Affiliation:
1. Università degli Studi di Milano
Abstract
Thermal expansion of some members of the synthetic solid solution åkermanite-gehlenite was measured (in the range 25-1200°C) for the very first time, with the aim of clarifying the behaviour of this solid solution both with respect to composition and temperature. The results confirmed the non-ideal behaviour at room temperature (negative excess molar volume), and showed a different non-ideal response at high temperature. In fact, excess molar volume is different during the heating and cooling stages: for Xak<0.5 it becomes, from almost ideal, strongly positive at high temperature, while for Xak>0.5 it is always negative. It can then be inferred that (i) lattice dimensions are very sensitive to cation diffusion activated by temperature, (ii) intra-crystalline partition mechanisms, and their effects on the structural features, vary as a function of composition in the solid solution studied.
Publisher
Trans Tech Publications, Ltd.
Subject
Mechanical Engineering,Mechanics of Materials,Condensed Matter Physics,General Materials Science
Reference12 articles.
1. B. E. Warren: Kristallogr. Vol. 74 (1930), p.131.
2. T. V. Charlu, R. C. Newton and O. J. Kleppa: Geochim. Cosmochim. Acta. Vol. 45 (1981), p.1609.
3. B. C. Hemingway, H. T. Evans Jr., G. L Nord, H. T. Haselton Jr., R. A. Robie and J. J. McGee: Canadian Mineralogist. Vol. 24 (1986), p.425.
4. M. Kimata and N. Ii: N. Jahrb. Mineral Mh. Vol. 1 (1981), p.1.
5. M. Kimata and N. Ii: N. Jahrb. Mineral Abh. Vol. 144 (1982), p.254.
Cited by
3 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献