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Some successful approaches to quantitative mineral analysis as revealed by the 3RD Reynolds Cup contest
Details of the quantitative techniques successfully applied to artificial rock mixtures distributed for the third Clay Minerals Society Reynolds Cup (RC) contest are presented. Participants each received three samples, two containing 17 minerals each and a third containing ten minerals. The true com...
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Published in: | Clays and clay minerals 2006-12, Vol.54 (6), p.748-760 |
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description | Details of the quantitative techniques successfully applied to artificial rock mixtures distributed for the third Clay Minerals Society Reynolds Cup (RC) contest are presented. Participants each received three samples, two containing 17 minerals each and a third containing ten minerals. The true composition of the samples was unknown to all participants during the contest period. The results submitted were ranked by summing the deviations from the actual compositions (bias). The top three finishers used mainly X-ray diffraction (XRD) for identification and quantification. The winner obtained an average bias of 11.3% per sample by using an internal standard and modified single-line reference intensity ratio (RIR) method based on pure mineral standards. Full-pattern fitting by genetic algorithm was used to measure the integrated intensity of the diagnostic single-line reflections chosen for quantification. Elemental-composition optimization was used separately to constrain phase concentrations that were uncertain because the reference mineral standards were lacking or not ideal. Cation exchange capacity, oriented-sample XRD analysis, and thermogravimetric analysis were also used as supplementary techniques. The second-place finisher obtained an average bias of 13.9%, also by using an RIR method, but without an added internal standard and with intensity measured by whole-pattern fitting. The third-place finisher, who obtained an average bias of 15.3%, used the Rietveld method for quantification and identification of minor phases (using difference plots). This participant also used scanning electron microscopy (with X-ray microanalysis) to identify minor components and verify the composition of structures used in Rietveld analysis. As in the previous contests, successful quantification appears to be more dependent on analyst experience than on the analytical technique or software used. |
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Participants each received three samples, two containing 17 minerals each and a third containing ten minerals. The true composition of the samples was unknown to all participants during the contest period. The results submitted were ranked by summing the deviations from the actual compositions (bias). The top three finishers used mainly X-ray diffraction (XRD) for identification and quantification. The winner obtained an average bias of 11.3% per sample by using an internal standard and modified single-line reference intensity ratio (RIR) method based on pure mineral standards. Full-pattern fitting by genetic algorithm was used to measure the integrated intensity of the diagnostic single-line reflections chosen for quantification. Elemental-composition optimization was used separately to constrain phase concentrations that were uncertain because the reference mineral standards were lacking or not ideal. Cation exchange capacity, oriented-sample XRD analysis, and thermogravimetric analysis were also used as supplementary techniques. The second-place finisher obtained an average bias of 13.9%, also by using an RIR method, but without an added internal standard and with intensity measured by whole-pattern fitting. The third-place finisher, who obtained an average bias of 15.3%, used the Rietveld method for quantification and identification of minor phases (using difference plots). This participant also used scanning electron microscopy (with X-ray microanalysis) to identify minor components and verify the composition of structures used in Rietveld analysis. As in the previous contests, successful quantification appears to be more dependent on analyst experience than on the analytical technique or software used.