Hydrothermal Synthesis, Structure, and Characterization of a Mixed-Valent Iron(II/III) Phosphate, NaFe3.67(PO4)3: A New Variation of the Alluaudite Structure Type

A mixed-valent Fe(II/III) phosphate, NaFe3.67(PO4)3, has been synthesized by high-temperature/high-pressure hydrothermal methods and characterized by single-crystal X-ray diffraction, EDAX, magnetic susceptibility, Mössbauer, infrared, and diffuse reflectance spectroscopies, DTA, and bond valence su...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Journal of solid state chemistry 1998-08, Vol.139 (1), p.152-160
Hauptverfasser: Korzenski, Michael B., Schimek, George L., Kolis, Joseph W., Long, Gary J.
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 160
container_issue 1
container_start_page 152
container_title Journal of solid state chemistry
container_volume 139
creator Korzenski, Michael B.
Schimek, George L.
Kolis, Joseph W.
Long, Gary J.
description A mixed-valent Fe(II/III) phosphate, NaFe3.67(PO4)3, has been synthesized by high-temperature/high-pressure hydrothermal methods and characterized by single-crystal X-ray diffraction, EDAX, magnetic susceptibility, Mössbauer, infrared, and diffuse reflectance spectroscopies, DTA, and bond valence sum calculations. The compound crystallizes in the monoclinic space groupC2/c(No. 15) witha=11.881(4) Å,b=12.564(3) Å,c=6.522(2) Å,β=115.09(2)°,V=881.7(5) Å3, andZ=4 withR/Rw=0.029/0.033. It exhibits a three-dimensional channel-like structure with an open framework that is similar to the naturally occurring iron-containing mineral alluaudite, NaFe3(PO4)3. In alluaudite there are two distinct channels, one which contains the sodium cations and the second which remains empty. In the title phase, this second channel is partially occupied by a square-planar iron atom. The Mössbauer spectral parameters are consistent with the structure and indicate that the fully occupied iron sites are octahedral Fe(II) and the square-planar iron is Fe(III). Structural comparisons to a number of phosphates and arsenates that also possess the alluaudite-type structure, including NaCu4(AsO4)3and NaMn4(AsO4)3are discussed.
doi_str_mv 10.1006/jssc.1998.7823
format Article
fullrecord <record><control><sourceid>elsevier_cross</sourceid><recordid>TN_cdi_crossref_primary_10_1006_jssc_1998_7823</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S0022459698978239</els_id><sourcerecordid>S0022459698978239</sourcerecordid><originalsourceid>FETCH-LOGICAL-c230t-897ca87665075733a209e609bdb104fd8b249d3adc453a7c9f3ec122bac672023</originalsourceid><addsrcrecordid>eNp1kD1v2zAQhomiBeomWTtz6JAAlsIPSRS7GUYSC0gcA06MbsKZPME0FMkg6bTOz-kvrQwX6dTpbrjnfQ8PIV85SzljxfU2BJNyrctUlUJ-ICPOdJ4oUfz4SEaMCZFkuS4-ky8hbBnjPC-zEfk9O1jfxw36F2jp8tANa3BhTJfR703cexxT6CydbsCDiejdG0TXd7RvKNAH9wttsoIWu0gr33eXVXVdVdUVXWz6sNtAHPA53KJMC3W5eMyu5Hc6oXP8SVfg3XvSUEonbbuHvXUR_3XTp8MOz8mnBtqAF3_nGXm-vXmazpL7x7tqOrlPjJAsJqVWBkpVFDlTuZISBNNYML22a86yxpZrkWkrwZosl6CMbiQaLsQaTKEEE_KMpKdc4_sQPDb1zrsX8Ieas_pouD4aro-G66PhAfh2AnYQDLSNh8648E4JqeSADWfl6QyH518d-joYh51B6zyaWNve_a_hDyKKjxM</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>Hydrothermal Synthesis, Structure, and Characterization of a Mixed-Valent Iron(II/III) Phosphate, NaFe3.67(PO4)3: A New Variation of the Alluaudite Structure Type</title><source>Access via ScienceDirect (Elsevier)</source><creator>Korzenski, Michael B. ; Schimek, George L. ; Kolis, Joseph W. ; Long, Gary J.</creator><creatorcontrib>Korzenski, Michael B. ; Schimek, George L. ; Kolis, Joseph W. ; Long, Gary J.