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THE INFLUENCE OF CHEMICAL COMPOSITIONS ON THE PHYSICAL PROPERTIES OF SODA‐LIME GLASSES 1
Author(s) -
Gill J. W.,
Rueckel W. C.
Publication year - 1931
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/j.1151-2916.1931.tb17083.x
Subject(s) - lime , softening point , softening , mineralogy , refractive index , chemical composition , materials science , soda lime glass , soda lime , analytical chemistry (journal) , chemistry , composite material , metallurgy , chromatography , organic chemistry , optoelectronics
Nineteen soda‐lime glasses covering the commercial field were prepared, melted, and fined for 2 hours. The chemical composition of the raw materials was determined by usual analytical methods; the refractive index was determined by an Abbé refractometer; density, by the normal suspension method; and softening point, by the Littleton method with the furnace as specified in Jour. Amer. Ceram. Soc. , 10 [4], 259‐63 (1927). The data indicate the following points: (1) When the silica was kept constant by increasing the dolomitic lime at the expense of soda an increase in softening point of 11 to 12°C per 1% increase was obtained. Likewise the density increases 0.004 and the refractive index 0.0015 per 1% increase of lime. (2) When the soda was kept constant the softening point was practically constant. The density decreases 0.011 and the refractive index 0.0030 per 1% increase of silica at the expense of lime. (3) When the lime was kept constant the increase in softening point per 1% increase in silica varied as follows : 5% lime 21°C, 8% lime 17°C, 10% lime 15°C, and 12% lime 12°C. The density decreased 0.008 and the refractive index 0.0015 per 1% increase in silica at the expense of soda. (4) A thermo‐chemical relation of the softening points and the chemical compositions (calculated) closely paralleling the “liquidus” surfaces of Feild and Roysters' system: CaO‐Na 2 O‐SiO 2 .