</description><identifier>ISSN: 0009-8604</identifier><identifier>EISSN: 1552-8367</identifier><identifier>DOI: 10.1346/CCMN.2006.0540609</identifier><identifier>CODEN: CLCMAB</identifier><language>eng</language><publisher>Boulder, CO: Clay Minerals Society</publisher><subject>cation exchange capacity ; chemical composition ; chemical properties ; clay mineralogy ; Clay Minerals ; Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; experimental studies ; geochemistry ; Mineralogy ; Pure Reference Minerals ; Quantitative Analysis ; Reference Intensity Ratio ; Reynolds Cup ; Rietveld ; rock, sediment, soil ; samples ; sed rocks, sediments ; Sedimentary petrology ; sheet silicates ; Silicates ; standard materials ; The Clay Minerals Society ; Whole-Pattern Fitting ; X-ray diffraction data</subject><ispartof>Clays and clay minerals, 2006-12, Vol.54 (6), p.748-760</ispartof><rights>GeoRef, Copyright 2020, American Geosciences Institute. 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Participants each received three samples, two containing 17 minerals each and a third containing ten minerals. The true composition of the samples was unknown to all participants during the contest period. The results submitted were ranked by summing the deviations from the actual compositions (bias). The top three finishers used mainly X-ray diffraction (XRD) for identification and quantification. The winner obtained an average bias of 11.3% per sample by using an internal standard and modified single-line reference intensity ratio (RIR) method based on pure mineral standards. Full-pattern fitting by genetic algorithm was used to measure the integrated intensity of the diagnostic single-line reflections chosen for quantification. Elemental-composition optimization was used separately to constrain phase concentrations that were uncertain because the reference mineral standards were lacking or not ideal. Cation exchange capacity, oriented-sample XRD analysis, and thermogravimetric analysis were also used as supplementary techniques. The second-place finisher obtained an average bias of 13.9%, also by using an RIR method, but without an added internal standard and with intensity measured by whole-pattern fitting. The third-place finisher, who obtained an average bias of 15.3%, used the Rietveld method for quantification and identification of minor phases (using difference plots). This participant also used scanning electron microscopy (with X-ray microanalysis) to identify minor components and verify the composition of structures used in Rietveld analysis. As in the previous contests, successful quantification appears to be more dependent on analyst experience than on the analytical technique or software used.</description><subject>cation exchange capacity</subject><subject>chemical composition</subject><subject>chemical properties</subject><subject>clay mineralogy</subject><subject>Clay Minerals</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>experimental studies</subject><subject>geochemistry</subject><subject>Mineralogy</subject><subject>Pure Reference Minerals</subject><subject>Quantitative Analysis</subject><subject>Reference Intensity Ratio</subject><subject>Reynolds Cup</subject><subject>Rietveld</subject><subject>rock, sediment, soil</subject><subject>samples</subject><subject>sed rocks, sediments</subject><subject>Sedimentary petrology</subject><subject>sheet silicates</subject><subject>Silicates</subject><subject>standard materials</subject><subject>The Clay Minerals Society</subject><subject>Whole-Pattern Fitting</subject><subject>X-ray diffraction data</subject><issn>0009-8604</issn><issn>1552-8367</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><recordid>eNqNkU1v1DAQhiMEEkvhB3DzBS4oy8QfiXNCKAVaqbRSac_RrD3ZpnKcre0U7b_Hy67ElZEsv7IePSPPFMX7CtaVkPXnrvt5veYA9RqUhBraF8WqUoqXWtTNy2IFAG2pa5CvizcxPgLwWgq-Kra_5olYXIyhGIfFMdztwozmgSJLM3ta0KcxYRqfiU2jp4AZ8ej2cYwMIwv0TOjIss2epQdi4vac3dLez85G1i07ZmafKKa3xasBXaR3p_usuP_-7a67KK9uflx2X6_KrQSVSk1GEg60MdJCq1GgVi2Xm8YqsLVsVQNaaaUG3RBxK2zdaLJWcNtUqCwXZ8XHozf_4mnJjftpjIacQ0_zEnvetrKqdP0foFJK8oPxwwnEaNANAb0ZY78L44Rh31d5wLpSMnNfjtzot-QT9o_zEvKkYm-mfMzUH9bTw99S8hTyC4Z0CG02fDoatjRHM5I39HsOzv4zZUPTQwW61eIPDfyYdQ</recordid><startdate>20061201</startdate><enddate>20061201</enddate><creator>Omotoso, Oladipo</creator><creator>McCarty, Douglas K</creator><creator>Hillier, Stephen</creator><creator>Kleeberg, Reinhard</creator><general>Clay Minerals Society</general><general>The Clay Minerals Society</general><scope>IQODW</scope><scope>7QQ</scope><scope>8FD</scope><scope>JG9</scope></search><sort><creationdate>20061201</creationdate><title>Some successful approaches to quantitative mineral analysis as revealed by the 3RD Reynolds Cup contest</title><author>Omotoso, Oladipo ; McCarty, Douglas K ; Hillier, Stephen ; Kleeberg, Reinhard</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-g405t-8ec4eafebc4d098a3a85924b7d50d64957085855f87ee2d3d678edd32d71a5d23</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2006</creationdate><topic>cation