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Interfacial Reactions Between Anorthite (CaAl 2 Si 2 O 8 ) and Al 7075 Alloy at 850°C and 1150°C
Author(s) -
Adabifiroozjaei Esmaeil,
Koshy Pramod,
Rastkerdar Ebad,
Sorrell Charles C.
Publication year - 2016
Publication title -
journal of the american ceramic society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.9
H-Index - 196
eISSN - 1551-2916
pISSN - 0002-7820
DOI - 10.1111/jace.14091
Subject(s) - anorthite , spinel , alloy , gehlenite , melilite , materials science , scanning electron microscope , analytical chemistry (journal) , phase (matter) , transmission electron microscopy , mineralogy , energy dispersive x ray spectroscopy , metallurgy , chemistry , composite material , nanotechnology , organic chemistry , chromatography
The present work reports an investigation of the interactions of Al 7075 alloy and anorthite at 850°C (150 h) and 1150°C (24 h). Transmission electron microscopy, electron probe microanalysis, X‐ray diffraction, and scanning electron microscopy coupled with energy‐dispersive spectroscopy were used to identify the mineralogical and microstructural changes at the metal–ceramic interface. At 850°C, the phase formation mechanisms were (a) Si 4+ –Al 3+ interdiffusion between the Al alloy and anorthite to form calcium dialuminate ( CA 2 ) and Ca 2+ –Mg 2+ interdiffusion between the Al alloy and calcium dialuminate to form spinel. At 1150°C, spinel + Al 2 O 3 and calcium hexaluminate ( CA 6 ) + CA 2 were the major and minor phase mixtures, respectively in the corroded area. A thin layer of calcium monoaluminate ( CA ), gehlenite, and Si was present in the immediate vicinity of anorthite. The early stages of corrosion at 1150°C and 850°C were identical. However, due to thickening of the corroded region ( viz ., spinel formation) and enhanced evaporation of Mg at the higher temperature, the interdiffusion path evolves from Si 4+ –Al 3+ + Ca 2+ –Mg 2+ to Si 4+ –Al 3+ + Ca 2+ –Al 3+ , thus establishing the following phase evolution path at the interface: Anorthite → Gehlenite → CA → CA 2 → CA 6 → Al 2 O 3