Bubble attachment time and FTIR analysis of water structure in the flotation of sylvite, bischofite and carnallite |
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Authors: | Qinbo CaoXuming Wang Jan D. MillerFangqin Cheng Yong Jiao |
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Affiliation: | a Research Center for Environmental Science and Engineering, Shanxi University, No. 92, Wucheng Road, Taiyuan, Shanxi 030006, China b Department of Metallurgical Engineering, College of Mines and Earth Sciences, University of Utah, 135S 1460E 412 WBB, Salt Lake City, UT 84112, USA c Department of Chemical Engineering, Qinhai University, No. 251, Ning Road, Xining, Qinhai 810016, China |
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Abstract: | Water structure is the most important parameter that influences the flotation of soluble salts. In this paper bubble attachment time measurements and FTIR analyses were performed to investigate the effect of water structure on the flotation behavior of sylvite (KCl), bischofite (MgCl2·6H2O) and carnallite (KMgCl3·6H2O). The results from bubble attachment time measurements suggest that collector adsorption at the surface of KCl induces flotation with either the cationic collector, ODA, or anionic collector, SDS. In contrast bubble attachment did not occur for bischofite (MgCl2·6H2O) or carnallite (KMgCl3·6H2O). Results show that the surface charge is not a determining factor in the flotation of soluble salts.Further, the interaction between water molecules and the three chloride salts dissolved in aqueous solution were studied by measuring the shift in the hydrogen-bonding of water molecules. The results indicate that KCl is a structure breaker salt, while MgCl2·6H2O and KMgCl3·6H2O are structure maker salts.Viscosities for the brines of these three salts were determined. The results give additional evidence of differences in water structure and are in good agreement with the FTIR and bubble attachment results. The findings provide further evidence that water structure plays an important role in the flotation of soluble salts. |
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Keywords: | Soluble salts Water structure Bubble attachment time Sylvite Bischofite Carnallite |
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