Abstract
Here we introduce a technique for simultaneous measurement of surface normal retreat rates of specific cleavage faces by vertical scanning interferometry and the bulk dissolution rate of a mineral powder. A hydrothermal reactor is used to contain both a well-characterized powder and oriented single crystals with a masked reference surface at elevated temperatures. We show examples using both anorthite and albite reacted at temperatures between 150 and 200 °C. In the case of albite, dissolution rates of fine-grained powders are substantially enhanced compared to those prevailing on large single-crystal cleavage surfaces. Rates developed on the (010) albite cleavage surface are also substantially faster than those on the (001) face, where etch-pit development was relatively modest and surface normal retreat was not detectable within the time frame of the experiment. The reasons for this difference are not immediately clear, but may be related to anisotropy in the distribution of Al-O-Si vs. Si-O-Si bonds in the albite structure, (010) twinning expressed on the (001) surface, and possible disruption of kink propagation across the twin plane.
© 2015 by Walter de Gruyter Berlin/Boston
Articles in the same Issue
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Articles in the same Issue
- Indialite in xenolithic rocks from Somma-Vesuvius volcano (Southern Italy): Crystal chemistry and petrogenetic features
- Coexisting chromian omphacite and diopside in tremolite schist from the Chugoku Mountains, SW Japan: The effect of Cr on the omphacite-diopside immiscibility gap
- 2111 biopyribole intermediate between pyroxene and amphibole: Artifact or natural product?
- Coexisting clinopyroxene/spinel and amphibole/spinel symplectites in metatroctolites from the Buck Creek ultramafic body, North Carolina Blue Ridge
- The T-X dependence of the isosymmetric displacive phase transition in synthetic Fe3+-Al zoisite: A temperature-dependent infrared spectroscopy study
- A kinetic study of the exsolution of pentlandite (Ni,Fe)9S8from the monosulfide solid solution (Fe,Ni)S
- Single-crystal plagioclase feldspar dissolution rates measured by vertical scanning interferometry
- A simple empirical method for high-quality electron microprobe analysis of fluorine at trace levels in Fe-bearing minerals and glasses
- Constraints on mingling of crystal populations from off-center zoning profiles: A statistical approach
- Pyribole evolution during tremolite synthesis from oxides
- Solution calorimetric determination of the enthalpies of formation of NH4-bearing minerals buddingtonite and tobelite
- Dehydration dynamics of bikitaite: Part I. In situ synchrotron powder X-ray diffraction study
- Dehydration dynamics of bikitaite: Part II. Ab initio molecular dynamics study
- Phosphate mineral associations in the Cañada pegmatite (Salamanca, Spain): Paragenetic relationships, chemical compositions, and implications for pegmatite evolution
- An improved equation for crystal size distribution in second-phase influenced aggregates
- Vibrational spectroscopy of pyrope-majorite garnets: Structural implications
- The modulated crystal structure of antigorite: The m = 17 polysome
- Structural variations in mercurian tetrahedrite
- A computational investigation of the Al/Fe/Mg order-disorder behavior in the dioctahedral sheet of phyllosilicates
- Investigation of Al/Si ordering in tetrahedral phyllosilicate sheets by Monte Carlo simulation
- Equations of state of ZrSiO4phases in the upper mantle
- High pressure behavior, transformation and crystal structure of synthetic iron-free pigeonite
- In situ determination of the compressibility of synthetic pure zircon (ZrSiO4) and the onset of the zircon-reidite phase transition
- Halite-sylvite thermoelasticity
- Spiral growth of grossular under hydrothermal conditions
- Incomplete retention of radiation damage in zircon from Sri Lanka
- Shirozulite, KMn32+(Si3Al)O10(OH)2, a new manganese-dominant trioctahedral mica: Description and crystal structure
- Novel phase transition in orthoenstatite
- In situ observation of the thermal decomposition of weddelite by heating stage environmental scanning electron microscopy