The presence of the β1 phase in dental amalgam after 60°C heating has been confirmed by x‐ray diffraction, metallography, microhardness tests, and electron beam analysis. It appeared that the γ1 → β1 transformation began at preferred sites, believed to be possibly areas deficient in Hg, and grew outward from these sites. Even after heating for nearly a year, however, some γ1 still remained in the sample.
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L. B. Johnson (1967) studied this question.
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