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Alkali influence on the water speciation and the environment of protons in silicate glasses revealed by 1H MAS NMR spectroscopy

  • Charles Le Losq EMAIL logo , George D. Cody and Bjorn O. Mysen
Published/Copyright: April 9, 2015
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American Mineralogist
From the journal American Mineralogist Volume 100 Issue 2-3

Abstract

Water can form different chemical bonds with the ionic entities composing silicate melts. Because of that, its influence on the physico-chemical properties of magmas can vary with silicate composition and water content, temperature, and pressure. To further our understanding of how silicate chemical composition governs proton distribution in magmas, the environment of protons in hydrous alkali (Li, Na, K) silicate glasses was varied as a function of the type of alkali metal and total water content. From 1H MAS NMR spectroscopy, H+ are distributed among five different structural environments in alkali silicate glasses. One of these environments is in the form of H2O molecules (H2Omol). The four others are the proton environments associated with Si-OH bonding, and perhaps also with M-OH bonding (with M = Li, Na, or K). Those environments differ in their O-O distance and extent of hydrogen bonding. H2Omol species are located in an environment with an O-O distance of ~290 pm. OH- groups are in environments with O-O distances from 240 to 305 pm. The ionic radius of the alkalis, and hence their ionic field strength, determines the fraction of water dissolved as H2Omol and OH- groups, as well as the distribution of protons in the various OH- environments. The mean volume of the H+ oxygen coordination sphere was calculated using the 1H+ NMR signal intensity and the mean O-O distance around H+. Increasing ionic radius of the alkali metal in silicate glasses results in a decrease of this mean volume. The partial molar volume of water in the corresponding melts determined through other technics seems to vary in a comparable way. Therefore, the chemical composition of silicate melts may control the partial molar volume of dissolved water because of its influence on the structural environment of protons. This probably also plays a role in determining water solubility.

Keywords: Water; silicate glasses; proton solid-state NMR; proton environment
Received: 2014-8-18
Accepted: 2014-4-10
Published Online: 2015-4-9
Published in Print: 2015-2-1

© 2015 by Walter de Gruyter Berlin/Boston

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  1. Anhydrite: An important sulfur binder limiting the climatic impact of subaerial volcanic eruptions
  2. Tweed, twins, and holes
  3. The chemical behavior of fluids released during deep subduction based on fluid inclusions
  4. In situ observation of the pyroxene-majorite transition in Na2MgSi5O12 using synchrotron radiation and Raman spectroscopy of Na-majorite
  5. Prevalence of growth twins among anhedral plagioclase microlites
  6. Intrinsic conditions of magma genesis at the Lunar Crater Volcanic Field (Nevada), and implications for internal plumbing and magma ascent
  7. A rock fragment related to the magnesian suite in lunar meteorite Allan Hills (ALHA) 81005
  8. Trinitite redux: Mineralogy and petrology
  9. Pauloabibite, trigonal NaNbO3, isostructural with ilmenite, from the Jacupiranga carbonatite, Cajati, São Paulo, Brazil
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  14. Carbonate mineralization in percolated olivine aggregates: Linking effects of crystallographic orientation and fluid flow
  15. The catalytic effect of bound extracellular polymeric substances excreted by anaerobic microorganisms on Ca-Mg carbonate precipitation: Implications for the “dolomite problem”
  16. Experimental study along the magnesio-hornblende–glaucophane join
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  18. Stability and adhesion of calcite/montmorillonite assembly
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  27. Balestraite, KLi2VSi4O10O2, the first member of the mica group with octahedral V5+
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  29. Complete substitution of Fe2+ by Mg in Fe4O5: The crystal structure of the Mg2Fe2O5 end-member
  30. The effect of H2O on F and Cl solubility and solution mechanisms of in aluminosilicate melts at high pressure and high temperature
  31. The elasticity of MgAl2O4–MnAl2O4 spinels by Brillouin scattering and an empirical approach for bulk modulus prediction
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https://doi.org/10.2138/am-2015-5004
Keywords for this article
Water; silicate glasses; proton solid-state NMR; proton environment

