Abstract
We have investigated the thermal expansion of several synthetic feldspars, including Li-feldspar, rubicline (Rb-microcline), Rb-sanidine, and buddingtonite (NH4-feldspar). When analyzed in conjunction with earlier data on both ordered and disordered Na- and K-feldspars, it is clear that the coefficient of thermal expansion (α) decreases dramatically, and linearly, with increasing room-temperature volume. For “AlSi3” feldspars, then, chemical expansion limits thermal expansion. The relationship between α and room-temperature volume provides a useful predictive tool based simply on the volume of a feldspar at room temperature. This relationship also reveals that volumes of K-Na mixing in naturally occurring alkali feldspars decrease with increasing temperature.
© 2015 by Walter de Gruyter Berlin/Boston
Articles in the same Issue
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- Amorphous materials: Properties, structure, and durability: Quantitative Raman spectroscopy: Speciation of Na-silicate glasses and melts
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- High-pressure behavior of gypsum: A single-crystal X-ray study
- Presence and zoning of hydrous components in leucite from the Alban Hills volcano, Rome, Italy
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- A simple predictive model for the thermal expansion of AlSi3 feldspars
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- High-pressure study on lead fluorapatite
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- Leucite at high pressure: Elastic behavior, phase stability, and petrological implications
- Thermodynamic mixing properties of Rb-K feldspars
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- A lattice dynamical study of the aragonite and post-aragonite phases of calcium carbonate rock
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- Factors affecting heat transfer in natural SiO2 solids
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Articles in the same Issue
- Amorphous materials: Properties, structure, and durability: Atomic structure and transport properties of MgO-Al2O3 melts: A molecular dynamics simulation study
- Amorphous Materials: Properties, structure, and durability: Oxidation state of iron in hydrous phono-tephritic melts
- Amorphous materials: Properties, structure, and durability: Quantitative Raman spectroscopy: Speciation of Na-silicate glasses and melts
- Dissolution-reprecipitation of zircon at low-temperature, high-pressure conditions (Lanzo Massif, Italy)
- High-pressure behavior of gypsum: A single-crystal X-ray study
- Presence and zoning of hydrous components in leucite from the Alban Hills volcano, Rome, Italy
- Herderite from Mogok, Myanmar, and comparison with hydroxyl-herderite from Ehrenfriedersdorf, Germany
- Application of Raman spectroscopy to quantify trace water concentrations in glasses and garnets
- Neutron diffraction study of δ-AlOOD at high pressure and its implication for symmetrization of the hydrogen bond
- A simple predictive model for the thermal expansion of AlSi3 feldspars
- New data on PGE alloy minerals from a very old collection (probably 1890s), California
- High-pressure study on lead fluorapatite
- High-pressure Al-rich hexagonal phases—What are their kin?
- Leucite at high pressure: Elastic behavior, phase stability, and petrological implications
- Thermodynamic mixing properties of Rb-K feldspars
- Demicheleite, BiSBr, a new mineral from La Fossa crater, Vulcano, Aeolian Islands, Italy
- A lattice dynamical study of the aragonite and post-aragonite phases of calcium carbonate rock
- Water in natural olivine—determined by proton-proton scattering analysis
- Factors affecting heat transfer in natural SiO2 solids
- A solution model for high-temperature PbS-AgSbS2-AgBiS2 galena
- Incorporation of molybdate anion into β-FeOOH
- Disordering of Fe2+ over octahedrally coordinated sites of tourmaline
- Raman spectroscopy of CaIrO3 postperovskite up to 30 GPa
- The thermal behavior of richterite
- The crystal structure of kelyanite, (Hg2)6(SbO6)BrCl2
- Comparison of crystallographic orientations between living (Emiliania huxleyi and Gephyrocapsa oceanica) and fossil (Watznaueria barnesiae) coccoliths using electron microscopes
- Letter. Iron partitioning between perovskite and post-perovskite: A transmission electron microscope study
- Letter. An isosymmetric phase transition of orthopyroxene found by high-temperature X-ray diffraction