Studies in the system CaO-Al 2 O 3 -SiO 2 -H 2 O--[Part] 2, The system CaSiO 3 -H 2 O

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ID: 295109
1960
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Abstract
Phase equilibria in the system CaSiO 3 -H 2 O were studied, and a p-T curve constructed for the upper stability of xonotlite. The maximum stability of xonotlite is about 420 degrees C. at 20,000 p.s.i. for CaSiO 3 .1/5H 2 O, but is raised to about 500 degrees C. by the substitution of 7.5 weight % SrSiO 3 . At higher contents of SrSiO 3 a new anhydrous phase appears, herein called mu -(Ca,Sr)SiO 3 . Well-crystallized 11Aa tobermorite, having the composition 4CaO.5SiO 2 .5H (sub 29O is stable up to about 285 degrees C. 15-30,000 p.s.i., where it decomposes to xonotlite (+ truscottite + H 2 O). The crystallization of scawtite and its relation to the tobermorite decomposition is discussed. New data on the phases are presented and the petrological and crystallo-chemical significance discussed.
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Authors Dean A. Buckner, Debraj Roy, R. Roy
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Journal american journal of science
Year 1960
DOI
10.2475/ajs.258.2.132
URL
https://doi.org/10.2475/ajs.258.2.132
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