{"title":"Quantitative Interpretation of Isotope Correlation Coefficient Ratios in Solid Diffusion","authors":"Yuxi Jing","doi":"10.22158/asir.v6n4p124","DOIUrl":null,"url":null,"abstract":"The correlation coefficient f is crucial in the calculation of the absolute diffusion coefficient D, especially for the vacancy mechanism. The current study for f is complex and contains many approximations and assumptions. However, f can be ignored when considering the isotope effect, which has only been stated qualitatively by previous authors and not explained from a quantitative perspective. In this paper, we will explain the reason why f can be neglected in the isotope diffusion effect by finding the most essential formula and source of f, as a way to save the most troublesome step in the calculation of the isotope diffusion effect.","PeriodicalId":356167,"journal":{"name":"Applied Science and Innovative Research","volume":"39 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2022-11-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Applied Science and Innovative Research","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.22158/asir.v6n4p124","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
The correlation coefficient f is crucial in the calculation of the absolute diffusion coefficient D, especially for the vacancy mechanism. The current study for f is complex and contains many approximations and assumptions. However, f can be ignored when considering the isotope effect, which has only been stated qualitatively by previous authors and not explained from a quantitative perspective. In this paper, we will explain the reason why f can be neglected in the isotope diffusion effect by finding the most essential formula and source of f, as a way to save the most troublesome step in the calculation of the isotope diffusion effect.