</creatorcontrib><description>A mixed-valent Fe(II/III) phosphate, NaFe3.67(PO4)3, has been synthesized by high-temperature/high-pressure hydrothermal methods and characterized by single-crystal X-ray diffraction, EDAX, magnetic susceptibility, Mössbauer, infrared, and diffuse reflectance spectroscopies, DTA, and bond valence sum calculations. The compound crystallizes in the monoclinic space groupC2/c(No. 15) witha=11.881(4) Å,b=12.564(3) Å,c=6.522(2) Å,β=115.09(2)°,V=881.7(5) Å3, andZ=4 withR/Rw=0.029/0.033. It exhibits a three-dimensional channel-like structure with an open framework that is similar to the naturally occurring iron-containing mineral alluaudite, NaFe3(PO4)3. In alluaudite there are two distinct channels, one which contains the sodium cations and the second which remains empty. In the title phase, this second channel is partially occupied by a square-planar iron atom. The Mössbauer spectral parameters are consistent with the structure and indicate that the fully occupied iron sites are octahedral Fe(II) and the square-planar iron is Fe(III). Structural comparisons to a number of phosphates and arsenates that also possess the alluaudite-type structure, including NaCu4(AsO4)3and NaMn4(AsO4)3are discussed.</description><identifier>ISSN: 0022-4596</identifier><identifier>EISSN: 1095-726X</identifier><identifier>DOI: 10.1006/jssc.1998.7823</identifier><identifier>CODEN: JSSCBI</identifier><language>eng</language><publisher>San Diego, CA: Elsevier Inc</publisher><subject>Condensed matter: electronic structure, electrical, magnetic, and optical properties ; Condensed matter: structure, mechanical and thermal properties ; Exact sciences and technology ; Inorganic compounds ; Magnetic properties and materials ; Magnetic resonances and relaxations in condensed matter, mössbauer effect ; Magnetically ordered materials: other intrinsic properties ; Mossbauer effect; other γ-ray spectroscopy ; Mössbauer effect; other γ-ray spectroscopy ; Physics ; Salts ; Saturation moments and magnetic susceptibilities ; Structure of solids and liquids; crystallography ; Structure of specific crystalline solids</subject><ispartof>Journal of solid state chemistry, 1998-08, Vol.139 (1), p.152-160</ispartof><rights>1998 Academic Press</rights><rights>1998 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c230t-897ca87665075733a209e609bdb104fd8b249d3adc453a7c9f3ec122bac672023</citedby><cites>FETCH-LOGICAL-c230t-897ca87665075733a209e609bdb104fd8b249d3adc453a7c9f3ec122bac672023</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1006/jssc.1998.7823$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,780,784,3550,27924,27925,45995</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&amp;idt=2373100$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Korzenski, Michael B.</creatorcontrib><creatorcontrib>Schimek, George L.</creatorcontrib><creatorcontrib>Kolis, Joseph W.</creatorcontrib><creatorcontrib>Long, Gary J.</creatorcontrib><title>Hydrothermal Synthesis, Structure, and Characterization of a Mixed-Valent Iron(II/III) Phosphate, NaFe3.67(PO4)3: A New Variation of the Alluaudite Structure Type</title><title>Journal of solid state chemistry</title><description>A mixed-valent Fe(II/III) phosphate, NaFe3.67(PO4)3, has been synthesized by high-temperature/high-pressure hydrothermal methods and characterized by single-crystal X-ray diffraction, EDAX, magnetic susceptibility, Mössbauer, infrared, and diffuse reflectance spectroscopies, DTA, and bond valence sum calculations. The compound crystallizes in the monoclinic space groupC2/c(No. 15) witha=11.881(4) Å,b=12.564(3) Å,c=6.522(2) Å,β=115.09(2)°,V=881.7(5) Å3, andZ=4 withR/Rw=0.029/0.033. It exhibits a three-dimensional channel-like structure with an open framework that is similar to the naturally occurring iron-containing mineral alluaudite, NaFe3(PO4)3. In alluaudite there are two distinct channels, one which contains the sodium cations and the second which remains empty. In the title phase, this second channel is partially occupied by a square-planar iron atom. The Mössbauer spectral parameters are consistent with the structure and indicate that the fully occupied iron sites are octahedral Fe(II) and the square-planar iron is Fe(III). Structural comparisons to a number of phosphates and arsenates that also possess the alluaudite-type structure, including NaCu4(AsO4)3and NaMn4(AsO4)3are discussed.