Article(id=1325115698502041741, tenantId=1146029695717560320, journalId=1255847867265597444, issueId=1325115694651670631, articleNumber=null, orderNo=null, doi=null, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=null, receivedDate=1331913600000, receivedDateStr=2012-03-17, revisedDate=1335974400000, revisedDateStr=2012-05-03, acceptedDate=null, acceptedDateStr=null, onlineDate=1793861801982, onlineDateStr=2026-11-05, pubDate=1387036800000, pubDateStr=2013-12-15, doiRegisterDate=null, doiRegisterDateStr=null, onlineIssueDate=1793861801982, onlineIssueDateStr=2026-11-05, onlineJustAcceptDate=null, onlineJustAcceptDateStr=null, onlineFirstDate=null, onlineFirstDateStr=null, sourceXml=null, magXml=null, createTime=1793861801982, creator=13701087609, updateTime=1793861801982, updator=13701087609, issue=Issue{id=1325115694651670631, tenantId=1146029695717560320, journalId=1255847867265597444, year='2013', volume='27', issue='6', pageStart='793', pageEnd='945', issueExtLink='null', onlineDate='null', pubDate='1387036800000', pubDateStr='2013-12-15', beforeIssueId=null, nextIssueId=null, price=null, status=1, issueComplete=1, articleOrder=1, issueType=-1, specialIssue=null, createTime=1793861801063, creator='13701087609', updateTime=1793861801063, updator='13701087609', preIssue=null, nextIssue=null, articleTotal=null, ext=null, issueFiles=null, downloadFileDto=null}, startPage=828, endPage=832, ext={EN=ArticleExt(id=1325115698917277838, articleId=1325115698502041741, tenantId=1146029695717560320, journalId=1255847867265597444, language=EN, title=X-Ray Diffraction Investigation of Chalcopyrite under High Pressure and Temperature, columnId=null, journalTitle=Chinese Journal of High Pressure Physics, columnName=null, runingTitle=null, highlight=null, articleAbstract=

In situ angle dispersive X-ray diffraction measurements for a natural chalcopyrite were performed by using heating diamond anvil cell instrument with synchrotron radiation at BSRF up to 32.0 GPa and 628 K. The phase transition of chalcopyrite from chalcopyrite structure to rocksalt structure is around 6.0 GPa. A fit to the high temperature third-order Birch-Murnaghan equation of state yielded an isothermal bulk modulus K0=109(3) GPa, a temperature derivative of the bulk modulus (∂K/∂T)p=-0.033(4) GPa·K-1, and a thermal expansion coefficient α0=2.0(2)×10-5 K-1 of rocksalt structure phase of chalcopyrite for the first time.

, authors=Da-Wei FAN1, Shu-Yi WEI1, 3, Jing LIU2, Hong-Sen XIE1, authorsList=Da-Wei FAN, Shu-Yi WEI, Jing LIU, Hong-Sen XIE, authorCompany=null, correspAuthors=null, authorNote=null, correspAuthorsNote=null, copyrightStatement=null, copyrightOwner=null, extLink=null, articleAbsUrl=null, sourceXml=null, magXml=null, pdfUrl=null, pdf=null, pdfFileSize=null, pdfExtLink=null, richHtmlUrl=null, mobilePdfUrl=null, reviewReport=null, pdfFirstPage=null, abstractGraph=null, abstractGraphContent=null, abstractVideo=null, citation=null, cebUrl=null, magXmlContent=null, mapNumber=null, fund=null), CN=ArticleExt(id=1325115699139575951, articleId=1325115698502041741, tenantId=1146029695717560320, journalId=1255847867265597444, language=CN, title=天然黄铜矿原位高温高压X射线衍射研究, columnId=0, journalTitle=高压物理学报, columnName=, runingTitle=null, highlight=null, articleAbstract=

在金刚石压腔高压装置(DAC)上,采用外加温实验技术和同步辐射角度色散X射线衍射技术,在最高温度628 K和最高压力32.0 GPa条件下,对天然黄铜矿进行了相变及热状态方程研究。实验样品在约6.0 GPa条件下发生了Chalcopyrite-Rocksalt相变。获得了天然黄铜矿的高温高压实验数据,并根据二阶Birch-Murnaghan状态方程,对所获得的实验数据进行了状态方程拟合,首次获得了天然黄铜矿Rocksalt相的体弹模量K0=109(3)GPa,体弹模量的温度导数(∂K/∂T)p=-0.033(4)GPa·K-1和热膨胀系数α0=2.0(2)×10-5 K-1。

