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The Fusibility Test

The fusibilit)t test is also a qualitative assay that consists of observing the melting ability of a tiny mineral fragment held in the dart of the blowpipe flame. Historically this simple test was based on the experimental observation made by the first mineralogists and chemists that [Pg.770]

Easy fusible 1 525°C Stibnite [Sb,S,] Coarse splinters that fuse easily in the flame of a candle or a match. [Pg.770]

Fusible 3 1050°C Almandine [Fe3Af(SiO,)3l Coarse splinters easily fuse to give a globule at the tip of the blowpipe, and only finest splinters rounded in a Bunsen burner. [Pg.770]

Fusible with difficulties 5 1300°C Orthoclase [KAlSijOJ Fused only in fine splinters or on thin edges underthe blowpipe. [Pg.770]

Infusible 7 1760°C Quartz [SiOJ Entirely infusible under the dart of the blowpipe, and retaining the edge in all its sharpness. [Pg.770]


See other pages where The Fusibility Test is mentioned: [Pg.151]    [Pg.770]    [Pg.771]   


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