Jonathan Stebbins
Professor of Geological Sciences, Emeritus
Earth & Planetary Sciences
Academic Appointments
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Emeritus Faculty, Acad Council, Earth & Planetary Sciences
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Affiliate, Precourt Institute for Energy
Administrative Appointments
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Postdoctoral Fellow, Lawrence Berkeley Laboratory (1984 - 1985)
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Assistant Professor of Geology, Stanford University (1985 - 1990)
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Associate Professor of Geology, Stanford University (1990 - 1993)
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Associate Professor Geological & Environmental Sciences, Stanford University (1993 - 1996)
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Associate Dean for Academic Affairs, School of Earth Sciences (1996 - 1999)
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Professor Geological & Environmental Sciences, Stanford University (1996 - Present)
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Professor by Courtesy Materials Science and Engineering, Stanford University (1997 - Present)
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Chariman, Dept. of Geological and Environmental Sciences (1999 - 2004)
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Chairman, Dept. of Geological and Environmental Sciences (2009 - 2012)
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member, University Committee on Postdoctoral Scholars (2009 - 2010)
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member, School of Earth Sciences Council (2012 - 2015)
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member, Faculty Senate Committee on Undergraduate Standard and Policies (C-USP) (2012 - 2014)
Honors & Awards
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Graduate Fellow, National Science Foundation (1977 - 1980)
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Member, National Science Foundation, Presidential Young Investigators (1986-1991)
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Fellow, American Ceramic Society (19--)
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Fellow, American Geophysical Union (19--)
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Fellow, Mineralogical Society of America (1990)
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Mineralogical Society of America Award, Mineralogical Society of America (1992)
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G.W. Morey Award, Glass and Optical Materials Division of the American Ceramic Society (1995)
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Fellow in Undergraduate Education, Bass University (2003-2008)
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Geochemistry Fellow, Geochemical Society and European Association of Geochemistry (2009)
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Bunsen Medal, European Geosciences Union (2009)
Boards, Advisory Committees, Professional Organizations
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Member, School of Earth Sciences Computer Committee, Stanford University (1987 - 1999)
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Associate Editor, American Mineralogist (1990 - 1999)
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Freshman Advisor, Stanford University (1991 - 1999)
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Member, Earth Systems Steering Committee, Stanford University (1991 - 2002)
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Organizer (with D. Dingwell and P. McMillan), MSA Short Course "Structure, Dynamics and Properties of Silicate Melts" (1995 - 1995)
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Councillor, Mineralogical Society of America (1995 - 1997)
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University Undergraduate Advisory Council, Stanford University (1996 - 1999)
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Associate Dean for Academic Affairs, School of Earth Sciences, Stanford University (1996 - 1999)
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Member, Earth Sciences Council, Stanford University (1996 - 2007)
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Faculty Senate, Stanford University (1997 - 1999)
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Chairman, Dept. of Geological & Environmental Sciences, Stanford University (1999 - 2004)
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Invited speaker, International Silicate Melts Workshop (1999 - 1999)
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Invited speaker:, Conference on NMR in Earth Sciences, Cambridge University (2000 - 2000)
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Invited Speaker, Corning Science Fellows Conference; Goldschmidt Conference in Geochemistry; ACS Rocky Mountain Conference on Analytical Chemistry; Varian NMR User's Conference; NSF Workshop on Solid-State Chemistry; Varian, Inc. NMR Group Seminar (2001 - 2001)
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Marsh O'Neill Award Committee, Stanford Univesity (2001 - 2001)
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Member, Materials Council, Stanford University (2002 - 2006)
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Member, Judicial Affairs Board, Stanford University (2002 - 2003)
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Invited Speaker, American Ceramic Society National Meeting; Goldschmidt Conference on Geochemistry; International Mineralogical Association; Virginia Polytechnic Institute (2002 - 2002)
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Invited Speaker, Goldschmidt Conference on Geochemistry (2003 - 2003)
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Invited speaker, American Ceramic Society, Glass and Optical Materials Mtg.; AGU session on melt structure and properties; Plenary lecture: European Conference on Mineralogy and Spectroscopy (2004 - 2004)
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Chairman, School Undergraduate Program Committee, Stanford University (2004 - 2005)
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Invited Speaker, COMPRES workshop on high pressure melts, Albuquerque NM;Saint-Gobaine Glass Research Center, Paris; Centre de Recherche sur les MatÈriaux a Haute Temperature, OrlÈans, France; Symposium on Structure and Properties of Silicate Glasses and Melts, Institut de Physique du Globe de Paris (2005 - 2005)
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Member, NSF review panel (2005 - 2005)
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Invited seminar, Centre de Recherche sur les Matriaux a Haute Temperature, Orleans, France (2005 - 2005)
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Humgrove Lecturer, University of Utrecht (2005 - 2005)
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Invited speaker, European Geophysical Union (2005 - 2005)
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Committee of Visitors, NSF Division of Materials Research (2005 - 2005)
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Plenary speaker, Silicate Melt Workshop, Ludwig-Maximilians-University, Munich (2005 - 2005)
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Guest Editor (with Roberto Moretti and Pascal Richet), Silicate Melts volume of "Chemical Geology" (2005 - 2005)
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Invited speaker, International Mineralogical Association conference; Materials Research Society national meeting (2006 - 2006)
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Guest editor (with G. Henderson and G. Calas), "Glasses and Melts" issue of "Elements" magazine (2006 - 2006)
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Allan Cox Medal committee, Stanford University (2007 - 2007)
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Invited Speaker, Canadian Society of Chemistry annual mtg., 5th Alpine NMR conference, 8th Silicate Melt Workshop, DOE Geofluids Workshop (2007 - 2007)
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Invited Speaker, Rocky Mountain Conference on Analytical Chemistry (2008 - 2008)
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Member, Nanoscale Sciences and Engineering Shared Facilities Program Committee (2008 - Present)
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Chairman, Dept. of Geological and Environmental Sciences, Stanford University (2009 - 2012)
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Member, University Committee on Postdoctoral Scholars, Stanford University (2009 - 2010)
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Invited speaker, European Geosciences Union (Bunsen Medal Lecture); U.C. Davis, Dept. of Geology; PacRim Conference on Ceramic and Glass Technology; Institut de Physique du Globe, Paris; IUPAC Int. Conf. on High Temperature Chemistry (2009 - 2009)
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Invited speaker, Glass and Optical Materials Div., American Ceramic Society, annual mtg.; keynote speaker, Goldschmidt Conference on Geochemistry (2010 - 2010)
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Invited speaker, Glass and Optical Materials Div., American Ceramic Society, annual mtg.; NSF Workshop on Emerging Research in Ceramics, Carbon, Glasses and Composites; Vaughan Symposium, Rocky Mt. Conference on Analytical Chemistry; AGU annual mtg (2012 - 2012)
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keynote speaker, Goldschmidt Conference on Geochemistry; (2012 - 2012)
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Member, School of Earth Sciences Council, Stanford University (2012 - Present)
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Invited Speaker, Corning "Realizing the Vision" symposium (2015 - Present)
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Member, Faculty Senate Committee on Undergraduate Standards and Policy (C-USP), Stanford University (2012 - Present)
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Invited Speaker, Corning Glass Research Summit (2014 - 2014)
Professional Education
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PhD, UC Berkeley, Geology (1983)
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M.A., University of California, Berkeley, Geology (1980)
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A.B., Harvard University, Geological Sciences (1977)
Current Research and Scholarly Interests
Research
My research is focused on the measurement of the structure and dynamics in (mostly) inorganic materials, with the goal of understanding and predicting their thermodynamic and transport properties. These in turn fundamentally control a wide range of geological and technological phenomena. My students, postdocs, and I work primarily on disordered materials, including minerals, glassy and molten silicates and oxides, and ceramics. Our primary research tool is nuclear magnetic resonance (NMR). The materials that we study come from the natural laboratory of the Earth or are synthesized in our own labs. The problems that we address are tied to large-scale processes in geology and geophysics, as well as to those in high-tech industries. Among the former are the mechanisms of viscous flow in magmas and of solid solution in minerals from the crust to the lower mantle; among the latter are the optimization of glasses for flat screen computer displays and optical data transmission and of oxide ceramics for fuel cells.
Teaching
I have long taught a course in introductory geochemistry for undergrads at the beginnings of their careers in Earth sciences. Topics range from the formation of the chemical elements in stellar interiors, to high pressure and temperature phase equilibria, to aqueous solution chemistry, formation of oil and coal, and even the origin of life. At the advanced level I give a course on thermodynamics and structure of minerals and melts aimed at all graduate students who work with these "geomaterials." Recently I have begun teaching a course for advanced undergrads and for grad students on igneous processes.
Professional Activities
Geochemical Society Fellow (2009); European Geosciences Union Bunsen Medal (2009); American Ceramic Society Morey Award (1995); Mineralogical Society of America Award (1992); NSF Presidential Young Investigator (1986-91); associate dean, School of Earth Sciences (1996-1999); chair, GES (1999-2004); participation in professional societies, scientific conferences, and proposal and journal reviews in geochemistry, geophysics, mineralogy, inorganic chemistry, glass science, ceramics, and solid-state NMR
2023-24 Courses
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Independent Studies (4)
- Graduate Independent Study
MATSCI 399 (Aut, Win, Spr, Sum) - Master's Research
MATSCI 200 (Aut, Win, Spr, Sum) - Ph.D. Research
MATSCI 300 (Aut, Win, Spr, Sum) - Practical Training
MATSCI 299 (Aut, Win, Spr, Sum)
- Graduate Independent Study
All Publications
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Evidence for Mixed Mg Coordination Environments in Silicate Glasses: Results from 25Mg NMR Spectroscopy at 35.2 T.
The journal of physical chemistry. B
2023
Abstract
The Mg-O coordination environment of silicate glasses of composition CaMgSi2O6, Na2MgSi3O8, and K2MgSi5O12 is probed using ultrahigh-field (35.2 T) 25Mg magic angle spinning nuclear magnetic resonance (MAS NMR) and triple-quantum MAS NMR spectroscopy. These spectra clearly reveal the coexistence of 4-fold- (MgIV) and 6-fold- (MgVI) coordinated Mg in all glasses. The MgIV/MgVI ratio implies an average Mg-O coordination number of ∼5 for CaMgSi2O6 glass, bringing NMR results for the first time in good agreement with those reported in previous studies based on diffraction and X-ray absorption spectroscopy, thus resolving a decade-long controversy regarding Mg coordination in alkaline-earth silicate glasses. The Mg-O coordination number decreases to ∼4.5 in the alkali-Mg silicate glasses, indicating that Mg competes effectively with the low field strength alkali cations for the nonbridging oxygen in the structure to attain tetrahedral coordination. This work illustrates the promise of ultrahigh-field NMR spectroscopy in structural studies involving nuclides with low gyromagnetic ratio.
View details for DOI 10.1021/acs.jpcb.3c06419
View details for PubMedID 38032847
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Germanate anomaly and its temperature dependence: An ultra-high field 17O NMR spectroscopic study of sodium germanate glasses
JOURNAL OF NON-CRYSTALLINE SOLIDS-X
2023; 18
View details for DOI 10.1016/j.nocx.2023.100175
View details for Web of Science ID 001208981800011
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Templated encapsulation of platinum-based catalysts promotes high-temperature stability to 1,100°C.
Nature materials
2022
Abstract
Stable catalysts are essential to address energy and environmental challenges, especially for applications in harsh environments (for example, high temperature, oxidizing atmosphere and steam). In such conditions, supported metal catalysts deactivate due to sintering-a process where initially small nanoparticles grow into larger ones with reduced active surface area-but strategies to stabilize them can lead to decreased performance. Here we report stable catalysts prepared through the encapsulation of platinum nanoparticles inside an alumina framework, which was formed by depositing an alumina precursor within a separately prepared porous organic framework impregnated with platinum nanoparticles. These catalysts do not sinter at 800°C in the presence of oxygen and steam, conditions in which conventional catalysts sinter to a large extent, while showing similar reaction rates. Extending this approach to Pd-Pt bimetallic catalysts led to the small particle size being maintained at temperatures as high as 1,100°C in air and 10% steam. This strategy can be broadly applied to other metal and metal oxides for applications where sintering is a major cause of material deactivation.
View details for DOI 10.1038/s41563-022-01376-1
View details for PubMedID 36280703
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Monolayer Support Control and Precise Colloidal Nanocrystals Demonstrate Metal-Support Interactions in Heterogeneous Catalysts.
Advanced materials (Deerfield Beach, Fla.)
2021: e2104533
Abstract
Electronic and geometric interactions between active and support phases are critical in determining the activity of heterogeneous catalysts, but metal-support interactions are challenging to study. Here, it is demonstrated how the combination of the monolayer-controlled formation using atomic layer deposition (ALD) and colloidal nanocrystal synthesis methods leads to catalysts with sub-nanometer precision of active and support phases, thus allowing for the study of the metal-support interactions in detail. The use of this approach in developing a fundamental understanding of support effects in Pd-catalyzed methane combustion is demonstrated. Uniform Pd nanocrystals are deposited onto Al2 O3 /SiO2 spherical supports prepared with control over morphology and Al2 O3 layer thicknesses ranging from sub-monolayer to a 4nm thick uniform coating. Dramatic changes in catalytic activity depending on the coverage and structure of Al2 O3 situated at the Pd/Al2 O3 interface are observed, with even a single monolayer of alumina contributing an order of magnitude increase in reaction rate. By building the Pd/Al2 O3 interface up layer-by-layer and using uniform Pd nanocrystals, this work demonstrates the importance of controlled and tunable materials in determining metal-support interactions and catalyst activity.
