{"title":"方解石解理上的无位错热蚀坑","authors":"A.J. Shah, J.R. Pandya","doi":"10.1016/0376-4583(85)90048-2","DOIUrl":null,"url":null,"abstract":"<div><p>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 <em>V</em><sub>t</sub> and <em>V</em><sub>s</sub> of the tangential dissolution of ledges and the surface dissolution respectively were determined in the above temperature range. The activation energies <em>E</em><sub>t th</sub> and <em>E</em><sub>s th</sub> 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.</p></div>","PeriodicalId":22037,"journal":{"name":"Surface Technology","volume":"25 1","pages":"Pages 59-64"},"PeriodicalIF":0.0000,"publicationDate":"1985-05-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0376-4583(85)90048-2","citationCount":"0","resultStr":"{\"title\":\"Non-dislocation thermal etch pits on calcite cleavages\",\"authors\":\"A.J. Shah, J.R. Pandya\",\"doi\":\"10.1016/0376-4583(85)90048-2\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>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 <em>V</em><sub>t</sub> and <em>V</em><sub>s</sub> of the tangential dissolution of ledges and the surface dissolution respectively were determined in the above temperature range. The activation energies <em>E</em><sub>t th</sub> and <em>E</em><sub>s th</sub> 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.</p></div>\",\"PeriodicalId\":22037,\"journal\":{\"name\":\"Surface Technology\",\"volume\":\"25 1\",\"pages\":\"Pages 59-64\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1985-05-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/0376-4583(85)90048-2\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Surface Technology\",\"FirstCategoryId\":\"1087\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/0376458385900482\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Surface Technology","FirstCategoryId":"1087","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/0376458385900482","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
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.