1939
DOI: 10.1021/j150395a007
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Studies in Gelation and Film Formation. II. Studies in Clay Films.

Abstract: In a previous publication (5) it was demonstrated that self-supporting, coherent films could be obtained from bentonite gels3 ****by spreading the gels on an appropriate support and drying them in this condition. The films so obtained have become generally known as Alsifilm (aZuminum silicate film). Since they are entirely composed of pure clay, they offer a new and interesting condition of matter for colloidal studies.

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Cited by 15 publications
(7 citation statements)
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“…The first clay paper was shaped from bentonite by Hauser in 1938. [3,4] It was not highly transparent and not prepared with the aim of giving it a high gas-barrier property. Claybased artificial nacre had been studied, [5][6][7][8] but it was not highly transparent.…”
mentioning
confidence: 99%
“…The first clay paper was shaped from bentonite by Hauser in 1938. [3,4] It was not highly transparent and not prepared with the aim of giving it a high gas-barrier property. Claybased artificial nacre had been studied, [5][6][7][8] but it was not highly transparent.…”
mentioning
confidence: 99%
“…Completely self-supporting clay membranes were first described by Hauser and Le Beau. 19 They observed that when sols of such substances as sodium and hydrogen bentonite were converted to gels and then completely desiccated, long, interlacing filaments resulted which were tied together by tridimensional crosslinkages, producing a coherent, self-supporting network. The technique of Hauser and Le Beaulg has been employed by Marshall and co-workers2",21 to make mineral membranes 0.1 to 0.5 mm.…”
Section: (A) Inorganic Membranesmentioning
confidence: 99%
“…A purified, monodisperse bentonite sol of 1 per cent concentration, produced by supercentrifuging and containing particles ranging in apparent spherical diameter between 15 and 50 mp, proved particularly suitable (42) for studies of stream double refraction, because such a sol is quite clear to the eye, has practically the same viscosity and surface tension as water, and exhibits pronounced birefringence a t extremely low rates of flow and for any temperature up to the boiling point of water (44). This is actually the case, but permanent effects can only be expected if truly colloidal clays are used, becauqe only then can one eliminate sedimentation of the disperse phase (3).…”
Section: F Rheopexymentioning
confidence: 99%