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How
the Products Work
About Zeolites
| FAQ's | Mineralologist
Report
The
Zeolite Group of Minerals
The
zeolites are a popular group of minerals for collectors and an
important group of minerals for industrial and other purposes.
They combine rarity, beauty, complexity and unique crystal habits.
Typically forming in the cavities, or vesicles, of volcanic rocks,
zeolites are the result of very low grade metamorphism. Some form
from just subtle amounts of heat and pressure and can just barely
be called metamorphic while others are found in obviously metamorphic
regimes. Zeolite crystals have been grown on board the space shuttle
and are undergoing extensive research into their formation and
unique properties.
The
zeolites are framework silicates consisting of interlocking tetrahedrons
of SiO4 and AlO4. In order to be a zeolite the ratio (Si +Al)/O
must equal 1/2. The alumino-silicate structure is negatively charged
and attracts the positive cations that reside within. Unlike most
other tectosilicates, zeolites have large vacant spaces or cages
in their structures that allow space for large cations such as
sodium, potassium, barium and calcium and even relatively large
molecules and cation groups such as water, ammonia, carbonate
ions and nitrate ions. In the more useful zeolites, the spaces
are interconnected and form long wide channels of varying sizes
depending on the mineral. These channels allow the easy movement
of the resident ions and molecules into and out of the structure.
Zeolites are characterized by their ability to lose and adsorb
water without damage to their crystal structures. The large channels
explain the consistent low specific gravity of these minerals.
Zeolites
have many useful purposes. They can perform ion exchange, filtering,
odor removal, chemical sieve and gas absorption tasks. The most
well known use for zeolites is in water softeners. Calcium in
water can cause it to be "hard" and capable of forming
scum and other problems. Zeolites charged with the much less damaging
sodium ions can allow the hard water to pass through its structure
and exchange the calcium for the sodium ions. This process is
reversable. In a similar way zeolites can adsorb ions and molecules
and thus act as a filter for odor control, toxin removal and as
a chemical sieve. Zeolites can have the water in their structures
driven off by heat with the basic structure left intact. Then
other solutions can be pushed through the structure. The zeolites
can then act as a delivery system for the new fluid. This process
has applications in medicine, livestock feeds and other types
of research. Zeolites added to livestock feed have been shown
to adsorb toxins that are damaging and even fatal to the growth
of the animals, while the basic structure of the zeolite is biologically
neutral. Aquarium hobbyists are seeing more zeolite products in
pet stores as zeolites make excellent removers of ammonia and
other toxins. Most municipal water supplies are processed through
zeolites before public consumption. These uses of zeolites are
extremely important for industry, although synthetic zeolites
are now doing the bulk of the work.
Zeolites
have basically three different structural variations.
There are chain-like structures whose minerals form acicular
or needle-like prismatic crystals, ie natrolite.
- Sheet-like
structures where the crystals are flattened platy or tabular
with usually good basal cleavages, ie heulandite.
- And
framework structures where the crystals are more equant in
dimensions, ie Chabazite.
A
zeolite can be thought of in terms of a house, where the structure
of the house (the doors, windows, walls and roof) is really the
zeolite while the furniture and people are the water, ammonia
and other molecules and ions that can pass in and out of the structure.
The chain-like structures can be thought of like towers or high
wire pylons. The sheet-like structures can be thought of like
large office buildings with the sheets analogous to the floors
and very few walls between the floors. And the framework structures
like houses with equally solid walls and floors. All these structures
are still frameworks (like the true tectosilicates that zeolites
are).
These
variations make the zeolite group very diverse, crystal habit-wise.
Otherwise zeolites are typically soft to moderately hard, light
in density, transparent to translucent and have similar origins.
There are about 45 natural minerals that are recognized members
of the Zeolite Group. Industrially speaking, the term zeolite
includes natural silicate zeolites, synthetic materials and phosphate
minerals that have a zeolite like structure. The complexity of
this combined group is extensive with over 120 structural variations
and more are being discovered or made every year. Collecting zeolites
can be very enjoyable and fulfilling.
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© 1995-2002 by Amethyst Galleries, Inc.
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are the property of Amethyst Galleries, Inc., and may not be copied
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