4.7 Article

Aging shapes Cr(VI) speciation in five different soils

Journal

SCIENCE OF THE TOTAL ENVIRONMENT
Volume 804, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.scitotenv.2021.150066

Keywords

Cr(VI) speciation; Aging; Immobilization; Chemical kinetic equations; Multireaction model

Funding

  1. Natural Sciences and Engineering Re-search Council of Canada [RGPIN-2014-04770]
  2. Natural Science Foundation of Hunan Province of China [2020JJ4098]

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In this study, sequential extraction methods were used to analyze the transformations of Cr fractions in soils spiked with Cr(VI) over a 240-day incubation period. The results showed a continuous decrease in available Cr(VI) and an increase in immobile Cr(VI) and Cr(III) over time. Modeling analysis revealed that Cr(VI) reduction and immobilization were occurring concurrently in soils, with different favorable conditions.
To make sound decisions regarding management of heavy metal contamination in soils, it is necessary to understand contaminant transformations over extended periods. In this study, sequential extraction methods were applied to quantify the changes of Cr fractions [available Cr(VI), immobile Cr(VI) and immobile Cr(III)] in five contrasting soils spiked with Cr(VI) over a 240-day incubation. Results showed that available Cr(VI) in soils continually decreased during aging, with a sharp decline occurring in the first 30 days. The best fit of available Cr(VI) data was obtained using an Elovich model for Brunisol and Anthrosol-1, a fractional power model for Anthrosol2, and a pseudo first-order kinetic model for Luvisol-1 and Luvisol-2. After aging for 240 days, immobile Cr(VI) increased by 4.5-31% and immobile Cr(III) increased by 68-95% of total spiked Cr(VI) in Brunisol, Anthrosol-1 and Anthrosol-2. The two Luvisol soils had relatively high reduction rates with no Cr(VI) immobilized. A multireaction model was developed in MATLAB Simulink toolbox to describe transformation flow rates among soluble Cr(VI), adsorbed Cr(VI), immobilized Cr(VI) and immobilized Cr(III) in soils with aging. We conclude that (i) Cr(VI) reduction and immobilization were occurring concurrently in soils and competing for available Cr(VI) species; (ii) Cr(VI) reduction is favored by low soil pH and high organic carbon, while Cr(VI) immobilization occurs with cations (such as Ca2+) and Fe oxides. (C) 2021 Elsevier B.V. All rights reserved.

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