</description><subject>Condensed matter: electronic structure, electrical, magnetic, and optical properties</subject><subject>Condensed matter: structure, mechanical and thermal properties</subject><subject>Exact sciences and technology</subject><subject>Inorganic compounds</subject><subject>Magnetic properties and materials</subject><subject>Magnetic resonances and relaxations in condensed matter, mössbauer effect</subject><subject>Magnetically ordered materials: other intrinsic properties</subject><subject>Mossbauer effect; other γ-ray spectroscopy</subject><subject>Mössbauer effect; other γ-ray spectroscopy</subject><subject>Physics</subject><subject>Salts</subject><subject>Saturation moments and magnetic susceptibilities</subject><subject>Structure of solids and liquids; crystallography</subject><subject>Structure of specific crystalline solids</subject><issn>0022-4596</issn><issn>1095-726X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1998</creationdate><recordtype>article</recordtype><recordid>eNp1kD1v2zAQhomiBeomWTtz6JAAlsIPSRS7GUYSC0gcA06MbsKZPME0FMkg6bTOz-kvrQwX6dTpbrjnfQ8PIV85SzljxfU2BJNyrctUlUJ-ICPOdJ4oUfz4SEaMCZFkuS4-ky8hbBnjPC-zEfk9O1jfxw36F2jp8tANa3BhTJfR703cexxT6CydbsCDiejdG0TXd7RvKNAH9wttsoIWu0gr33eXVXVdVdUVXWz6sNtAHPA53KJMC3W5eMyu5Hc6oXP8SVfg3XvSUEonbbuHvXUR_3XTp8MOz8mnBtqAF3_nGXm-vXmazpL7x7tqOrlPjJAsJqVWBkpVFDlTuZISBNNYML22a86yxpZrkWkrwZosl6CMbiQaLsQaTKEEE_KMpKdc4_sQPDb1zrsX8Ieas_pouD4aro-G66PhAfh2AnYQDLSNh8648E4JqeSADWfl6QyH518d-joYh51B6zyaWNve_a_hDyKKjxM</recordid><startdate>199808</startdate><enddate>199808</enddate><creator>Korzenski, Michael B.</creator><creator>Schimek, George L.</creator><creator>Kolis, Joseph W.</creator><creator>Long, Gary J.</creator><general>Elsevier Inc</general><general>Elsevier</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>199808</creationdate><title>Hydrothermal Synthesis, Structure, and Characterization of a Mixed-Valent Iron(II/III) Phosphate, NaFe3.67(PO4)3: A New Variation of the Alluaudite Structure Type</title><author>Korzenski, Michael B. ; Schimek, George L. ; Kolis, Joseph W. ; Long, Gary J.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c230t-897ca87665075733a209e609bdb104fd8b249d3adc453a7c9f3ec122bac672023</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1998</creationdate><topic>Condensed matter: electronic structure, electrical, magnetic, and optical properties</topic><topic>Condensed matter: structure, mechanical and thermal properties</topic><topic>Exact sciences and technology</topic><topic>Inorganic compounds</topic><topic>Magnetic properties and materials</topic><topic>Magnetic resonances and relaxations in condensed matter, mössbauer effect</topic><topic>Magnetically ordered materials: other intrinsic properties</topic><topic>Mossbauer effect; other γ-ray spectroscopy</topic><topic>Mössbauer effect; other γ-ray spectroscopy</topic><topic>Physics</topic><topic>Salts</topic><topic>Saturation moments and magnetic susceptibilities</topic><topic>Structure of solids and liquids; crystallography</topic><topic>Structure of specific crystalline solids</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Korzenski, Michael B.</creatorcontrib><creatorcontrib>Schimek, George L.</creatorcontrib><creatorcontrib>Kolis, Joseph W.</creatorcontrib><creatorcontrib>Long, Gary J.</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><jtitle>Journal of solid state chemistry</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Korzenski, Michael B.