压力对磁铁矿居里温度的影响:随机交换相互作用场法

IF 0.7 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
V. I. Belokon, O. I. Dyachenko, O. A. Gorodnikov, A. D. Burtsev
{"title":"压力对磁铁矿居里温度的影响:随机交换相互作用场法","authors":"V. I. Belokon,&nbsp;O. I. Dyachenko,&nbsp;O. A. Gorodnikov,&nbsp;A. D. Burtsev","doi":"10.1134/S1069351326700011","DOIUrl":null,"url":null,"abstract":"<p>The effect of pressure on the Curie temperature of magnetite is examined using the random exchange interaction field method. It is known that compression of the crystal lattice leads to increased overlap of electronic orbitals, which enhances exchange interaction and increases the Curie temperature. A parametric model of pressure dependence of the Curie temperature, which takes into account the magnetic Grüneisen parameter and isothermal compressibility, is constructed. The obtained theoretical results are in good agreement with experimental data, demonstrating linear dependence of the Curie temperature on pressure. The model can be used to analyze implications of lithostatic and shock pressure for the magnetic properties of magnetite and related minerals, which is important for the correct interpretation of paleomagnetic data.</p>","PeriodicalId":602,"journal":{"name":"Izvestiya, Physics of the Solid Earth","volume":"62 1","pages":"144 - 149"},"PeriodicalIF":0.7000,"publicationDate":"2026-05-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"The Effect of Pressure on the Curie Temperature of Magnetite: A Random Exchange Interaction Field Method\",\"authors\":\"V. I. Belokon,&nbsp;O. I. Dyachenko,&nbsp;O. A. Gorodnikov,&nbsp;A. D. Burtsev\",\"doi\":\"10.1134/S1069351326700011\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>The effect of pressure on the Curie temperature of magnetite is examined using the random exchange interaction field method. It is known that compression of the crystal lattice leads to increased overlap of electronic orbitals, which enhances exchange interaction and increases the Curie temperature. A parametric model of pressure dependence of the Curie temperature, which takes into account the magnetic Grüneisen parameter and isothermal compressibility, is constructed. The obtained theoretical results are in good agreement with experimental data, demonstrating linear dependence of the Curie temperature on pressure. The model can be used to analyze implications of lithostatic and shock pressure for the magnetic properties of magnetite and related minerals, which is important for the correct interpretation of paleomagnetic data.</p>\",\"PeriodicalId\":602,\"journal\":{\"name\":\"Izvestiya, Physics of the Solid Earth\",\"volume\":\"62 1\",\"pages\":\"144 - 149\"},\"PeriodicalIF\":0.7000,\"publicationDate\":\"2026-05-26\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Izvestiya, Physics of the Solid Earth\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://link.springer.com/article/10.1134/S1069351326700011\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Izvestiya, Physics of the Solid Earth","FirstCategoryId":"89","ListUrlMain":"https://link.springer.com/article/10.1134/S1069351326700011","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0

摘要

采用随机交换相互作用场法研究了压力对磁铁矿居里温度的影响。已知晶格压缩导致电子轨道重叠增加,从而增强交换相互作用,提高居里温度。建立了考虑磁粒尼森参数和等温可压缩性的居里温度压力依赖的参数化模型。所得理论结果与实验数据吻合较好,表明居里温度与压力呈线性关系。该模型可用于分析静岩压力和冲击压力对磁铁矿及相关矿物磁性的影响,对古地磁资料的正确解释具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

The Effect of Pressure on the Curie Temperature of Magnetite: A Random Exchange Interaction Field Method

The Effect of Pressure on the Curie Temperature of Magnetite: A Random Exchange Interaction Field Method

The effect of pressure on the Curie temperature of magnetite is examined using the random exchange interaction field method. It is known that compression of the crystal lattice leads to increased overlap of electronic orbitals, which enhances exchange interaction and increases the Curie temperature. A parametric model of pressure dependence of the Curie temperature, which takes into account the magnetic Grüneisen parameter and isothermal compressibility, is constructed. The obtained theoretical results are in good agreement with experimental data, demonstrating linear dependence of the Curie temperature on pressure. The model can be used to analyze implications of lithostatic and shock pressure for the magnetic properties of magnetite and related minerals, which is important for the correct interpretation of paleomagnetic data.

求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
Izvestiya, Physics of the Solid Earth
Izvestiya, Physics of the Solid Earth 地学-地球化学与地球物理
CiteScore
1.60
自引率
30.00%
发文量
60
审稿时长
6-12 weeks
期刊介绍: Izvestiya, Physics of the Solid Earth is an international peer reviewed journal that publishes results of original theoretical and experimental research in relevant areas of the physics of the Earth''s interior and applied geophysics. The journal welcomes manuscripts from all countries in the English or Russian language.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术官方微信
小红书