassium aluminosilicate glasses: High-resolution 17O and 27Al MAS NMR results
Abstract
Change in configuration and structure with composition are important components of thermodynamic and transport properties of most aluminosilicate melts, but the complex interactions, particularly in metaluminous and peraluminous compositions, are not yet well understood. In this paper, we present high-resolution 27Al and 17O MAS and 3QMAS NMR data on several calcium and potassium aluminosilicate glasses prepared at several SiO2 isopleths, ranging from peralkaline to peraluminous compositions. In all calcium aluminosilicate glasses, the VAl content increases with increasing Al content, while the NBO content decreases (in one series, below the limit of detection), consistent with other recent NMR studies of calcium aluminosilicate glasses. An increase in VAl content per total Al is also observed as the glass approaches the calcia-silica binary. In the potassium aluminosilicate glasses, NBO is directly quantified for the first time in metaluminous and peraluminous compositions; VAl is below the detection limit. We discuss possible mechanisms for the incorporation of alumina into the melt structure and show how changes in the VAl content as a function of composition may be used to eliminate mechanisms that do not fit the observed data. We also explore reactions, which show the difficulty of explaining the NBO present on the metaluminous join with only the observed VAl, implying the necessity of multiple reactions producing NBO in such compositions.
© 2015 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
- Comparative in situ X-ray diffraction study of San Carlos olivine: Influence of water on the 410 km seismic velocity jump in Earth’s mantle
- Visualizing trace element distribution in quartz using cathodoluminescence, electron microprobe, and laser ablation-inductively coupled plasma-mass spectrometry
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- Translation interface modulation in NC-pyrrhotites: Direct imaging by TEM and a model toward understanding partially disordered structural states
- Crystal chemistry of Ti-rich fluorophlogopite from Presidente Olegario, Alto Paranaíba igneous province, Brazil
- First-principles study of diffusion and viscosity of anorthite (CaAl2Si2O8) liquid at high pressure
- Aluminous and alkali-deficient tourmaline from the Singhbhum Shear Zone, East Indian shield: Insight for polyphase boron infiltration during regional metamorphism
- Effect of lactate, glycine, and citrate on the kinetics of montmorillonite dissolution
- Acid neutralization by dissolution of alkaline paper mill wastes and implications for treatment of sulfide-mine drainage
- Fast ion conduction character and ionic phase-transition in silver sulfosalts: The case of fettelite [Ag6As2S7][Ag10HgAs2S8]
- Structure of walstromite, BaCa2Si3O9, and its relationship to CaSiO3-walstromite and wollastonite-II
- Cathodoluminescence properties and trace element signature of hydrothermal quartz: A fingerprint of growth dynamics
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- PVT equation of state of epsilon iron and its densities at inner core conditions
- Pressure-induced structural phase transition of the iron end-member of ringwoodite (g-Fe2SiO4) investigated by X-ray diffraction and Mössbauer spectroscopy
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- The crystal structure of δ-Al(OH)3: Neutron diffraction measurements and ab initio calculations
- Electrical properties of natural and synthetic nano-crystalline MgTiO3 geikielite at mantle pressure and temperature conditions
- Density measurement of liquid FeS at high pressures using synchrotron X-ray absorption
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- Ambrinoite, (K,NH4)2(As,Sb)8S13·H2O, a new mineral from Upper Susa Valley, Piedmont, Italy: The first natural (K,NH4)-hydrated sulfosalt
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- Quantitative Raman spectroscopy: Challenges, shortfalls, and solutions—Application to calcium silicate glasses
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