A bio-inspired attention model of anticipation in gaze-contingency experiments with infants
Model experiments of superlubricity of graphite
Transcript of Model experiments of superlubricity of graphite
Model experiments of superlubricity of graphite
Martin Dienwiebel a,*,1, Namboodiri Pradeep a, Gertjan S. Verhoeven a,Henny W. Zandbergen b, Joost W.M. Frenken a,*
a Kamerlingh Onnes Laboratory, Leiden University, P.O. Box 9504, 2300 RA Leiden, The Netherlandsb Laboratory of Materials Science, Delft University of Technology, Rotterdamseweg 137, 2628 AL Delft, The Netherlands
Received 6 September 2004; accepted for publication 20 December 2004
Available online 27 December 2004
Abstract
Graphite is known to be a good solid lubricant. The low-friction behavior is traditionally ascribed to the low resis-
tance to shear. We have recently observed that the ultra-low friction found in friction force microscopy experiments on
graphite is due to a effect called superlubricity [M. Dienwiebel, G. S. Verhoeven, N. Pradeep, J.W.M. Frenken, J.A.
Heimberg, H.W. Zandbergen, Phys. Rev. Lett. 92 (2004) 126101]. Here, we provide additional experimental evidence
that superlubricity has been taken place between a small graphite flake attached to the scanning tip and the graphite
surface. Finally, we speculate about the significance of this for the lubricating properties of graphite.
� 2004 Elsevier B.V. All rights reserved.
Keywords: Tribology; Friction; Atomic force microscopy; Graphite
1. Introduction
Graphite is undoubtedly the most common so-
lid lubricant. Mainly used as flaky powder, it is
e.g. applied where liquid lubricants cannot be
used, especially in high-temperature applications,
or as friction reducing additive in oils and poly-
mers and as brushes in electrical motors. It is not
surprising that research on the tribological proper-
ties of graphite has a long history and it is well
established that the friction coefficient for many
materials against graphite in ambient conditions
is in the range of 0.08–0.18 (see e.g. [1]). Tradition-
ally, the good lubricating properties of lamellar
solids are ascribed to the weak interaction between
adjacent graphite layers [2]. However, the intuitive
idea that this would lead to ‘‘easy shear’ ’ has been
argued to be unsatisfactory. Finch [3] has pointed
0039-6028/$ - see front matter � 2004 Elsevier B.V. All rights reserved.
doi:10.1016/j.susc.2004.12.011
* Corresponding authors. Tel.: +49 721 95505956; fax: +49
721 9550528 (M. Dienwiebel).
E-mail addresses: [email protected] (M. Dienwie-
bel), [email protected] (J.W.M. Frenken).
URL: http://www.physics.leidenuniv.nl1 Present address: IAVF Antriebstechnik AG, Im Schlehert
32, 76187 Karlsruhe, Germany.
Surface Science 576 (2005) 197–211
www.elsevier.com/locate/susc
out that simultaneous rupture of all bonds in a
plane, i.e. cleavage would require a very high en-
ergy. This is supported by the fact that graphite
does not shear readily, unless a high compression
is superimposed [1]. Savage and others [4–6] have
found that the friction coefficient for metals
against graphite is much higher (0.8) in vacuum
and that wear is very heavy. The high friction
was still observed after admission of hydrogen or
nitrogen. Only after admission of a few ppm of
oxygen or certain organic vapors, low friction
and low wear were restored. It has been shown
that when metal is sliding on graphite in air,
graphite is transferred to the metal surface, while
in vacuum metal is transferred to the graphite sur-
face [7]. Moreover it has been shown, that a metal
oxide layer tends to fix the transferred graphite to
the metal, leading to a smooth transfer film [8].
The combination of these observations strongly
suggests that the low friction is only obtained
when graphite slides over graphite.
The first atomic-scale friction experiment has
been performed by Mate et al. [9] using a tungsten
tip sliding over a highly ordered pyrolytic graphite
(HOPG) surface under ambient conditions. These
authors found friction coefficients between 0.005
and 0.015. Unlike in frictional force microscopy
(FFM) experiments on other materials, where usu-
ally a power law behavior is found, FF = (FN)a,
with a < 1, the dependence of the friction force
FF on the normal load FN was found to be almost
linear on graphite. Similar friction versus load
behavior and similar friction coefficients have been
observed in subsequent FFM experiments on
graphite with a variety of tip materials [10–13].
In FFM experiments on graphite and other
materials such as e.g. alkali-halides the scanning
tip performs so-called ‘‘stick-slip’’ motion, jump-
ing discontinuously over single lattice spacings.
