
Special
Nanomaterials
249
capillary force, which is the fundamental concept of using supercritical
drying and is discussed above. Another is' to manipulate the inbalance
between the huge capillary force and the small mechanical strength of the
gel network,
so
that the gel network is strong enough to resist the capil-
lary force during the removal of solvent. Organic components is incorpo-
rated into inorganic gel network to change the surface chemistry of the
silica gel network and, thus,
to
minimize the capillary force and prevent
the collapse of gel network. Organic components can be introduced
through either copolymerization with organic components introduced
in the form
of
organic precurs~r,~~~,~~~ or self-assembly with solvent
exchange.'39 The incorporation of organic components into silica gel net-
work resulted in the formation of highly porous silica under ambient con-
ditions, with a porosity of 75% or higher and a specific surface area of
1000
m2/g. Organic aerogels can be made by polymerizing organic pre-
cursors and subsequent supercritical drying of aged wet gels. The most
extensively studied organic aerogels are the resorcinol-formaldehyde
(RF)
and formaldehyde (MF)
aerogel^.'^^,'^'
Carbon aerogels are formed by
pyrolysis of organic aerogels, typically at temperatures above 500°C.
Carbon aerogels retain the high surface area and pore volume of their
parent organic aerogels.'42
6.3.3.
Crystalline microporous materials: zeolites
Zeolites are crystalline aluminosilicates and were first discovered in
1756.143,'44 There are
34
naturally occurring zeolites and nearly
100
syn-
thetic type zeolites. A zeolite has a three-dimensional framework structure
with uniformly sized pores of molecular dimensions, typically ranging
from
-0.3
to
1
nm in diameter, and pore volumes vary from about 0.1 to
0.35cc/g. Zeolites have a broad diverse spectrum of applications, and
examples include catalysts, adsorbents and molecular sieves. Many review
articles and books have been p~blished.'~~-'~~ Details of the structures and
specific names of various zeolites have been summarized in litera-
ture.'48-150 Only a brief description is given below.
Zeolites are tectoaluminosilicates with a formal composition
M2/,0~A1203.xSi02.yH20
(n
=
valence state of the mobile cation,
Mf
and
x
22),
in that they are composed of
TO4
tetrahedra
(T
=
tetrahedral atom,
i.e. Si, Al), each oxygen atom is shared between adjacent tetrahedral,
which leads to the framework ratio of
O/T
being equal to
2
for all zeo-
lite~.'~'
A
dimensional framework is formed by 4-corner connecting TO4
tetrahedra. When a zeolite is made of pure silica without any defects, each