</au><au>Schimek, George L.</au><au>Kolis, Joseph W.</au><au>Long, Gary J.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Hydrothermal Synthesis, Structure, and Characterization of a Mixed-Valent Iron(II/III) Phosphate, NaFe3.67(PO4)3: A New Variation of the Alluaudite Structure Type</atitle><jtitle>Journal of solid state chemistry</jtitle><date>1998-08</date><risdate>1998</risdate><volume>139</volume><issue>1</issue><spage>152</spage><epage>160</epage><pages>152-160</pages><issn>0022-4596</issn><eissn>1095-726X</eissn><coden>JSSCBI</coden><abstract>A mixed-valent Fe(II/III) phosphate, NaFe3.67(PO4)3, has been synthesized by high-temperature/high-pressure hydrothermal methods and characterized by single-crystal X-ray diffraction, EDAX, magnetic susceptibility, Mössbauer, infrared, and diffuse reflectance spectroscopies, DTA, and bond valence sum calculations. The compound crystallizes in the monoclinic space groupC2/c(No. 15) witha=11.881(4) Å,b=12.564(3) Å,c=6.522(2) Å,β=115.09(2)°,V=881.7(5) Å3, andZ=4 withR/Rw=0.029/0.033. It exhibits a three-dimensional channel-like structure with an open framework that is similar to the naturally occurring iron-containing mineral alluaudite, NaFe3(PO4)3. In alluaudite there are two distinct channels, one which contains the sodium cations and the second which remains empty. In the title phase, this second channel is partially occupied by a square-planar iron atom. The Mössbauer spectral parameters are consistent with the structure and indicate that the fully occupied iron sites are octahedral Fe(II) and the square-planar iron is Fe(III). Structural comparisons to a number of phosphates and arsenates that also possess the alluaudite-type structure, including NaCu4(AsO4)3and NaMn4(AsO4)3are discussed.</abstract><cop>San Diego, CA</cop><pub>Elsevier Inc</pub><doi>10.1006/jssc.1998.7823</doi><tpages>9</tpages></addata></record>
fulltext fulltext
identifier ISSN: 0022-4596
ispartof Journal of solid state chemistry, 1998-08, Vol.139 (1), p.152-160
issn 0022-4596
1095-726X
language eng
recordid cdi_crossref_primary_10_1006_jssc_1998_7823
source Access via ScienceDirect (Elsevier)
subjects Condensed matter: electronic structure, electrical, magnetic, and optical properties
Condensed matter: structure, mechanical and thermal properties
Exact sciences and technology
Inorganic compounds
Magnetic properties and materials
Magnetic resonances and relaxations in condensed matter, mössbauer effect
Magnetically ordered materials: other intrinsic properties
Mossbauer effect
other γ-ray spectroscopy
Mössbauer effect
other γ-ray spectroscopy
Physics
Salts
Saturation moments and magnetic susceptibilities
Structure of solids and liquids
crystallography
Structure of specific crystalline solids
title Hydrothermal Synthesis, Structure, and Characterization of a Mixed-Valent Iron(II/III) Phosphate, NaFe3.67(PO4)3: A New Variation of the Alluaudite Structure Type
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-20T18%3A42%3A23IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-elsevier_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Hydrothermal%20Synthesis,%20Structure,%20and%20Characterization%20of%20a%20Mixed-Valent%20Iron(II/III)%20Phosphate,%20NaFe3.67(PO4)3:%20A%20New%20Variation%20of%20the%20Alluaudite%20Structure%20Type&rft.jtitle=Journal%20of%20solid%20state%20chemistry&rft.au=Korzenski,%20Michael%20B.&rft.date=1998-08&rft.volume=139&rft.issue=1&rft.spage=152&rft.epage=160&rft.pages=152-160&rft.issn=0022-4596&rft.eissn=1095-726X&rft.coden=JSSCBI&rft_id=info:doi/10.1006/jssc.1998.7823&rft_dat=%3Celsevier_cross%3ES0022459698978239%3C/elsevier_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rft_els_id=S0022459698978239&rfr_iscdi=true