A systematic evaluation of Flow Field Flow Fractionation and single-particle ICP-MS to obtain the size distribution of organo-mineral iron oxyhydroxide colloids

被引:21
作者
Moens, Claudia [1 ]
Waegeneers, Nadia [2 ]
Fritzsche, Andreas [3 ]
Nobels, Peter [4 ]
Smolders, Erik [1 ]
机构
[1] Katholieke Univ Leuven, Dept Earth & Environm Sci, Kasteelpk Arenberg 20 Bus 2459, B-3001 Leuven, Belgium
[2] Sciensano, Serv Trace Elements & Nanomat, Leuvensesteenweg 17, B-3080 Tervuren, Belgium
[3] Friedrich Schiller Univ, Inst Geowissensch, Burgweg 11, D-07749 Jena, Germany
[4] Wageningen Univ & Res, Dept Environm Sci, POB 47, NL-6700 AA Wageningen, Netherlands
关键词
Flow Field Flow Fractionation; Single-particle inductively coupled; plasma-mass spectrometry; Triple quadrupole mass spectrometry; Organo-mineral iron oxyhydroxide colloids; Particle size distribution; Multimethod comparison; INDUCTIVELY-COUPLED PLASMA; MASS-SPECTROMETRY; RICH COLLOIDS; NANOPARTICLES; SPECTROSCOPY; PHOSPHORUS; SPECIATION; POLYPHOSPHATES; SEDIMENTATION; FILTRATION;
D O I
10.1016/j.chroma.2019.04.032
中图分类号
Q5 [生物化学];
学科分类号
071010 ; 081704 ;
摘要
Colloidal iron(III) oxyhydroxides (FeOx) are important reactive adsorbents in nature. This study was set up to determine the size of environmentally relevant FeOx colloids with new methods, i.e. Flow Field Flow Fractionation (FIFFF-UV-ICP-MS) and single-particle ICP-MS/MS (sp-ICP-MS) and to compare these with standard approaches, i.e. dynamic light scattering (DLS), nanoparticle tracking analysis (NTA), microscopy (TEM), membrane filtration, centrifugation and dialysis. Seven synthetic nano- and submicron FeOx with different mineralogy and coating were prepared and two soil solutions were included. The FIFFF was optimized for Fe recovery, yielding 70-90%. The FIFFF determines particle size with high resolution in a 1 mM NH4HCO3 (pH 8.3) background and can detect Fe-NOM complexes <5 nm and organo-mineral FeOx particles ranging 5-300 nm. The sp-ICP-MS method had a size detection limit for FeOx of about 32-47 nm. The distribution of hydrodynamic diameters of goethite particles detected with FIFFF, NTA and DLS were similar but the values were twice as large as the Fe cores of particles detected with sp-ICP-MS and TEM. Conventional fractionation by centrifugation and dialysis generally yielded similar fractions as FIFFF but membrane filtration overestimated the large size fractions. Particles formed from Fe(II) oxidation in the presence of NOM showed strikingly smaller organo-mineral Fe-Ox colloids as the NOM/Fe ratio increased. The soil solution obtained with centrifugation of an acid peat was dominated by small (<30 nm) Fe-OM complexes and organo-mineral FeOx colloids whereas that of a mineral pH neutral soil mainly contains larger (30-200 nm) Fe-rich particles. The FIFFF-UV-ICP-MS is recommended for environmental studies of colloidal FeOx since it has a wide size detection range, it fractionates in an environmentally relevant background (1 mM NH4HCO3) and it has acceptable element recoveries. (C) 2019 Elsevier B.V. All rights reserved.
引用
收藏
页码:203 / 214
页数:12
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