方解石解理上的无位错热蚀坑

A.J. Shah, J.R. Pandya
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引用次数: 0

摘要

在540 ~ 625℃的空气中,在天然方解石晶体解理面上观察到具有菱形轮廓的热蚀坑。在此温度范围内,分别测定了切向溶解和表面溶解的热腐蚀速率Vt和v。分别计算了切向热溶解和表面热溶解的活化能Et和Es,并与方解石解理上产生位错蚀坑的受控化学溶解的活化能Et和Es进行了比较。活化能的定量研究表明,方解石解理面上的热蚀坑起源于无位错的位置,如扭结、台阶和/或杂质中心。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Non-dislocation thermal etch pits on calcite cleavages

Thermal etch pits with rhombic outlines on the cleavage surfaces of natural calcite crystals are observed in a narrow range of etching temperature between 540 and 625 °C in air. The thermal etch rates Vt and Vs of the tangential dissolution of ledges and the surface dissolution respectively were determined in the above temperature range. The activation energies Et th and Es th of tangential thermal dissolution and surface thermal dissolution respectively are calculated and are compared with those of controlled chemical dissolution initiated to produce dislocation etch pits on calcite cleavages. A quantitative study of the activation energies suggests that the thermal etch pits on calcite cleavage faces originate at dislocation-free sites such as kinks, steps and/or impurity centres.

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