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OxyEMG: an application for determination of the oxyspinel group end-members based on electron microprobe analyses
The Oxyspinel group End-Member Generator (OxyEMG) is an improved version of the EMG application. This new version allows for calculating, based on electron microprobe analysis (EMPA), the proportions of 31 end-member components in an oxyspinel composition. These components are MgAl2O4 (spinel), FeAl...
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Published in: | European journal of mineralogy (Stuttgart) 2024-01, Vol.36 (1), p.87-98 |
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description | The Oxyspinel group End-Member Generator (OxyEMG) is an improved version of the EMG application. This new version allows for calculating, based on electron microprobe analysis (EMPA), the proportions of 31 end-member components in an oxyspinel composition. These components are MgAl2O4 (spinel), FeAl2O4 (hercynite), MnAl2O4 (galaxite), ZnAl2O4 (gahnite), NiAl2O4 (chihmingite), CuAl2O4 (thermaerogenite), MgFe2O4 (magnesioferrite), Fe3O4 (magnetite), MnFe2O4 (jacobsite), ZnFe2O4 (franklinite), NiFe2O4 (trevorite), CuFe2O4 (cuprospinel), FeMn2O4, MgMn2O4, Mn3O4 (hausmannite), ZnMn2O4 (hetaerolite), MgCr2O4 (magnesiochromite), FeCr2O4 (chromite), MnCr2O4 (manganochromite), ZnCr2O4 (zincochromite), NiCr2O4 (nichromite), CoCr2O4 (cochromite), MgV2O4 (magnesiocoulsonite), FeV2O4 (coulsonite), MnV2O4 (vuorelainenite), Co3O4 (guite), TiMg2O4 (qandilite), TiFe2O4 (ulvöspinel), SiMg2O4 (ringwoodite), SiFe2O4 (ahrensite) and GeFe2O4 (brunogeierite). Compared with the older version, OxyEMG allows for (a) calculating 12 additional oxyspinel group end-member compositions (chihmingite, thermaerogenite, hausmannite, hetaerolite, FeMn2O4, MgMn2O4, cuprospinel, cochromite, guite, ringwoodite, ahrensite and brunogeierite), (b) discriminating the cation valency not only for Fe2+–Fe3+ but also for Mn2+–Mn3+ and Co2+–Co3+, and (c) changing the method to calculate the components of the magnetite and ulvöspinel prisms. As in EMG, this new version is an application that does not require an installation process and was created with the purpose of performing calculations to obtain cation proportions (per formula unit, p.f.u.), end-members of the oxyspinel group, a ΣR3+ value, a ΣR2+ value, ΣR3+ / ΣR2+ ratios, redistribution proportions for the corresponding end-members in the magnetite or ulvöspinel prisms, and a data validation section to check the results. |
doi_str_mv | 10.5194/ejm-36-87-2024 |
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Luján</creator><creatorcontrib>Ferracutti, Gabriela R. ; Asiain, Lucía M. ; Antonini, Antonella S. ; Tanzola, Juan E. ; Ganuza, M. Luján</creatorcontrib><description>The Oxyspinel group End-Member Generator (OxyEMG) is an improved version of the EMG application. This new version allows for calculating, based on electron microprobe analysis (EMPA), the proportions of 31 end-member components in an oxyspinel composition. These components are MgAl2O4 (spinel), FeAl2O4 (hercynite), MnAl2O4 (galaxite), ZnAl2O4 (gahnite), NiAl2O4 (chihmingite), CuAl2O4 (thermaerogenite), MgFe2O4 (magnesioferrite), Fe3O4 (magnetite), MnFe2O4 (jacobsite), ZnFe2O4 (franklinite), NiFe2O4 (trevorite), CuFe2O4 (cuprospinel), FeMn2O4, MgMn2O4, Mn3O4 (hausmannite), ZnMn2O4 (hetaerolite), MgCr2O4 (magnesiochromite), FeCr2O4 (chromite), MnCr2O4 (manganochromite), ZnCr2O4 (zincochromite), NiCr2O4 (nichromite), CoCr2O4 (cochromite), MgV2O4 (magnesiocoulsonite), FeV2O4 (coulsonite), MnV2O4 (vuorelainenite), Co3O4 (guite), TiMg2O4 (qandilite), TiFe2O4 (ulvöspinel), SiMg2O4 (ringwoodite), SiFe2O4 (ahrensite) and GeFe2O4 (brunogeierite). Compared with the older version, OxyEMG allows for (a) calculating 12 additional oxyspinel group end-member compositions (chihmingite, thermaerogenite, hausmannite, hetaerolite, FeMn2O4, MgMn2O4, cuprospinel, cochromite, guite, ringwoodite, ahrensite and brunogeierite), (b) discriminating the cation valency not only for Fe2+–Fe3+ but also for Mn2+–Mn3+ and Co2+–Co3+, and (c) changing the method to calculate the components of the magnetite and ulvöspinel prisms. As in EMG, this new version is an application that does not require an installation process and was created with the purpose of performing calculations to obtain cation proportions (per formula unit, p.f.u.), end-members of the oxyspinel group, a ΣR3+ value, a ΣR2+ value, ΣR3+ / ΣR2+ ratios, redistribution proportions for the corresponding end-members in the magnetite or ulvöspinel prisms, and a data validation section to check the results.