Abstract
The mechanisms of layer structure formation in the two phase region of peritectic systems are discussed. Under diffusive growth conditions, a banded structure is predicted within a narrow composition range in the hypoperitectic composition. Experimental studies show the formation of an oscillatory structure in the hyperperitectic region. It is shown that this structure is induced by convection in the melt, and it is a novel structure in which a large single tree-like structure of primary phase is surrounded by the peritectic phase. Basic ideas of convection that lead to this tree-like morphology are described.
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Acknowledgement
This research was supported in part by the NASA Microgravity Science and Applications Division under Grant NAG8-1254. This work was carried out in part at the Ames Laboratory, which is operated for the U. S. Department of Energy by Iowa State University, under contract no. W-7405-Eng-82, supported by the director of Energy Research, Office of Basis Energy Sciences. Appreciation is expressed to J. S. Park for providing us with experimental results prior to their publication.
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Mazumder, P., Trivedi, R. & Karma, A. Mechanisms of Layer Structure Formation in Peritectic Alloys. MRS Online Proceedings Library 481, 39–44 (1997). https://doi.org/10.1557/PROC-481-39
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DOI: https://doi.org/10.1557/PROC-481-39