Issue 1149, 1971

An improved oxalate method for the determination of active oxygen in manganese dioxide

Abstract

Of the various methods available for the determination of active oxygen in managanese dioxide, the oxalate method is preferred because of its simplicity and reproducibility. However, it tends to give higher results than the iron(II) and Bunsen methods, the discrepancies being greater with synthetic materials than with ores. In confirmation of the work of other authors it has been shown that there is a Mn2+ catalysed loss of oxalate that causes the high results. It is concluded that the loss is caused by oxidation by oxygen dissolved in the reagent solutions. With the addition of Cu2+ or Fe3+, the oxalate method gives results that are comparable with those of the iron(II) method. The stabilisation of oxalate with Fe3+ has been used to speed up the time taken to dissolve samples by boiling them under reflux.

Article information

Article type
Paper

Analyst, 1971,96, 865-869

An improved oxalate method for the determination of active oxygen in manganese dioxide

D. S. Freeman and W. G. Chapman, Analyst, 1971, 96, 865 DOI: 10.1039/AN9719600865

To request permission to reproduce material from this article, please go to the Copyright Clearance Center request page.

If you are an author contributing to an RSC publication, you do not need to request permission provided correct acknowledgement is given.

If you are the author of this article, you do not need to request permission to reproduce figures and diagrams provided correct acknowledgement is given. If you want to reproduce the whole article in a third-party publication (excluding your thesis/dissertation for which permission is not required) please go to the Copyright Clearance Center request page.

Read more about how to correctly acknowledge RSC content.

Social activity

Spotlight

Advertisements