Effects of continuous flow centrifugation on measurements of trace elements in river water: Intrinsic contamination and particle fragmentation

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Abstract

Continuous flow centrifugation (CFC) is a well-established technique used in natural surface water studies to collect large amounts of suspended solids, thus allowing a broad spectrum of measurements. However, a potential contamination or changes in the particle size distribution during the centrifugation may restrain the use of CFC effluents for element analysis in the colloidal and dissolved fractions. In this paper we evaluate the possibility of using the effluent of a Westfalia centrifuge (type KA2-06-075, 9700 rpm) for such analysis. This evaluation is based on two laboratory experiments with deionized and tap water and two field experiments in rivers. Elemental concentration changes across the CFC were assessed from the CFC influent and effluent after a filtration at 0.45 μm. Significant increases were found, mainly in the field experiments at a high suspended solids level and a slightly acid pH. A hypothesis was made on the origin of these increases as a superposition of a centrifuge intrinsic contamination and a particle fragmentation effect. A numerical model based on elemental concentration measurements (inductively coupled plasma mass spectrometry) gave a particle fragmentation level of 0.55% (mass percentage of particles broken up into smaller fragments during centrifugation). In another experiment, a direct particle counting (single particle counter) shows an excess of particles smaller than 500 nm in the CFC effluent, corresponding to a fragmentation level of 0.11%. In consequence, the use of CFC effluent for element analysis is possible in low-turbidity river or lake waters, but should be carefully considered in waters with high suspended matter contents. Copyright © 2006 John Wiley & Sons, Ltd.

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Rossé, P., Vignati, D., & Dominik, J. (2006). Effects of continuous flow centrifugation on measurements of trace elements in river water: Intrinsic contamination and particle fragmentation. Hydrological Processes, 20(13), 2745–2754. https://doi.org/10.1002/hyp.6064

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