{"title":"MnO-TeO2体系的相平衡","authors":"Y.Y. Ivanova","doi":"10.1016/0390-6035(82)90088-8","DOIUrl":null,"url":null,"abstract":"<div><p>Glass formation and phase equilibria of the MnO-TeO<sub>2</sub> system in the 0 to 50 mol% MnO range are studied. It is found that the glass-formation region in air is larger than in an inert atmosphere and varies within 10 to 37 mol% MnO.</p><p>The existence of four tellurites of manganese is confirmed and the nature of their melting is established.</p></div>","PeriodicalId":18221,"journal":{"name":"Materials Chemistry","volume":"7 4","pages":"Pages 449-453"},"PeriodicalIF":0.0000,"publicationDate":"1982-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0390-6035(82)90088-8","citationCount":"3","resultStr":"{\"title\":\"Phase equilibria in the MnO-TeO2 system\",\"authors\":\"Y.Y. Ivanova\",\"doi\":\"10.1016/0390-6035(82)90088-8\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Glass formation and phase equilibria of the MnO-TeO<sub>2</sub> system in the 0 to 50 mol% MnO range are studied. It is found that the glass-formation region in air is larger than in an inert atmosphere and varies within 10 to 37 mol% MnO.</p><p>The existence of four tellurites of manganese is confirmed and the nature of their melting is established.</p></div>\",\"PeriodicalId\":18221,\"journal\":{\"name\":\"Materials Chemistry\",\"volume\":\"7 4\",\"pages\":\"Pages 449-453\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1982-07-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/0390-6035(82)90088-8\",\"citationCount\":\"3\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Materials Chemistry\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/0390603582900888\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Materials Chemistry","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/0390603582900888","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Glass formation and phase equilibria of the MnO-TeO2 system in the 0 to 50 mol% MnO range are studied. It is found that the glass-formation region in air is larger than in an inert atmosphere and varies within 10 to 37 mol% MnO.
The existence of four tellurites of manganese is confirmed and the nature of their melting is established.