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Structural arrangement, coordination shell

In B cristobalite this angle is 180 whereas in a and B quartz and a cristobalite it ranges between 143 and 150 . Thus a silicagel may be considered as formed of small units, involving the second coordination shell, which are characterized by structural arrangements such as those found for these crystalline solids. [Pg.166]

See other pages where Structural arrangement, coordination shell is mentioned: [Pg.63]    [Pg.374]    [Pg.234]    [Pg.30]    [Pg.67]    [Pg.18]    [Pg.77]    [Pg.81]    [Pg.490]    [Pg.239]    [Pg.88]    [Pg.555]    [Pg.254]    [Pg.93]    [Pg.493]    [Pg.103]    [Pg.113]    [Pg.90]    [Pg.554]    [Pg.935]    [Pg.166]    [Pg.161]    [Pg.182]    [Pg.168]    [Pg.919]    [Pg.382]    [Pg.272]    [Pg.132]    [Pg.159]    [Pg.209]    [Pg.169]    [Pg.113]    [Pg.230]    [Pg.48]    [Pg.313]    [Pg.164]    [Pg.93]    [Pg.119]    [Pg.142]    [Pg.85]    [Pg.277]    [Pg.196]    [Pg.162]    [Pg.310]    [Pg.72]    [Pg.74]    [Pg.89]    [Pg.177]    [Pg.312]    [Pg.315]   
See also in sourсe #XX -- [ Pg.166 ]



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Coordination Structures

Coordination shell

Shell structure

Structural Arrangements

Structural arrangement, coordination

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