Abstract
The mineral lawsonite, CaAl2Si2O7(OH)2⋅H2O, was deuterated to about 93% in a thermobalance by H2O-D2O gas-phase exchange at temperatures between 375 and 425 °C. The kinetics of this reaction are reported and diffusion coefficients for the H2O-D2O exchange are calculated from thermogravimetric measurements.
Received: 2000-7-12
Accepted: 2001-6-20
Published Online: 2015-3-26
Published in Print: 2001-10-1
© 2015 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
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- Geochemical modeling of bacterially induced mineralization of schwertmannite and jarosite in sulfuric acid spring water
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Articles in the same Issue
- Recalibration of the GASP geobarometer in light of recent garnet and plagioclase activity models and versions of the garnet-biotite geothermometer
- Compositional zoning and element partitioning in nickeloan tourmaline from a metamorphosed karstbauxite from Samos, Greece
- Occurrence of apatite associated with magnetite in an ophiolite complex (Othrys), Greece
- Overpressures induced by coesite-quartz transition in zircon
- Geochemical modeling of bacterially induced mineralization of schwertmannite and jarosite in sulfuric acid spring water
- H2O-D2O exchange in lawsonite
- Composition and temperature dependence of cation ordering in Ni-Mg olivine solid solutions: a time-of-flight neutron powder diffraction and EXAFS study
- Thermal conductivity of spinels and olivines from vibrational spectroscopy: Ambient conditions
- Elasticity of six polycrystalline silicate garnets at pressure up to 3.0 GPa
- The crystal chemistry of birefringent natural uvarovites: Part I. Optical investigations and UV-VIS-IR absorption spectroscopy
- The crystal chemistry of birefringent natural uvarovites: Part II. Single-crystal X-ray structures
- Ferroanthophyllite in Rockport grunerite: A transmission electron microscopy study
- Crystal structure of a new (21)-clinopyribole synthesized at high temperature and pressure
- The Mg(Fe)SiO3 orthoenstatite-clinoenstatite transitions at high pressures and temperatures determined by Raman-spectroscopy on quenched samples
- Raman spectroscopic studies of phase E to 19 GPa
- The crystal structures of the low-temperature phases of leonite-type compounds, K2Me(SO4)2·4H2O (Me2+ = Mg, Mn, Fe)
- Carraraite and zaccagnaite, two new minerals from the Carrara marble quarries: their chemical compositions, physical properties, and structural features
- Pristine surface growth features on 100 Ma garnet phenocrysts: Interference imaging results
- Oxygen triclusters in crystalline CaAl4O7 (grossite) and in calcium aluminosilicate glasses: 17O NMR
- Low-temperature heat capacity of pentlandite
- Calcium segregation at antiphase boundaries in pigeonite