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In situ determination of V(V) by diffusive gradients in thin films and inductively coupled plasma mass spectrometry techniques using amberlite IRA-410 resin as a binding layer

dc.contributor.authorLuko, Karen Silva [UNESP]
dc.contributor.authorMenegário, Amauri Antonio [UNESP]
dc.contributor.authorSuárez, Carlos Alfredo [UNESP]
dc.contributor.authorTafurt-Cardona, Makenly [UNESP]
dc.contributor.authorPedrobom, Jorge Henrique [UNESP]
dc.contributor.authorRolisola, Ana Marta Cavinato Marchini [UNESP]
dc.contributor.authorSulato, Everton Tiago [UNESP]
dc.contributor.authorKiang, Chang Hung [UNESP]
dc.contributor.institutionUniversidade Estadual Paulista (Unesp)
dc.date.accessioned2018-12-11T17:08:04Z
dc.date.available2018-12-11T17:08:04Z
dc.date.issued2017-01-15
dc.description.abstractAmberlite IRA-410 anionic exchange resin was evaluated as the binding layer for sampling V(V) by using Diffusive Gradients in Thin Films (DGT). V(V) was determined by inductively coupled plasma mass spectrometry (ICP-MS). Mass vs. time DGT deployments (ionic strength = 0.03 mol L−1 NaNO3, pH = 5.6 and T = 23.5 ± 0.5 °C) was characterized by excellent linear relationship (R2 = 0.9993) and a significant retention of V(V) by the binding layer. An exchange capacity of at least 40 μg V g−1 resin was achieved for the proposed binding layer. The diffusion coefficient obtained (7.13 ± 0.6 10−6 cm2 s−1) agrees with the literature. The accumulation rate of V(V) was not significantly affected by ionic strength of solutions up to 0.03 mol L−1 and for the entire studied pH range (from 3 to 9). Furthermore, when comparing the concentrations obtained using IRA-410-DGT and those obtained by direct measurement of the solution concentrations, the proposed approach provided a reduction of the 35Cl16O interference on V(V) determination by ICP-MS. Determination of V in normal mode (without collision cell) in solutions containing analyte:Cl− concentration ratio up to 1:500,000 was not affected by interference of 35Cl16O+ polyatomic ion even when normal mode ICP-MS was used. Potential interfering ions on sampling V(V) by DGT (PO4 3− and SO4 2−) showed no significant effects on the accumulation rate of V(V). Laboratory tests performed using synthetic samples, natural freshwater and acid drainage water showed an excellent performance (recoveries from 93% to 110%). For in situ deployment, measurements of V(V) by the proposed approach was not significantly different (95.5%) from the value of dissolved V concentration.en
dc.description.affiliationCentro de Estudos Ambientais Universidade Estadual Paulista
dc.description.affiliationInstituto de Geociências e Meio Ambiente IGCE UNESP - Universidade Estadual Paulista
dc.description.affiliationUnespCentro de Estudos Ambientais Universidade Estadual Paulista
dc.description.affiliationUnespInstituto de Geociências e Meio Ambiente IGCE UNESP - Universidade Estadual Paulista
dc.description.sponsorshipCoordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)
dc.description.sponsorshipConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
dc.description.sponsorshipIdCNPq: 162530/2013-7
dc.description.sponsorshipIdCNPq: 307097/2013-7
dc.format.extent32-40
dc.identifierhttp://dx.doi.org/10.1016/j.aca.2016.11.031
dc.identifier.citationAnalytica Chimica Acta, v. 950, p. 32-40.
dc.identifier.doi10.1016/j.aca.2016.11.031
dc.identifier.file2-s2.0-84999749828.pdf
dc.identifier.issn1873-4324
dc.identifier.issn0003-2670
dc.identifier.lattes1989662459244838
dc.identifier.scopus2-s2.0-84999749828
dc.identifier.urihttp://hdl.handle.net/11449/173856
dc.language.isoeng
dc.relation.ispartofAnalytica Chimica Acta
dc.relation.ispartofsjr1,512
dc.rights.accessRightsAcesso aberto
dc.sourceScopus
dc.subject35Cl16O
dc.subjectAgarose
dc.subjectDGT
dc.subjectICP-MS
dc.subjectVanadium
dc.titleIn situ determination of V(V) by diffusive gradients in thin films and inductively coupled plasma mass spectrometry techniques using amberlite IRA-410 resin as a binding layeren
dc.typeArtigo
dspace.entity.typePublication
unesp.author.lattes5919521356445801[2]
unesp.author.lattes1989662459244838[8]
unesp.author.orcid0000-0002-1111-9758[2]

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