Investigating the Influence of Non‐Spectral Matrix Effects in the Determination of Twenty‐Two Trace Elements in Rock Samples by ICP‐QMS
The influence of non‐spectral matrix effects on the determination of twenty‐two trace elements (Rb, Sr, Y, Cs, Ba, lanthanides, Pb, Th and U) in rock samples using ICP‐MS was investigated. Three types of multi‐element solutions were synthesised containing the twenty‐two trace elements, In, Tl and te...
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description | The influence of non‐spectral matrix effects on the determination of twenty‐two trace elements (Rb, Sr, Y, Cs, Ba, lanthanides, Pb, Th and U) in rock samples using ICP‐MS was investigated. Three types of multi‐element solutions were synthesised containing the twenty‐two trace elements, In, Tl and ten major rock‐forming elements with varying mass fractions mimicking the compositions of basalt, peridotite and dolomite. The synthetic solutions were conditioned to have dilution factors (DF) of 1000–10000. The extent of sensitivity suppression relative to the DF = 10000 solution became more significant for smaller DF solutions, which was not constant across different elements in a single solution but displayed general dependence on m/z. This indicates that at least two internal standards (e.g., In and Tl) are required for the correction of sensitivity variation. On the basis of the results, a new isotope dilution‐internal standardisation method for the determination of twenty‐two trace elements with ICP‐MS was developed, in which the sensitivity variation was corrected by monitoring two enriched isotopes, 113In and 203Tl. This method, coupled with the quantitative correction of interference from oxides and hydroxides, achieved precise determination of twenty‐two trace elements in some rock reference materials with reproducibilities of ±2% for basaltic to andesitic samples.
Key Points
The influence of non‐spectral matrix effects on the determination of twenty‐two trace elements in rock samples with ICP‐MS was investigated using three types of synthetic solutions mimicking the compositions of basalt, peridotite and dolomite.
The extent of sensitivity suppression became more significant for solutions with smaller dilution factor, which was not constant across different elements in a single solution but displayed general dependence on m/z.
A new isotope dilution‐internal standardisation method was developed for the determination of twenty‐two trace elements with ICP‐MS, in which the sensitivity variation is corrected by monitoring two enriched isotopes, 113In and 203Tl. |
doi_str_mv | 10.1111/ggr.12147 |
format | Article |
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Key Points
The influence of non‐spectral matrix effects on the determination of twenty‐two trace elements in rock samples with ICP‐MS was investigated using three types of synthetic solutions mimicking the compositions of basalt, peridotite and dolomite.
The extent of sensitivity suppression became more significant for solutions with smaller dilution factor, which was not constant across different elements in a single solution but displayed general dependence on m/z.
A new isotope dilution‐internal standardisation method was developed for the determination of twenty‐two trace elements with ICP‐MS, in which the sensitivity variation is corrected by monitoring two enriched isotopes, 113In and 203Tl.</description><identifier>ISSN: 1639-4488</identifier><identifier>EISSN: 1751-908X</identifier><identifier>DOI: 10.1111/ggr.12147</identifier><language>eng</language><publisher>Hoboken: Wiley Subscription Services, Inc</publisher><subject>Basalt ; Dilution ; Dolomite ; Dolostone ; Hydroxides ; ICP‐MS ; internal standardisation ; Isotope dilution ; Isotopes ; Lanthanides ; Methods ; non‐spectral matrix effects ; Oxides ; Peridotite ; rock samples ; Rocks ; Sediment samples ; Solutions ; Trace elements</subject><ispartof>Geostandards and geoanalytical research, 2017-06, Vol.41 (2), p.221-242</ispartof><rights>2016 The Authors. Geostandards and Geoanalytical Research © 2016 International Association of Geoanalysts</rights><rights>Geostandards and Geoanalytical Research © 2017 International Association of