4.7 Article

Study on the sulfidation behavior of smithsonite

Journal

APPLIED SURFACE SCIENCE
Volume 329, Issue -, Pages 315-320

Publisher

ELSEVIER SCIENCE BV
DOI: 10.1016/j.apsusc.2014.12.167

Keywords

Smithsonite; Sulfidation behavior; Surface; Adsorption

Funding

  1. National Natural Science Foundation of China [51204078, KKGE201121001]
  2. Natural Science Foundation of Yunnan Province Education Department [2012J085, 2013FD058]
  3. Natural Science Foundation of Science and Technology Department [2012J085, 2013FD058]
  4. Analysis and Testing Foundation of Kunming University of Science and Technology [20130539]

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Zinc extraction from low-grade mineral resources of oxidized zinc has recently become a focus of study. Sulfidation is an important process in oxidized ore flotation. In this study, the influence of sulfur ion adsorption on smithsonite surface was investigated with the use of zeta potential, inductively coupled plasma (ICP), scanning electron microscope (SEM), and X-ray photoelectron spectroscopic studies. Zeta potential measurements of sodium sulfide showed that sulfur ions were adsorbed onto the surface of pure smithsonite, as evidenced by the increased negative charge and the decrease in the pH(IEP) of smithsonite from 7.7 to 6 after sodium sulfide treatment. The ICP test revealed the gradual reduction in sulfur ion adsorption onto the surface of smithsonite in pulp sulfur. After 30 min of absorption, C-S in the solution declined from 1000 10(-6) mol/L to 1.4 10(-6) mol/L. SEM results showed that the mineral surface was partially changed to ZnS film after sodium sulfide treatment, whereas EDS analysis results showed that 2% S is contained on the smithsonite surface. X-ray photoelectron spectroscopy results indicated the presence of a characteristic signal peak of sulfur ions after sulfidation. Sulfur concentration increased to 11.89%, whereas oxygen concentration decreased from 42.31% to 13.74%. Sulfur ions were not only present during chemical adsorption, but were also incorporated into the crystal lattices of minerals by the exchange reaction between S2- and CO32- ions. (C) 2014 Elsevier B.V. All rights reserved.

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