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Traceable and accurate quantification of iron in seawater using isotope dilution calibration strategies by triple quadrupole ICP-MS/MS: Characterization measurements of iron in a candidate seawater CRM

dc.contributor.authorAn, Betul
dc.contributor.authorCan, Suleyman Z.
dc.contributor.authorBakirdere, Sezgin
dc.date.accessioned2026-06-27T14:29:49Z
dc.date.issued2020
dc.description.abstractAccurate quantification of iron is crucial for the characterization of a candidate seawater certified reference material. Isotope dilution mass spectrometry as a primary method is one of the option for this purpose. In this study, triethylamine (TEA) assisted Mg(OH)(2) co-precipitation is developed and combined with isotope dilution mass spectrometry for the characterization of candidate certified reference material, UME CRM 1206. The analytical protocol of co-precipitation was optimized to achieve reproducible yields of similar to 100% Fe with high salt rejection (residual salinity similar to 0.003%). Three calibration strategies, single, double and triple isotope dilution mass spectrometry (IDMS) coupled with co-precipitation were investigated in terms of metrological aspects. The determination of Fe was carried out by ICP-MS with tandem configuration (ICP-MS/MS) using NH3/He cell gas which was optimized for the minimum background equivalence concentration to be able to measure highly accurate Fe-56/Fe-57 ratio with the highest possible sensitivity. The background corrected typical procedural blank levels and limit of detection calculated based on three times the standard deviation of blanks were found as 9 ng/kg (0.16 nM) and 11 ng/kg (0.20 nM) for single IDMS, respectively. Trueness of the developed analytical methods has been demonstrated using CASS-6 and NMIA MX014 with complete and very precise recoveries. SI-traceable values with combined uncertainty (k = 2) were obtained for single, double and triple IDMS as (12.70 +/- 0.16) ng/g, (12.728 +/- 0.084) ng/g and (12.732 +/- 0.062) ng/g, respectively. The relative combined uncertainty for each approach was calculated as 0.64%, 0.33% and 0.24%, respectively.en
dc.description.urihttps://doi.org/10.1016/j.talanta.2019.120503
dc.identifier.doi10.1016/j.talanta.2019.120503
dc.identifier.eissn1873-3573
dc.identifier.issn0039-9140
dc.identifier.pubmed31892083
dc.identifier.urihttps://hdl.handle.net/20.500.14981/61294
dc.identifier.volume209
dc.identifier.wos000509632900022
dc.language.isoeng
dc.publisherELSEVIER
dc.relation.ispartofTALANTA
dc.subjectIsotope dilution mass spectrometry
dc.subjectSingle dilution
dc.subjectDouble dilution
dc.subjectTriple dilution
dc.subjectSeawater
dc.subjectIron
dc.subjectTriethylamine
dc.subjectMg(OH)(2) co-precipitation
dc.subjectPLASMA-MASS SPECTROMETRY
dc.subjectREDUCED GRAPHENE OXIDE
dc.subjectDETECTOR DEAD-TIME
dc.subjectVOLTAMMETRIC DETERMINATION
dc.subjectCHELATING RESIN
dc.subjectDISSOLVED IRON
dc.subjectMETALS
dc.subjectFE
dc.subjectPRECONCENTRATION
dc.subjectELEMENTS
dc.subjectChemistry
dc.titleTraceable and accurate quantification of iron in seawater using isotope dilution calibration strategies by triple quadrupole ICP-MS/MS: Characterization measurements of iron in a candidate seawater CRM
dc.typeArticle
dspace.entity.typePublication
local.import.sourceWOS

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