Structural Phase Transitions on AgCuS Stromeyerite Mineral under Compression
The structural behavior of mineral Stromeyerite, AgCuS, has been studied by means of angle-dispersive X-ray diffraction measurements up to 13 GPa and ab initio total-energy calculations. Two high-pressure phase transitions are found at 1.4 and 5.7 GPa, from the initial distorted Ni2In-type phase (Au...
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Veröffentlicht in: | Inorganic chemistry 2013-01, Vol.52 (1), p.355-361 |
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description | The structural behavior of mineral Stromeyerite, AgCuS, has been studied by means of angle-dispersive X-ray diffraction measurements up to 13 GPa and ab initio total-energy calculations. Two high-pressure phase transitions are found at 1.4 and 5.7 GPa, from the initial distorted Ni2In-type phase (AuRbS-type, RP, space group Cmc21) through an anti-PbClF-type phase (HP1, space group P4/nmm) to a monoclinic distortion of this latter phase (HP2, space group P21/m). The collapse of the metal–metal interatomic distances at the RP–HP1 transition suggests a stronger metallic behavior of the high-pressure phase. The compressibility of the lattice parameters and the equation of state of the first pressure-induced phase have been experimentally determined. First-principles calculations present an overall agreement with the experimental results in terms of the high-pressure sequence and provide chemical insight into the AgCuS behavior under hydrostatic pressure. |
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Two high-pressure phase transitions are found at 1.4 and 5.7 GPa, from the initial distorted Ni2In-type phase (AuRbS-type, RP, space group Cmc21) through an anti-PbClF-type phase (HP1, space group P4/nmm) to a monoclinic distortion of this latter phase (HP2, space group P21/m). The collapse of the metal–metal interatomic distances at the RP–HP1 transition suggests a stronger metallic behavior of the high-pressure phase. The compressibility of the lattice parameters and the equation of state of the first pressure-induced phase have been experimentally determined. First-principles calculations present an overall agreement with the experimental results in terms of the high-pressure sequence and provide chemical insight into the AgCuS behavior under hydrostatic pressure.</description><identifier>ISSN: 0020-1669</identifier><identifier>EISSN: 1520-510X</identifier><identifier>DOI: 10.1021/ic302116b</identifier><identifier>PMID: 23244465</identifier><language>eng</language><publisher>United States: American Chemical Society</publisher><ispartof>Inorganic chemistry, 2013-01, Vol.52 (1), p.355-361</ispartof><rights>Copyright © 2012 American Chemical Society</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a381t-7d756f48fab0d072294357f7fe862610471c27457160d84a6312ae4e20607f843</citedby><cites>FETCH-LOGICAL-a381t-7d756f48fab0d072294357f7fe862610471c27457160d84a6312ae4e20607f843</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://pubs.acs.org/doi/pdf/10.1021/ic302116b$$EPDF$$P50$$Gacs$$H</linktopdf><linktohtml>$$Uhttps://pubs.acs.org/doi/10.1021/ic302116b$$EHTML$$P50$$Gacs$$H</linktohtml><link.rule.ids>314,780,784,2765,27076,27924,27925,56738,56788</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/23244465$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Santamaria-Perez, D</creatorcontrib><creatorcontrib>Morales-Garcia, A</creatorcontrib><creatorcontrib>Martinez-Garcia, D</creatorcontrib><creatorcontrib>Garcia-Domene, B</creatorcontrib><creatorcontrib>Mühle, C</creatorcontrib><creatorcontrib>Jansen, M</creatorcontrib><title>Structural Phase Transitions on AgCuS Stromeyerite Mineral under Compression</title><title>Inorganic chemistry</title><addtitle>Inorg. Chem</addtitle><description>The structural behavior of mineral Stromeyerite, AgCuS, has been studied by means of angle-dispersive X-ray diffraction measurements up to 13 GPa and ab initio total-energy calculations. Two high-pressure phase transitions are found at 1.4 and 5.7 GPa, from the initial distorted Ni2In-type phase (AuRbS-type, RP, space group Cmc21) through an anti-PbClF-type phase (HP1, space group P4/nmm) to a monoclinic distortion of this latter phase (HP2, space group P21/m). The collapse of the metal–metal interatomic distances at the RP–HP1 transition suggests a stronger metallic behavior of the high-pressure phase. The compressibility of the lattice parameters and the equation of state of the first pressure-induced phase have been experimentally determined. First-principles calculations present an overall agreement with the experimental results in terms of the high-pressure sequence and provide chemical insight into the AgCuS behavior under hydrostatic pressure.