View details for DOI 10.1002/adma.202104533
View details for PubMedID 34535919
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Composition and pressure effects on the structure, elastic properties and hardness of aluminoborosilicate glass
JOURNAL OF NON-CRYSTALLINE SOLIDS
2020; 530
View details for DOI 10.1016/j.jnoncrysol.2019.119797
View details for Web of Science ID 000513989300013
- Anionic speciation in sodium and potassium silicate glasses near the metasilicate ([Na,K]2SiO3) composition: 29Si, 17O, and 23Na NMR. J. Non-Cryst. Solids: X 2020; 6: 1000491-12
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Tuning the bandgap of Cs2AgBiBr6 through dilute tin alloying.
Chemical science
2019; 10 (45): 10620-10628
Abstract
The promise of lead halide hybrid perovskites for optoelectronic applications makes finding less-toxic alternatives a priority. The double perovskite Cs2AgBiBr6 (1) represents one such alternative, offering long carrier lifetimes and greater stability under ambient conditions. However, the large and indirect 1.95 eV bandgap hinders its potential as a solar absorber. Here we report that alloying crystals of 1 with up to 1 atom% Sn results in a bandgap reduction of up to ca. 0.5 eV while maintaining low toxicity. Crystals can be alloyed with up to 1 atom% Sn and the predominant substitution pathway appears to be a ∼2 : 1 substitution of Sn2+ and Sn4+ for Ag+ and Bi3+, respectively, with Ag+ vacancies providing charge compensation. Spincoated films of 1 accommodate a higher Sn loading, up to 4 atom% Sn, where we see mostly Sn2+ substitution for both Ag+ and Bi3+. Density functional theory (DFT) calculations ascribe the bandgap redshift to the introduction of Sn impurity bands below the conduction band minimum of the host lattice. Using optical absorption spectroscopy, photothermal deflection spectroscopy, X-ray absorption spectroscopy, 119Sn NMR, redox titration, single-crystal and powder X-ray diffraction, multiple elemental analysis and imaging techniques, and DFT calculations, we provide a detailed analysis of the Sn content and oxidation state, dominant substitution sites, and charge-compensating defects in Sn-alloyed Cs2AgBiBr6 (1:Sn) crystals and films. An understanding of heterovalent alloying in halide double perovskites opens the door to a wider breadth of potential alloying agents for manipulating their band structures in a predictable manner.
View details for DOI 10.1039/c9sc02581b
View details for PubMedID 32110348
View details for PubMedCentralID PMC7020786
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Tuning the bandgap of Cs2AgBiBr6 through dilute tin alloying
CHEMICAL SCIENCE
2019; 10 (45): 10620–28
View details for DOI 10.1039/c9sc02581b
View details for Web of Science ID 000498611100018
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Pentacoordinated and hexacoordinated silicon cations in a potassium silicate glass: Effects of pressure and temperature
JOURNAL OF NON-CRYSTALLINE SOLIDS
2019; 505: 234–40
View details for DOI 10.1016/j.jnoncrysol.2018.11.001
View details for Web of Science ID 000459643000028
- Pentacoordinated silicon in ambient pressure potassium and lithium silicate glasses: temperature and compositional effects and analogies to alkali borate and germanate systems J. Non-Cryst. Solids: X 2019; 1: 100012-1-12
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Toward the wider application of Si-29 NMR spectroscopy to paramagnetic transition metal silicate minerals and glasses: Fe(II), Co(II), and Ni(II) silicates
AMERICAN MINERALOGIST
2018; 103 (5): 776–91
View details for DOI 10.2138/am-2018-6370
View details for Web of Science ID 000431122500010
- NMR at high temperature Modern Methods in Solids State NMR: A Practitioner's Guide edited by Hodgkinson, P. 2018
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Structural changes in calcium aluminoborosilicate glasses recovered from pressures of 1.5 to 3 GPa: Interactions of two network species with coordination number increases
JOURNAL OF NON-CRYSTALLINE SOLIDS
2017; 478: 50–57
View details for DOI 10.1016/j.jnoncrysol.2017.09.053
View details for Web of Science ID 000414890600007
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Toward the wider application of Si-29 NMR spectroscopy to paramagnetic transition metal silicate minerals: Copper(II) silicates
AMERICAN MINERALOGIST
2017; 102 (12): 2406–14
View details for DOI 10.2138/am-2017-6176
View details for Web of Science ID 000417990500005
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Bond length-bond angle correlation in densified silica-Results from O-17 NMR spectroscopy
JOURNAL OF CHEMICAL PHYSICS
2017; 146 (18)
View details for DOI 10.1063/1.4983041
View details for Web of Science ID 000401368900027
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Solid-state NMR and short-range order in crystalline oxides and silicates: a new tool in paramagnetic resonances.
Acta crystallographica. Section C, Structural chemistry
2017; 73: 128-136
Abstract
Most applications of high-resolution NMR to questions of short-range order/disorder in inorganic materials have been made in systems where ions with unpaired electron spins are of negligible concentration, with structural information extracted primarily from chemical shifts, quadrupolar coupling parameters, and nuclear dipolar couplings. In some cases, however, the often-large additional resonance shifts caused by interactions between unpaired electron and nuclear spins can provide unique new structural information in materials with contents of paramagnetic cations ranging from hundreds of ppm to several per cent and even higher. In this brief review we focus on recent work on silicate, phosphate, and oxide materials with relatively low concentrations of paramagnetic ions, where spectral resolution can remain high enough to distinguish interactions between NMR-observed nuclides and one or more magnetic neighbors in different bonding configurations in the first, second, and even farther cation shells. We illustrate the types of information available, some of the limitations of this approach, and the great prospects for future experimental and theoretical work in this field. We give examples for the effects of paramagnetic transition metal, lanthanide, and actinide cation substitutions in simple oxides, pyrochlore, zircon, monazite, olivine, garnet, pyrochlores, and olivine structures.
View details for DOI 10.1107/S2053229616015606
View details for PubMedID 28257006
- Constraints on aluminum and scandium substitution mechanisms in forsterite, periclase, and larnite: high resolution NMR American Mineralogist 2017; 102: 1244-1253
- Multinuclear NMR investigation of temperature effects on structural reactions involving non-bridging oxygens in multicomponent oxide glasses JOURNAL OF NON-CRYSTALLINE SOLIDS 2017; 471: 179-186
- The role of modifier cations in network modifier cation coordination increases with pressure in aluminosilicate glasses and melts from 1 to 3 GPa Am Mineral. 2017; 102: 1657-1666
- Structural investigation of hydrous sodium borosilicate glasses j. Non-Cryst. Solids 2017; 465: 39-48
- “Free” oxide ions in silicate melts: thermodynamic considerations and probable effects of temperature Chemical Geology 2017; 461: 2-12
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Investigating lanthanide dopant distributions in Yttrium Aluminum Garnet (YAG) using solid state paramagnetic NMR.
Solid state nuclear magnetic resonance
2016; 79: 11-22
Abstract
This paper demonstrates the approach of using paramagnetic effects observed in NMR spectra to investigate the distribution of lanthanide dopant cations in YAG (yttrium aluminum garnet, Y3Al5O12) optical materials, as a complimentary technique to optical spectroscopy and other standard methods of characterization. We investigate the effects of Ce(3+), Nd(3+), Yb(3+), Tm(3+), and Tm(3+)-Cr(3+) on (27)Al and (89)Y NMR spectra. We note shifted resonances for both AlO4 and AlO6 sites. In some cases, multiple shifted peaks are observable, and some of these can be empirically assigned to dopant cations in known configurations to the observed nuclides. In many cases, AlO6 peaks shifted by more than one magnetic neighbor can be detected. In general, we observe that the measured intensities of shifted resonances, when spinning sidebands are included, are consistent with predictions from models with dopant cations that are randomly distributed throughout the lattice. In at least one set of (27)Al spectra, we identify two sub-peaks possibly resulting from two paramagnetic cations with magnetically coupled spin states neighboring the observed nucleus. We identify systematic changes in the spectra related to known parameters describing the magnetic effects of lanthanide cations, such as larger shift distances when the expectation value of electron spins is greater. We lastly comment on the promise of this technique in future analyses of laser and other crystalline oxide materials.
View details for DOI 10.1016/j.ssnmr.2016.10.001
View details for PubMedID 27794215
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Network oxygen sites in calcium aluminoborosilicate glasses: Results from O-17{Al-27} and O-17{B-11} double resonance NMR
JOURNAL OF NON-CRYSTALLINE SOLIDS
2016; 447: 248-254
View details for DOI 10.1016/j.jnoncrysol.2016.06.024
View details for Web of Science ID 000381841200037
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Detection of "free" oxide ions in low-silica Ca/Mg silicate glasses:. Results from O-17 -> Si-29 HETCOR NMR
JOURNAL OF NON-CRYSTALLINE SOLIDS
2016; 445: 1-6
View details for DOI 10.1016/j.jnoncrysol.2016.04.042
View details for Web of Science ID 000379560100001
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Transition Metal Dopant Cation Distributions in MgO and CaO: New Inferences from Paramagnetically Shifted Resonances in O-17, Mg-25, and Ca-43 NMR Spectra
JOURNAL OF PHYSICAL CHEMISTRY C
2016; 120 (20): 11111-11120
View details for DOI 10.1021/acs.jpcc.6b02710
View details for Web of Science ID 000376840900043
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Order, disorder and mixing: The atomic structure of amorphous mixtures of titania and tantala
JOURNAL OF NON-CRYSTALLINE SOLIDS
2016; 438: 59-66
View details for DOI 10.1016/j.jnoncrysol.2016.02.009
View details for Web of Science ID 000373545300008
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Glass structure, melt structure, and dynamics: Some concepts for petrology
AMERICAN MINERALOGIST
2016; 101 (3-4): 753-768
View details for DOI 10.2138/am-2016-5386
View details for Web of Science ID 000374626100022
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Response of complex networks to compression: Ca, La, and Y aluminoborosilicate glasses formed from liquids at 1 to 3 GPa pressures.
journal of chemical physics
2016; 144 (4): 044502-?
Abstract
Aluminoborosilicate glasses containing relatively high field strength modifiers (Ca, La, and Y) have been compressed at pressures up to 3 GPa and near the glass transition temperature (Tg) and quenched to room temperature at high pressure followed by decompression. Structural changes were quantified with high-resolution (27)Al and (11)B MAS nuclear magnetic resonance at 14.1-18.8 T. The changes with pressure in Al and B coordinations in the recovered samples are quite large with more than 50% decreases in tetrahedral aluminum ((IV)Al) and 200%-300% increases in tetrahedral boron ((IV)B). Glasses with higher field strength modifiers (La and Y) contain more high coordinated aluminum ((V,V I)Al) at all pressures studied. More high coordinated boron also correlates with higher field strength modifier if all three compositions are compared on an isothermal basis. Although lowering fictive temperature and increasing pressure both increase Al and B coordinations, our study shows that the actual mechanisms for structural changes are most probably different for temperature and pressure effects. Using a rough thermodynamic model to extrapolate to higher pressures, it appears that a simple non-bridging oxygen (NBO) consumption mechanism is not sufficient to convert all the aluminum to octahedral and boron to tetrahedral coordination, suggesting other mechanisms for structural changes could occur at high pressure as NBO becomes depleted.
View details for DOI 10.1063/1.4940691
View details for PubMedID 26827221
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Separating the effects of composition and fictive temperature on Al and B coordination in Ca, La, Y aluminosilicate, aluminoborosilicate and aluminoborate glasses
JOURNAL OF NON-CRYSTALLINE SOLIDS
2016; 432: 384-392
View details for DOI 10.1016/j.jnoncrysol.2015.10.035
View details for Web of Science ID 000367769300028
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Structure of amorphous silica-hafnia and silica-zirconia thin-film materials: The role of a metastable equilibrium state in non-glass-forming oxide systems
JOURNAL OF NON-CRYSTALLINE SOLIDS
2015; 429: 5-12
View details for DOI 10.1016/j.jnoncrysol.2015.08.030
View details for Web of Science ID 000365055300002
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Tricluster oxygen atoms in crystalline and glassy SrB4O7: High resolution B-11 and O-17 nuclear magnetic resonance analysis
JOURNAL OF NON-CRYSTALLINE SOLIDS
2015; 428: 105-111
View details for DOI 10.1016/j.jnoncrysol.2015.08.014
View details for Web of Science ID 000363345200016
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Aluminosilicate melts and glasses at 1 to 3 GPa: Temperature and pressure effects on recovered structural and density changes
AMERICAN MINERALOGIST
2015; 100 (10): 2298-2307
View details for DOI 10.2138/am-2015-5258
View details for Web of Science ID 000362694600028
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An investigation of local Fe2+ order-disorder in a mantle grospydite garnet using paramagnetically shifted Al-27 and Si-29 MAS NMR resonances
EUROPEAN JOURNAL OF MINERALOGY
2015; 27 (4): 463-470
View details for DOI 10.1127/ejm/2015/0027-2448
View details for Web of Science ID 000358821100001
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Transition metal cation site preferences in forsterite (Mg2SiO4) determined from paramagnetically shifted NMR resonances
AMERICAN MINERALOGIST
2015; 100 (5-6): 1265-1276
View details for DOI 10.2138/am-2015-5150
View details for Web of Science ID 000354665700029
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Order within disorder: The atomic structure of ion-beam sputtered amorphous tantala (a-Ta2O5)
APL MATERIALS
2015; 3 (3)
View details for DOI 10.1063/1.4913586
View details for Web of Science ID 000352450200004
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Cation order-disorder in Fe-bearing pyrope and grossular garnets: A Al-27 and Si-29 MAS NMR and Fe-57 Mossbauer spectroscopy study
AMERICAN MINERALOGIST
2015; 100 (2-3): 536-547
View details for DOI 10.2138/am-2015-5062
View details for Web of Science ID 000350096600020
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The structure of ion beam sputtered amorphous alumina films and effects of Zn doping: High-resolution Al-27 NMR
JOURNAL OF NON-CRYSTALLINE SOLIDS
2014; 405: 1-6
View details for DOI 10.1016/j.jnoncrysol.2014.08.022
View details for Web of Science ID 000347266400001
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Cation Field Strength Effects on Boron Coordination in Binary Borate Glasses
JOURNAL OF THE AMERICAN CERAMIC SOCIETY
2014; 97 (9): 2794-2801
View details for DOI 10.1111/jace.13100
View details for Web of Science ID 000341826500017
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Modifier cation (Ba, Ca, La, Y) field strength effects on aluminum and boron coordination in aluminoborosilicate glasses: the roles of fictive temperature and boron content
APPLIED PHYSICS A-MATERIALS SCIENCE & PROCESSING
2014; 116 (2): 479-490
View details for DOI 10.1007/s00339-014-8369-4
View details for Web of Science ID 000339337200007
- NMR spectroscopy in inorganic Earth materials Spectroscopic Methods in Mineralogy and Materials Sciences edited by Henderson, G. S., Neuville, D., Downs, R. T. Mineralogical Society of America. 2014: 605–653
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(31)P magic angle spinning NMR study of flux-grown rare-Earth element orthophosphate (monazite/xenotime) solid solutions: evidence of random cation distribution from paramagnetically shifted NMR resonances.