Geoanalysts</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a4307-607157661c2e38044d44a700c77499682e792da70880f363720bf5583dc021953</citedby><cites>FETCH-LOGICAL-a4307-607157661c2e38044d44a700c77499682e792da70880f363720bf5583dc021953</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1111%2Fggr.12147$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1111%2Fggr.12147$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,27901,27902,45550,45551</link.rule.ids></links><search><creatorcontrib>Yokoyama, Tetsuya</creatorcontrib><creatorcontrib>Nagai, Yuichiro</creatorcontrib><creatorcontrib>Hinohara, Yu</creatorcontrib><creatorcontrib>Mori, Tomohiko</creatorcontrib><title>Investigating the Influence of Non‐Spectral Matrix Effects in the Determination of Twenty‐Two Trace Elements in Rock Samples by ICP‐QMS</title><title>Geostandards and geoanalytical research</title><description>The influence of non‐spectral matrix effects on the determination of twenty‐two trace elements (Rb, Sr, Y, Cs, Ba, lanthanides, Pb, Th and U) in rock samples using ICP‐MS was investigated. Three types of multi‐element solutions were synthesised containing the twenty‐two trace elements, In, Tl and ten major rock‐forming elements with varying mass fractions mimicking the compositions of basalt, peridotite and dolomite. The synthetic solutions were conditioned to have dilution factors (DF) of 1000–10000. The extent of sensitivity suppression relative to the DF = 10000 solution became more significant for smaller DF solutions, which was not constant across different elements in a single solution but displayed general dependence on m/z. This indicates that at least two internal standards (e.g., In and Tl) are required for the correction of sensitivity variation. On the basis of the results, a new isotope dilution‐internal standardisation method for the determination of twenty‐two trace elements with ICP‐MS was developed, in which the sensitivity variation was corrected by monitoring two enriched isotopes, 113In and 203Tl. This method, coupled with the quantitative correction of interference from oxides and hydroxides, achieved precise determination of twenty‐two trace elements in some rock reference materials with reproducibilities of ±2% for basaltic to andesitic samples.
Key Points
The influence of non‐spectral matrix effects on the determination of twenty‐two trace elements in rock samples with ICP‐MS was investigated using three types of synthetic solutions mimicking the compositions of basalt, peridotite and dolomite.
The extent of sensitivity suppression became more significant for solutions with smaller dilution factor, which was not constant across different elements in a single solution but displayed general dependence on m/z.
A new isotope dilution‐internal standardisation method was developed for the determination of twenty‐two trace elements with ICP‐MS, in which the sensitivity variation is corrected by monitoring two enriched isotopes, 113In and 203Tl.</description><subject>Basalt</subject><subject>Dilution</subject><subject>Dolomite</subject><subject>Dolostone</subject><subject>Hydroxides</subject><subject>ICP‐MS</subject><subject>internal standardisation</subject><subject>Isotope dilution</subject><subject>Isotopes</subject><subject>Lanthanides</subject><subject>Methods</subject><subject>non‐spectral matrix effects</subject><subject>Oxides</subject><subject>Peridotite</subject><subject>rock samples</subject><subject>Rocks</subject><subject>Sediment samples</subject><subject>Solutions</subject><subject>Trace elements</subject><issn>1639-4488</issn><issn>1751-908X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><recordid>eNp1kE1OwzAUhCMEEqWw4AaWWLFIayeOf5aolBKp5acNErvITe2QkjjBSSnZcQEkzshJcBu2vI2fRt_Mk8dxzhEcIDvDNDUD5CFMD5weogFyOWTPh3YnPncxZuzYOanrNYQB5gHqOV-hfpd1k6WiyXQKmhcJQq3yjdSJBKUCd6X--fxeVDJpjMjBTDQm-wBjpaxQg0zvHdeykabItM0o9c4VbaVuWmuMtiWIjLBZ41wWVtx75mXyChaiqHJZg2ULwtGDZR9ni1PnSIm8lmd_b995uhlHo1t3ej8JR1dTV2AfUpdAigJKCEo86TOI8QpjQSFMKMWcE-ZJyr2VVRiDyic-9eBSBQHzVwn0EA_8vnPR5VamfNvY_8frcmO0PRkjxgnhmPrMUpcdlZiyro1UcWWyQpg2RjDetR3btuN925Ydduw2y2X7PxhPJvPO8Qt4-YKc</recordid><startdate>201706</startdate><enddate>201706</enddate><creator>Yokoyama, Tetsuya</creator><creator>Nagai, Yuichiro</creator><creator>Hinohara, Yu</creator><creator>Mori, Tomohiko</creator><general>Wiley Subscription Services, Inc</general><scope>AAYXX</scope><scope>CITATION</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>201706</creationdate><title>Investigating the Influence of Non‐Spectral Matrix Effects in the Determination of Twenty‐Two Trace Elements in Rock