HYDROTHERMAL SYNTHESIS OF AMMONIUM ILLITE

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dc.contributor.author Šucha V.
dc.contributor.author Elsass F.
dc.contributor.author Eberl D.D.
dc.contributor.author Kuchta L..
dc.contributor.author Madejová J.
dc.contributor.author Komadel P.
dc.contributor.author Gates W.P.
dc.date.accessioned 2021-01-06T07:51:19Z
dc.date.available 2021-01-06T07:51:19Z
dc.date.issued 1998
dc.identifier https://elibrary.ru/item.asp?id=31871605
dc.identifier.citation American Mineralogist, 1998, , 1, 58-67
dc.identifier.issn 0003-004X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/22300
dc.description.abstract Synthetic gel and glass of illitic composition, natural kaolinite, and mixed-layer illitesmectite were used as starting materials for hydrothermal synthesis of ammonium illite. Ammonium illite was prepared from synthetic gel by hydrothermal treatment at 300 degrees C. The onset of crystallization began within 3 h, and well-crystallized ammonium illite appeared at 24 h. Increasing reaction time (up to four weeks) led to many illite layers per crystal. In the presence of equivalent proportions of potassium and ammonium, the gel was transformed to illite with equimolar contents of K and NH 4 . In contrast, synthesis using glass under the same conditions resulted in a mixture of mixed-layer ammonium illite-smectite with large expandability and discrete illite. Hydrothermal treatments of the fine fractions of natural kaolinite and illite-smectite produced ammonium illite from kaolinite but the illite-smectite remained unchanged.
dc.title HYDROTHERMAL SYNTHESIS OF AMMONIUM ILLITE
dc.type Статья


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