</description><identifier>ISSN: 1617-4011</identifier><identifier>ISSN: 0935-1221</identifier><identifier>EISSN: 1617-4011</identifier><identifier>DOI: 10.5194/ejm-36-87-2024</identifier><language>eng</language><publisher>Göttingen: Copernicus GmbH</publisher><subject>Cations ; Chemical elements ; Chromite ; Composition ; Electron probe microanalysis ; Electron probes ; Hausmannite ; Hercynite ; Intermetallic compounds ; Iron compounds ; Magnetite ; Manganese ; Mathematical analysis ; Mineralogical research ; Nickel aluminides ; Nickel base alloys ; Nickel compounds ; Prisms ; Properties ; Solid solutions ; Spinel group ; Testing</subject><ispartof>European journal of mineralogy (Stuttgart), 2024-01, Vol.36 (1), p.87-98</ispartof><rights>COPYRIGHT 2024 Copernicus GmbH</rights><rights>2024. This work is published under https://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-a390t-24d26f7f7987d6db20ed400e0c79a0c7032f364af66e6c5024edd0bd30b9d7953</cites><orcidid>0000-0002-0869-9616 ; 0000-0002-6330-3426</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/2915464963/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/2915464963?pq-origsite=primo$$EHTML$$P50$$Gproquest$$Hfree_for_read</linktohtml><link.rule.ids>314,776,780,860,2096,25731,27901,27902,36989,44566,74869</link.rule.ids></links><search><creatorcontrib>Ferracutti, Gabriela R.</creatorcontrib><creatorcontrib>Asiain, Lucía M.</creatorcontrib><creatorcontrib>Antonini, Antonella S.</creatorcontrib><creatorcontrib>Tanzola, Juan E.</creatorcontrib><creatorcontrib>Ganuza, M. Luján</creatorcontrib><title>OxyEMG: an application for determination of the oxyspinel group end-members based on electron microprobe analyses</title><title>European journal of mineralogy (Stuttgart)</title><description>The Oxyspinel group End-Member Generator (OxyEMG) is an improved version of the EMG application. This new version allows for calculating, based on electron microprobe analysis (EMPA), the proportions of 31 end-member components in an oxyspinel composition. These components are MgAl2O4 (spinel), FeAl2O4 (hercynite), MnAl2O4 (galaxite), ZnAl2O4 (gahnite), NiAl2O4 (chihmingite), CuAl2O4 (thermaerogenite), MgFe2O4 (magnesioferrite), Fe3O4 (magnetite), MnFe2O4 (jacobsite), ZnFe2O4 (franklinite), NiFe2O4 (trevorite), CuFe2O4 (cuprospinel), FeMn2O4, MgMn2O4, Mn3O4 (hausmannite), ZnMn2O4 (hetaerolite), MgCr2O4 (magnesiochromite), FeCr2O4 (chromite), MnCr2O4 (manganochromite), ZnCr2O4 (zincochromite), NiCr2O4 (nichromite), CoCr2O4 (cochromite), MgV2O4 (magnesiocoulsonite), FeV2O4 (coulsonite), MnV2O4 (vuorelainenite), Co3O4 (guite), TiMg2O4 (qandilite), TiFe2O4 (ulvöspinel), SiMg2O4 (ringwoodite), SiFe2O4 (ahrensite) and GeFe2O4 (brunogeierite). Compared with the older version, OxyEMG allows for (a) calculating 12 additional oxyspinel group end-member compositions (chihmingite, thermaerogenite, hausmannite, hetaerolite, FeMn2O4, MgMn2O4, cuprospinel, cochromite, guite, ringwoodite, ahrensite and brunogeierite), (b) discriminating the cation valency not only for Fe2+–Fe3+ but also for Mn2+–Mn3+ and Co2+–Co3+, and (c) changing the method to calculate the components of the magnetite and ulvöspinel prisms. As in EMG, this new version is an application that does not require an installation process and was created with the purpose of performing calculations to obtain cation proportions (per formula unit, p.f.u.), end-members of the oxyspinel group, a ΣR3+ value, a ΣR2+ value, ΣR3+ / ΣR2+ ratios, redistribution proportions for the corresponding end-members in the magnetite or ulvöspinel prisms, and a data validation section to check the results.