Fujisawa et al. [14] have shown, using a two-
dimensional FFM, that lateral force images can
be explained by two-dimensional, i.e. ‘‘zig-zag’’
atomic-scale stick-slip motion. A simple classical
mechanics model [15], the so-called Tomlinson
model, in which a single-atom tip is dragged
through a sinusoidal potential, reproduced the
experimental lateral force maps of the graphite
surface quite well [16,17]. However, the normal
forces that were used in the simulations had to
be chosen one to two orders of magnitude lower
than those in the experiments [18].
We have recently shown that the ultra-low fric-
tion coefficients of graphite, found in FFM exper-
iments are caused by ‘‘superlubricity’’ between
graphite surfaces [19]. The term superlubricity
has been introduced by Shinjo and Hirano [20]
and it describes the notion that friction might van-
ish almost completely even when two crystalline
surfaces slide over each other in dry contact. This
phenomenon was first demonstrated in a quasi-
static calculation for rigid crystals with fcc, bcc
and hcp symmetry and different orientations [21].
In a consecutive study the same authors used a
Frenkel–Kontorova model (F–K model) to study
the transition from kinetic friction to superlubric-
ity in one and two dimensions. They concluded
that one way to observe this transition experimen-
tally, is to change the commensurability between
the two surfaces. The concept of superlubricity
only takes into account energy dissipation due to
excitation of phonons. Other dissipative processes,
such as ‘‘electronic friction’’ or ‘‘quantum fric-
tion’’ [22], will not depend on the degree of com-
mensurability. Therefore, even in the case of
complete, phononic superlubricity, the total fric-
tion force will not be identical to zero. The similar-
ity of the term ‘‘superlubricity’’ with similar terms
such as ‘‘superconductivity’’ and ‘‘superfluidity’’ is
therefore misleading. Nonetheless, under appro-
priate conditions, superlubricity might cause a
reduction of the friction force by orders of magni-
tude. In this article, we give a more complete ac-
count of our experimental results and we provide
firm evidence for superlubricity occurring in fric-
tion force microscopy experiments on a graphite
substrate.
2. Experimental
We have performed measurements on HOPG
samples using a homebuilt FFM [23] that allows
quantitative tracking of the forces on the scanning
tip in three directions, with a high resolution in the
lateral forces, down to 15 pN. The key feature of
our microscope is a dedicated friction force sensor,
198 M. Dienwiebel et al. / Surface Science 576 (2005) 197–211
the Tribolever [24]. It combines low and symmetric
spring constants of 5.75 ± 0.15 N/m in the two lat-
eral directions with a high stiffness of 26 ± 1 N/m
in the normal direction. The Tribolever was cali-
brated using the ‘‘added mass’’ method, developed
by Cleveland et al. [25]. A tungsten tip was glued
into the Tribolever using silver epoxy, such that
it extended 50–60 lm out of the device. The
displacements of the Tribolever tip in the X-, Y-
and Z-directions are monitored using four all-
glass-fiber interferometers. The instrument can
rotate the sample to change the relative orientation
between the tip and sample lattices. Initial mea-
surements have been performed on HOPG graph-
ite of grade ZYH, which has a nominal grain size
in the range of 30–40 nm and a mosaic spread of
3.5� ± 1.5� according to the supplier [26]. How-
ever, on our particular sample we found only
larger grains. Later measurements have been per-
formed on grade ZYA graphite, which possesses
a lateral grain size of up to 10 mm and a mosaic
spread of 0.4� ± 0.1�. The samples were cut to a
size of 2 mm · 2 mm. Therefore, the grade ZYA
sample consisted probably of a single graphite
crystal, while the grade ZYH sample was polycrys-
talline. The HOPG was freshly cleaved using
Scotch tape and then mounted in the FFM inside
a small chamber, which was continuously flushed
with dry nitrogen. The measurements were typi-
cally performed at humidities of 1–10 ± 1% RH.
The scanning speed in the experiments was
v = 30 nm/s. All force maps were recorded in the
form of two-dimensional ‘‘images’’ with 512 ·
512 pixels.
We performed two different types of measure-
ments. In the case of ‘‘lateral force imaging’’, the
external normal load FN was set to a constant value
using the feedback loop of the scan electronics.
Zero normal load was defined as the load at which
the Tribolever was not bent in the normal direc-
tion. When the tip was scanned over the surface,
we recorded the lateral forces in the two perpendic-
ular directions defined by the X- and the Y-axes of
the Tribolever, both during the forward and during
the reverse scan lines. Other than with a conven-
tional AFM cantilever, with the Tribolever it is
possible to choose any sliding direction in the mea-
surement, and always record the lateral forces par-
allel and perpendicular to the scan direction with
equal sensitivity. The lateral force was defined as
the lateral spring constant times the lateral dis-
placement of the Tribolever pyramid with respect
to the FFM base: F latX ;Y
¼ kTriboleverX ;Y
DxTriboleverX ;Y
. In gen-
eral, the X direction of the Tribolever and the fast
scanning direction (which is the ‘‘x direction’’ in a
lateral force image) will be rotated with respect to
each other. In the following, X and Y denote the
directions of the Tribolever axes, and x and y as
the fast and slow scan axes of the lateral force im-
age. By changing the fast sliding direction x, also
the angle between the x direction and the lattice
orientation changes.