Articles in the same Issue

  1. Anhydrite: An important sulfur binder limiting the climatic impact of subaerial volcanic eruptions
  2. Tweed, twins, and holes
  3. The chemical behavior of fluids released during deep subduction based on fluid inclusions
  4. In situ observation of the pyroxene-majorite transition in Na2MgSi5O12 using synchrotron radiation and Raman spectroscopy of Na-majorite
  5. Prevalence of growth twins among anhedral plagioclase microlites
  6. Intrinsic conditions of magma genesis at the Lunar Crater Volcanic Field (Nevada), and implications for internal plumbing and magma ascent
  7. A rock fragment related to the magnesian suite in lunar meteorite Allan Hills (ALHA) 81005
  8. Trinitite redux: Mineralogy and petrology
  9. Pauloabibite, trigonal NaNbO3, isostructural with ilmenite, from the Jacupiranga carbonatite, Cajati, São Paulo, Brazil
  10. Kojonenite, a new palladium tin telluride mineral from the Stillwater Layered Igneous Intrusion, Montana, U.S.A.
  11. Cathodoluminescence dependence on feldspar mineral structure and implications for forensic geology
  12. Non-invasive assessment of the formation of tourmaline nodules by X-ray microtomography and computer modeling
  13. Alkali influence on the water speciation and the environment of protons in silicate glasses revealed by 1H MAS NMR spectroscopy
  14. Carbonate mineralization in percolated olivine aggregates: Linking effects of crystallographic orientation and fluid flow
  15. The catalytic effect of bound extracellular polymeric substances excreted by anaerobic microorganisms on Ca-Mg carbonate precipitation: Implications for the “dolomite problem”
  16. Experimental study along the magnesio-hornblende–glaucophane join
  17. Direct observation of Ca-Na ordering and structure polarity in Ca-rich intermediate plagioclase feldspar with incommensurate modulated structure
  18. Stability and adhesion of calcite/montmorillonite assembly
  19. Experimental and modeled chlorine solubilities in aluminosilicate melts at 1 to 7000 bars and 700 to 1250 °C: Applications to magmas of Augustine Volcano, Alaska
  20. Cation order-disorder in Fe-bearing pyrope and grossular garnets: A 27Al and 29Si MAS NMR and 57Fe Mössbauer spectroscopy study
  21. Trace and minor elements in galena: A reconnaissance LA-ICP-MS study
  22. A refined monoclinic structure for a variety of “hydrohematite”
  23. Mössbauer spectroscopic study of natural eosphorite, [(Mn,Fe)AlPO4(OH)2H2O]
  24. P-V-T equation of state of Ca3Cr2Si3O12 uvarovite garnet by using a diamond-anvil cell and in-situ synchrotron X-ray diffraction
  25. Possible new Ca-REE-Bi phosphate minerals from a tungsten-rich calcsilicate skarn, Sierra Nevada Mountains, California
  26. Klebelsbergite, Sb4O4SO4(OH)2: Stability relationships, formation in Nature, and refinement of its structure
  27. Balestraite, KLi2VSi4O10O2, the first member of the mica group with octahedral V5+
  28. Prediction of enthalpies of formation of hydrous sulfates
  29. Complete substitution of Fe2+ by Mg in Fe4O5: The crystal structure of the Mg2Fe2O5 end-member
  30. The effect of H2O on F and Cl solubility and solution mechanisms of in aluminosilicate melts at high pressure and high temperature
  31. The elasticity of MgAl2O4–MnAl2O4 spinels by Brillouin scattering and an empirical approach for bulk modulus prediction
  32. Synthesis of stoichiometric nickel aluminate spinel nanoparticles
  33. New Mineral Names
  34. Book Review
  35. American Mineralogist thanks the year 2014 reviewers
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