Samples by ICP‐QMS</title><author>Yokoyama, Tetsuya ; Nagai, Yuichiro ; Hinohara, Yu ; Mori, Tomohiko</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a4307-607157661c2e38044d44a700c77499682e792da70880f363720bf5583dc021953</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Basalt</topic><topic>Dilution</topic><topic>Dolomite</topic><topic>Dolostone</topic><topic>Hydroxides</topic><topic>ICP‐MS</topic><topic>internal standardisation</topic><topic>Isotope dilution</topic><topic>Isotopes</topic><topic>Lanthanides</topic><topic>Methods</topic><topic>non‐spectral matrix effects</topic><topic>Oxides</topic><topic>Peridotite</topic><topic>rock samples</topic><topic>Rocks</topic><topic>Sediment samples</topic><topic>Solutions</topic><topic>Trace elements</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Yokoyama, Tetsuya</creatorcontrib><creatorcontrib>Nagai, Yuichiro</creatorcontrib><creatorcontrib>Hinohara, Yu</creatorcontrib><creatorcontrib>Mori, Tomohiko</creatorcontrib><collection>CrossRef</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Geostandards and geoanalytical research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Yokoyama, Tetsuya</au><au>Nagai, Yuichiro</au><au>Hinohara, Yu</au><au>Mori, Tomohiko</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Investigating the Influence of Non‐Spectral Matrix Effects in the Determination of Twenty‐Two Trace Elements in Rock Samples by ICP‐QMS</atitle><jtitle>Geostandards and geoanalytical research</jtitle><date>2017-06</date><risdate>2017</risdate><volume>41</volume><issue>2</issue><spage>221</spage><epage>242</epage><pages>221-242</pages><issn>1639-4488</issn><eissn>1751-908X</eissn><abstract>The influence of non‐spectral matrix effects on the determination of twenty‐two trace elements (Rb, Sr, Y, Cs, Ba, lanthanides, Pb, Th and U) in rock samples using ICP‐MS was investigated. Three types of multi‐element solutions were synthesised containing the twenty‐two trace elements, In, Tl and ten major rock‐forming elements with varying mass fractions mimicking the compositions of basalt, peridotite and dolomite. The synthetic solutions were conditioned to have dilution factors (DF) of 1000–10000. The extent of sensitivity suppression relative to the DF = 10000 solution became more significant for smaller DF solutions, which was not constant across different elements in a single solution but displayed general dependence on m/z. This indicates that at least two internal standards (e.g., In and Tl) are required for the correction of sensitivity variation. On the basis of the results, a new isotope dilution‐internal standardisation method for the determination of twenty‐two trace elements with ICP‐MS was developed, in which the sensitivity variation was corrected by monitoring two enriched isotopes, 113In and 203Tl. This method, coupled with the quantitative correction of interference from oxides and hydroxides, achieved precise determination of twenty‐two trace elements in some rock reference materials with reproducibilities of ±2% for basaltic to andesitic samples.
Key Points
The influence of non‐spectral matrix effects on the determination of twenty‐two trace elements in rock samples with ICP‐MS was investigated using three types of synthetic solutions mimicking the compositions of basalt, peridotite and dolomite.
The extent of sensitivity suppression became more significant for solutions with smaller dilution factor, which was not constant across different elements in a single solution but displayed general dependence on m/z.
A new isotope dilution‐internal standardisation method was developed for the determination of twenty‐two trace elements with ICP‐MS, in which the sensitivity variation is corrected by monitoring two enriched isotopes, 113In and 203Tl.</abstract><cop>Hoboken</cop><pub>Wiley Subscription Services, Inc</pub><doi>10.1111/ggr.12147</doi><tpages>22</tpages></addata></record> |
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subjects | Basalt Dilution Dolomite Dolostone Hydroxides ICP‐MS internal standardisation Isotope dilution Isotopes Lanthanides Methods non‐spectral matrix effects Oxides Peridotite rock samples Rocks Sediment samples Solutions Trace elements |
title | Investigating the Influence of Non‐Spectral Matrix Effects in the Determination of Twenty‐Two Trace Elements in Rock Samples by ICP‐QMS |
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