Postglacial ecosystem development of a hydrothermal landscape in Yellowstone National Park. [PDF]
Whitlock C +10 more
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Ion exchange selectivity governs phase selection in zeolite synthesis.
Rais A +6 more
europepmc +1 more source
Waste-Derived Zeolite-P (GIS): Synthesis, Polymorphism, Characterization, and Adsorption Applications for Water Purification and Selective Gas Separation. [PDF]
Boudia RA, Bellucci S, Adjdir M.
europepmc +1 more source
A short review of the sustainable utilization of coal gangue in environmental applications. [PDF]
Gao L, Liu Y, Xu K, Bai L, Guo N, Li S.
europepmc +1 more source
CDW-Based Geopolymers: Pro and Cons of Using Unselected Waste. [PDF]
Capasso I +5 more
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What drives porosity in aluminosilicate zeolites?
Vandenabeele D +3 more
europepmc +1 more source
Synthesis and structure of analcime and analcime-zirconia composite derived from coal fly ash cenospheres [PDF]
Abstract Cubic analcime and analcime-zirconia composite with the Si/Al ratio of 2.04 and 2.16, respectively, was synthesized by hydrothermal treatment of coal fly ash cenospheres (Si/Al = 2.7) at 150 °C. The scanning electron microscopy with energy dispersive spectroscopy (SEM-EDS), powder X-ray diffraction (PXRD), X-ray photoelectron spectroscopy ...
Sergey N Vereshchagin +2 more
exaly +4 more sources
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The crystal structure of analcime
Microporous and Mesoporous Materials, 1998Abstract Crystals of analcime were synthesized; the size was about 200 μm. The diffraction data were collected with both cubic system and trigonal system from the same crystal. The crystal parameters were completely cubic and the space group was Ia3d, but the R-factor only dropped to about 10%.
Yoshinobu Yokomori
exaly +2 more sources
An experimental study of the replacement of leucite by analcime
Leucite and analcime have open framework aluminosilicate structures, where ion exchange by cation substitution has been previously used to explain the replacement of one phase by another.
Thomas Stephan +2 more
exaly +1 more source
AbstractSynthetic analcime crystals were grown on hydrothermal conditions using different starting materials. The morphology of the crystals was compared with respect to natural analcime and the observations of HÖLLER as well as the Donnay‐Harker rule and geo‐metrical considerations.
H. Ghobarkar, W. Franke
openaire +1 more source

