The general theory of such equilibria will be studied later under the head of the phase rule.
When the equilibria become more complex difficulties of interpretation of the experimental results often arise.
From Reicher's determinations, the exact transition point is 95.6°; it rises with increasing pressure about 0.05° for one atmosphere; the density of the rhombic form is greater than that of the monoclinic. The equilibria of these modifications may be readily represented on a pressure-temperature diagram.
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