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Prieto, Manuel, Putnis, Andrew, Arribas, Jose, Fernandez-Diaz, Lurdes (1992) Ontogeny of baryte crystals grown in a porous medium. Mineralogical Magazine, 56 (385) 587-598 doi:10.1180/minmag.1992.056.385.15

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Reference TypeJournal (article/letter/editorial)
TitleOntogeny of baryte crystals grown in a porous medium
JournalMineralogical MagazineISSN0026-461X
AuthorsPrieto, ManuelAuthor
Putnis, AndrewAuthor
Arribas, JoseAuthor
Fernandez-Diaz, LurdesAuthor
Year1992 (December)Volume56
Issue385
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_56/56-385-587.pdf+
DOIdoi:10.1180/minmag.1992.056.385.15Search in ResearchGate
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Mindat Ref. ID1873Long-form Identifiermindat:1:5:1873:3
GUID0
Full ReferencePrieto, Manuel, Putnis, Andrew, Arribas, Jose, Fernandez-Diaz, Lurdes (1992) Ontogeny of baryte crystals grown in a porous medium. Mineralogical Magazine, 56 (385) 587-598 doi:10.1180/minmag.1992.056.385.15
Plain TextPrieto, Manuel, Putnis, Andrew, Arribas, Jose, Fernandez-Diaz, Lurdes (1992) Ontogeny of baryte crystals grown in a porous medium. Mineralogical Magazine, 56 (385) 587-598 doi:10.1180/minmag.1992.056.385.15
In(1992, December) Mineralogical Magazine Vol. 56 (385) Mineralogical Society
Abstract/NotesAbstractThe development of the morphology of baryte crystals grown in a silica gel medium is related to the changes in supersaturation. Nucleation occurs when the supersaturation in the system exceeds a threshold value which depends on the supersaturation rate, i.e. the rate at which the supersaturation is changing at the nucleation site. During growth the supersaturation decreases, although a high level of supersaturation is maintained throughout. These experimental results compare well with the morphological development predicted from theoretical models based on the periodic bond chain theory. The ontogeny of natural harytes corresponds, in considerable detail, to the experimental observations made here and strongly suggests that similarly high supersaturations have prevailed in nature. This correspondence indicates that the technique of crystal growth in a porous silica gel medium provides a good experimental model of studying natural growth processes.


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