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phenolic group and the weakly basic character of
the tertiary amine group. The addition of a small
account of HClO4 solution results in a great alter-
ation of the y–A isotherm. For example, at pH
6.0, the collapse pressure is decreased to about 20
mN m−1. Further decrease in the subphase pH
leads to further reduction of collapse pressure. At
pH 5.0, the y–A isotherm is a typical expanded
isotherm with a very low collapse pressure of 13
mN m−1. On the contrary, in basic subphases,
with increasing pH values, the isotherm of HIHQ
have a tendency to increasing the condensed
phase, but the collapse pressure does not obvi-
ously change.
This means that HIHQ can form stable mono-
layers on neutral and basic subphases, but on
acidic subphase the y–A isotherms are of the
liquid expanded type and HIHQ cannot form
stable monolayers. Usually, the imine group is
unstable in basic solution, but the imine group of
HIHQ confers an unusual stability on the mono-
layer on basic subphases, showing the difference
between the air–water interface and the bulk so-
lution. In 1951, Davies suggested that the surface
pressure could be conceived of as the sum of two
components, an electrostatic term and a nonelec-
trostatic term [11]. HIHQ exists as a deprotonated
species in basic subphases, which can form a
stable, diffuse electric double layer at air–water
interface with the counterion (Na+). Therefore,
the electric double layers with a net zero charge
reduce the electrostatic repulsion between the am-
phiphiles and facilitate the formation of a close-
packed condensed film [12]. The protonated
species cannot form a stable monolayer on acidic
subphase. Increase of acidity in subphase would
causes large change of collapse pressure. This may
be explained by the increase of solubility of
HIHQ, namely, the protonation of the nitrogen
atom in the quinoline, which prevents HIHQ
from forming a condensed film [13].
The collapse pressure (ymax) of an HIHQ
monolayer at different pH values of aqueous sub-
phases can be obtained from the y–A isotherms.
Plotting the collapse pressure as a function of pH
value of the subphase, (Fig. 2) shows the pro-
nounced dependence of ymax on the pH values in
the subphases. With increasing pH values, the
ymax increases gradually, then a steep increase is
observed at ca. pH 8.0. But the further increase of
the pH value leads to a small decrease of ymax
.
From this result, we can see that HIHQ can be
used as a material to form LB film only on the
subphases with pH greater than 5.5, in which an
HIHQ monolayer with a surface pressure greater
than 20 mN m−1 can be obtained.
As mentioned above, in the pH range of 5–10,
a small change of the pH values of the subphase
can cause a large modification of the properties of
the HIHQ monolayer. It can thus be deduced that
the association-dissociation of two coordination
groups N and OH of HIHQ with the H+ ion
occurs in the subphase pH range 5–10.
3.3. Influence of acidity on the absorption of
HIHQ solution
The UV-visible spectra of HIHQ in ethanol at
different medium are shown in Fig. 3. The most
important features are the presence of three bands
at ca. 255, 292 and 380 nm. They are assigned to
1
1
1
the Bb, Lb and La bands of the quinoline ring,
respectively, and are due to pp* transitions.
Although the position of the 1Bb band hardly
1
changes on going from low to high pH, the La
1
and Lb bands are more sensitive both in terms of
frequency and intensity. For example, the absorp-
tion of the 1La band of HIHQ at various pH
values is quite different (see Fig. 4). The absorp-
tion maximum at 381 nm was bathochromically
Fig. 2. Plot of collapse pressure versus pH values of subphase.