The comparison between amine thioacetate and amyl xanthate collector performances for pyrite flotation and its application to tailings desulphurization
Introduction
Throughout the world, mining operations extract both base and precious metals from sulphide ores. The mining process generates substantial quantities of tailings containing various amounts of sulphides, with pyrite being the most common component. Sulphide minerals oxidize in the presence of water and oxygen (Lowson, 1982; Evangelou, 1995). The presence of Thiobacilli bacteria can accelerate sulphide oxidation under certain geochemical conditions. It result from this reactions acid mine drainage pollution (AMD). Although numerous, the methods used to prevent AMD are usually quite expensive. A relatively new alternative has been recently proposed to reduce mine site reclamation costs. This alternative method consists of separating the sulphide fraction from the mine waste prior to final storage. The obtained concentrate can be later managed more easily due to its reduced volume (Bussière et al., 1995; Benzaazoua et al., 1998a).
There is extensive literature on sulphide flotation, especially on pyrite. Many authors have worked on sulphide concentration by non-selective flotation for mineral processing purposes (preparation of concentrates intended for gold and/or silver hydrometallurgy) and some for waste management strategy. From the available literature, we can mention the work of Benzaazoua et al. (2000) who demonstrated the feasibility of environmental desulphurization on four different Canadian tailings. McLaughlin and Stuparyk (1994) evaluated the production of low sulphur tailings at INCO’s Clarabelle concentrator. Balderama (1995) worked on different tailings impoundments in the United States to control acid mine drainage. Leppinen et al. (1997) focused on recovering residual sulphide minerals from the tailings at the Pyhasalami Cu–Zn mine in Finland. Others authors who have studied this topic are Luszczkiewicz and Sztaba (1995), Humber (1995), Bussière et al. (1995) and Benzaazoua et al. (1998b).
For the non-selective flotation of sulphide mineral, the most commonly used and most investigated reagents are the xanthate-based collectors, which are characterized by their ability to collect sulphides in general. They are very selective because of the length of their radical chains (Crozier, 1992). Amyl xanthate is generally used for the non-selective flotation of sulphides (including pyrite) because of its collecting ability. However, in some cases, pyrite flotation may be inhibited. The main factors for the phenomenon of pyrite inhibition are:
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The surface state of the grains can be affected by natural oxidation or oxidation by dissolved cyanides as demonstrated by Wet et al. (1997).
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The pH of the pulp: especially when the xanthate concentration is low, a pH of above 10 causes depression of the mineral (Duc, 1992). At higher xanthate concentration, this effect disappears (Kongolo, 1991; Benzaazoua and Kongolo, 2003).
Other collectors have also been used successfully for non-selective sulphide flotation. This has been demonstrated by the works of Bradshaw and O’Connor (1994) on thiocarbamates, O’Connor and Dunne (1991) on mercaptobenzothiazoles and Hodgkinson et al. (1994) on amines.
The paper presents the results of a work on the optimization of pyrite flotation conditions. This process is intended to be used in an environmental tailings desulphurization process. Two main collectors investigated were, the well-known potassium amyl xanthate (KAX) and the cocoalkyl amine thioacetate (Armac). Two techniques were used to find qualitative and quantitative evaluation data for the two collectors in this study. The method for determination of KAX and Armac concentration in solution was developed using an UV–Vis spectrophotometer. The superficial phases within the pyrite grain surfaces were analyzed by diffuse reflectance infrared spectroscopy. The pH conditions (natural pH and alkaline pH in the presence of soda ash and hydrated lime) of collector adsorption were the primary subjects of study. Due to the need for simplification, pure pyrite doted with like-tailings particle size distribution was used for surface characterization. Finally, the potential application to mine tailings is shown in presence of cyanides for both collectors. It was necessary to destroy the cyanides for tailings desulphurization with KAX by washing and sulphide activation.
Section snippets
Spectroscopic methods
In this study, different spectroscopic methods were used for qualitative and quantitative characterization of the Armac collectors interactions compared to those of KAX for pyrite surfaces.
Adsorption isotherms of KAX and Armac on pyrite in closed reactors
The isotherms of adsorption were built for the two collectors to compare their affinities for pyrite at both natural pH and alkaline pH levels. Moreover, the influence of the pH regulator type was studied when using both sodium hydroxide (NaOH) and the more commonly used lime (Ca(OH)2) in mineral processing.
Practical application regarding the desulphurization process
In order to go head in the understanding of the KAX and Armac interactions with pyrite and to verify the findings obtained on pure pyrite samples, a complementary short study was done with pyrite bearing tailings. The pulp physico-chemistry is quite complicated when dealing with previously processed pulp. The most commonly used collector for sulphide flotation from tailings is amyl xanthate (KAX). However, when the tailings contain cyanides (Case of the gold treatment residues), the authors
Conclusions
The construction of the adsorption isotherms corresponding to the different conditioning modes made it possible to highlight that Armac C is adsorbed in higher amounts compared to the potassium amyl xanthate on the pyrite surfaces at a pH level of 11. Using diffuse reflectance infrared spectroscopy, it has been shown that valence vibration of the alkyl chains (3000 and 2800 cm−1) are a good quantitative indicator of the presence of collector on the surface of the pyrite. Infrared measurements
Acknowledgements
This work was financed through the “Fonds Institutionnel de Recherche” of the University of Quebec in Abitibi Temiscamingue and includes a contribution from the LEM laboratory of the Geology School of Nancy. We would like to thank particularly Edith Bouquet for the UV spectrometry measurements and Nil Gaudet for the Denver tests.
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