Inorganic chemistry
2013; 52 (21): 12605-12615
Abstract
We present (31)P magic angle spinning nuclear magnetic resonance spectra of flux-grown solid solutions of La(1-x)Ce(x)PO4 (x between 0.027 and 0.32) having the monoclinic monazite structure, and of Y(1-x)M(x)PO4 (M = V(n+), Ce(3+), Nd(3+), x between 0.001 and 0.014) having the tetragonal zircon structure. Paramagnetically shifted NMR resonances are observed in all samples due to the presence of paramagnetic V(n+), Ce(3+), and Nd(3+) in the diamagnetic LaPO4 or YPO4. As a first-order observation, the number and relative intensities of these peaks are related to the symmetry and structure of the diamagnetic host phase. The presence of paramagnetic shifts allows for increased resolution between NMR resonances for distinct atomic species which leads to the observation of low intensity peaks related to PO4 species having more than one paramagnetic neighbor two or four atomic bonds away. Through careful analysis of peak areas and comparison with predictions for simple models, it was determined that solid solutions in the systems examined here are characterized by complete disorder (random distribution) of diamagnetic La(3+) or Y(3+) with the paramagnetic substitutional species Ce(3+) and Nd(3+). The increased resolution given by the paramagnetic interactions also leads to the observation of splitting of specific resonances in the (31)P NMR spectra that may be caused by local, small-scale distortions from the substitution of ions having dissimilar ionic radii.
View details for DOI 10.1021/ic401757z
View details for PubMedID 24131129
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Interaction between composition and temperature effects on non-bridging oxygen and high-coordinated aluminum in calcium aluminosilicate glasses
AMERICAN MINERALOGIST
2013; 98 (11-12): 1980-1987
View details for DOI 10.2138/am.2013.4511
View details for Web of Science ID 000327049100008
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Effects of annealing on the structure of ion beam sputtered amorphous tantalum oxide: Oxygen-17 NMR spectra and relaxation times
JOURNAL OF NON-CRYSTALLINE SOLIDS
2013; 378: 158-162
View details for DOI 10.1016/j.jnoncrysol.2013.07.003
View details for Web of Science ID 000327279800025
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Tunable plasticity in amorphous silicon carbide films.
ACS applied materials & interfaces
2013; 5 (16): 7950-7955
Abstract
Plasticity plays a crucial role in the mechanical behavior of engineering materials. For instance, energy dissipation during plastic deformation is vital to the sufficient fracture resistance of engineering materials. Thus, the lack of plasticity in brittle hybrid organic-inorganic glasses (hybrid glasses) often results in a low fracture resistance and has been a significant challenge for their integration and applications. Here, we demonstrate that hydrogenated amorphous silicon carbide films, a class of hybrid glasses, can exhibit a plasticity that is even tunable by controlling their molecular structure and thereby leads to an increased and adjustable fracture resistance in the films. We decouple the plasticity contribution from the fracture resistance of the films by estimating the "work-of-fracture" using a mean-field approach, which provides some insight into a potential connection between the onset of plasticity in the films and the well-known rigidity percolation threshold.
View details for DOI 10.1021/am402046e
View details for PubMedID 23876200
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Interactions between network cation coordination and non-bridging oxygen abundance in oxide glasses and melts: Insights from NMR spectroscopy
CHEMICAL GEOLOGY
2013; 346: 34-46
View details for DOI 10.1016/j.chemgeo.2012.09.021
View details for Web of Science ID 000319639900005
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Oxide ion speciation in potassium silicate glasses: New limits from O-17 NMR
JOURNAL OF NON-CRYSTALLINE SOLIDS
2013; 368: 17-22
View details for DOI 10.1016/j.jnoncrysol.2013.02.024
View details for Web of Science ID 000319103700002
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Temperature and modifier cation field strength effects on aluminoborosilicate glass network structure
JOURNAL OF NON-CRYSTALLINE SOLIDS
2013; 362: 73-81
View details for DOI 10.1016/j.jnoncrysol.2012.11.005
View details for Web of Science ID 000315935500013
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Challenges in Ceramic Science: A Report from the Workshop on Emerging Research Areas in Ceramic Science
JOURNAL OF THE AMERICAN CERAMIC SOCIETY
2012; 95 (12): 3699-3712
View details for DOI 10.1111/jace.12033
View details for Web of Science ID 000312145600001
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Estimating accuracy of O-17 NMR measurements in oxide glasses: Constraints and evidence from crystalline and glassy calcium and barium silicates
JOURNAL OF NON-CRYSTALLINE SOLIDS
2012; 358 (22): 2999-3006
View details for DOI 10.1016/j.jnoncrysol.2012.07.032
View details for Web of Science ID 000310047100011
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Incorporation of Fe and Al in MgSiO3 perovskite: An investigation by Al-27 and Si-29 NMR spectroscopy
AMERICAN MINERALOGIST
2012; 97 (11-12): 1955-1964
View details for DOI 10.2138/am.2012.4101
View details for Web of Science ID 000311066600016
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Properties of impurity-bearing ferrihydrite I. Effects of Al content and precipitation rate on the structure of 2-line ferrihydrite
GEOCHIMICA ET COSMOCHIMICA ACTA
2012; 92: 275-291
View details for DOI 10.1016/j.gca.2012.06.010
View details for Web of Science ID 000307885900019
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Non-stoichiometric non-bridging oxygens and five-coordinated aluminum in alkaline earth aluminosilicate glasses: Effect of modifier cation size
JOURNAL OF NON-CRYSTALLINE SOLIDS
2012; 358 (15): 1783-1789
View details for DOI 10.1016/j.jnoncrysol.2012.05.022
View details for Web of Science ID 000307028900011
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Natural hydrous amorphous silica: Quantitation of network speciation and hydroxyl content by Si-29 MAS NMR and vibrational spectroscopy
AMERICAN MINERALOGIST
2012; 97 (1): 203-211
View details for DOI 10.2138/am.2012.3921
View details for Web of Science ID 000298893400020
- Quadrupolar NMR in the Earth Sciences NMR of Quadrupolar Nuclei in Solid Materials, and Encyclopedia of Magnetic Resonance (online publication) edited by Wasylishen, R. E., Ashbrook, S. E., Wimperis, S. John Wiley & Sons, Ltd.. 2012: 387–400
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High-temperature in situ B-11 NMR study of network dynamics in boron-containing glass-forming liquids
JOURNAL OF NON-CRYSTALLINE SOLIDS
2011; 357 (24): 3944-3951
View details for DOI 10.1016/j.jnoncrysol.2011.08.013
View details for Web of Science ID 000296269300011
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Temperature calibration for high-temperature MAS NMR to 913 K: Cu-63 MAS NMR of CuBr and CuI, and Na-23 MAS NMR of NaNbO3
SOLID STATE NUCLEAR MAGNETIC RESONANCE
2011; 40 (2): 45-50
Abstract
The solid-state phase transitions of CuBr, CuI and NaNbO(3) can be readily observed using (63)Cu and (23)Na high-temperature magic-angle spinning nuclear magnetic resonance spectroscopy. Temperature has large, linear effects on the peak maximum of (63)Cu in each solid phase of CuBr and CuI, and there is large jump in shift across each phase transition. The (23)Na MAS NMR peak intensities and the line widths in NaNbO(3) also clearly show its high-temperature transition to the cubic phase. These data can be used to calibrate high-temperature MAS NMR probes up to 913 K, which is two hundred degrees higher than the commonly-used temperature calibration based on the chemical shift of (207)Pb in Pb(NO(3))(2).
View details for DOI 10.1016/j.ssnmr.2011.04.004
View details for Web of Science ID 000295020700003
View details for PubMedID 21546224
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Structure of Amorphous Tantalum Oxide and Titania-Doped Tantala: O-17 NMR Results for Sol-Gel and Ion-Beam-Sputtered Materials
CHEMISTRY OF MATERIALS
2011; 23 (15): 3460-3465
View details for DOI 10.1021/cm200630m
View details for Web of Science ID 000293357100010
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Paramagnetic interactions in the P-31 NMR spectroscopy of rare earth element orthophosphate (REPO4, monazite/xenotime) solid solutions
AMERICAN MINERALOGIST
2011; 96 (8-9): 1343-1353
View details for DOI 10.2138/am.2011.3816
View details for Web of Science ID 000293993500018
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Variable-temperature Al-27 and Si-29 NMR studies of synthetic forsterite and Fe-bearing Dora Maira pyrope garnet: Temperature dependence and mechanisms of paramagnetically shifted peaks
AMERICAN MINERALOGIST
2011; 96 (7): 1090-1099
View details for DOI 10.2138/am.2011.3686
View details for Web of Science ID 000292372400014
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Raman, Brillouin, and nuclear magnetic resonance spectroscopic studies on shocked borosilicate glass
JOURNAL OF APPLIED PHYSICS
2011; 109 (11)
View details for DOI 10.1063/1.3592346
View details for Web of Science ID 000292214700030
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Non-bridging oxygen and high-coordinated aluminum in metaluminous and peraluminous calcium and potassium aluminosilicate glasses: High-resolution O-17 and Al-27 MAS NMR results
AMERICAN MINERALOGIST
2011; 96 (5-6): 841-853
View details for DOI 10.2138/am.2011.3680
View details for Web of Science ID 000290605300017
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Quench rate and temperature effects on boron coordination in aluminoborosilicate melts
JOURNAL OF NON-CRYSTALLINE SOLIDS
2010; 356 (41-42): 2097-2108
View details for DOI 10.1016/j.jnoncrysol.2010.08.015
View details for Web of Science ID 000283475800003
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Silicon coordination in rutile and TiO2-II at ambient and high pressures: Si-29 NMR
AMERICAN MINERALOGIST
2010; 95 (7): 968-973
View details for DOI 10.2138/am.2010.3491
View details for Web of Science ID 000279737700009
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Probing the electrical properties of highly-doped Al:ZnO nanowire ensembles
JOURNAL OF APPLIED PHYSICS
2010; 107 (7)
View details for DOI 10.1063/1.3360930
View details for Web of Science ID 000276795400081
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Effects of e-beam curing on glass structure and mechanical properties of nanoporous organosilicate thin films
INTERNATIONAL JOURNAL OF MATERIALS RESEARCH
2010; 101 (2): 228-235
View details for DOI 10.3139/146.110275
View details for Web of Science ID 000275653100008
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Structural response of a highly viscous aluminoborosilicate melt to isotropic and anisotropic compressions
JOURNAL OF CHEMICAL PHYSICS
2009; 131 (10)
View details for DOI 10.1063/1.3223282
View details for Web of Science ID 000269814800030
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Simultaneous aluminum, silicon, and sodium coordination changes in 6 GPa sodium aluminosilicate glasses
AMERICAN MINERALOGIST
2009; 94 (8-9): 1205-1215
View details for DOI 10.2138/am.2009.3177
View details for Web of Science ID 000269093200013
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Cation field strength effects on high pressure aluminosilicate glass structure: Multinuclear NMR and La XAFS results
GEOCHIMICA ET COSMOCHIMICA ACTA
2009; 73 (13): 3914-3933
View details for DOI 10.1016/j.gca.2009.03.040
View details for Web of Science ID 000267229800014
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Forsterite, hydrous and anhydrous wadsleyite and ringwoodite (Mg2SiO4): Si-29 NMR results for chemical shift anisotropy, spin-lattice relaxation, and mechanism of hydration
AMERICAN MINERALOGIST
2009; 94 (7): 905-915
View details for DOI 10.2138/am.2009.3184
View details for Web of Science ID 000268149400005
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Confirmation of octahedrally coordinated phosphorus in AlPO4-containing stishovite by P-31 NMR
EUROPEAN JOURNAL OF MINERALOGY
2009; 21 (4): 667-671
View details for DOI 10.1127/0935-1221/2009/0021-1953
View details for Web of Science ID 000270166000001
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Effects of cation field strength on the structure of aluminoborosilicate glasses: High-resolution B-11, Al-27 and Na-23 MAS NMR
JOURNAL OF NON-CRYSTALLINE SOLIDS
2009; 355 (9): 556-562
View details for DOI 10.1016/j.jnoncrysol.2009.01.025
View details for Web of Science ID 000265991400007
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Forsterite, wadsleyite, and ringwoodite (Mg2SiO4): Si-29 NMR constraints on structural disorder and effects of paramagnetic impurity ions
AMERICAN MINERALOGIST
2009; 94 (4): 626-629
View details for DOI 10.2138/am.2009.3140
View details for Web of Science ID 000265157000023
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Effects of the degree of polymerization on the structure of sodium silicate and aluminosilicate glasses and melts: An O-17 NMR study
GEOCHIMICA ET COSMOCHIMICA ACTA
2009; 73 (4): 1109-1119
View details for DOI 10.1016/j.gca.2008.10.040
View details for Web of Science ID 000263633300016
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Sc-2(WO4)(3) and Sc-2(MoO4)(3) and Their Solid Solutions: Sc-45, O-17, and Al-27 MAS NMR Results at Ambient and High Temperature
CHEMISTRY OF MATERIALS
2009; 21 (2): 309-315
View details for DOI 10.1021/cm8024632
View details for Web of Science ID 000262605200019
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THE DIVERSITY OF NUCLEAR MAGNETIC RESONANCE SPECTROSCOPY
NATO Advanced Study Institute on Biophysics and the Challenges of Emerging Threats
SPRINGER. 2009: 65–81
View details for Web of Science ID 000267755300005
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Characterization of Phase Separation and Thermal History Effects in Magnesium Silicate Glass Fibers by Nuclear Magnetic Resonance Spectroscopy
JOURNAL OF THE AMERICAN CERAMIC SOCIETY
2009; 92 (1): 68-74
View details for DOI 10.1111/j.1551-2916.2008.02844.x
View details for Web of Science ID 000262229500012
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Anomalous resonances in Si-29 and Al-27 NMR spectra of pyrope ([Mg,Fe](3)Al2Si3O12) garnets: effects of paramagnetic cations
PHYSICAL CHEMISTRY CHEMICAL PHYSICS
2009; 11 (32): 6906-6917
Abstract
In oxide and silicate materials, particularly naturally-occurring minerals with contents of iron oxides greater than a few percent, paramagnetic impurities are well-known to broaden MAS NMR peaks, decrease relaxation times, and even cause overall loss of signal intensity. However, detection of resolved, discrete peaks that are shifted in frequency by nearby unpaired electron spins is rare in such systems. We report here high-resolution (27)Al and (29)Si spectra for synthetic and natural samples of pyrope garnet ([Mg,Fe](3)Al(2)Si(3)O(12)), the latter containing up to 3.5 wt% FeO. For both nuclides, spectra contain anomalous NMR peaks at frequencies that are 25 to 200 ppm from normal ranges, possibly through pseudocontact shifts induced by paramagnetic cations. Quantitation of peak areas suggests that signals from nuclides with such cations in their first shell may be broadened enough to be unobservable, while those with paramagnetics in their second cation shells may be substantially shifted. Overall spin-lattice relaxation rates are greatly enhanced by such impurities, and shifted resonances relax much faster than the unshifted main peaks. A high symmetry crystal structure (in this case cubic), which limits the number of different cation-cation distances in each shell, combined with a relatively low (non-cubic) symmetry for the sites hosting the magnetic cations, may be needed to readily detect such features.
