Isoionic point and minimum solubility of carbonate minerals Article

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Overview

abstract

• Mineral/aqueous solution equilibria on magnesite suspensions open to the atmosphere show that the pH of minimum solubility of carbonate minerals is not equivalent to the isoionic point of the mineral suspension. For magnesite suspensions, the isoionic point occurs at pH 8.4, whereas the minimum solubility of the mineral occurs at pH values higher than 10.4. © 1988.

authors

• López Valdivieso Alejandro

publication date

• 1988-01-01

published in

• Minerals Engineering  Journal

Research

keywords

• isoionic point; Magnesite; minimum solubility HYDROGEN ION CONCENTRATION; MAGNESITE - Solubility; CARBONATE MINERALS; HYDROGEN ION CONCENTRATION EFFECTS; ISOIONIC POINT; ORE TREATMENT

Identity

Digital Object Identifier (DOI)

• 10.1016/0892-6875(88)90070-2

Additional Document Info

start page

• 85

end page

• 87

volume

• 1

issue

• 1