Effective removal of hexavalent chromium with magnetically reduced graphene oxide bentonite

  • Cao S
  • Guo J
  • Ma J
  • et al.
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Abstract

Water pollution by hexavalent chromium (Cr(VI)) is widespread and problematic. As a result, more research into economic Cr(VI) removal is needed. In this study, we created and employed an adsorption–reduction mechanism to remove Cr(VI). Magnetically reduced graphene oxide bentonite (MrGO-BT) is acid resistant and can undergo magnetic separation. The hydroxyl group of chitosan (CS) condensed with the functional groups on the surface of bentonite (BT), and the MrGO-BT sandwich has been fabricated and constructed from an Fe 3 O 4 core layer sandwiched by reduced graphene oxide (rGO) and a BT shell, with CS acting as a crosslinker. Cr(VI) elimination by MrGO-BT was exothermic and spontaneous according to thermodynamic analyses. The adsorption kinetics and adsorption isotherms were characterized by the pseudo-second order kinetic theory and the Langmuir model, respectively. Regarding the elimination of Cr(VI), the greatest adsorption ability for Cr(VI) elimination achieved was 91.5 mg g –1 . Fourier-transform infrared spectroscopy and X-ray photoelectron spectroscopy suggested that Cr(VI) was reduced by C–O–H on MrGO-BT to produce Cr(III) and H–C=O, and that Cr(III) chelated with amino groups or exchanged with BT after intercalation. In addition, the introduction of Cu 2+ increased the positive charge of MrGO-BT and amplified the electrostatic interaction between Cr 2 O 7 2− and HCrO 4 – , which is what caused Cr(VI) to be eliminated. Cu 2+ and reduced Cr(III) combined with -NH 2 on the surface of MrGO-BT to form -NH-Cr(III) or -NH-Cu 2+ , and Cr(VI) elimination via chelation and ion exchange was confirmed. MrGO-BT is shown to be an adsorbent with high acid resistance and good magnetic responsiveness and stability.

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Cao, S., Guo, J., Ma, J., Chen, E., Pang, J., Zhang, S., … Wang, S. (2023). Effective removal of hexavalent chromium with magnetically reduced graphene oxide bentonite. Clay Minerals, 58(1), 7–18. https://doi.org/10.1180/clm.2023.4

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