S. Tomura, Yasuo Shibasaki, Hiroyuki Mizuta, T. Maeda
{"title":"球形高岭石中莫来石的析出","authors":"S. Tomura, Yasuo Shibasaki, Hiroyuki Mizuta, T. Maeda","doi":"10.2109/JCERSJ1950.94.1092_917","DOIUrl":null,"url":null,"abstract":"of mullite from the spherical kaolinite at 900°-1400℃ has been studied by means of electron microscopy and powder X-ray diffractometry. The starting kaolinite which has spherical shape with concentric layering has been synthe under hydrothermal condition. The following results in were to the difference in lattice deformation of the kaolinite","PeriodicalId":17274,"journal":{"name":"Journal of the Ceramic Association, Japan","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"1986-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"Exsolution of Mullite from Spherical Kaolinite\",\"authors\":\"S. Tomura, Yasuo Shibasaki, Hiroyuki Mizuta, T. Maeda\",\"doi\":\"10.2109/JCERSJ1950.94.1092_917\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"of mullite from the spherical kaolinite at 900°-1400℃ has been studied by means of electron microscopy and powder X-ray diffractometry. The starting kaolinite which has spherical shape with concentric layering has been synthe under hydrothermal condition. The following results in were to the difference in lattice deformation of the kaolinite\",\"PeriodicalId\":17274,\"journal\":{\"name\":\"Journal of the Ceramic Association, Japan\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1986-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of the Ceramic Association, Japan\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.2109/JCERSJ1950.94.1092_917\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of the Ceramic Association, Japan","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.2109/JCERSJ1950.94.1092_917","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
of mullite from the spherical kaolinite at 900°-1400℃ has been studied by means of electron microscopy and powder X-ray diffractometry. The starting kaolinite which has spherical shape with concentric layering has been synthe under hydrothermal condition. The following results in were to the difference in lattice deformation of the kaolinite
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