{"title":"氧化学计量学对磁铁矿磁晶各向异性的影响","authors":"E.M. Gyorgy, H.M. O'Bryan Jr.","doi":"10.1016/0031-9163(66)90382-9","DOIUrl":null,"url":null,"abstract":"<div><p>Data are presented to show that |<em>K</em><sub>1</sub>| of magnetite decreases with decreasing Fe<sup>2+</sup> content. Recently published results which indicate an opposite behavior are discussed.</p></div>","PeriodicalId":101027,"journal":{"name":"Physics Letters","volume":"23 9","pages":"Pages 513-514"},"PeriodicalIF":0.0000,"publicationDate":"1966-11-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0031-9163(66)90382-9","citationCount":"9","resultStr":"{\"title\":\"The effect of oxygen stoichiometry on the magneto-crystalline anisotropy of magnetite\",\"authors\":\"E.M. Gyorgy, H.M. O'Bryan Jr.\",\"doi\":\"10.1016/0031-9163(66)90382-9\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Data are presented to show that |<em>K</em><sub>1</sub>| of magnetite decreases with decreasing Fe<sup>2+</sup> content. Recently published results which indicate an opposite behavior are discussed.</p></div>\",\"PeriodicalId\":101027,\"journal\":{\"name\":\"Physics Letters\",\"volume\":\"23 9\",\"pages\":\"Pages 513-514\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1966-11-28\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/0031-9163(66)90382-9\",\"citationCount\":\"9\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Physics Letters\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/0031916366903829\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Physics Letters","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/0031916366903829","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
The effect of oxygen stoichiometry on the magneto-crystalline anisotropy of magnetite
Data are presented to show that |K1| of magnetite decreases with decreasing Fe2+ content. Recently published results which indicate an opposite behavior are discussed.
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