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Experimental investigation of the reaction forsterite + H2O ⇌ serpentine + brucite

✍ Scribed by W. Johannes


Publisher
Springer
Year
1968
Tongue
English
Weight
429 KB
Volume
19
Category
Article
ISSN
0010-7999

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✦ Synopsis


A new determination of the equilibrium reaction: 2 Mg2[SiOt] @ 3 H~O ~ 1 Mgs[(OH)41 Si~05] ~-1 Mg(OH)~ forsterite serpentine brucite yielded equilibrium temperatures which lie (at identical H20-pressures ) about 60~ lower than all previously published data ( BowEN and TV~TLE, 1949;YODER, 1952; t~TAgA~A et al., 1966; KITAgARA and KENNEDY, 1967). It has been shown that the above authors have determined not the stable equilibrium curve but instead a metastable "synthesis boundary"t.

The actual (stable) equilibrium curve is located at 0,5 kb and 350 ~ C 2,0 kb and 380 ~ C 3,5 kb and 400 ~ C 5,0 kb and 420 ~ C 6,5 kb and 430 ~ C.


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