Issue 1252, 1980

Complexometric determination of calcium and magnesium in calcite and limestone after selective precipitation of magnesium quinolin-8-olate from a homogeneous solution

Abstract

A simple complexometric method has been developed for the determination of magnesium directly and of calcium by difference at pH ∼ 10, using EDTA in a single aliquot of solution. The method is based on the joint titration of calcium and magnesium with EDTA at pH ∼ 10 and the release of EDTA from the magnesium-EDTA complex by selective precipitation of magnesium quinolin-8-olate from a homogeneous solution with potassium quinolin-8-olate and a known excess of calcium ions at 50–60 °C. The EDTA released is a direct measure of magnesium, and is titrated with calcium solution at 10 °C. The interfering ions, such as zinc, cadmium, manganese and iron are masked by potassium cyanide during the joint titration of calcium and magnesium. Precipitation of the dark coloured iron(III) quinolin-8-olate from the iron(III)-cyanide complex has effectively been prevented by reducing the latter to the iron(II)-cyanide complex with ascorbic acid. Aluminium and titanium, unless present in large amounts (more than 5 mg), have no effect on the method. The method has been successfully applied to the determination of calcium and magnesium in calcite and limestone.

Article information

Article type
Paper

Analyst, 1980,105, 720-725

Complexometric determination of calcium and magnesium in calcite and limestone after selective precipitation of magnesium quinolin-8-olate from a homogeneous solution

B. C. Sinha and S. K. Roy, Analyst, 1980, 105, 720 DOI: 10.1039/AN9800500720

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