The basic structural unit of feldspar is a tetrahedron, which consists of four oxygen atoms surrounding a silicon atom or an aluminum atom. Each such tetrahedron shares an oxygen atom with another tetrahedron to form a three-dimensional skeleton. Large radius alkali or alkaline earth metal cations are located in large voids within the framework with coordination numbers of 8 (in monoclinic feldspar) or 9 (in triclinic feldspar).
Albite powder, a triclinic glassy crystal, generally colorless, white, yellow, red or black, is a type of feldspar. Albite powder is a framework silicate structure with a specific gravity of 2.62 and a Mohs hardness of 6 - 6.5, of which the content of anorthite is less than 10%. Albite is a sodium mineral of the plagioclase solid solution series, most common in pegmatites and granites.
Albite powder is a kind of feldspar, a common feldspar mineral, and a sodium aluminosilicate. Albite powder is generally a glassy crystal, colorless or white, yellow, red, green or black.
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