1960•American Journal of ScienceRequires access

Studies in the system Mn-O--The Mn 2 O 3 -Mn 3 O 4 and Mn 3 O 4 -MnO equilibria

Walter C. Hahn, Arnulf Muan

Open publisher page 115 citations

Abstract

As a first step in an investigation of phase relations in the system Mn-O, the equilibria 6Mn 2 O 3 = 4Mn 3 O 4 + O 2 and 2Mn 3 O 4 = 6MnO + O 2 have been studied in the temperature intervals 845 to 1029 degrees C. and 1248 to 1562 degrees C., respectively, and at O 2 partial pressures ranging from 0.21 to 1 atm. and from 10 (super -3.66) to 0.21 atm. respectively. The conditions for coexistence of 2 crystalline phases in stable univariant equilibria are expressed as follows: Mn 2 O 3 , Mn 3 O 4 : log p (sub O 2 = 8.05 - 10100 . 1/T; Mn 3 O 4 , MnO : log p (sub O 2 = 13.31 - 26000 . 1/T. Exploratory runs in the solidus temperature region for the composition range between MnO and Mn 3 O 4 indicate the presence of a eutectic at approximately 1540 degrees C. An explanation is offered for the poor agreement among previously published data on these equilibria.

About this research paper

What this paper is about

As a first step in an investigation of phase relations in the system Mn-O, the equilibria 6Mn 2 O 3 = 4Mn 3 O 4 + O 2 and 2Mn 3 O 4 = 6MnO + O 2 have been studied in the temperature intervals 845 to 1029 degrees C. and 1248 to 1562 degrees C., respectively, and at O 2 partial pressures ranging from 0.21 to 1 atm. and from 10 (super -3.66) to 0.21 atm. respectively. The conditions for coexistence of 2 crystalline phases in stable univariant equilibria are expressed as follows: Mn 2 O 3 , Mn 3 O 4 : log p (sub O 2 = 8.05 - 10100 . 1/T; Mn 3 O 4 , MnO : log p (sub O 2 = 13.31 - 26000 . 1/T. Exploratory runs in the solidus temperature region for the composition range between MnO and Mn 3 O 4 indicate the presence of a eutectic at approximately 1540 degrees C. An explanation is offered for the poor agreement among previously published data on these equilibria.

Why it matters

OpenAlex reports 115 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

As a first step in an investigation of phase relations in the system Mn-O, the equilibria 6Mn 2 O 3 = 4Mn 3 O 4 + O 2 and 2Mn 3 O 4 = 6MnO + O 2 have been studied in the temperature intervals 845 to 1029 degrees C. and 1248 to 1562 degrees C., respectively, and at O 2 partial pressures ranging from 0.21 to 1 atm. and from 10 (super -3.66) to 0.21 atm. respectively. The conditions for coexistence of 2 crystalline phases in stable univariant equilibria are expressed as follows: Mn 2 O 3 , Mn 3 O 4 : log p (sub O 2 = 8.05 - 10100 . 1/T; Mn 3 O 4 , MnO : log p (sub O 2 = 13.31 - 26000 . 1/T. Exploratory runs in the solidus temperature region for the composition range between MnO and Mn 3 O 4 indicate the presence of a eutectic at approximately 1540 degrees C. An explanation is offered for the poor agreement among previously published data on these equilibria.

Key concepts: Solidus, Manganese, Eutectic system, Crystallography, Analytical Chemistry (journal), Chemistry, Materials science, Mineralogy

Related papers

Back to paper searchBrowse research topicsOriginal source
Studies in the system Mn-O--The Mn 2 O 3 -Mn 3 O 4 and Mn 3 O 4 -MnO equilibria — Research Paper | ScholarLens