Letters
J. Phys. Chem. B, Vol. 109, No. 3, 2005 1065
backbone conformation. Clearly, the degree of hydration of 3
is much less (ca. 15% of the total electron density) than that
for 14+. The limiting area of 3 on the water surface at a surface
pressure Π of 20 mN/m is also much smaller than that for the
[2]rotaxanes, i.e., approximately 80 Å2 for 3 as opposed to 180
Å2 for 14+ and 24+. Hence, the absence of the tetracationic
cyclophane results in a noticeably different molecular arrange-
ment and degree of hydration in Langmuir layers, suggesting a
closer packed monolayer with a less tilted/folded conformation.
In an attempt to elucidate the structural response to oxidation,
the electron density profiles for oxidized Langmuir films of 14+
,
supposedly containing the species 16+, were found to differ only
insignificantly from those obtained for the starting (unoxidized)
state 14+. This observation indicates that no net reorganization
of the electrons takes place in the vertical direction. Hence,
movement of the cyclophane, if any, would have to either (i)
occur predominantly in the plane of the film or (ii) be
accompanied by an opposite rearrangement of the water
molecules and counterions. To address these issues, experiments
employing longer and less hydrophilic rotaxanes are in progress.
In summary, we provide, by use of surface sensitive
synchrotron X-ray techniques, evidence for strongly tilted and/
or folded conformations for the rotaxane molecules in the
Langmuir films of 14+ and 24+, which have been used2d in the
preparation of molecular crossbar memory devices. The folded
conformation is presumably a result of the hydrophilic nature
of the tetracationic cyclophane and its counterions. These
observations are also supported by recent Langmuir-Blodgett
studies15 of other related amphiphilic bistable [2]rotaxanes.
Furthermore, we have established that the monolayers are highly
hydrated and show no in-plane crystalline order, and that it is
possible, based on electron density profiles, to resolve and
differentiate between (super)structures of closely related [2]ro-
taxanes (14+ vs 24+). The electron density profiles may serve
as important future references for molecular modeling of the
switching mechanism in amphiphilic rotaxanes in condensed
Langmuir films. This work is currently in progress.16
Figure 4. Electron density profiles for Langmuir films of the
amphiphlic bistable [2]rotaxane 14+ derived from synchrotron X-ray
reflectivity measurements at the air/water interface at applied surface
pressures Π ) 0.5, 4, and 20 mN/m, corresponding to mean molecular
areas of 470, 265, and 180 Å2, respectively. The shaded section
illustrates the approximate position of the interface to the bulk water.
profiles of 14+ measured at three different surface pressures, Π
) 0.5, 4, and 20 mN m-1, corresponding to mean molecular
areas of ∼470, 265, and 180 Å2. Assuming that the monolayer
is homogeneous, Figure 4 shows that the thickness of the [2]-
rotaxane monolayers increases from 22 Å, in very expanded
monolayers (Π ) 0.5 mN m-1), to over 23 Å in slightly
compressed monolayers (Π ) 4 mN m-1), and ultimately to
33 Å in moderately condensed monolayers (Π ) 20 mN m-1).
This progression suggests that this [2]rotaxane, when spread
on the water surface, initially adopts a very tilted conformation
in which the molecule is more or less lying down with large
parts exposed to the water surface. This picture is also supported
by the absence of texture in the Brewster angle micrographs of
the Langmuir film and the absence of crystallographic order,
effects that are otherwise frequently observed in Langmuir films
of more hydrophobic molecules that spontaneously form
2-dimensional islands when spread at the water surface.
In the case of the sterically encumbered [2]rotaxane 24+, a
similar monolayer thickness (ca. 31 Å) and mean molecular area
(180 Å2) were found at 20 mN/m (Figure 2, right). However,
the detailed electron density profile and, in particular, the degree
of hydration differ significantly. Hence, for 24+ where the
cyclophane is confined to the “upper” station (DNP), less
hydration of the monolayer is observed than for 14+, where the
cyclophane is predominantly on the “lower” (MPTTF) station.
From comparison of the electron density profiles of 14+ and
Acknowledgment. This research was funded by the Danish
Natural Science Research Council (SNF, projects #21-03-0317,
#21-03-0014, and #21-02-0414) in Odense, Denmark, and by
the Defense Advanced Research Projects Agency (DARPA) in
the United States. We thank HASYLAB at DESY in Hamburg
for beam time at beam line BW1 and DANSYNC for financial
support.
Supporting Information Available: The synthesis of 24+
and 3, Langmuir film details and X-ray reflectivity data. This
material is available free of charge via the Internet at http://
pubs.acs.org.
References and Notes
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F. M.; Stoddart, J. F.; Venturi, M.; White, A. J. P.; Williams, D. J. J. Org.
Chem. 2000, 65, 1924-1936. (b) Jeppesen, J. O.; Perkins, J.; Becher, J.;
Stoddart, J. F. Org. Lett. 2000, 2, 3547-3550. (c) Jeppesen, J. O.; Perkins,
J.; Becher, J.; Stoddart, J. F. Angew. Chem., Int. Ed. 2001, 40, 1216-1221.
(d) Tseng, H.-R.; Vignon, S. A.; Stoddart, J. F. Angew. Chem., Int. Ed.
2003, 42, 1491-1495. (e) Jeppesen, J. O.; Nielsen, K. A.; Perkins, J.;
Vignon, S. A.; Di Fabio, A.; Ballardini, R.; Gandolfi, M. T.; Venturi, M.;
Balzani, V.; Becher, J.; Stoddart, J. F. Chem. Eur. J. 2003, 9, 2982-3007.
(f) Yamamoto, T.; Tseng, H.-R.; Stoddart, J. F.; Balzani, V.; Credi, A.;
Marchioni, F.; Venturi, M. Collect. Czech. Chem. Commun. 2003, 68, 1488-
1514. (g) Tseng, H.-R.; Vignon, S. A.; Celestre, P. C.; Perkins, J.; Jeppesen,
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2
4+, it is clearly evident that it is possible to distinguish between
the case where the cyclophane is located around the MPTTF
recognition site (14+) and when it is located around the DNP
recognition site (24+).
The monolayer thickness of the dumbbell 3 is around 41 Å,
a value much closer to that expected for a stretched and nontilted
(2) (a) Collier, C. P.; Mattersteig, G.; Wong, E. W.; Luo, Y.; Beverly,
K.; Sampaio, J.; Raymo, F. M.; Stoddart, J. F.; Heath, J. R. Science 2000,