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Micaceous vermiculite, glauconite, and mixed-layered kaolinite-montmorillonite examination by ultramicrotomy and high resolution electron microscopy

Journal Article · · Soil Sci. Soc. Am., Proc.; (United States)
Electron optical fringes of the layer structures of micaceous vermiculite (Colorado), glauconite (Wisconsin), and mixed-layered kaolinite-montmorillonite (Mexico) were observed after separation of clay fractions, saturation with various cations, embedment in Epoxy, thin sectioning normal to the (001) planes by a diamond-knife ultramicrotome, and high resolution, diffraction contrast electron microscopy. In the thin section of Cs-saturated micaceous vermiculite, the electron optical fringes at 10 A may represent the basal crystallographic spacing of unweathered K mica; fringes at 11 A and 5.5 A may represent the (001) and (002) crystallographic basal orders of Cs vermiculite with the interlayers nearly closed; and fringes at 12.5 A may represent incompletely collapsed vermiculite (possibly lower layer charge and/or hydrous metal oxide-interlayered). The K-saturated glauconite particles occur as thin crystal packets consisting of 5 to 20 layers of mica + vermiculite + montmorillonite with 10 A spacing; occasional interstratified 14 A spacings are believed to represent the Raman-Jackson chlorite. A Mg-saturated, mixed-layer kaolinite-montmorillonite from Mexico showed interleaving among the electron optical (001) fringes of kaolinite (7 A), montmorillonite (12 to 14 A), micaceous vermiculite (10 A), and regularly interstratified kaolinite-montmorillonite (19 A).
OSTI ID:
7340734
Journal Information:
Soil Sci. Soc. Am., Proc.; (United States), Journal Name: Soil Sci. Soc. Am., Proc.; (United States) Vol. 39:4; ISSN SSSAA
Country of Publication:
United States
Language:
English