Ammonium fluorosilicate has three major
polymorphs: α-(NH4)2[SiF6] form is
cubic (
space group Fm3m, No. 225) and corresponds to the mineral cryptohalite. The β form is
trigonal (scalenohedral) and occurs in nature as mineral bararite. (Note: trigonal symmetry is part of the hexagonal group, but not all hexagonal crystals are trigonal.) The silicon atoms of α-(NH4)2[SiF6] (alpha), have
cubic close packing (CCP). The γ form has
hexagonal close packing and the β-(NH4)2[SiF6] has primitive hexagonal packing. In all three phases, 12
fluorine atoms neighbor the (NH4)+. it does not appear one
polymorph has ever turned into another. Even so, ammonium fluorosilicate assumes a trigonal form at pressures of 0.2 to 0.3
GPa. The reaction is irreversible. If it is not bararite, the phase is at least very closely related. The
hydrogen bonding in (NH4)2[SiF6] allows this salt to change phases in ways that normal salts cannot. Interactions between
cations and
anions are especially important in how
ammonium salts change phase. (To learn more about the β-structure, see
Bararite.) ==Natural occurrence==