Article
Macromolecules, Vol. 43, No. 16, 2010 6645
separated by 1.2 nm (approximately four layers) for HBF-2
(Figure 5, part B2) and 0.64 nm (approximately two layers) for
HBF-3 (Figure 5, part B3).
Acknowledgment. This work was funded by the Project
House “ENERCHEM” of the Max Planck Society. We would
€
like to thank Soren Selve from the TU Berlin for his aid and
patience with TEM imaging and Regina Rothe from the Max
Planck Institute of Colloids and Interface for the water adsorp-
tion measurements.
The architectural stability and porosity of HBF-1, HBF-2, and
HBF-3 was initially studied by measuring nitrogen adsorption,
however the results in the order of magnitude of approximately
30 m2 g-1 external surface area indicated that the pores are
essentially not accessible from the outside. This is a standard
problem of organic frameworks where smaller amounts of
organic side products or monomers can easily block a majority
of the channel system in a dynamic fashion. The fact that the
pores are in principle open to the outside can be deduced from the
fact that we were able to remove all but tiny traces of salt by
simple washing with water.
Supporting Information Available: Figures showing NMR
spectra, FTIR spectra, TGA plots, TEM images, DSC plots,
and PXRD analysis, and a table of elemental microanalysis
data.This material is available free of charge via the Internet at
References and Notes
Subsequently, a water adsorption study was performed on the
guest-free materials, and commercially available graphite and
clay (kaolinite) were chosen as reference systems. Samples of
“as-synthesized” HBF-1, HBF-2, HBF-3, graphite and clay were
evacuated at 10-5 Torr vacuum pressure and heated to 180 °C for
12 h to remove solvents. The samples were then used for
measurement of the isotherm from 0 to 1 bar water vapor
pressure, which shows gradual uptake at p/p0 from 0.05 to 0.6,
and some features of accessible micropores for HBF-3 (cf.
Supporting Information). The slow rise in the isotherm occurring
at higher pressures is due to the existence of a small population of
external mesopores between the crystallites; this feature is not
uncommon for particles with platelet morphology.35 Unfortu-
nately, the Brunauer-Emmett-Teller (BET) model cannot be
reliably applied to water adsorption, so no apparent surface area
can be given. A powder X-ray diffraction experiment was
performed to monitor the effect of water on the dried and
evacuated frameworks. Although it should be noted, that the
general intensity of the all reflections is attenuated due to low
contrast between the constituent light atoms (C, N, H) and water,
the general finding is that the uptake of water is accompanied
by a broadening of the peak at 26 to 27° (in terms of 2θ), which
was identified as an indicator of layer-to-layer ordering, while the
principal (hk0) reflection persist (cf. Supporting Information).
This suggests that the water uptake is accompanied by
swelling and disordering of individual layers of the framework.
Overall, this study shows that the materials HBF-1, HBF-2,
and HBF-3 behave analogous to previously known layered
materials (especially clays) with respect to water uptake, and
that these laterally continuous polymers can principally be
separated into mono- or at least oligo-layers by physical
exfoliation.
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Conclusion
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