Preconcentration and Atomic Spectrometric Determination of Rare Earth Elements (rees) in Natural Water Samples by Inductively Coupled Plasma Atomic Emission Spectrometry
| dc.contributor.author | Pasinli, Türker | |
| dc.contributor.author | Eroğlu, Ahmet Emin | |
| dc.contributor.author | Shahwan, Talal | |
| dc.coverage.doi | 10.1016/j.aca.2005.04.076 | |
| dc.date.accessioned | 2014-07-25T03:25:27Z | |
| dc.date.available | 2014-07-25T03:25:27Z | |
| dc.date.issued | 2005 | |
| dc.description.abstract | The usage of a variety of sorbents has been shown as promising matrix removal/preconcentration strategies for the determination of rare earth elements (REEs) in various natural water samples by inductively coupled plasma atomic emission spectrometry (ICP-AES). The sorption efficiency of various zeolites (clinoptilolite, mordenite, zeolite Y, zeolite Beta), ion-exchangers (Amberlite CG-120, Amberlite IR-120, Rexyn 101, Dowex 50W X18) and chelating resins (Muromac, Chelex 100, Amberlite IRC-718) towards REEs was investigated in terms of solution pH, shaking time and sorbent amount. The results have shown that most of the materials can take up REEs at a wide pH range. The experiments were continued with clinoptilolite, zeolite Y and Chelex 100 and it was demonstrated that all three materials displayed very fast kinetics for REE sorption (higher than 96% in 1 min). Desorption from the sorbents was realized with 2.0 M HNO3 for clinoptilolite and 0.1 M HNO3 for zeolite Y and Chelex 100. Only the lower concentration range (0.01–2.0 mg l−1) of matrix-matched standards were used in quantitation although the calibration graphs were linear at least up to 10.0 mg l−1 for all REEs studied. The limit of detection (3 s) without preconcentration was 0.1, 1.0, and 0.2 μg l−1 for Eu, La, and Yb, respectively. The validity of the method with the selected sorbents was checked through spike recovery experiments. | en_US |
| dc.description.sponsorship | IYTE | en_US |
| dc.identifier.citation | Pasinli, T., Eroğlu, Ahmet E., & Shahwan, T. (2005). Preconcentration and atomic spectrometric determination of rare earth elements (REEs) in natural water samples by inductively coupled plasma atomic emission spectrometry. Analytica Chimica Acta, 547(1), 42–49. doi:10.1016/j.aca.2005.04.076 | en_US |
| dc.identifier.doi | 10.1016/j.aca.2005.04.076 | en_US |
| dc.identifier.doi | 10.1016/j.aca.2005.04.076 | |
| dc.identifier.issn | 0003-2670 | |
| dc.identifier.issn | 1873-4324 | |
| dc.identifier.issn | 0003-2670 | |
| dc.identifier.scopus | 2-s2.0-23044434002 | |
| dc.identifier.uri | https://hdl.handle.net/11147/4087 | |
| dc.identifier.uri | http://doi.org/10.1016/j.aca.2005.04.076 | |
| dc.language.iso | en | en_US |
| dc.publisher | Elsevier Ltd. | en_US |
| dc.relation.ispartof | Analytica Chimica Acta | en_US |
| dc.rights | info:eu-repo/semantics/openAccess | en_US |
| dc.subject | Rare earth element | en_US |
| dc.subject | Inductively coupled plasma atomic emission spectrometry (ICP-AES) | en_US |
| dc.subject | Preconcentration | en_US |
| dc.subject | Clinoptilolite | en_US |
| dc.subject | Zeolite Y | en_US |
| dc.subject | Chelex 100 | en_US |
| dc.title | Preconcentration and Atomic Spectrometric Determination of Rare Earth Elements (rees) in Natural Water Samples by Inductively Coupled Plasma Atomic Emission Spectrometry | en_US |
| dc.type | Article | en_US |
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| gdc.author.institutional | Eroğlu, Ahmet Emin | |
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| gdc.description.department | İzmir Institute of Technology. Chemistry | en_US |
| gdc.description.endpage | 49 | |
| gdc.description.issue | 1 | en_US |
| gdc.description.publicationcategory | Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı | en_US |
| gdc.description.scopusquality | Q1 | |
| gdc.description.startpage | 42 | |
| gdc.description.volume | 547 | en_US |
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| gdc.oaire.keywords | Clinoptilolite | |
| gdc.oaire.keywords | Inductively coupled plasma atomic emission spectrometry (ICP-AES) | |
| gdc.oaire.keywords | Zeolite Y | |
| gdc.oaire.keywords | Chelex 100 | |
| gdc.oaire.keywords | Rare earth element | |
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