The recovery of magnesium oxide and hydrogen chloride from magnesium chloride brines and molten salt hydrates
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Authors
de Bakker, Jan
Date
2011-03-11T21:38:26Z
Type
thesis
Language
eng
Keyword
Extractive metallurgy , Nickel , Magnesium chloride , Molten salt hydrates , Brines
Alternative Title
Abstract
Hydrochloric acid leaching of saprolite nickel ores has been proposed as an effective means of recovering nickel and cobalt. However, the leach produces a concentrated brine of magnesium chloride which must be hydrolyzed to recover the HCl lixiviant. The processing of carnallite similarly produces a concentrated MgCl2 brine; converting this brine into HCl and MgO provides an attractive way of adding value while effectively disposing of this waste product.
Direct pyrohydrolysis of magnesium chloride brines by the reaction,
MgCl2,a + H2Oa MgOs + 2HClg
is energy-intensive as large volumes of water must be evaporated. The energy cost is high, and the HCl stream produced is limited to approximately 20 wt% HCl. This thesis explores alternative methods of obtaining HCl from aqueous magnesium chloride solutions. Two methods are considered: the hydrolysis, under autogenous pressure, of concentrated MgCl2 molten salt hydrates; and the precipitation of magnesium hydroxychloride compounds such as 2MgO·MgCl2·6H2O and 3MgO·MgCl2·11H2O, which are subsequently decomposed at high temperature.
Considerable experimental difficulties were encountered in studying pressure hydrolysis of molten salt hydrates, despite extensive equipment modifications. Ultimately, the work moved on to precipitation and decomposition of hydroxychlorides. This was found to bear promise, and conceptual flowsheets based on these reactions are presented. A phase stability diagram giving the areas of predominance of the different hydroxychloride phases is presented, and fundamental thermochemical data are derived. The results of a kinetic study on magnesium hydroxychloride thermal decomposition are also presented.
Description
Thesis (Ph.D, Mining Engineering) -- Queen's University, 2011-03-11 10:14:53.455
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