-
sites View of
dioctahedral sheet structure of mica. The
binding sites for
apical oxygen are
shown as
white spheres. View of
dioctahedral sheet structure...
-
commonly known as montmorillonite.
Diosmectite is a
contraction of "
dioctahedral smectite". Its
effectiveness in
improving stool consistency is the result...
- endmember, to palygorskite, the
least magnesic, most Al- Fe- bearing,
dioctahedral endmember.
Originally named meerschaum by
Abraham Gottlob Werner in 1788...
- 233.3 pm (Sb−Clax). At low temperatures, SbCl5
converts to the dimer,
dioctahedral Sb2Cl10,
structurally related to
niobium pentachloride. PCl5 is prepared...
-
Phengite is a
series name for
dioctahedral micas of
composition K(Al,Mg)2(OH)2(Si,Al)4O10. It is
common for Mg or Fe2+ to
substitute for Al on the Y site...
-
alumina (AlO6).
Kaolinite is a soft, earthy,
usually white,
mineral (
dioctahedral phyllosilicate clay),
produced by the
chemical weathering of aluminium...
-
group due to
structural similarities.
Smectite group which includes dioctahedral smectites, such as montmorillonite,
nontronite and beidellite, and trioctahedral...
- all of the
sites may be occupied. In that case, the
mineral is
termed dioctahedral,
whereas in
other case it is
termed trioctahedral. The
layers are weakly...
-
Christopher J. (2003). "Ab
initio determination of edge
surface structures for
dioctahedral 2:1 phyllosilicates:
implications for acid-base reactivity" (PDF). Clays...
-
layer of O' octahedra, only two-thirds of
whose sites are
occupied (
dioctahedral layer).
Unoccupied octahedral sites are
called "vacant sites". This layer...
