Determination of ultra-trace level of Th in seawater by ICP-SFMS after matrix separation and preconcentration.

Journal: Analytica chimica acta
Published Date:

Abstract

This article describes the development and validation of an analytical procedure for the matrix separation, preconcentration and determination of sub-ng kg levels Th in a small volume (20 mL) of seawater samples. The matrix separation and Th preconcentration was carried out using a commercially available ion-chelation system seaFAST-pico. The acidified to pH < 2 seawater samples were mixed on-line with the ammonium acetate buffer (pH of 6.0 ± 0.2) before loading on the column containing resin with iminodiacetic and ethylenediaminetriacetic functional groups. At this pH, Th was quantitatively retained on the resin, demonstrating a good affinity (selectivity) for Th in seawater matrix. The element retained on the resin was eluted using only 0.2 mL of 1.8 M HNO enabling to achieve high preconcentration factor. The pretreatment procedure, with two sample loading cycles (each one 10 mL), was accomplished in about 25 min. Determining Th mass fraction in seawater samples was based on isotope dilution inductively coupled plasma mass spectrometry (ID ICP-MS) method, which was considered as the most accurate calibration strategy for precise quantification of Th mass fraction in seawater samples. ISO/IEC17025 and Eurachem guidelines were followed to perform the validation of the developed in this study procedure. In the case of seawater samples with natural level of thorium the major contributions to the expanded uncertainty arose from the uncertainty associated with isotopic ratio measurements in the isotopically spiked sample, followed by the correction for procedural blank and the correction for mass discrimination effect. The estimated method detection limit for Th was 0.005 ng kg. The developed method was successfully applied to the determination of Th mass fraction in seawater reference samples: IAEA-443, SLEW-3, NASS-4, NASS-6, and CASS-5. Although Th is not certified in any of the seawater reference materials, a good agreement was obtained between the results in this study and data published elsewhere.

Authors

  • Irena Wysocka
    International Atomic Energy Agency, Environmental Laboratories, 4 Quai Antoine 1(er), 98000 Monaco; Polish Geological Institute National Research Institute, Rakowiecka 4, 00-975 Warsaw, Poland.
  • Emilia Vassileva
    International Atomic Energy Agency, Environmental Laboratories, 4 Quai Antoine 1(er), 98000 Monaco. Electronic address: e.vasileva-veleva@iaea.org.

Keywords

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