exchange capacity</topic><topic>chemical composition</topic><topic>chemical properties</topic><topic>clay mineralogy</topic><topic>Clay Minerals</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>experimental studies</topic><topic>geochemistry</topic><topic>Mineralogy</topic><topic>Pure Reference Minerals</topic><topic>Quantitative Analysis</topic><topic>Reference Intensity Ratio</topic><topic>Reynolds Cup</topic><topic>Rietveld</topic><topic>rock, sediment, soil</topic><topic>samples</topic><topic>sed rocks, sediments</topic><topic>Sedimentary petrology</topic><topic>sheet silicates</topic><topic>Silicates</topic><topic>standard materials</topic><topic>The Clay Minerals Society</topic><topic>Whole-Pattern Fitting</topic><topic>X-ray diffraction data</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Omotoso, Oladipo</creatorcontrib><creatorcontrib>McCarty, Douglas K</creatorcontrib><creatorcontrib>Hillier, Stephen</creatorcontrib><creatorcontrib>Kleeberg, Reinhard</creatorcontrib><collection>Pascal-Francis</collection><collection>Ceramic Abstracts</collection><collection>Technology Research Database</collection><collection>Materials Research Database</collection><jtitle>Clays and clay minerals</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Omotoso, Oladipo</au><au>McCarty, Douglas K</au><au>Hillier, Stephen</au><au>Kleeberg, Reinhard</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Some successful approaches to quantitative mineral analysis as revealed by the 3RD Reynolds Cup contest</atitle><jtitle>Clays and clay minerals</jtitle><stitle>Clays Clay Miner</stitle><date>2006-12-01</date><risdate>2006</risdate><volume>54</volume><issue>6</issue><spage>748</spage><epage>760</epage><pages>748-760</pages><issn>0009-8604</issn><eissn>1552-8367</eissn><coden>CLCMAB</coden><abstract>Details of the quantitative techniques successfully applied to artificial rock mixtures distributed for the third Clay Minerals Society Reynolds Cup (RC) contest are presented. Participants each received three samples, two containing 17 minerals each and a third containing ten minerals. The true composition of the samples was unknown to all participants during the contest period. The results submitted were ranked by summing the deviations from the actual compositions (bias). The top three finishers used mainly X-ray diffraction (XRD) for identification and quantification. The winner obtained an average bias of 11.3% per sample by using an internal standard and modified single-line reference intensity ratio (RIR) method based on pure mineral standards. Full-pattern fitting by genetic algorithm was used to measure the integrated intensity of the diagnostic single-line reflections chosen for quantification. Elemental-composition optimization was used separately to constrain phase concentrations that were uncertain because the reference mineral standards were lacking or not ideal. Cation exchange capacity, oriented-sample XRD analysis, and thermogravimetric analysis were also used as supplementary techniques. The second-place finisher obtained an average bias of 13.9%, also by using an RIR method, but without an added internal standard and with intensity measured by whole-pattern fitting. The third-place finisher, who obtained an average bias of 15.3%, used the Rietveld method for quantification and identification of minor phases (using difference plots). This participant also used scanning electron microscopy (with X-ray microanalysis) to identify minor components and verify the composition of structures used in Rietveld analysis. As in the previous contests, successful quantification appears to be more dependent on analyst experience than on the analytical technique or software used.</abstract><cop>Boulder, CO</cop><pub>Clay Minerals Society</pub><doi>10.1346/CCMN.2006.0540609</doi><tpages>13</tpages></addata></record> |
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subjects | cation exchange capacity chemical composition chemical properties clay mineralogy Clay Minerals Earth sciences Earth, ocean, space Exact sciences and technology experimental studies geochemistry Mineralogy Pure Reference Minerals Quantitative Analysis Reference Intensity Ratio Reynolds Cup Rietveld rock, sediment, soil samples sed rocks, sediments Sedimentary petrology sheet silicates Silicates standard materials The Clay Minerals Society Whole-Pattern Fitting X-ray diffraction data |
title | Some successful approaches to quantitative mineral analysis as revealed by the 3RD Reynolds Cup contest |
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