The
zeolites form a large family of hydrous silicates which
show close similarities in composition and in their associations
and mode of occurrence. Aluminosilicate minerals such
as chabazite, goosecreekite, heulandite, laumonite scolecite & stilbite with
a unique interconnecting lattice structure. This lattice structure
is arranged to form a honeycomb framework of consistent diameter
interconnecting channels and pores. Negatively charged alumina
and neutrally charged silica tetrahedral building blocks are
stacked to produce the open three-dimensional honeycomb framework. Zeolites actually
attract odors & gases and trap them in its crystalline
structure. They are secondary minerals found typically in cavitiies
and veins in basic igneous
rocks.
The zeolite group is compromised of about 45 species.
The
main zeolite formula is M2/nO.Al2O3.xSiO2.yH2O,
with M defining the compensating cation with valence n. The
structural component is Mx/n[(AlO2)x(SiO2)y].zH2O, with the general
structure as arrangements of tetrahedra in building units from
ring structures to polyhedra.