1884
DOI: 10.1038/scientificamerican08231884-7199bsupp
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Gold and Silver in the Vapor of Phosphorus

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Cited by 5 publications
(7 citation statements)
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“…P4010 und dem molekularen Phosphor(III)-oxid P40~ (Maxwell, Hendricks & Deming, 1937;Hampson & Stosick, 1938) noch von einem Phosphoroxid unbekannten Molekulargewichtes mit der empirischen Formel POe berichtet (Hautefeuille & Perrey, 1884;Thorpe & Tutton, 1886, 1890West, 1902;Emmet & Schultz, 1939). Heinz (1963) wies vor kurzem nach, dass dieses Oxid Phosphor der Oxydationsstufen III und V enthiilt und dass das Phosphor-Sauerstoff-Verhi~ltnis in dieser Verbindung variieren kann.…”
Section: Augemeinesunclassified
“…P4010 und dem molekularen Phosphor(III)-oxid P40~ (Maxwell, Hendricks & Deming, 1937;Hampson & Stosick, 1938) noch von einem Phosphoroxid unbekannten Molekulargewichtes mit der empirischen Formel POe berichtet (Hautefeuille & Perrey, 1884;Thorpe & Tutton, 1886, 1890West, 1902;Emmet & Schultz, 1939). Heinz (1963) wies vor kurzem nach, dass dieses Oxid Phosphor der Oxydationsstufen III und V enthiilt und dass das Phosphor-Sauerstoff-Verhi~ltnis in dieser Verbindung variieren kann.…”
Section: Augemeinesunclassified
“…Synthetic emerald crystals have always been of considerable interest for gemstones and other applications. The first successful synthesis of emerald crystals was reported by Hautefeuille and Perrey in 1888 [1,2]. They grew emerald crystals from Li2Mo207 and LiVO3 fluxes [1,2].…”
Section: Introductionmentioning
confidence: 98%
“…The first successful synthesis of emerald crystals was reported by Hautefeuille and Perrey in 1888 [1,2]. They grew emerald crystals from Li2Mo207 and LiVO3 fluxes [1,2]. Because enherald melts incongruently [3], the crystals have been mainly grown by the flux and hydrothermal methods.…”
Section: Introductionmentioning
confidence: 98%
“…Long time ago, Hautefeuille and Perrey, starting from a stoichiometric oxide mixture and using a flux method, were successful in synthesizing the first emerald single crystals (emerald is a colored variety of the mineral beryl ‐ nominally A l 2 B e 3 ( S i 6 O 18 ))‐ where the typical green color is due to trace amounts of Cr in the structure, substituting for Al at the octahedral sites) . The syntheses were done using the ‘flux method’, whereby a stoichiometric mixture of Be, Al, and Si oxides, doped with Cr, was kept at 800°C for 15days in a Pt crucible, with LiMo 4 to decrease the melting temperature of the system.…”
Section: Introductionmentioning
confidence: 99%