{"title":"镧、镝和铋的非晶铁氧体结构","authors":"A.I. Rykov, Yu.t. Pavlukhin, N.I. Syrotina, V.V. Boldyrev","doi":"10.1016/0168-7336(89)80004-X","DOIUrl":null,"url":null,"abstract":"<div><p>Mechanical activation of the lanthanum, dysprosium, and bismuth morphotropic series of ferrites with perovskite structure leads to the formation of amorphous materials. Mössbauer spectra indicate lowering of the Fe<sup>3+</sup> coordination number on amorphization. X-ray diffraction reveals the changes in the short-range order of the arrangement of the heavy cations with respect to the starting crystalline samples, as well as structural differences between the amorphous ferrites. The structure of the amorphous LaFeO<sub>3</sub> can be described as quasicrystalline with trigonal-prismatic La<sup>3+</sup> configuration. Structural differences between the amorphous samples are due to distortions in the perovskite cells of the original crystal namely: an ionic misfit in DyFeO<sub>3</sub>, and covalency of the chemical bonds in BiFeO<sub>3</sub>.</p></div>","PeriodicalId":101061,"journal":{"name":"Reactivity of Solids","volume":"7 1","pages":"Pages 29-42"},"PeriodicalIF":0.0000,"publicationDate":"1989-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0168-7336(89)80004-X","citationCount":"3","resultStr":"{\"title\":\"Structure of amorphous ferrites of lanthanum, dysprosium, and bismuth\",\"authors\":\"A.I. Rykov, Yu.t. Pavlukhin, N.I. Syrotina, V.V. Boldyrev\",\"doi\":\"10.1016/0168-7336(89)80004-X\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Mechanical activation of the lanthanum, dysprosium, and bismuth morphotropic series of ferrites with perovskite structure leads to the formation of amorphous materials. Mössbauer spectra indicate lowering of the Fe<sup>3+</sup> coordination number on amorphization. X-ray diffraction reveals the changes in the short-range order of the arrangement of the heavy cations with respect to the starting crystalline samples, as well as structural differences between the amorphous ferrites. The structure of the amorphous LaFeO<sub>3</sub> can be described as quasicrystalline with trigonal-prismatic La<sup>3+</sup> configuration. Structural differences between the amorphous samples are due to distortions in the perovskite cells of the original crystal namely: an ionic misfit in DyFeO<sub>3</sub>, and covalency of the chemical bonds in BiFeO<sub>3</sub>.</p></div>\",\"PeriodicalId\":101061,\"journal\":{\"name\":\"Reactivity of Solids\",\"volume\":\"7 1\",\"pages\":\"Pages 29-42\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1989-04-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/0168-7336(89)80004-X\",\"citationCount\":\"3\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Reactivity of Solids\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/016873368980004X\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Reactivity of Solids","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/016873368980004X","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Structure of amorphous ferrites of lanthanum, dysprosium, and bismuth
Mechanical activation of the lanthanum, dysprosium, and bismuth morphotropic series of ferrites with perovskite structure leads to the formation of amorphous materials. Mössbauer spectra indicate lowering of the Fe3+ coordination number on amorphization. X-ray diffraction reveals the changes in the short-range order of the arrangement of the heavy cations with respect to the starting crystalline samples, as well as structural differences between the amorphous ferrites. The structure of the amorphous LaFeO3 can be described as quasicrystalline with trigonal-prismatic La3+ configuration. Structural differences between the amorphous samples are due to distortions in the perovskite cells of the original crystal namely: an ionic misfit in DyFeO3, and covalency of the chemical bonds in BiFeO3.