View details for DOI 10.1039/b904731j
View details for Web of Science ID 000268676700004
View details for PubMedID 19652824
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Temperature effects on the network structure of oxide melts and their consequences for configurational heat capacity
CHEMICAL GEOLOGY
2008; 256 (3-4): 80-91
View details for DOI 10.1016/j.chemgeo.2008.03.011
View details for Web of Science ID 000261563200002
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Ca-Mg mixing in aluminosilicate glasses: An investigation using O-17 MAS and 3QMAS and Al-27 MAS NMR
JOURNAL OF NON-CRYSTALLINE SOLIDS
2008; 354 (40-41): 4644-4653
View details for DOI 10.1016/j.jnoncrysol.2008.05.049
View details for Web of Science ID 000260232600021
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Effects of UV cure on glass structure and fracture properties of nanoporous carbon-doped oxide thin films
JOURNAL OF APPLIED PHYSICS
2008; 104 (4)
View details for DOI 10.1063/1.2968438
View details for Web of Science ID 000259265100026
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High resolution O-17 MAS and triple-quantum MAS NMR studies of gallosilicate glasses
JOURNAL OF NON-CRYSTALLINE SOLIDS
2008; 354 (27): 3120-3128
View details for DOI 10.1016/j.jnoncrysol.2008.01.026
View details for Web of Science ID 000256816700004
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Temperature effects on non-bridging oxygen and aluminum coordination number in calcium aluminosilicate glasses and melts
GEOCHIMICA ET COSMOCHIMICA ACTA
2008; 72 (3): 910-925
View details for DOI 10.1016/j.gca.2007.11.018
View details for Web of Science ID 000252662000014
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Cation order/disorder behavior and crystal chemistry of pyrope-grossular garnets: An O-17 3QMAS and Al-27 MAS NMR spectroscopic study
AMERICAN MINERALOGIST
2008; 93 (1): 134-143
View details for DOI 10.2138/am.2008.2623
View details for Web of Science ID 000252377400016
- Structure, local environment, and ionic conductivity in scandia stabilized zirconia Solid State Ionics 2008; 179: 1442-1445
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Sodium germanate glasses and crystals: NMR constraints on variation in structure with composition
JOURNAL OF NON-CRYSTALLINE SOLIDS
2007; 353 (52-54): 4732-4742
View details for DOI 10.1016/j.jnoncrysol.2007.06.066
View details for Web of Science ID 000252513800016
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In situ high temperature Al-27 NMR study of structure and dynamics in a calcium aluminosilicate glass and melt
JOURNAL OF NON-CRYSTALLINE SOLIDS
2007; 353 (44-46): 4001-4010
View details for DOI 10.1016/j.jnoncrysol.2007.06.030
View details for Web of Science ID 000250971900001
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Vacancy and cation distribution in yttria-doped ceria: An Y-89 and O-17 MAS NMR study
CHEMISTRY OF MATERIALS
2007; 19 (23): 5742-5747
View details for DOI 10.1021/cm0715388
View details for Web of Science ID 000250803900038
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High temperature O-17 MAS NMR study scandia and yttria stabilized of calcia, magnesia, zirconia
SOLID STATE IONICS
2007; 178 (27-28): 1499-1506
View details for DOI 10.1016/j.ssi.2007.01).008
View details for Web of Science ID 000251694300003
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Scandium-45 NMR of pyrope-grossular garnets: Resolution of multiple scandium sites and comparison with X-ray diffraction and X-ray absorption spectroscopy
AMERICAN MINERALOGIST
2007; 92 (11-12): 1875-1880
View details for DOI 10.2138/am.2007.2601
View details for Web of Science ID 000251101000012
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Germanosilicate and alkali germanosilicate glass structure: New insights from high-resolution oxygen-17 NMR
JOURNAL OF NON-CRYSTALLINE SOLIDS
2007; 353 (30-31): 2910-2918
View details for DOI 10.1016/j.jnoncrysol.2007.05.122
View details for Web of Science ID 000249670300013
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Effect of structural transitions on properties of high-pressure silicate melts: Al-27 NMR, glass densities, and melt viscosities
AMERICAN MINERALOGIST
2007; 92 (7): 1093-1104
View details for DOI 10.2138/am.2007.2530
View details for Web of Science ID 000247890700014
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Aluminum substitution in rutile titanium dioxide: New constraints from high-resolution Al-27 NMR
CHEMISTRY OF MATERIALS
2007; 19 (7): 1862-1869
View details for DOI 10.1021/cm0629053
View details for Web of Science ID 000245208100044
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Effect of UV cure on adhesive and cohesive failure of low-k films: Implications for integration
Advanced Metallization Conference 2006
MATERIALS RESEARCH SOCIETY. 2007: 327–330
View details for Web of Science ID 000245813300046
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Constraining O-17 and Al-27 NMR spectra of high-pressure crystals and glasses: New data for jadeite, pyrope, grossular, and mullite
AMERICAN MINERALOGIST
2007; 92 (1): 210-216
View details for DOI 10.2138/am.2007.2284
View details for Web of Science ID 000243611000023
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Glasses and melts: Linking geochemistry and materials science
ELEMENTS
2006; 2 (5): 265-268
View details for Web of Science ID 000241646200007
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The structure of silicate glasses and melts
ELEMENTS
2006; 2 (5): 269-273
View details for Web of Science ID 000241646200008
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Disorder and the extent of polymerization in calcium silicate and aluminosilicate glasses: O-17NMR results and quantum chemical molecular orbital calculations
GEOCHIMICA ET COSMOCHIMICA ACTA
2006; 70 (16): 4275-4286
View details for DOI 10.1016/j.gca.2006.06.1550
View details for Web of Science ID 000240213900017
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Scandium coordination in solid oxides and stabilized zirconia: Sc-45 NMR
CHEMISTRY OF MATERIALS
2006; 18 (16): 3855-3859
View details for DOI 10.1021/cm0605901
View details for Web of Science ID 000239396900037
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Oxygen sites and network coordination in sodium germanate glasses and crystals: High-resolution oxygen-17 and sodium-23 NMR
JOURNAL OF PHYSICAL CHEMISTRY B
2006; 110 (25): 12427-12437
Abstract
Sodium germanate glasses are well-studied materials in which, unlike silicates but analogous to borates, the major structural consequence of alkali addition is generally thought to involve a coordination number increase of the network-forming Ge cations. However, the nature of this change, in particular quantifying fractions of nonbridging oxygens and of five- and/or six-coordinated Ge, has remained unresolved. We present here high-resolution 17O results, including triple-quantum MAS NMR (3QMAS), on a series of crystalline model compounds that allow the definition of ranges of chemical shifts corresponding to oxygens bonded to various coordinations of Ge. These include quartz- and rutile-structured GeO2, Na4Ge9O20, Na2Ge4O9, and Na2GeO3 (germanium dioxide, sodium enneagermanate, sodium tetragermanate, and sodium metagermanate). 3QMAS spectra of Na-germanate glasses ranging from 0% to 27% Na2O clearly show the development of partially resolved peaks as alkali is added, corresponding to signals from nonbridging oxygens (in the highest Na glasses) and to oxygen bridging between one four-coordinated and one higher coordinated Ge. As in conventional models of this system, nonbridging oxygen contents are much lower than in corresponding silicates. Although we do not directly distinguish between five- and six-coordinated Ge, modeling of bridging oxygen populations and comparison with measured speciation suggest that substantial proportions of both species are likely to be present. High-field 23Na MAS NMR shows systematic decreases in mean Na-O bond distance and/or coordination number with increasing alkali content that can be compared with published results for high-temperature liquids. These results, as well as comparison of molar volumes of glasses and high-temperature liquids, suggest the possibility of significant temperature effects on liquid structure.
View details for DOI 10.1021/jp0615510
View details for Web of Science ID 000238446900033
View details for PubMedID 16800569
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Physics, chemistry and rheology of silicate melts and glasses - Preface
CHEMICAL GEOLOGY
2006; 229 (1-3): 1-1
View details for DOI 10.1016/j.chemgeo.2006.01.006
View details for Web of Science ID 000237989600001
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Quench rate and temperature effects on framework ordering in aluminosilicate melts
AMERICAN MINERALOGIST
2006; 91 (5-6): 753-761
View details for Web of Science ID 000237813500005
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Aluminum substitution in stishovite and MgSiO3 perovskite: High-resolution Al-27 NMR
AMERICAN MINERALOGIST
2006; 91 (2-3): 337-343
View details for Web of Science ID 000235472000014
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UV curing effects on glass structure and mechanical properties of organosilicate low-k thin films
9th International Interconnect Technology Conference (IITC)
IEEE, ELECTRON DEVICES SOC & RELIABILITY GROUP. 2006: 149–151
View details for Web of Science ID 000238974400045
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The effect of fictive temperature on the structural environment of fluorine in silicate and aluminosilicate glasses
JOURNAL OF THE AMERICAN CERAMIC SOCIETY
2006; 89 (1): 57-64
View details for DOI 10.1111/j.1551-2916.2005.00677.x
View details for Web of Science ID 000234482600009
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The development of a rapid quenching device for the study of the dependence of glass structure on fictive temperature
REVIEW OF SCIENTIFIC INSTRUMENTS
2006; 77 (1)
View details for DOI 10.1063/1.2162751
View details for Web of Science ID 000234979400017
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The effect of fictive temperature on the structure of E-glass: A high resolution, multinuclear NMR study
JOURNAL OF NON-CRYSTALLINE SOLIDS
2005; 351 (46-48): 3571-3578
View details for DOI 10.1016/j.noncrysol.2005.09.026
View details for Web of Science ID 000233652500001
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Network connectivity in aluminoborosilicate glasses: A high-resolution B-11, Al-27 and O-17 NMR study
JOURNAL OF NON-CRYSTALLINE SOLIDS
2005; 351 (43-45): 3508-3520
View details for DOI 10.1016/j.jnoncrysol.2005.08.033
View details for Web of Science ID 000233151200016
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The effect of fictive temperature on Al coordination in high-pressure (10 GPa) sodium aluminosilicate glasses
AMERICAN MINERALOGIST
2005; 90 (8-9): 1453-1457
View details for Web of Science ID 000231412500024
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Aluminium coordination in natural silica glasses from the Libyan Desert (Egypt): high field NMR results
9th International Conference on the Structure of Non-Crystalline Materials (NCM9)
SOC GLASS TECHNOLOGY. 2005: 340–44
View details for Web of Science ID 000234597300007
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Aluminum coordination and the densification of high-pressure aluminosilicate glasses
AMERICAN MINERALOGIST
2005; 90 (7): 1218-1222
View details for DOI 10.2138/am.2005.1836
View details for Web of Science ID 000230414500025
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Site connectivities in sodium aluminoborate glasses: multinuclear and multiple quantum NMR results
SOLID STATE NUCLEAR MAGNETIC RESONANCE
2005; 27 (1-2): 37-49
Abstract
In a series of sodium aluminoborate glasses, we have applied triple-quantum magic-angle spinning (3QMAS) 17O NMR to obtain high-resolution information about the connections among various network structural units, to explore the mixing of aluminum and boron species. Oxygen-17 3QMAS spectra reveal changes in connectivities between AlO4 ([4]Al), AlO5 and AlO6 ([5,6]Al), BO3 ([3]B) and BO4 ([4]B) units, by quantifying populations of bridging oxygens such as Al-O-Al, Al-O-B and B-O-B and of non-bridging oxygens. Several linkages such as [4]Al-O-[4]Al and three-coordinated oxygen associated with [5,6]Al in Al-O-Al, [4]Al-O-[4]B, [4]Al-O-[3]B and [5,6]Al-O-[3]B in Al-O-B as well as [4]B-O-[3]B and [3]B-O-[3]B in B-O-B can be distinguished for the first time. The fractions of these linkages were calculated from models of random mixing and of mixing with maximum avoidance of tetrahedral-tetrahedral linkages. The results suggest that the structure of all of glasses in this study is well approximated by the latter model. However, the energetic "penalty" for formation of [4]Al-O-[4]B may be somewhat less than for [4]Al-O-[4]Al and [4]B-O-[4]B. In general, the new results presented here are similar to those obtained on glasses in this system by 27Al{11B} REDOR NMR (J. Phys. Chem. B 104 (2000) 6541), but provide considerably more detail on network connectivity and ordering schemes.
