2005
DOI: 10.1021/es0483802
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Field-Flow Fractionation−Inductively Coupled Plasma Mass Spectrometry:  An Alternative Approach to Investigate Metal−Humic Substances Interaction

Abstract: Interaction between metal ions and humic matter was investigated using a hyphenated technique, field-flow fractionation-inductively coupled plasma mass spectrometry (FFF-ICP-MS). Aggregation of a metal-spiked commercial Aldrich humic acid in an aqueous solution of calcium ion or in seawater was examined over time intervals of 0-4320 min. The aggregation was demonstrated by shifts in peak maximum of humic matter from smaller size (2.9 nm) to larger size (5.1 or 5.8 nm in Ca2+ solution or in seawater, respective… Show more

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Cited by 71 publications
(37 citation statements)
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“…However, earlier studies concerning the freeze fractionation of inorganic ions have suggested that freezing rejects preferably smaller ions with larger diffusion coefficients (e.g., 2 × 10 −9 m 2 s −1 for K + ) than larger ions with smaller diffusion coefficients (e.g., 0.5 × 10 −9 m 2 s −1 for SO 4 2− ; Granskog et al, 2004;Maus et al, 2011). The diffusion coefficients of humic-like DOM, shown in our analyses, can range over four-fold like those of major inorganic ions in seawater (Hassellöv, 2005;Siripinyanond et al, 2005). If diffusion plays a major role in the process of selective rejection of DOM as suggested for inorganic ions, we should have observed a shift towards larger molecules in the samples collected from ice in our LC-SEC measurements.…”
Section: Selective Incorporation Of Dom Fractions During Ice Formationmentioning
confidence: 54%
“…However, earlier studies concerning the freeze fractionation of inorganic ions have suggested that freezing rejects preferably smaller ions with larger diffusion coefficients (e.g., 2 × 10 −9 m 2 s −1 for K + ) than larger ions with smaller diffusion coefficients (e.g., 0.5 × 10 −9 m 2 s −1 for SO 4 2− ; Granskog et al, 2004;Maus et al, 2011). The diffusion coefficients of humic-like DOM, shown in our analyses, can range over four-fold like those of major inorganic ions in seawater (Hassellöv, 2005;Siripinyanond et al, 2005). If diffusion plays a major role in the process of selective rejection of DOM as suggested for inorganic ions, we should have observed a shift towards larger molecules in the samples collected from ice in our LC-SEC measurements.…”
Section: Selective Incorporation Of Dom Fractions During Ice Formationmentioning
confidence: 54%
“…Another technique widely used for size separation of humic materials is fi eld -fl ow fractionation (FFF) (e.g., Baalousha et al, 2006 ;Boehme and Wells, 2006 ;Geckeis et al, 2003 ;Hassil ' ov et al, 2007;Siripinyanond et al, 2005 ;Suteerapataranon et al, 2006 ;Zanardi -Lamardo et al, 2002 ). This technique was developed and introduced in 1966 by Giddings (1966) as a method for the separation and characterization of materials ranging in size from macromolecules to particulates.…”
Section: Field -Flow Fractionation ( Fff )mentioning
confidence: 99%
“…Size characteristics were reported by several authors (Baalousha et al, 2006 ;Boehme and Wells, 2006 ;Geckeis et al, 2003 ;Siripinyanond et al, 2005 ;Suteerapataranon et al, 2006 ;Zanardi -Lamardo et al, 2002 ). Over the past decade, about 20 papers were published on FlFFF fractionation of humic materials.…”
Section: Use Of Field -Flow Fractionation For the Separation Of Humicmentioning
confidence: 99%
“…Therefore, in environment as well as health monitoring, the detection of Cu 2+ is undoubtedly important. As a result, various analytical techniques for Cu 2+ detection have been developed such as by atomic absorption/emission spectroscopy [8], inductively coupled plasma mass spectrometry (ICP-MS) [9], and capillary electrophoresis [10]. However, all of these methods require expensive and sophisticated instruments combined with complicated sample pretreatment and therefore impractical for a real-time experiment.…”
Section: Introductionmentioning
confidence: 99%