Reference Type | Journal (article/letter/editorial) |
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Title | Phase relationships in the join Ca(OH)2–CaCO3–Ca3(PO4)2–H2O at 1000 bars |
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Journal | Mineralogical Magazine |
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Authors | Biggar, G. M. | Author |
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Year | 1969 (March) | Volume | 37 |
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Issue | 285 |
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Publisher | Mineralogical Society |
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Download URL | https://rruff.info/doclib/MinMag/Volume_37/37-285-75.pdf+ |
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DOI | doi:10.1180/minmag.1969.037.285.08Search in ResearchGate |
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| Generate Citation Formats |
Mindat Ref. ID | 6235 | Long-form Identifier | mindat:1:5:6235:4 |
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|
GUID | 0 |
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Full Reference | Biggar, G. M. (1969) Phase relationships in the join Ca(OH)2–CaCO3–Ca3(PO4)2–H2O at 1000 bars. Mineralogical Magazine, 37 (285) 75-82 doi:10.1180/minmag.1969.037.285.08 |
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Plain Text | Biggar, G. M. (1969) Phase relationships in the join Ca(OH)2–CaCO3–Ca3(PO4)2–H2O at 1000 bars. Mineralogical Magazine, 37 (285) 75-82 doi:10.1180/minmag.1969.037.285.08 |
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In | (1969, March) Mineralogical Magazine Vol. 37 (285) Mineralogical Society |
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Abstract/Notes | SummaryPhase equilibria involving calcite, apatite, portlandite, liquid, and vapour were determined at 1000 bars. Calcite, apatite, and portlandite melt at 654 °C to form a liquid of composition (wt %), Ca(OH)2 53 %, CaCO3 46 %, Ca3(PO4)2 1 %. With water present melting occurs at 635 °C to form a similar liquid with a low water content. The X-ray diffraction patterns of the equilibrium apatites were not significantly different from synthetic hydroxyapatite. |
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