View details for DOI 10.1016/j.ssnmer.2004.08.003
View details for Web of Science ID 000225955000007
View details for PubMedID 15589726
- The effect of composition, compression, and decompression on the structure of high pressure aluminosilicate glasses: an investigation utilizing 17O and 27Al NMR Frontiers of High Pressure Research edited by Chen, J., Wang, Y., Duffy, T. S., Shen, G., Dobrzhinetskaya, L. F. Elsevier, Amsterdam. 2005: 211–240
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Structural mechanisms of compression and decompression in high-pressure K2Si4O9 glasses: an investigation utilizing Raman and NMR spectroscopy of glasses and crystalline materials
CHEMICAL GEOLOGY
2004; 213 (1-3): 137-151
View details for DOI 10.1016/j.chemgeo.2004.08.038
View details for Web of Science ID 000226015700012
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Correlated structural distributions in silica glass
PHYSICAL REVIEW B
2004; 70 (6)
View details for DOI 10.1103/PhysRevB.70.064202
View details for Web of Science ID 000223716300032
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F-19NMR study of the ordering of high field strength cations at fluoride sites in silicate and aluminosilicate glasses
JOURNAL OF NON-CRYSTALLINE SOLIDS
2004; 337 (2): 142-149
View details for DOI 10.1016/j.jnoncrysol.2004.03.123
View details for Web of Science ID 000222530300007
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Pressure-induced structural changes in a borosilicate glass-forming liquid: boron coordination, non-bridging oxygens, and network ordering
JOURNAL OF NON-CRYSTALLINE SOLIDS
2004; 337 (2): 196-200
View details for DOI 10.1016/j.jnoncrysol.2004.03.115
View details for Web of Science ID 000222530300016
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Ca-Mg and K-Mg mixing around non-bridging O atoms in silicate glasses: An investigation using O-17 MAS and 3QMAS NMR
AMERICAN MINERALOGIST
2004; 89 (5-6): 777-784
View details for Web of Science ID 000221680000011
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Calcium and strontium hexaluminates: NMR evidence that "pentacoordinate" cation sites are four-coordinated
JOURNAL OF PHYSICAL CHEMISTRY B
2004; 108 (12): 3681-3685
View details for DOI 10.1021/jp037615d
View details for Web of Science ID 000220323500001
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Thermodynamic properties of analcime solid solutions
AMERICAN JOURNAL OF SCIENCE
2004; 304 (1): 21-66
View details for Web of Science ID 000189188000002
- Structure of Cl-containing silicate and aluminosilicate glasses; a 35Cl MAS-NMR study Geochimica et Cosmochimica Acta 2004; 68: 5059-5069
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Site preference and Si/B mixing in mixed-alkali borosilicate glasses: A high-resolution B-11 and O-17 NMR study
CHEMISTRY OF MATERIALS
2003; 15 (20): 3913-3921
View details for DOI 10.1021/cm034427r
View details for Web of Science ID 000185747100028
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Nature of silicon-boron mixing in sodium borosilicate glasses: A high-resolution B-11 and O-17 NMR study
JOURNAL OF PHYSICAL CHEMISTRY B
2003; 107 (37): 10063-10076
View details for DOI 10.1021/jp0340481
View details for Web of Science ID 000185345400019
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O-17 and Al-27 MAS and 3QMAS NMR study of synthetic and natural layer silicates
CHEMISTRY OF MATERIALS
2003; 15 (13): 2605-2613
View details for DOI 10.1021/cm030165h
View details for Web of Science ID 000183810600017
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Bonding preferences of non-bridging O atoms: Evidence from O-17 MAS and 3QMAS NMR on calcium aluminate and low-silica Ca-aluminosilicate glasses
AMERICAN MINERALOGIST
2003; 88 (7): 949-954
View details for Web of Science ID 000184045300001
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Aluminum substitution in MgSiO3 perovskite: Investigation of multiple mechanisms by Al-27 NMR
AMERICAN MINERALOGIST
2003; 88 (7): 1161-1164
View details for Web of Science ID 000184045300026
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The distribution of sodium ions in aluminosilicate glasses: A high-field Na-23 MAS and 3Q MAS NMR study
GEOCHIMICA ET COSMOCHIMICA ACTA
2003; 67 (9): 1699-1709
View details for DOI 10.1016/S0016-7037(02)00026-7
View details for Web of Science ID 000182589900009
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Nature of cation mixing and ordering in Na-Ca silicate glasses and melts
JOURNAL OF PHYSICAL CHEMISTRY B
2003; 107 (14): 3141-3148
View details for DOI 10.1021/jp027489y
View details for Web of Science ID 000182037800009
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O atom sites in natural kaolinite and muscovite: O-17 MAS and 3QMAS NMR study
AMERICAN MINERALOGIST
2003; 88 (4): 493-500
View details for Web of Science ID 000182214400003
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Si-Al disorder and solid solutions in analcime, chabazite, and wairakite
AMERICAN MINERALOGIST
2003; 88 (2-3): 410-423
View details for Web of Science ID 000180922300017
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Solid-state NMR study of metastable immiscibility in alkali borosilicate glasses
JOURNAL OF NON-CRYSTALLINE SOLIDS
2003; 315 (3): 239-255
View details for Web of Science ID 000180270100004
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Order/disorder in natrolite group zeolites: A Si-29 and Al-27 MAS NMR study
AMERICAN MINERALOGIST
2002; 87 (10): 1307-1320
View details for Web of Science ID 000178631900006
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Effect of extraframework species on O-17 NMR chemical shifts in zeolite A
MICROPOROUS AND MESOPOROUS MATERIALS
2002; 55 (3): 239-251
View details for Web of Science ID 000178419900002
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Dynamics in ceramics
SCIENCE
2002; 297 (5585): 1285-1287
View details for Web of Science ID 000177573900027
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Materials science. Dynamics in ceramics.
Science (New York, N.Y.)
2002; 297 (5585): 1285-7
View details for DOI 10.1126/science.1075881
View details for PubMedID 12193772
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Fluorine sites in calcium and barium oxyfluorides: F-19NMR on crystalline model compounds and glasses
JOURNAL OF NON-CRYSTALLINE SOLIDS
2002; 306 (2): 160-168
View details for Web of Science ID 000176877300007
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Disordering during melting: An O-17 NMR study of crystalline and glassy CaTiSiO5 (titanite)
AMERICAN MINERALOGIST
2002; 87 (4): 572-579
View details for Web of Science ID 000174849200023
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New opportunities for high-resolution solid-state NMR spectroscopy of oxide materials at 21.1-and 18.8-t fields
SOLID STATE NUCLEAR MAGNETIC RESONANCE
2002; 21 (1-2): 105-115
Abstract
We present here high-resolution solid state NMR spectra of several oxide and silicate materials that illustrate the improvements obtainable with very high external fields (18.8 and 21.1 T), with probes capable of tuning to a wide frequency range that allow observations of nuclides from high to low magnetogyric ratio. We discuss 27Al MAS spectra for the zeolite scolecite (CaAl2Si3O10 x 3H2O), 17O MAS data for analcime (NaAlSi2O6 x H2O), calcium monoaluminate (CaAI2O4), and titanite (CaTiSiO5), 39K spin-echo spectra for leucite (KAlSi2O6), microline (KAlSiO8), muscovite (KAl2(AlSi3O10)(OH2) and a potassium aluminosolicate glass, and preliminary 73Ge spin-echo MAS spectra for crystalline and glassy germanium dioxide (GeO2).
View details for DOI 10.1006/snmr.2001.0051
View details for Web of Science ID 000174305700008
View details for PubMedID 11949814
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Chloride ion sites in silicate and aluminosilicate glasses: A preliminary study by Cl-35 solid-state NMR
AMERICAN MINERALOGIST
2002; 87 (2-3): 359-363
View details for Web of Science ID 000173697700022
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Oxygen sites in hydrous aluminosilicate glasses: The role of Al-O-Al and H2O
GEOCHIMICA ET COSMOCHIMICA ACTA
2002; 66 (2): 291-301
View details for Web of Science ID 000173340200008
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Extent of intermixing among framework units in silicate glasses and melts
GEOCHIMICA ET COSMOCHIMICA ACTA
2002; 66 (2): 303-309
View details for Web of Science ID 000173340200009
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Topological disorder and reactivity of borosilicate glasses: Quantum chemical calculations and O-17 and B-11 NMR study
JOURNAL OF PHYSICAL CHEMISTRY B
2001; 105 (50): 12583-12595
View details for DOI 10.1021/jp012119f
View details for Web of Science ID 000172945700022
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An O-17 NMR investigation of crystalline sodium metasilicate: Implications for the determination of local structure in alkali silicates
JOURNAL OF PHYSICAL CHEMISTRY B
2001; 105 (49): 12257-12265
View details for Web of Science ID 000172727200006
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Three-coordinated boron-11 chemical shifts in borates
INORGANIC CHEMISTRY
2001; 40 (24): 6239-6246
Abstract
Despite the importance of (11)B nuclear magnetic resonance (NMR) in structural studies of borate glasses, no clear means of correlating NMR parameters with the number of nonbridging oxygens on three-coordinate boron has been demonstrated. In this work, a series of anhydrous, polycrystalline, binary borates has been examined by (11)B magic-angle spinning (MAS) NMR to obtain precise measurements of their three-coordinate boron isotropic chemical shifts. The shifts generally increase with the replacement of bridging oxygens by nonbridging oxygens, ranging from 14.6 ppm in crystalline B(2)O(3) to 22.5 ppm in magnesium orthoborate. The underlying physical basis for this trend is satisfactorily accounted for by considering second neighbor effects using bond valence sums. These data are supportive of a structural model for B(2)O(3) glass in which 72% of the boron atoms are in rings. High-field MAS NMR experiments (B(0) = 18.8 T) indicate that the boron shielding is anisotropic, with greater anisotropy measured for three-coordinate borons possessing one or two nonbridging oxygens, than for those with zero or three nonbridging oxygens.
