{"title":"Stress-Induced Effects in the Incommensurate Phase of Quartz","authors":"M. Vallade, M. Petit","doi":"10.1002/PSSA.2211110116","DOIUrl":null,"url":null,"abstract":"The stress-induced changes of the amplitudes and of the modulation wave-vectors of the “triple-q” incommensurate phase of quartz-like crystals are calculated using a phenomenological theory, in the small stress limit. The temperature dependence of these changes and in particular their behaviour at the “triple-q”-“single-q” transition are also discussed. \n \n \n \nLes changements des amplitudes et des vecteurs d'onde de modulation induits par une contrainte dans la phase incommensurable „triple-q” de cristaux du type du quartz sont calcules en utilisant une theorie phenomenologique, dans la limite des faibles contraintes. La dependance en temperature de ces changements, et en particulier leur comportement a la transition „triple-q”-„mono-q” sont egalement discutes.","PeriodicalId":240242,"journal":{"name":"16 January","volume":"55 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1989-01-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"16 January","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1002/PSSA.2211110116","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1
Abstract
The stress-induced changes of the amplitudes and of the modulation wave-vectors of the “triple-q” incommensurate phase of quartz-like crystals are calculated using a phenomenological theory, in the small stress limit. The temperature dependence of these changes and in particular their behaviour at the “triple-q”-“single-q” transition are also discussed.
Les changements des amplitudes et des vecteurs d'onde de modulation induits par une contrainte dans la phase incommensurable „triple-q” de cristaux du type du quartz sont calcules en utilisant une theorie phenomenologique, dans la limite des faibles contraintes. La dependance en temperature de ces changements, et en particulier leur comportement a la transition „triple-q”-„mono-q” sont egalement discutes.