{"title":"氧化铁纳米粒子的摩斯鲍尔研究","authors":"Christina Karra, Charalampos Sarafidis","doi":"10.1002/appl.202400008","DOIUrl":null,"url":null,"abstract":"<p>Magnetic nanoparticles have recently attracted attention for biochemical and medical applications like drug delivery and hyperthermia for a variety of reasons with most important being their stability, chemical compatibility, and suitable magnetic properties like moderate specific mass magnetization. Cobalt ferrites are a well-studied family of materials and the partial substitution of Fe<sup>3+</sup> cations by rare earth (RE) ones may be used to tune the magnetic properties. In the present work pure and substituted Co ferrite nanoparticles with nominal stoichiometry CoFe<sub>2−<i>x</i></sub>R<sub><i>x</i></sub>O<sub>4</sub> (R = Yb, Gd; <i>x</i> = 0.05, 0.1, 0.3) synthesized by the co-precipitation method are studied with <sup>57</sup>Fe Mössbauer spectroscopy to determine the incorporation of RE ions in the spinel lattice. The fitting procedure was based on the standard spinel model using two sextets for the octahedral and the tetrahedral coordinated positions of Fe atoms. All isomer shift values were found within the typical range of high spin ferric ions while quadrupole splitting values strongly suggest that there is a substitution preference; RE ions replace iron ones in octahedral sites. The inversion parameter was found to decrease with RE content (lowest value about 0.534 for CoFe<sub>1.90</sub>Yb<sub>0.10</sub>O<sub>4</sub>) and thermal treatment always results in changing the material toward normal spinel, while pure CoFe<sub>2</sub>O<sub>4</sub> was inverse. Thermal treatment of substituted materials in ambient air at temperature range 1500–1700 K for 12 h increase crystallite size and changes the degree of inversion.</p>","PeriodicalId":100109,"journal":{"name":"Applied Research","volume":"3 6","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-05-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/appl.202400008","citationCount":"0","resultStr":"{\"title\":\"Mössbauer study of iron oxide nanoparticles\",\"authors\":\"Christina Karra, Charalampos Sarafidis\",\"doi\":\"10.1002/appl.202400008\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>Magnetic nanoparticles have recently attracted attention for biochemical and medical applications like drug delivery and hyperthermia for a variety of reasons with most important being their stability, chemical compatibility, and suitable magnetic properties like moderate specific mass magnetization. Cobalt ferrites are a well-studied family of materials and the partial substitution of Fe<sup>3+</sup> cations by rare earth (RE) ones may be used to tune the magnetic properties. In the present work pure and substituted Co ferrite nanoparticles with nominal stoichiometry CoFe<sub>2−<i>x</i></sub>R<sub><i>x</i></sub>O<sub>4</sub> (R = Yb, Gd; <i>x</i> = 0.05, 0.1, 0.3) synthesized by the co-precipitation method are studied with <sup>57</sup>Fe Mössbauer spectroscopy to determine the incorporation of RE ions in the spinel lattice. The fitting procedure was based on the standard spinel model using two sextets for the octahedral and the tetrahedral coordinated positions of Fe atoms. All isomer shift values were found within the typical range of high spin ferric ions while quadrupole splitting values strongly suggest that there is a substitution preference; RE ions replace iron ones in octahedral sites. The inversion parameter was found to decrease with RE content (lowest value about 0.534 for CoFe<sub>1.90</sub>Yb<sub>0.10</sub>O<sub>4</sub>) and thermal treatment always results in changing the material toward normal spinel, while pure CoFe<sub>2</sub>O<sub>4</sub> was inverse. Thermal treatment of substituted materials in ambient air at temperature range 1500–1700 K for 12 h increase crystallite size and changes the degree of inversion.</p>\",\"PeriodicalId\":100109,\"journal\":{\"name\":\"Applied Research\",\"volume\":\"3 6\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2024-05-18\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://onlinelibrary.wiley.com/doi/epdf/10.1002/appl.202400008\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Applied Research\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://onlinelibrary.wiley.com/doi/10.1002/appl.202400008\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Applied Research","FirstCategoryId":"1085","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1002/appl.202400008","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
摘要
近来,磁性纳米粒子在生化和医疗领域(如药物输送和热疗)的应用备受关注,原因有很多,其中最重要的是其稳定性、化学兼容性和合适的磁性,如适度的比质量磁化。钴铁氧体是一种经过深入研究的材料,用稀土(RE)阳离子部分取代 Fe3+ 阳离子可用于调整磁性能。本研究采用共沉淀法合成了纯钴铁氧体纳米颗粒和替代钴铁氧体纳米颗粒,其标称化学计量为 CoFe2-xRxO4(R = Yb、Gd;x = 0.05、0.1、0.3),并利用 57Fe 莫斯堡尔光谱进行了研究,以确定尖晶石晶格中 RE 离子的加入情况。拟合过程基于标准尖晶石模型,使用两个六面体分别表示铁原子的八面体和四面体配位位置。发现所有异构体偏移值都在高自旋铁离子的典型范围内,而四极分裂值则强烈表明存在一种替代偏好;RE 离子取代了八面体位点上的铁离子。研究发现,反转参数随 RE 含量的增加而减小(CoFe1.90Yb0.10O4 的最低值约为 0.534),热处理总是导致材料向正常尖晶石方向转变,而纯 CoFe2O4 则呈反转状态。在 1500-1700 K 的温度范围内,在环境空气中对替代材料进行 12 小时的热处理,可增加晶粒尺寸并改变反转程度。本文受版权保护。
Magnetic nanoparticles have recently attracted attention for biochemical and medical applications like drug delivery and hyperthermia for a variety of reasons with most important being their stability, chemical compatibility, and suitable magnetic properties like moderate specific mass magnetization. Cobalt ferrites are a well-studied family of materials and the partial substitution of Fe3+ cations by rare earth (RE) ones may be used to tune the magnetic properties. In the present work pure and substituted Co ferrite nanoparticles with nominal stoichiometry CoFe2−xRxO4 (R = Yb, Gd; x = 0.05, 0.1, 0.3) synthesized by the co-precipitation method are studied with 57Fe Mössbauer spectroscopy to determine the incorporation of RE ions in the spinel lattice. The fitting procedure was based on the standard spinel model using two sextets for the octahedral and the tetrahedral coordinated positions of Fe atoms. All isomer shift values were found within the typical range of high spin ferric ions while quadrupole splitting values strongly suggest that there is a substitution preference; RE ions replace iron ones in octahedral sites. The inversion parameter was found to decrease with RE content (lowest value about 0.534 for CoFe1.90Yb0.10O4) and thermal treatment always results in changing the material toward normal spinel, while pure CoFe2O4 was inverse. Thermal treatment of substituted materials in ambient air at temperature range 1500–1700 K for 12 h increase crystallite size and changes the degree of inversion.