Minerals Beneficiation - Streaming Potential Studies. Quartz Flotation with Cationic Collectors

The American Institute of Mining, Metallurgical, and Petroleum Engineers
A. M. Gaudin D. W. Fuerstenau
Organization:
The American Institute of Mining, Metallurgical, and Petroleum Engineers
Pages:
5
File Size:
389 KB
Publication Date:
Jan 1, 1956

Abstract

By streaming potential techniques, the zeta potential of quartz has been measured as a function of the concentration of dodecylammonium salts at different pH values. These experiments indicate that adsorption of dodecylammonium ions takes place as individual aminium ions until a certain critical concentration is reached in the double layer, at which point the adsorbed collector ions begin to associate into patches of ions, called hemi-micelles. Because of its effect on the surface potential of quartz, pH controls the adsorption of dodecylammonium ions. The value of cooperating agents and nonionized constituents of flotation systems is discussed. A PREVIOUS investigation' of the role of pH in the flotation of quartz with anionic collectors is here extended to an inquiry of how the cationic collector, dodecylammonium acetate, is adsorbed at the quartz-solution interface. The equilibrium amount of this collector adsorbed by quartz has already been measured as a function of concentration and pH.2,3 The weight of prior evidence has suggested that two mechanisms are involved in the adsorption of this collector by quartz, but with existing adsorption measurements alone it is not possible to determine what the mechanisms are. Gaudin and Bloecher2 postulated that a polymolec-ular adsorption coating begins to form before the first monolayer has been completed. Gaudin and Morrow4 indicated that a similar situation might exist in the film of dodecylammonium ions on hematite. A study of electrokinetic potentials at the quartz-solution interface provides some detail toward a fuller understanding of the adsorption mechanism. Experimental Results The zeta potential at the quartz-solution interface was calculated from streaming potential data measured with the apparatus described in detail in a thesis by Fuerstenau5 and briefly in a paper by Gaudin and Fuerstenau.1 The quartz used in these experiments was a 48/65-mesh fraction prepared in the manner described previously.' Zeta potential of quartz was obtained for various amounts of the amine salt at pH 4, 7, 10, 11. In
Citation

APA: A. M. Gaudin D. W. Fuerstenau  (1956)  Minerals Beneficiation - Streaming Potential Studies. Quartz Flotation with Cationic Collectors

MLA: A. M. Gaudin D. W. Fuerstenau Minerals Beneficiation - Streaming Potential Studies. Quartz Flotation with Cationic Collectors. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1956.

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