XPS CHARACTERIZATION OF CHALCOPYRITE, TETRAHEDRITE, AND TENNANTITE SURFACE PRODUCTS AFTER DIFFERENT CONDITIONING .1. AMYL XANTHATE SOLUTIONAT PH 10

Citation
Ja. Mielczarski et al., XPS CHARACTERIZATION OF CHALCOPYRITE, TETRAHEDRITE, AND TENNANTITE SURFACE PRODUCTS AFTER DIFFERENT CONDITIONING .1. AMYL XANTHATE SOLUTIONAT PH 10, Langmuir, 12(10), 1996, pp. 2531-2543
Citations number
22
Categorie Soggetti
Chemistry Physical
Journal title
ISSN journal
07437463
Volume
12
Issue
10
Year of publication
1996
Pages
2531 - 2543
Database
ISI
SICI code
0743-7463(1996)12:10<2531:XCOCTA>2.0.ZU;2-9
Abstract
Characterization of the surface products formed by the interaction of amyl xanthate solution at pH 10 with mineral samples of chalcopyrite ( CuFeS2), tetrahedrite (Cu12Sb4S13), and tennantite (CU12As4S13) was ca rried out by X-ray photoelectron spectroscopy (XPS). The experimental data collected directly after solution treatment and after successive sputterings have led us to determine the in-depth distribution of the different types of surface products formed by the diffusion of atoms f rom the bulk to the interface region and their interaction with aerate d aqueous xanthate solution. The xanthate adsorption takes place by an electrochemical mechanism which involves the formation of cuprous xan thate (hydrophobic species) and metal hydroxides (hydrophilic species) . In general, the following in-depth surface composition was found for the investigated mineral samples in contact with the xanthate solutio n: (i) the outermost layer contains the cuprous xanthate complex, whic h causes hydrophobic properties, and a small amount of metal hydroxide species (depending on the mineral sample), and (ii) below this hydrop hobic layer are gradual changes leading to a structure with a composit ion very similar to the one expected for the bulk mineral sample. All the mineral samples show a copper enrichment in the interface region f ormed as a result of diffusion of copper atoms to the interface provok ed by the adsorbed xanthate molecules. Sulfur-enriched structures, whi ch were observed after treatment in solution without xanthate, are not observed in the presence of xanthate solution. The adsorbed amount of xanthate as well as the structure of the outermost layer, which is re sponsible for the mineral sample's hydrophobicity, varied dramatically . Tetrahedrite shows the fastest kinetics of xanthate adsorption with the formation of multilayer coverage of surface cuprous xanthate. On c halcopyrite and tennantite the adsorbed amount of xanthate is much low er, close to a monolayer coverage. The differences in the surface comp osition of these three minerals are governed mainly by a different mob ility of copper atoms in their crystalline structures in the presence of xanthate in solution. Other metal atoms present in the mineral samp les, i.e. antimony, arsenic, iron, zinc, and silver, do not take a sig nificant part in the formation of the outermost adsorption layer.