Phase equilibria and thermodynamics of the system Dy-Mg-Cl at 1073 K
Creators
- 1. Tohoku Univ., Sendai (Japan). Inst. for Adv. Mater. Process.
Description
The phase relations in the system Dy-Mg-Cl at 1073 K have been established by isothermal equilibration and chemical analysis of quenched samples. Liquid Mg-rich alloy was found to be in equilibrium with molten DyCl2. Therefore, DyCl2 can be synthesized by reduction of MgCl2 with excess of metallic Dy at 1073 K. The Gibbs energy of formation of DyCl2 at 1073 K was evaluated by two different methods. From voltammetric determination of decomposition voltage, the upper limit for the standard Gibbs energy of formation of DyCl2 was estimated to be -505(±20) kJ mol-1. A value of -543(±10) kJ mol-1 was deduced from phase relations using Gibbs-Duhem integration. The value for the standard Gibbs energy of DyCl2 indicates that the Dy2+ ion has a potential capability for reducing TiCl4 to metal titanium. At the same time, Mg is a reductant for Dy3+ produced during the reduction of TiCl4. Thus, it is thermodynamically confirmed that reduction of TiCl4 by magnesium using a reaction mediator in the salt phase is feasible. (orig.)
Additional details
Publishing Information
- Journal Title
- Journal of Alloys and Compounds
- Journal Volume
- 284
- Journal Issue
- 1-2
- Journal Page Range
- p. 282-288
- ISSN
- 0925-8388
- CODEN
- JALCEU
INIS
- Country of Publication
- Netherlands
- Country of Input or Organization
- Switzerland
- INIS RN
- 30018922
- Subject category
- S36: MATERIALS SCIENCE;
- Descriptors DEI
- DECOMPOSITION; DYSPROSIUM ALLOYS; EQUILIBRIUM; FORMATION HEAT; MAGNESIUM ALLOYS; PHASE DIAGRAMS; VOLTAMETRY
- Descriptors DEC
- ALLOYS; CHEMICAL REACTIONS; DIAGRAMS; ENTHALPY; INFORMATION; PHYSICAL PROPERTIES; RARE EARTH ALLOYS; REACTION HEAT; THERMODYNAMIC PROPERTIES
Optional Information
- Notes
- 20 refs.