Polymorphism and subsolidus equilibria in the system GeO 2 -TiO 2

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ID: 301190
1961
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Abstract
Evidence is presented for a metastable alpha- to beta-quartz transition in germania. The temperature of the stable inversion of the rutile to quartz form of GeO ~2~ is lowered by TiO ~2~ in solid solution. The maximum solid solubility of TiO ~2~ in the rutile form of GeO ~2~ is about 25 mole % at 1023 degrees C. + or - 5 degrees C. The solubility in the quartz form is about 30 mole % at 1050 degrees C. The solid solubility of GeO ~2~ in TiO ~2~ is about 40 mole % at 1050 degrees C.
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openalex_W2317109414 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors J. F. Sarver
Journal american journal of science
Year 1961
DOI
10.2475/ajs.259.9.709
URL
https://ajs.scholasticahq.com/article/58889.pdf
Keywords Keywords not found

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