</description><subject>Cations</subject><subject>Chemical elements</subject><subject>Chromite</subject><subject>Composition</subject><subject>Electron probe microanalysis</subject><subject>Electron probes</subject><subject>Hausmannite</subject><subject>Hercynite</subject><subject>Intermetallic compounds</subject><subject>Iron compounds</subject><subject>Magnetite</subject><subject>Manganese</subject><subject>Mathematical analysis</subject><subject>Mineralogical research</subject><subject>Nickel aluminides</subject><subject>Nickel base alloys</subject><subject>Nickel compounds</subject><subject>Prisms</subject><subject>Properties</subject><subject>Solid solutions</subject><subject>Spinel group</subject><subject>Testing</subject><issn>1617-4011</issn><issn>0935-1221</issn><issn>1617-4011</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><sourceid>PIMPY</sourceid><sourceid>DOA</sourceid><recordid>eNpNUc9LBCEYHaKg2rp2FjpP-Wt07RZRW1Dspc6i4-fmMjNOOgvtf5_bRoWgH4_n0_deVV0QfNUQxa9h3ddM1HNZU0z5QXVCBJE1x4Qc_puPq9Oc1xgTxjk-qT6Wn9v7l8UNMgMy49iF1kwhDsjHhBxMkPow7JHo0fQOKH5u8xgG6NAqxc2IYHB1D72FlJE1GRwqXOignVIZ-tCmOKZooTxgum2GfFYdedNlOP85Z9Xbw_3r3WP9vFw83d0-14YpPNWUOyq89FLNpRPOUgyOYwy4lcqUDTPqmeDGCwGibYpjcA5bx7BVTqqGzaqnva6LZq3HFHqTtjqaoL-BmFbapCm0HWhKmOPWtyUSyZ2AueWeYNY4yqmnYIvW5V6rWPnYQJ70Om5SMZQ1VaThgivBCutqz1qZIhoGH6dk2rIclBziAD4U_FZKJbhsmubvQgkp5wT-95sE612nunSqmdBzqXedsi8YxJVm</recordid><startdate>20240117</startdate><enddate>20240117</enddate><creator>Ferracutti, Gabriela R.</creator><creator>Asiain, Lucía M.</creator><creator>Antonini, Antonella S.</creator><creator>Tanzola, Juan E.</creator><creator>Ganuza, M. 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Luján</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>OxyEMG: an application for determination of the oxyspinel group end-members based on electron microprobe analyses</atitle><jtitle>European journal of mineralogy (Stuttgart)</jtitle><date>2024-01-17</date><risdate>2024</risdate><volume>36</volume><issue>1</issue><spage>87</spage><epage>98</epage><pages>87-98</pages><issn>1617-4011</issn><issn>0935-1221</issn><eissn>1617-4011</eissn><abstract>The Oxyspinel group End-Member Generator (OxyEMG) is an improved version of the EMG application. This new version allows for calculating, based on electron microprobe analysis (EMPA), the proportions of 31 end-member components in an oxyspinel composition. These components are MgAl2O4 (spinel), FeAl2O4 (hercynite), MnAl2O4 (galaxite), ZnAl2O4 (gahnite), NiAl2O4 (chihmingite), CuAl2O4 (thermaerogenite), MgFe2O4 (magnesioferrite), Fe3O4 (magnetite), MnFe2O4 (jacobsite), ZnFe2O4 (franklinite), NiFe2O4 (trevorite), CuFe2O4 (cuprospinel), FeMn2O4, MgMn2O4, Mn3O4 (hausmannite), ZnMn2O4 (hetaerolite), MgCr2O4 (magnesiochromite), FeCr2O4 (chromite), MnCr2O4 (manganochromite), ZnCr2O4 (zincochromite), NiCr2O4 (nichromite), CoCr2O4 (cochromite), MgV2O4 (magnesiocoulsonite), FeV2O4 (coulsonite), MnV2O4 (vuorelainenite), Co3O4 (guite), TiMg2O4 (qandilite), TiFe2O4 (ulvöspinel), SiMg2O4 (ringwoodite), SiFe2O4 (ahrensite) and GeFe2O4 (brunogeierite). Compared with the older version, OxyEMG allows for (a) calculating 12 additional oxyspinel group end-member compositions (chihmingite, thermaerogenite, hausmannite, hetaerolite, FeMn2O4, MgMn2O4, cuprospinel, cochromite, guite, ringwoodite, ahrensite and brunogeierite), (b) discriminating the cation valency not only for Fe2+–Fe3+ but also for Mn2+–Mn3+ and Co2+–Co3+, and (c) changing the method to calculate the components of the magnetite and ulvöspinel prisms. As in EMG, this new version is an application that does not require an installation process and was created with the purpose of performing calculations to obtain cation proportions (per formula unit, p.f.u.), end-members of the oxyspinel group, a ΣR3+ value, a ΣR2+ value, ΣR3+ / ΣR2+ ratios, redistribution proportions for the corresponding end-members in the magnetite or ulvöspinel prisms, and a data validation section to check the results.</abstract><cop>Göttingen</cop><pub>Copernicus GmbH</pub><doi>10.5194/ejm-36-87-2024</doi><tpages>12</tpages><orcidid>https://orcid.org/0000-0002-0869-9616</orcidid><orcidid>https://orcid.org/0000-0002-6330-3426</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Cations Chemical elements Chromite Composition Electron probe microanalysis Electron probes Hausmannite Hercynite Intermetallic compounds Iron compounds Magnetite Manganese Mathematical analysis Mineralogical research Nickel aluminides Nickel base alloys Nickel compounds Prisms Properties Solid solutions Spinel group Testing |
title | OxyEMG: an application for determination of the oxyspinel group end-members based on electron microprobe analyses |
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