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14.2 Chemical Structures of Clays and Organic-Salt Modifi cations 461
reaction, the divalent counter - cations in most natural clays could be exchanged
into different ions, including Na
+
, Cu
2+
, Zn
2+
, Mg
2+
, Ca
2+
and an acidifi ed H
+
form
[51] . The replacement priority for these cations are: Al
3+
> C a
2+
> M g
2+
> K
+
=
NH
4
+
> N a
+
[46, 52] . According to this exchange order, organic quaternary ammo-
nium salts can replace Na
+
ions, but not with divalent cations in Mg
2+
- MMT and
Ca
2+
- MMT. Therefore, for most natural clays, the sodium ion exchange is neces-
sary to facilitate the subsequent organic ion intercalation.
Synthetic fl uorine mica , which structurally is similar to sodium tetrasilicic
micas, is prepared from the Na
2
SiF
6
treatment of talc at high temperature [53, 54] .
The synthetic mica (Na
+
- Mica) is water - dispersible and generally used as an inor-
ganic thickener. This synthetic fl uorinated mica has an average dimension of
300 – 1000 nm in 80 – 100 nm for MMT. Another class of synthetic clays, layered -
double - hydroxide d ( LDH s), can be prepared from the coprecipitation of inorganic
salts. The chemical structure is described as [Mg
6
Al
2
(OH)
16
]CO
3
· 4H
2
O] in the
example of magnesium/aluminum hydroxides. Various metal hydroxides, includ-
ing Ni, Cu, or Zn for divalent and Al, Cr, Fe, V, or Ga for trivalent metal ions, and
anions such as CO
3
2−
, Cl
−
, SO
4
2−
, NO
3
−
, or other various organic anions, have been
reported [55 – 58] . These LDHs are classifi ed as anionic clays that can be organically
modifi ed through an anionic - exchange reaction, using substances such as carboxy-
lic acids, anionic polymers, organic phosphoric acids, and so on [58] . These syn-
thetic clays may have various applications, including heterogeneous catalysts,
optical materials, biomimetic catalysts, separation agents, and DNA reservoirs
[59 – 63] . Recently, Mg – Al LDHs were incorporated with poly(oxypropylene) -
bis - amindocarboxylic acid salt s ( POP - acid ) to result in a wide basal spacing of
92 Å [64] . This wide spacing, as well as the introduction of a hydrophobic POP
backbone, may open up new applications for this class of anionic clays.
14.2.2
Low - Molecular - Weight Intercalating Agents and X - Ray Diffraction d - Spacing
The common strategy for utilizing smectite clays is to alter their inherent
hydrophilic nature so that they become hydrophobic and organically compatible
with polymers. For the synthesis of polymer – clay nanocomposites, organic oniums
such as alkyl ammonium salts [22] are commonly used to intercalate the layered
minerals. The resultant organoclays are then suitable for the consequent process
of melt - blending with polymers and in situ polymerization. For example, sodium
montmorillonite (Na
+
- MMT), consisting of sodium ions on the silicate surface
( ≡ Si – O
−
Na
+
), can be intercalated with organic onium salts. The quaternary alkyl
ammonium (R
4
N
+
X
−
) or alkyl phosphonium (R
4
P
+
X
−
) salts are the common inter-
calating agents because of their commercial availability. The incorporation of
organic intercalating agents also resulted in a silicate gallery expansion. For
example, the C
18
- alkyl quaternary salts may intercalate Na
+
- MMT, causing a layer
space expansion to 20 − 30 Å basal spacing from the pristine 12 Å clay gallery. It is
noteworthy that the same organic quaternary salt may not exchange with natural
clays with divalent counter ions such as M
2+
- MMT [65] (where M
2+
= Mg
2+
or Ca
2+
).