</description><issn>0020-1669</issn><issn>1520-510X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><recordid>eNpt0E1Lw0AQBuBFFFurB_-A5CLoITr7kd30WIJfEFFoBW9hm0w0JcnW3eyh_94trT15mjk888K8hFxSuKPA6H1T8jCoXB6RMU0YxAmFz2MyBgg7lXI6ImfOrQBgyoU8JSPGmRBCJmOSzwfry8Fb3Ubv39phtLC6d83QmN5Fpo9mX5mfR0GZDjdomwGj16bHrfd9hTbKTLe26Fw4OCcntW4dXuznhHw8Piyy5zh_e3rJZnmseUqHWFUqkbVIa72EChRjU8ETVasaU8kkBaFoyZRIFJVQpUJLTplGgQwkqDoVfEJudrlra348uqHoGldi2-oejXcFZYqzJBUpBHq7o6U1zlmsi7VtOm03BYViW15xKC_Yq32sX3ZYHeRfWwFc74AuXbEy3vbhy3-CfgHO5nQW</recordid><startdate>20130107</startdate><enddate>20130107</enddate><creator>Santamaria-Perez, D</creator><creator>Morales-Garcia, A</creator><creator>Martinez-Garcia, D</creator><creator>Garcia-Domene, B</creator><creator>Mühle, C</creator><creator>Jansen, M</creator><general>American Chemical Society</general><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7X8</scope></search><sort><creationdate>20130107</creationdate><title>Structural Phase Transitions on AgCuS Stromeyerite Mineral under Compression</title><author>Santamaria-Perez, D ; Morales-Garcia, A ; Martinez-Garcia, D ; Garcia-Domene, B ; Mühle, C ; Jansen, M</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a381t-7d756f48fab0d072294357f7fe862610471c27457160d84a6312ae4e20607f843</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2013</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Santamaria-Perez, D</creatorcontrib><creatorcontrib>Morales-Garcia, A</creatorcontrib><creatorcontrib>Martinez-Garcia, D</creatorcontrib><creatorcontrib>Garcia-Domene, B</creatorcontrib><creatorcontrib>Mühle, C</creatorcontrib><creatorcontrib>Jansen, M</creatorcontrib><collection>PubMed</collection><collection>CrossRef</collection><collection>MEDLINE - Academic</collection><jtitle>Inorganic chemistry</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Santamaria-Perez, D</au><au>Morales-Garcia, A</au><au>Martinez-Garcia, D</au><au>Garcia-Domene, B</au><au>Mühle, C</au><au>Jansen, M</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Structural Phase Transitions on AgCuS Stromeyerite Mineral under Compression</atitle><jtitle>Inorganic chemistry</jtitle><addtitle>Inorg. Chem</addtitle><date>2013-01-07</date><risdate>2013</risdate><volume>52</volume><issue>1</issue><spage>355</spage><epage>361</epage><pages>355-361</pages><issn>0020-1669</issn><eissn>1520-510X</eissn><abstract>The structural behavior of mineral Stromeyerite, AgCuS, has been studied by means of angle-dispersive X-ray diffraction measurements up to 13 GPa and ab initio total-energy calculations. Two high-pressure phase transitions are found at 1.4 and 5.7 GPa, from the initial distorted Ni2In-type phase (AuRbS-type, RP, space group Cmc21) through an anti-PbClF-type phase (HP1, space group P4/nmm) to a monoclinic distortion of this latter phase (HP2, space group P21/m). The collapse of the metal–metal interatomic distances at the RP–HP1 transition suggests a stronger metallic behavior of the high-pressure phase. The compressibility of the lattice parameters and the equation of state of the first pressure-induced phase have been experimentally determined. First-principles calculations present an overall agreement with the experimental results in terms of the high-pressure sequence and provide chemical insight into the AgCuS behavior under hydrostatic pressure.</abstract><cop>United States</cop><pub>American Chemical Society</pub><pmid>23244465</pmid><doi>10.1021/ic302116b</doi><tpages>7</tpages></addata></record> |
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title | Structural Phase Transitions on AgCuS Stromeyerite Mineral under Compression |
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