View details for Web of Science ID 000172181400023
View details for PubMedID 11703125
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A solid solution model for Si-Al substitution in disordered FAU and LTA zeolites
MICROPOROUS AND MESOPOROUS MATERIALS
2001; 49 (1-3): 139-148
View details for Web of Science ID 000172090500013
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Oxygen triclusters in crystalline CaAl4O7 (grossite) and in calcium aluminosilicate glasses: O-17 NMR
AMERICAN MINERALOGIST
2001; 86 (10): 1307-1311
View details for Web of Science ID 000171445300019
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Comparison of FAM mixing to single-pulse mixing in O-17 3Q-and 5Q-MAS NMR of oxygen sites in zeolites
CHEMICAL PHYSICS LETTERS
2001; 344 (3-4): 325-332
View details for Web of Science ID 000170676000013
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Hydroxyl-contents and hydroxyl-related concentration quenching in erbium-doped aluminophosphate, aluminosilicate and fluorosilicate glasses
JOURNAL OF NON-CRYSTALLINE SOLIDS
2001; 286 (1-2): 118-131
View details for Web of Science ID 000169446800014
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Potassium hydrogen disilicate: A possible model compound for O-17 NMR spectra of hydrous silicate glasses
AMERICAN MINERALOGIST
2001; 86 (3): 341-347
View details for Web of Science ID 000167343900018
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The mechanism of solution of aluminum oxide in MgSiO3 perovskite
GEOPHYSICAL RESEARCH LETTERS
2001; 28 (4): 615-618
View details for Web of Science ID 000166916500015
- NMR studies of oxide glass structure Solid State NMR: Theory and Applications edited by Duer, M. Blackwell Scientific, Oxford. 2001: 391–436
- Direct observation of multiple oxygen sites in oxide glasses: recent advances from triple-quantum magic-angle spinning nuclear magnetic resonance Journal of Non-Crystalline Solids 2001; 293: 67-73
- Enhanced resolution and quantitation from “ultrahigh” field NMR spectroscopy of glasses J. Non-Cryst. Solids 2001; 293: 440-445
- Oxygen sites in silicate glasses: a new view from oxygen-17 NMR Chem. Geol. 2001; 174: 63-75
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Magnesium coordination environments in glasses and minerals: New insight from high-field magnesium-25 MAS NMR
AMERICAN MINERALOGIST
2000; 85 (10): 1459-1464
View details for Web of Science ID 000089728900015
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Non-bridging oxygen sites in barium borosilicate glasses: results from B-11 and O-17 NMR
JOURNAL OF NON-CRYSTALLINE SOLIDS
2000; 276 (1-3): 122-131
View details for Web of Science ID 000089578800014
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Quantification of five- and six-coordinated aluminum ions in aluminosilicate and fluoride-containing glasses by high-field, high-resolution Al-27 NMR
JOURNAL OF NON-CRYSTALLINE SOLIDS
2000; 275 (1-2): 1-6
View details for Web of Science ID 000089303100001
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Solid state NMR study of oxygen site exchange and Al-O-Al site concentration in analcime
AMERICAN MINERALOGIST
2000; 85 (7-8): 1030-1037
View details for Web of Science ID 000087965500018
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The structure of aluminosilicate glasses: High-resolution O-17 and Al-27 MAS and 3QMAS
JOURNAL OF PHYSICAL CHEMISTRY B
2000; 104 (17): 4091-4100
View details for Web of Science ID 000086873000013
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Al-O-Al and Si-O-Si sites in framework aluminosilicate glasses with Si/Al=1: quantification of framework disorder
JOURNAL OF NON-CRYSTALLINE SOLIDS
2000; 270 (1-3): 260-264
View details for Web of Science ID 000087244300029
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Fluoride sites in aluminosilicate glasses: High-resolution F-19 NMR results
AMERICAN MINERALOGIST
2000; 85 (5-6): 863-867
View details for Web of Science ID 000086992700028
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Si-29 CPMAS NMR investigations of silanol-group minerals and hydrous aluminosilicate glasses
AMERICAN MINERALOGIST
2000; 85 (5-6): 722-731
View details for Web of Science ID 000086992700008
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Cation ordering at fluoride sites in silicate glasses: a high-resolution F-19 NMR study
JOURNAL OF NON-CRYSTALLINE SOLIDS
2000; 262 (1-3): 1-5
View details for Web of Science ID 000085311800001
- Non-Bridging Oxygens in Borate Glasses: Characterization by 11B and 17O MAS and 3QMAS NMR Journal of Non-Crystalline Solids 2000; 276: 9-19
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Hydrogen speciation in hydrogen-loaded, germania-doped silica glass: a combined NMR and FTIR study of the effects of UV irradiation and heat treatment
JOURNAL OF NON-CRYSTALLINE SOLIDS
1999; 258 (1-3): 78-91
View details for Web of Science ID 000083475200009
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Reactive Al-O-Al sites in a natural zeolite: Triple-quantum oxygen-17 nuclear magnetic resonance
AMERICAN MINERALOGIST
1999; 84 (10): 1680-1684
View details for Web of Science ID 000083078900023
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Pentacoordinate silicon in high-pressure crystalline and glassy phases of calcium disilicate (CaSi2O5)
GEOPHYSICAL RESEARCH LETTERS
1999; 26 (16): 2521-2523
View details for Web of Science ID 000082011200029
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Multiple-quantum magic-angle spinning O-17 NMR studies of borate, borosilicate, and boroaluminate classes
JOURNAL OF THE AMERICAN CERAMIC SOCIETY
1999; 82 (6): 1519-1528
View details for Web of Science ID 000080947100025
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The degree of aluminum avoidance in aluminosilicate glasses
AMERICAN MINERALOGIST
1999; 84 (5-6): 937-945
View details for Web of Science ID 000080303500031
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Al-O-Al oxygen sites in crystalline aluminates and aluminosilicate glasses: High-resolution oxygen-17 NMR results
AMERICAN MINERALOGIST
1999; 84 (5-6): 983-986
View details for Web of Science ID 000080303500036
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Cation clustering and formation of free oxide ions in sodium and potassium lanthanum silicate glasses: nuclear magnetic resonance and Raman spectroscopic findings
JOURNAL OF NON-CRYSTALLINE SOLIDS
1999; 243 (2-3): 146-157
View details for Web of Science ID 000078355800006
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The structural role of lanthanum and yttrium in aluminosilicate glasses: A Al-27 and O-17 MAS NMR study
JOURNAL OF PHYSICAL CHEMISTRY B
1998; 102 (52): 10690-10697
View details for Web of Science ID 000077837200009
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Cation dynamics and premelting in lithium metasilicate (Li2SiO3) and sodium metasilicate (Na2SiO3): A high-temperature NMR study
AMERICAN MINERALOGIST
1998; 83 (11-12): 1277-1284
View details for Web of Science ID 000077410500016
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Shocked quartz: A Si-29 magic-angle-spinning nuclear magnetic resonance study
AMERICAN MINERALOGIST
1998; 83 (11-12): 1285-1292
View details for Web of Science ID 000077410500017
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Fast rotational reorientation of NO3- ions and its relation to the glass transition in Ca0.4K0.6(NO3)(1.4) liquid: A N-15 NMR spin-lattice-relaxation study
PHYSICAL REVIEW B
1998; 58 (13): 8379-8383
View details for Web of Science ID 000076232100043
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Oxygen speciation in hydrous silicate glasses: An oxygen-17 NMR study
JOURNAL OF THE AMERICAN CHEMICAL SOCIETY
1998; 120 (38): 9894-9901
View details for Web of Science ID 000076225200021
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Cation sites in mixed-alkali oxide glasses: correlations of NMR chemical shift data with site size and bond distance
SOLID STATE IONICS
1998; 112 (1-2): 137-141
View details for Web of Science ID 000076522900019
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Structure and dynamics of magnesium in silicate melts: A high-temperature Mg-25 NMR study
AMERICAN MINERALOGIST
1998; 83 (9-10): 1022-1029
View details for Web of Science ID 000076082900010
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On the structure of borosilicate glasses: a triple-quantum magic-angle spinning O-17 nuclear magnetic resonance study
JOURNAL OF NON-CRYSTALLINE SOLIDS
1998; 231 (3): 286-290
View details for Web of Science ID 000075517700011
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Oxygen sites in the zeolite stilbite: a comparison of static, MAS, VAS, DAS and triple quantum MAS NMR techniques
SOLID STATE NUCLEAR MAGNETIC RESONANCE
1998; 11 (3-4): 243-251
Abstract
Static, magic angle spinning (MAS), variable angle spinning (VAS), dynamic angle spinning (DAS) and triple quantum magic angle spinning (3QMAS) NMR techniques were applied to separate and quantify oxygen signals from Al-O-Si and Si-O-Si sites of 17O-enriched samples of the mineral stilbite, a natural zeolite. DAS experiments showed that there was a distribution of quadrupolar coupling constants, asymmetry parameters and isotropic chemical shifts. Two methods were used to study the quantification problem of DAS and 3QMAS. Our results showed that DAS was quantitative. In 3QMAS, signal intensity from sites with larger quadrupolar coupling constants was reduced because of less efficient excitation. All techniques have shown a clear difference in rates of exchange between the two types of sites with interchannel H2O molecules.
View details for Web of Science ID 000074865600012
View details for PubMedID 9694393
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Oxygen site exchange kinetics observed with solid state NMR in a natural zeolite
GEOCHIMICA ET COSMOCHIMICA ACTA
1998; 62 (10): 1803-1809
View details for Web of Science ID 000075157600011
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Temperature dependent structural changes in borate, borosilicate and boroaluminate liquids: high-resolution B-11, Si-29 and Al-27 NMR studies
JOURNAL OF NON-CRYSTALLINE SOLIDS
1998; 226 (1-2): 29-40
View details for Web of Science ID 000074426100005
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Phase relations in Na2O-SiO2 and K2Si4O9 systems up to 14 GPa and Si-29 NMR study of the new high-pressure phases: implications to the structure of high-pressure silicate glasses
International Symposium on Role of Magmas on the Evolution of the Earth
ELSEVIER SCIENCE BV. 1998: 9–21
View details for Web of Science ID 000074453000003
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Microscopic dynamics and viscous flow in a borosilicate glass-forming liquid
JOURNAL OF NON-CRYSTALLINE SOLIDS
1998; 224 (1): 80-85
View details for Web of Science ID 000072484800010
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Na-23 chemical shifts and local structure in crystalline, glassy, and molten sodium borates and germanates
SOLID STATE NUCLEAR MAGNETIC RESONANCE
1997; 10 (1-2): 9-17
Abstract
A simple correlation between average Na-O bond length and 23Na isotropic chemical shift in crystalline germanates and borates has been established, similar to existing correlations for sodium in silicates and carbonates. This empirical trend is discussed in terms of a decreasing paramagnetic contribution to the chemical shift with increasing average bond length. The correlation is then applied to data for sodium borate and germanate glasses and melts from room temperature to 1200 degrees C, where both structural and compositional effects on the chemical shift are apparent.
View details for PubMedID 9472786
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NMR evidence for excess non-bridging oxygen in an aluminosilicate glass
NATURE
1997; 390 (6655): 60-62
View details for Web of Science ID A1997YE47700049
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Disorder among network-modifier cations in silicate glasses: New constraints from triple-quantum O-17 NMR
AMERICAN MINERALOGIST
1997; 82 (11-12): 1116-1124
View details for Web of Science ID A1997YG09400009
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Anionic species determination in CaSiO3 glass using two-dimensional Si-29 NMR
JOURNAL OF PHYSICAL CHEMISTRY B
1997; 101 (20): 4004-4008
View details for Web of Science ID A1997WZ29000019
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Heterogeneous NO3- ion dynamics near the glass transition in the fragile ionic glass former Ca0.4K0.6(NO3)(1.4): A N-15 NMR study
PHYSICAL REVIEW LETTERS
1997; 78 (18): 3495-3498
View details for Web of Science ID A1997WX51800019
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Cross-polarization from quadrupolar nuclei to silicon using low-radio-frequency amplitudes during magic-angle spinning
JOURNAL OF PHYSICAL CHEMISTRY B
1997; 101 (16): 3240-3249
View details for Web of Science ID A1997WU63000031
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Multiple-quantum magic-angle spinning and dynamic-angle spinning NMR spectroscopy of quadrupolar nuclei
SOLID STATE NUCLEAR MAGNETIC RESONANCE
1997; 8 (1): 1-16
Abstract
Several aspects of the Multiple-Quantum Magic-Angle Spinning (MQMAS) technique (L. Frydman and J.S. Harwood, J. Am. Chem. Soc., 117 (1995) 5367) are compared with Dynamic-Angle Spinning (DAS). Examples of MQMAS spectra are shown for I = 3/2 nuclei with CQ up to 3.6 MHz, and for 27Al (I = 5/2) with CQ up to 10 MHz. The MQMAS linewidth is largely independent of the magnitude of the homonuclear dipolar interaction, while the spinning sideband manifold is similar to that observed in DAS experiments. MQMAS is technically simple and routinely useful for studying nuclei with short spin-lattice relaxation times, but care must be taken in its use for quantitative studies as the excitation of the triple-quantum coherence is not uniform. In this regard, MQMAS is most useful for samples with small quadrupolar coupling constants. In the specific case of 17O, DAS would give spectra with excellent resolution in comparison to MQMAS. The different advantages of DAS and MQMAS make them useful complementary techniques in many cases. Two additional methods are also presented for extracting the chemical shift anisotropy (CSA) directly for quadrupolar nuclei using the multiple-quantum scheme.
View details for Web of Science ID A1997WY62900001
View details for PubMedID 9178419
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Na-ion transport in borate and germanate glasses and liquids: A Na-23 and B-11 NMR spin-lattice-relaxation study
PHYSICAL REVIEW B
1997; 55 (6): 3512-3519
View details for Web of Science ID A1997WJ87500038
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Dynamics of Na in sodium aluminosilicate glasses and liquids
PHYSICS AND CHEMISTRY OF MINERALS
1996; 23 (8): 526-534
View details for Web of Science ID A1996WA58700005
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Magnesium site exchange in forsterite: A direct measurement by high-temperature Mg-25 NMR spectroscopy
AMERICAN MINERALOGIST
1996; 81 (11-12): 1315-1320
View details for Web of Science ID A1996WE45500002
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Silicon site distributions in an alkali silicate glass derived by two-dimensional Si-29 nuclear magnetic resonance
JOURNAL OF NON-CRYSTALLINE SOLIDS
1996; 204 (3): 294-300
View details for Web of Science ID A1996VV24500011
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Temperature effects on structure and dynamics in borate and borosilicate liquids: High-resolution and high-temperature NMR results
JOURNAL OF THE AMERICAN CERAMIC SOCIETY
1996; 79 (9): 2247-2256
View details for Web of Science ID A1996VJ72700003
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Triple-quantum two-dimensional Al-27 magic-angle spinning nuclear magnetic resonance spectroscopic study of aluminosilicate and aluminate crystals and glasses
JOURNAL OF THE AMERICAN CHEMICAL SOCIETY
1996; 118 (30): 7209-7214
View details for Web of Science ID A1996VA02600027
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Cation distribution in mixed alkali disilicate glasses
JOURNAL OF THE AMERICAN CHEMICAL SOCIETY
1996; 118 (14): 3493-3497
View details for Web of Science ID A1996UE65600022
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Ionic conduction and mixed cation effect in silicate glasses and liquids: Na-23 and Li-7 NMR spin-lattice relaxation and a multiple-barrier model of percolation
JOURNAL OF NON-CRYSTALLINE SOLIDS
1996; 197 (1): 53-64
View details for Web of Science ID A1996UJ19000007
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CATION DYNAMICS AND DIFFUSION IN LITHIUM ORTHOSILICATE - 2-DIMENSIONAL LI-6 NMR
SCIENCE
1995; 270 (5240): 1332-1334
View details for Web of Science ID A1995TF89900030
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LI-6 NUCLEAR-MAGNETIC-RESONANCE CHEMICAL-SHIFTS, COORDINATION-NUMBER AND RELAXATION IN CRYSTALLINE AND GLASSY SILICATES
SOLID STATE NUCLEAR MAGNETIC RESONANCE
1995; 5 (1): 103-112
Abstract
Unlike 7Li magic-angle spinning nuclear magnetic resonance (MAS NMR) spectra, 6Li MAS NMR spectra of silicates are dominated by chemical shift effects, often have a very high resolution and hence can provide significant structural information. In this study we demonstrate a good correlation between 6Li isotropic chemical shifts and oxygen coordination number, and use this result to describe the range of coordination environments for Li in silicate glasses. We also show that the second-order quadrupolar shift for 7Li can often be derived from 7Li and 6Li MAS spectra acquired at a single magnetic field. For a series of natural lepidolite samples with significant but varying contents of Mn and Fe, spin-lattice relaxation data show a power-law behavior and a three-dimensional distribution of paramagnetic centers, but homonuclear dipolar couplings can be important. The 6Li spectrum for lithium orthosilicate (which has three-, four-, five- and six-coordinated Li) is consistent with that predicted by the X-ray structure.