, authors=范大伟1, 魏舒怡1, 3, 刘景2, 谢鸿森1, authorsList=范大伟, 魏舒怡, 刘景, 谢鸿森, authorCompany=null, correspAuthors=null, authorNote=

范大伟(1982—),男,博士,副研究员,主要从事高温高压矿物物理学研究. E-mail:

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天然黄铜矿原位高温高压X射线衍射研究
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范大伟 1 , 魏舒怡 1, 3 , 刘景 2 , 谢鸿森 1
高压物理学报 | 2013,27(6): 828-832
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高压物理学报 | 2013 , 27 (6) : 828 -832
天然黄铜矿原位高温高压X射线衍射研究
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范大伟(1982—),男,博士,副研究员,主要从事高温高压矿物物理学研究. E-mail:

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范大伟1 , 魏舒怡1, 3, 刘景2, 谢鸿森1
作者信息
  • 1.中国科学院地球化学研究所地球内部物质高温高压实验室,贵州 贵阳 550002
  • 2.中国科学院高能物理研究所,北京 100049
  • 3.中国科学院研究生院,北京 100049
作者简介:

范大伟(1982—),男,博士,副研究员,主要从事高温高压矿物物理学研究. E-mail:

X-Ray Diffraction Investigation of Chalcopyrite under High Pressure and Temperature
Da-Wei FAN1 , Shu-Yi WEI1, 3, Jing LIU2, Hong-Sen XIE1
Affiliations
  • 1.Laboratory for High Temperature & High Pressure Study of the Earth's Interior of Institute of Geochemistry, Chinese Academy of Science, Guiyang 550002, China
  • 2.Institute of High Energy Physics, Chinese Academy of Science, Beijing 100049, China
  • 3.Graduate School of Chinese Academy of Science, Beijing 100049, China
出版时间: 2013-12-15
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在金刚石压腔高压装置(DAC)上,采用外加温实验技术和同步辐射角度色散X射线衍射技术,在最高温度628 K和最高压力32.0 GPa条件下,对天然黄铜矿进行了相变及热状态方程研究。实验样品在约6.0 GPa条件下发生了Chalcopyrite-Rocksalt相变。获得了天然黄铜矿的高温高压实验数据,并根据二阶Birch-Murnaghan状态方程,对所获得的实验数据进行了状态方程拟合,首次获得了天然黄铜矿Rocksalt相的体弹模量K0=109(3)GPa,体弹模量的温度导数(∂K/∂T)p=-0.033(4)GPa·K-1和热膨胀系数α0=2.0(2)×10-5 K-1。

状态方程  /  天然黄铜矿  /  高温高压  /  同步辐射

In situ angle dispersive X-ray diffraction measurements for a natural chalcopyrite were performed by using heating diamond anvil cell instrument with synchrotron radiation at BSRF up to 32.0 GPa and 628 K. The phase transition of chalcopyrite from chalcopyrite structure to rocksalt structure is around 6.0 GPa. A fit to the high temperature third-order Birch-Murnaghan equation of state yielded an isothermal bulk modulus K0=109(3) GPa, a temperature derivative of the bulk modulus (∂K/∂T)p=-0.033(4) GPa·K-1, and a thermal expansion coefficient α0=2.0(2)×10-5 K-1 of rocksalt structure phase of chalcopyrite for the first time.

equation of state  /  chalcopyrite  /  high pressure and high temperature  /  synchrotron radiation
范大伟, 魏舒怡, 刘景, 谢鸿森. 天然黄铜矿原位高温高压X射线衍射研究. 高压物理学报, 2013 , 27 (6) : 828 -832 .
Da-Wei FAN, Shu-Yi WEI, Jing LIU, Hong-Sen XIE. X-Ray Diffraction Investigation of Chalcopyrite under High Pressure and Temperature[J]. Chinese Journal of High Pressure Physics, 2013 , 27 (6) : 828 -832 .
  • 国家自然科学基金(41004035; 41374107; 41274105)
  • 2011年度中国科学院西部之光人才培养计划西部博士资助项目
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2013年第27卷第6期
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  • 接收时间:2012-03-17
  • 首发时间:2026-11-05
  • 出版时间:2013-12-15
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  • 收稿日期:2012-03-17
  • 修回日期:2012-05-03
基金
国家自然科学基金(41004035; 41374107; 41274105)
2011年度中国科学院西部之光人才培养计划西部博士资助项目
作者信息
    1.中国科学院地球化学研究所地球内部物质高温高压实验室,贵州 贵阳 550002
    2.中国科学院高能物理研究所,北京 100049
    3.中国科学院研究生院,北京 100049
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2种不同金属材料的力学参数
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鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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