View details for Web of Science ID A1995TA30400010
View details for PubMedID 8748648
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HIGH-TEMPERATURE NA-23 MAS NMR DATA FOR ALBITE - COMPARISON TO CHEMICAL-SHIFT MODELS
AMERICAN MINERALOGIST
1995; 80 (9-10): 878-884
View details for Web of Science ID A1995RY40300002
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SOLID-STATE O-17 MAGIC-ANGLE AND DYNAMIC-ANGLE SPINNING NMR-STUDY OF THE SIO2 POLYMORPH COESITE
JOURNAL OF PHYSICAL CHEMISTRY
1995; 99 (32): 12341-12348
View details for Web of Science ID A1995RN70600045
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SILICATE SPECIES EXCHANGE, VISCOSITY, AND CRYSTALLIZATION IN A LOW-SILICA MELT - IN-SITU HIGH-TEMPERATURE MAS NMR-SPECTROSCOPY
AMERICAN MINERALOGIST
1995; 80 (7-8): 861-864
View details for Web of Science ID A1995RN60900028
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STRUCTURAL ROLE OF ND3+ AND AL3+ CATIONS IN SIO2 GLASS - A SI-29 MAS-NMR SPIN-LATTICE RELAXATION, AL-27 NMR AND EPR STUDY
JOURNAL OF NON-CRYSTALLINE SOLIDS
1995; 188 (1-2): 54-62
View details for Web of Science ID A1995RM29100008
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CATION-EXCHANGE RATES AND MOBILITY IN ALUMINUM-DOPED LITHIUM ORTHOSILICATE - HIGH-RESOLUTION LI-6 NMR RESULTS
SOLID STATE IONICS
1995; 78 (1-2): L1-L8
View details for Web of Science ID A1995RD21300001
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MOBILITY AND RELAXATION DETERMINATIONS OF LITHIUM IN LITHIUM ALUMINATE CERAMICS USING SOLID-STATE NMR-SPECTROSCOPY
CHEMISTRY OF MATERIALS
1995; 7 (2): 363-367
View details for Web of Science ID A1995QG95800020
- High temperature nuclear magnetic resonance studies of oxide melts J. Non-Cryst. Solids 1995; 193: 298-305
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Dynamics and structure of silicate and oxide melts: Nuclear magnetic resonance studies
STRUCTURE, DYNAMICS AND PROPERTIES OF SILICATE MELTS
1995; 32: 191-246
View details for Web of Science ID A1995BE38D00007
- Structure, Dynamics and Properties of Silicate Liquids edited by Stebbins, J. F., McMillan, P., Dingwell, D. 1995
- Nuclear magnetic resonance of oxide glasses and melts Structure, Dynamics and Properties of Silicate Liquids Min. Soc. Am.. 1995: 191–246
- Nuclear magnetic resonance spectroscopy of silicates and oxides in geochemistry and geophysics Handbook of Physical Constants, v. 2 American Geophysical Union. 1995: 303–332
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OXYGEN DISPLACEMENT THROUGH THE FERROELECTRIC PHASE-TRANSITION OF BARIUM-TITANATE - HIGH-TEMPERATURE O-17 NMR
JOURNAL OF THE AMERICAN CERAMIC SOCIETY
1994; 77 (12): 3263-3266
View details for Web of Science ID A1994QC57000033
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DEOXYGENATION ANNEALING OF BI2SR2CACU2O8+DELTA SINGLE-CRYSTALS OBSERVED IN-SITU BY O-17 NMR
PHYSICA C-SUPERCONDUCTIVITY AND ITS APPLICATIONS
1994; 232 (1-2): 27-36
View details for Web of Science ID A1994PN71300006
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DIFFUSION AND THE DYNAMICS OF DISPLACIVE PHASE-TRANSITIONS IN CRYOLITE (NA3ALF6) AND CHIOLITE (NA5AL3F14) - MULTINUCLEAR NMR-STUDIES
PHYSICS AND CHEMISTRY OF MINERALS
1994; 21 (6): 373-386
View details for Web of Science ID A1994PR72400003
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A NEW DEVICE FOR EXPANSIVITY MEASUREMENTS OF LIQUIDS AT HIGH-TEMPERATURE AND PRESSURE AND EXPANSIVITY DATA FOR LIQUID-TIN TO 1450-DEGREES-C
REVIEW OF SCIENTIFIC INSTRUMENTS
1994; 65 (10): 3258-3262
View details for Web of Science ID A1994PL96800031
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THE STRUCTURAL OF MG IN SILICATE LIQUIDS - A HIGH-TEMPERATURE MG-25, NA-23, AND SI-29 NMR-STUDY
AMERICAN MINERALOGIST
1994; 79 (9-10): 848-861
View details for Web of Science ID A1994PM15900006
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COORDINATION ENVIRONMENTS OF B-IMPURITIES IN CALCITE AND ARAGONITE POLYMORPHS - A B-11 MAS NMR-STUDY
AMERICAN MINERALOGIST
1994; 79 (9-10): 819-825
View details for Web of Science ID A1994PM15900003
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THE NATURE OF THE GLASS-TRANSITION IN A SILICA-RICH OXIDE MELT
SCIENCE
1994; 265 (5176): 1206-1209
Abstract
The atomic-scale dynamics of the glass-to-liquid transition are, in general, poorly understood in inorganic materials. Here, two-dimensional magic angle spinning nuclear magnetic resonance spectra collected just above the glass transition of K(2)Si(4)O(9) at temperatures as high as 583 degrees C are presented. Rates of exchange for silicon among silicate species, which involves Si-O bond breaking, have been measured and are shown to be closely related in time scale to those defined by viscosity. Thus, even at viscosities as high as 10(10) pascal seconds, local bond breaking (in contrast to the cooperative motion of large clusters) is of major importance in the control of macroscopic flow and diffusion.
View details for Web of Science ID A1994PD42200028
View details for PubMedID 17787585
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PHASE-SEPARATION, CLUSTERING, AND FRACTAL CHARACTERISTICS IN GLASS - A MAGIC-ANGLE-SPINNING NMR SPIN-LATTICE RELAXATION STUDY
PHYSICAL REVIEW B
1994; 50 (2): 822-830
View details for Web of Science ID A1994NX63700022
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CORRELATIONS BETWEEN O-17 NMR PARAMETERS AND LOCAL-STRUCTURE AROUND OXYGEN IN HIGH-PRESSURE SILICATES - IMPLICATIONS FOR THE STRUCTURE OF SILICATE MELTS AT HIGH-PRESSURE
AMERICAN MINERALOGIST
1994; 79 (1-2): 31-42
View details for Web of Science ID A1994MX24600005
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NUCLEATION AND MEDIUM-RANGE ORDER IN SILICATE LIQUIDS - INFERENCES FROM NMR-SPECTROSCOPY
Symposium on Crystallization and Related Phenomena in Amorphous Materials, at the 1993 Fall Meeting of the Materials-Research-Society
MATERIALS RESEARCH SOC. 1994: 143–154
View details for Web of Science ID A1994BA13A00021
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BONDING AND DYNAMICAL PHENOMENA IN MGO - A HIGH-TEMPERATURE O-17 AND MG-25 NMR-STUDY
PHYSICS AND CHEMISTRY OF MINERALS
1994; 20 (8): 587-593
View details for Web of Science ID A1994PA51800008
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NA-23 NMR CHEMICAL-SHIFTS AND LOCAL NA COORDINATION ENVIRONMENTS IN SILICATE CRYSTALS, MELTS AND GLASSES
PHYSICS AND CHEMISTRY OF MINERALS
1993; 20 (5): 297-307
View details for Web of Science ID A1993ME58500001
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GEL SYNTHESIS OF AN ALBITE (NAALSI3O8) GLASS - AN NMR ANALYSIS
GEOCHIMICA ET COSMOCHIMICA ACTA
1993; 57 (16): 3949-3960
View details for Web of Science ID A1993LW38900010
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ACCEPTANCE OF THE MINERALOGICAL-SOCIETY-OF-AMERICA AWARD FOR 1992
AMERICAN MINERALOGIST
1993; 78 (7-8): 856-857
View details for Web of Science ID A1993LT31400025
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COMPOSITIONAL AND TEMPERATURE EFFECTS ON 5-COORDINATED SILICON IN AMBIENT-PRESSURE SILICATE-GLASSES
JOURNAL OF NON-CRYSTALLINE SOLIDS
1993; 160 (1-2): 116-125
View details for Web of Science ID A1993LP62900015
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TETRAHEDRAL DISORDER IN FIBROLITIC SILLIMANITE - COMPARISON OF SI-29 NMR AND NEUTRON-DIFFRACTION DATA
AMERICAN MINERALOGIST
1993; 78 (3-4): 461-464
View details for Web of Science ID A1993KY02300026
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KINETICS AND MECHANISM OF LIGAND-EXCHANGE OF AU(III), ZN(II), AND CD(II) CHLORIDES IN AQUEOUS-SOLUTION - AN NMR-STUDY FROM 28-98-DEGREES-C
GEOCHIMICA ET COSMOCHIMICA ACTA
1993; 57 (4): 721-731
View details for Web of Science ID A1993KN41200001
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A SI-29 MAS NMR-STUDY OF SUB-TG AMORPHIZATION OF STISHOVITE AT AMBIENT PRESSURE
PHYSICS AND CHEMISTRY OF MINERALS
1993; 19 (7): 480-485
View details for Web of Science ID A1993KN23700007
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DYNAMICS OF THE ALPHA-BETA PHASE-TRANSITIONS IN QUARTZ AND CRISTOBALITE AS OBSERVED BY INSITU HIGH-TEMPERATURE SI-29 NMR AND O-17 NMR
PHYSICS AND CHEMISTRY OF MINERALS
1992; 19 (5): 307-321
View details for Web of Science ID A1992JZ94900004
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SOLIDS AND LIQUIDS IN THE NAF-ALF3-AL2O3 SYSTEM - A HIGH-TEMPERATURE NMR-STUDY
JOURNAL OF THE AMERICAN CERAMIC SOCIETY
1992; 75 (11): 3001-3006
View details for Web of Science ID A1992JX13600015
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QUANTIFICATION OF THE DISORDER IN NETWORK-MODIFIED SILICATE-GLASSES
NATURE
1992; 358 (6381): 31-35
Abstract
Local order in silicate glasses has been observed by many experimental techniques to be similar to that in crystalline materials. Details of the intermediate-range order are more elusive, but essential for understanding the lack of long-range symmetry in glasses and the effect of composition on glass structure. Two-dimensional 17O dynamic-angle-spinning nuclear magnetic resonance experiments reveal intermediate-range order in the distribution of inter-tetrahedral (Si-O-Si) bond angles and a high degree of order in the disposition of oxygen atoms around the network-modifying cations.
View details for Web of Science ID A1992JB34100043
View details for PubMedID 1614527
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NUCLEAR-MAGNETIC-RESONANCE SPECTROSCOPY OF GEOLOGICAL-MATERIALS
MRS BULLETIN
1992; 17 (5): 45-52
View details for Web of Science ID A1992HU96800005
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EFFECTS OF HIGH-TEMPERATURE ON SILICATE LIQUID STRUCTURE - A MULTINUCLEAR NMR-STUDY
SCIENCE
1992; 255 (5044): 586-589
Abstract
The structure of a silicate liquid changes with temperature, and this substantially affects its thermodynamic and transport properties. Models used by geochemists, geophysicists, and glass scientists need to include such effects. In situ, high-temperature nuclear magnetic resonance (NMR) spectroscopy on (23)Na, (27)A1, and (29)Si was used to help determine the time-averaged structure of a series of alkali aluminosilicate liquids at temperatures to 1320 degrees C. Isotropic chemical shifts for (29)Si increase (to higher frequencies) with increasing temperature, probably in response to intermediate-range structural changes such as the expansion of bonds between nonbridging oxygens and alkali cations. In contrast, isotropic chemical shifts for (27)Al decrease with increasing temperature, indicating that more significant short-range structural changes take place for aluminum, such as an increase in mean coordination number. The spectrum of a sodium aluminosilicate glass clearly indicates that at least a few percent of six-coordinated aluminum was present in the liquid at high temperature.
View details for Web of Science ID A1992HB53100039
View details for PubMedID 17792382
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X-RAY-POWDER DIFFRACTION AND NA-23, AL-27, AND SI-29 MAS-NMR INVESTIGATION OF NEPHELINE-KALSILITE CRYSTALLINE SOLUTIONS
AMERICAN MINERALOGIST
1992; 77 (1-2): 19-29
View details for Web of Science ID A1992HE61600003
- The structure and dynamics of alkali silicate liquids: a view from NMR spectroscopy Chemical Geology 1992: 371-385
- Characterization of crystalline and amorphous silicates quenched from high pressure by 29Si MAS NMR spectroscopy High Pressure Research in Mineral Physics: Applications to Earth and Planetary Sciences American Geophysical Union. 1992: 89–100
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NUCLEAR-MAGNETIC-RESONANCE AT HIGH-TEMPERATURE
CHEMICAL REVIEWS
1991; 91 (7): 1353-1373
View details for Web of Science ID A1991GP76400005
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NMR EVIDENCE FOR 5-COORDINATED SILICON IN A SILICATE GLASS AT ATMOSPHERIC-PRESSURE
NATURE
1991; 351 (6328): 638-639
View details for Web of Science ID A1991FT11200060
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CHARACTERIZATION OF QUENCHED HIGH-PRESSURE PHASES IN CASIO3 SYSTEM BY XRD AND SI-29 NMR
GEOPHYSICAL RESEARCH LETTERS
1991; 18 (3): 463-466
View details for Web of Science ID A1991FC74800028
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LOCAL-STRUCTURE AND CHEMICAL-SHIFTS FOR 6-COORDINATED SILICON IN HIGH-PRESSURE MANTLE PHASES
SCIENCE
1991; 251 (4991): 294-298
Abstract
Most of the earth's mantle is made up of high-pressure silicate minerals that contain octahedrally coordinated silicon (Si(VI)), but many thermodynamically important details of cation site ordering remain unknown. Silicon-29 nuclear magnetic resonance (NMR) spectroscopy is potentially very useful for determining short-range structure. A systematic study of silicon-29 chemical shifts for Si(VI) has revealed empirical correlations between shift and structure that are useful in understanding several new calcium silicates. The observed ordering state of a number of high-pressure magnesium silicates is consistent with the results of previous x-ray diffraction studies.
View details for Web of Science ID A1991ET67800027
View details for PubMedID 17733286
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HIGH-RESOLUTION O-17 NMR OF SOLID SILICATES
JOURNAL OF THE AMERICAN CHEMICAL SOCIETY
1991; 113 (1): 32-38
View details for Web of Science ID A1991ER08200006
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PRESSURE-INDUCED SILICON COORDINATION AND TETRAHEDRAL STRUCTURAL-CHANGES IN ALKALI OXIDE-SILICA MELTS UP TO 12 GPA - NMR, RAMAN, AND INFRARED-SPECTROSCOPY
AMERICAN MINERALOGIST
1991; 76 (1-2): 8-26
View details for Web of Science ID A1991FF65000002
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OBSERVATION OF SLOW ATOMIC MOTIONS CLOSE TO THE GLASS-TRANSITION USING 2-D SI-29 NMR
JOURNAL OF NON-CRYSTALLINE SOLIDS
1990; 124 (2-3): 207-215
View details for Web of Science ID A1990EG59200013
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HIGH-TEMPERATURE SI-29 NMR INVESTIGATION OF SOLID AND MOLTEN SILICATES
JOURNAL OF THE AMERICAN CHEMICAL SOCIETY
1990; 112 (1): 32-39
View details for Web of Science ID A1990CH31900008
- The structure of NaAlSi3O8 liquids at high pressure:new constraints from NMR spectroscopy Am. Mineral. 1990; 75 (943-946): 943-946
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ALUMINUM IN RUTILE (TIO2) - CHARACTERIZATION BY SINGLE-CRYSTAL AND MAGIC-ANGLE-SPINNING NUCLEAR MAGNETIC-RESONANCE
JOURNAL OF THE AMERICAN CERAMIC SOCIETY
1989; 72 (11): 2198-2200
View details for Web of Science ID A1989CA08300034
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SILICON COORDINATION AND SPECIATION CHANGES IN A SILICATE LIQUID AT HIGH-PRESSURES
SCIENCE
1989; 245 (4921): 962-964
Abstract
Coordination and local geometry around Si cations in silicate liquids are of primary importance in controlling the chemical and physical properties of magmas. Pressure-induced changes from fourfold to sixfold coordination of Si in silicate glass samples quenched from liquids has been detected with (29)Si magic-angle spinning nuclear magnetic resonance spectrometry. Samples of Na(2)Si(2)O(5) glass quenched from 8 gigapascals and 1500 degrees C contained about 1.5 percent octahedral Si, which was demonstrably part of a homogeneous, amorphous phase. The dominant tetrahedral Si speciation in these glasses became disproportionated to a more random distribution of bridging and nonbridging oxygens with increasing pressure.
View details for Web of Science ID A1989AM93300023
View details for PubMedID 17780537
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NUCLEAR MAGNETIC-RESONANCE SPECTROSCOPY IN THE EARTH SCIENCES - STRUCTURE AND DYNAMICS
SCIENCE
1989; 245 (4915): 257-263
Abstract
Detailed knowledge of the structure and dynamics of the materials that make up the earth is necessary for fundamental understanding of most geological processes. Nuclear magnetic resonance spectroscopy is beginning to play an important role in investigations of inorganic solid materials, as well as of liquids and organic compounds; it has already contributed substantially to our knowledge of minerals and rocks, compositionally simplified analogs of magmas, and the surfaces of silicate crystals. The technique is particularly useful for determining local structure and ordering state in crystals, glasses, and liquids, and is sensitive to atomic motion at the time scales of diffusion and viscosity in silicates. New techniques offer promise for increased resolution for quadrupolar nuclei and for extension of experiments to high temperature and pressure.
View details for Web of Science ID A1989AF96200020
View details for PubMedID 17834676
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LACK OF LOCAL STRUCTURAL ORIENTATION IN OXIDE GLASSES QUENCHED DURING FLOW - NMR RESULTS
JOURNAL OF NON-CRYSTALLINE SOLIDS
1989; 110 (1): 1-12
View details for Web of Science ID A1989AK30000001
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THE SI-29 NMR SHIELDING TENSOR IN LOW QUARTZ
AMERICAN MINERALOGIST
1989; 74 (7-8): 956-959
View details for Web of Science ID A1989AK86200033
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O-17 NMR IN SOLIDS BY DYNAMIC-ANGLE SPINNING AND DOUBLE ROTATION
NATURE
1989; 339 (6219): 42-43
View details for Web of Science ID A1989U445100054
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MAGIC ANGLE SPINNING NMR OBSERVATION OF SODIUM SITE EXCHANGE IN NEPHELINE AT 500-DEGREES-C
PHYSICS AND CHEMISTRY OF MINERALS
1989; 16 (8): 763-766
View details for Web of Science ID A1989CB81700007
- Five- and six- coordinated Si in K2Si4O9 glass quenched from 1.9 GPa and 1200 C American Mineralogist 1989; 74: 965-968
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DISORDERING AND THE PROGRESS OF HYDRATION AT THE SURFACE OF DIOPSIDE - A CROSS-POLARIZATION MAS-NMR STUDY
GEOCHIMICA ET COSMOCHIMICA ACTA
1988; 52 (12): 3017-3021
View details for Web of Science ID A1988R676600024
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EFFECTS OF TEMPERATURE AND COMPOSITION ON SILICATE GLASS STRUCTURE AND DYNAMICS - SI-29 NMR RESULTS
JOURNAL OF NON-CRYSTALLINE SOLIDS
1988; 106 (1-3): 359-369
View details for Web of Science ID A1988R384000073
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EFFECTS OF TEMPERATURE ON THE STRUCTURES OF SILICATE LIQUIDS - SI-29 NMR RESULTS
GEOCHIMICA ET COSMOCHIMICA ACTA
1988; 52 (11): 2659-2669
View details for Web of Science ID A1988R037200009
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DIFFUSIVE MOTION IN ALKALI SILICATE MELTS - AN NMR-STUDY AT HIGH-TEMPERATURE
GEOCHIMICA ET COSMOCHIMICA ACTA
1988; 52 (2): 527-538
View details for Web of Science ID A1988M310000028
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A SI-29 NUCLEAR MAGNETIC-RESONANCE STUDY OF SILICON-ALUMINUM ORDERING IN LEUCITE AND ANALCITE
PHYSICS AND CHEMISTRY OF MINERALS
1988; 15 (4): 370-382
View details for Web of Science ID A1988M683200009
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NMR-SPECTROSCOPY AND DYNAMIC PROCESSES IN MINERALOGY AND GEOCHEMISTRY
REVIEWS IN MINERALOGY
1988; 18: 405-429
View details for Web of Science ID A1988N680300010
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IDENTIFICATION OF MULTIPLE STRUCTURAL SPECIES IN SILICATE-GLASSES BY SI-29 NMR
NATURE
1987; 330 (6147): 465-467
Abstract
Knowledge of the structure of silicate glasses is one key to understanding their chemical and physical properties, as well as those of the high-temperature liquids from which they form. Because first-neighbour ordering into SiO4 tetrahedra is well known, much of the recent discussion about glass structure has concerned intermediate-range order. One of the most fundamental questions that can be posed is the distribution of silicate tetrahedra with n bridging oxygens (shared between two tetrahedra), labelled as 'Qn' (0 less than or equal to n less than or equal to 4). This distribution is probably important in determining the properties of melts and glasses, but considerable controversy exists concerning the identification and quantification of such species. Here I present new evidence from 29Si NMR (nuclear magnetic resonance) spectroscopy that clearly resolves one significant part of this dispute: at least in sodium silicate glasses, a variety of species is present that is greater than that required by composition alone.
View details for Web of Science ID A1987L083900057
View details for PubMedID 2825026
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SPECIATION AND LOCAL-STRUCTURE IN ALKALI AND ALKALINE-EARTH SILICATE-GLASSES - CONSTRAINTS FROM SI-29 NMR-SPECTROSCOPY
JOURNAL OF NON-CRYSTALLINE SOLIDS
1987; 89 (3): 371-383
View details for Web of Science ID A1987G515500011
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RELAXATION MECHANISMS AND EFFECTS OF MOTION IN ALBITE (NAALSI3O8) LIQUID AND GLASS - A HIGH-TEMPERATURE NMR-STUDY
PHYSICS AND CHEMISTRY OF MINERALS
1987; 15 (2): 155-162
View details for Web of Science ID A1987L016700007
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PHASE-TRANSITIONS IN LEUCITE (KALSI2O6), ORTHORHOMBIC KALSIO4, AND THEIR IRON ANALOGS (KFESI2O6, KFESIO4)
AMERICAN MINERALOGIST
1986; 71 (7-8): 937-945
View details for Web of Science ID A1986D803800007
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DENSITY OF MOLTEN SODIUM ALUMINOSILICATES
JOURNAL OF THE AMERICAN CERAMIC SOCIETY
1986; 69 (5): 396-399
View details for Web of Science ID A1986C250000005
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NEW PROBE FOR HIGH-TEMPERATURE NMR-SPECTROSCOPY WITH PPM RESOLUTION
REVIEW OF SCIENTIFIC INSTRUMENTS
1986; 57 (1): 39-42
View details for Web of Science ID A1986AXA2000010
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DEFECTS AND SHORT-RANGE ORDER IN NEPHELINE GROUP MINERALS - A SI-29 NUCLEAR-MAGNETIC-RESONANCE STUDY
PHYSICS AND CHEMISTRY OF MINERALS
1986; 13 (6): 371-381
View details for Web of Science ID A1986E631100003
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A HIGH-TEMPERATURE HIGH-RESOLUTION NMR-STUDY OF NA-23, AL-27 AND SI-29 IN MOLTEN SILICATES
NATURE
1985; 314 (6008): 250-252
View details for Web of Science ID A1985ADT9900039
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HIGH-RESOLUTION SI-29 NMR-STUDY OF SILICATE AND ALUMINOSILICATE GLASSES - THE EFFECT OF NETWORK-MODIFYING CATIONS
AMERICAN MINERALOGIST
1985; 70 (3-4): 332-343
View details for Web of Science ID A1985AGG2200010
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HEAT-CAPACITIES AND ENTROPIES OF SILICATE LIQUIDS AND GLASSES
CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
1984; 86 (2): 131-148
View details for Web of Science ID A1984ST62100003
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THE HEAT OF FUSION OF FAYALITE
AMERICAN MINERALOGIST
1984; 69 (3-4): 292-297
View details for Web of Science ID A1984SN19300009
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THE HIGH-TEMPERATURE LIQUID AND GLASS HEAT CONTENTS AND THE HEATS OF FUSION OF DIOPSIDE, ALBITE, SANIDINE AND NEPHELINE
AMERICAN MINERALOGIST
1983; 68 (7-8): 717-730
View details for Web of Science ID A1983RF01300004
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SOME THERMODYNAMIC AND EXPERIMENTAL CONSTRAINTS ON THE MELTING OF ALBITE AT ATMOSPHERIC AND HIGH-PRESSURE
JOURNAL OF GEOLOGY
1982; 90 (6): 679-698
View details for Web of Science ID A1982PQ57100004
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THE PARTIAL MOLAR VOLUME OF FE2O3 IN MULTICOMPONENT SILICATE LIQUIDS AND THE PRESSURE-DEPENDENCE OF OXYGEN FUGACITY IN MAGMAS
MINERALOGICAL MAGAZINE
1982; 45: 237-245
View details for Web of Science ID A1982PH45700027
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HIGH-TEMPERATURE HEAT CONTENTS AND HEAT-CAPACITIES OF LIQUIDS AND GLASSES IN THE SYSTEM NAALSI3O8-CAAL2SI2O8
CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
1982; 80 (3): 276-284
View details for Web of Science ID A1982PP41600008
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THE ENTHALPY OF FUSION OF ANORTHITE
CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
1980; 74 (1): 95-102
View details for Web of Science ID A1980KL38200011
- The nature and petrogenesis of intra-oceanic plate alkaline eruptive and plutonic rocks: King's Trough, Northeast Atlantic J. Volcan. and Geotherm. 1978; 4: 333-361