One forward scan line and the subsequent re-
verse scan line together form a closed hysteresis
loop, that is often referred to as the ‘‘friction
loop’’. An example of such a friction loop is shown
in Fig. 1c. The area that is enclosed inside the fric-
tion loop corresponds to the dissipated energy dur-
ing the back and forth sliding. We calculated the
average friction force in the X and in the Y direc-
tion of the Tribolever by taking the difference be-
tween the mean value of the lateral force in the
forward direction and in the reverse direction:
F X ;Y �hF lat
fwdi � hF latrevi
2
� �
: ð1Þ
The mean value of the lateral force hFlati was only
obtained from those parts of the friction loop
where the lateral force had fully developed, e.g.
for x > 0.7 nm in the forward scan line and for
x < 2.3 nm in the reverse line in Fig. 1c.
To obtain the friction force, i.e. the component
of the average lateral force in the sliding direction,
we computed the appropriate vector addition of
the average lateral forces in the X- and the Y-
direction:
F F ¼ F X cos fþ F Y sin f; ð2Þ
where f denotes the angle between the X direction
of the Tribolever and the sliding direction of the
tip (x).
The second type of measurement that we per-
formed is referred to in the literature as ‘‘friction
force spectroscopy’’ [27]. Here, we initially set
the normal force FN to a positive value and low-
ered it at every line during the scan, until the tip
M. Dienwiebel et al. / Surface Science 576 (2005) 197–211 199
lost contact with the surface. From each single
line, i.e. each single FN value, one (FN,FF) data
point was obtained, using Eqs. (1) and (2).
Together, all the scan lines resulted in a friction
spectrum FF (FN).
3. Results
3.1. Lateral force images and friction loops
Fig. 1 shows typical lateral force images mea-
sured simultaneously in the forward X-direction
of the Tribolever (a) and in the direction perpen-
dicular to that (b) on the polycrystalline HOPG
surface. The x- and X-directions were aligned.
Not shown is the topography image (Z), obtained
at the constant normal force of FN = �3.2 nN
which does not reveal any surface features. The
rms roughness of 0.27 A, measured from the
topography image was caused by residual noise
in the detection of the Z position of the Tribolever.
The lateral force in the sliding direction exhibits a
typical saw tooth waveform (c), which can be ex-
plained by atomic-scale stick-slip motion, as has
been shown in several earlier experiments [9,14,
28,11]. Depending on the sliding direction, the lat-
eral force image in the perpendicular direction
shows different patterns. If the sliding direction is
parallel to one of the six symmetry directions of
the HOPG surface, the lateral force measured
perpendicular to the sliding direction shows a hor-
izontal stripe pattern (Fig. 1b). If the tip is scanned
under a different angle, the patterns in the X- and
the Y-images change and the tip performs a ‘‘zig-
zag’’ stick-slip movement over the graphite lattice.
This shows that the forces in the sliding direction
cannot be regarded independently from those in
the perpendicular direction. The zig-zag motion
is stronger for the Tribolever than for most ‘‘tradi-
tional’’ cantilevers, because of the equality of
kTriboleverx and kTribolever
y .
Fig. 1. Lateral force image of a tungsten tip on HOPG at FN = �3.2 nN. The tip is sliding in the x direction, which is aligned with one
symmetry direction of the surface. (a) Lateral forces in the forward x direction; grey scale: 1.7 nN. (b) Lateral forces in the
perpendicular y direction; grey scale: 93 pN. Image size 3 nm · 3 nm. (c) Experimental friction loop from (a), and (d) a force loop
calculated using a Tomlinson model for a single-atom tip. The calculation was performed using a potential energy amplitude of
V0 = 0.08 eV and lateral spring constants kx = ky = 1.8 N/m (see [39]). Throughout this paper the lateral forces during the forward scan
lines are plotted as black curves, the forces during the reverse scan lines are plotted as grey curves.
200 M. Dienwiebel et al. / Surface Science 576 (2005) 197–211
Fig. 1c and d shows a comparison between an
experimental friction force loop, obtained from
one forward scan line of Fig. 1a, plus the subse-
quent reverse line (c), and a theoretical friction
loop, obtained from a Tomlinson model calcula-
tion (d). The comparison shows good qualitative
agreement between the experimental and the
calculated friction loops, suggesting that our mea-
surements can be understood using a two-dimen-
sional Tomlinson model. However, to obtain
quantitative agreement between the force magni-
tudes in the calculated and experimental force
loops, we had to use a lateral spring constant in
the calculation which differed from the known
kTribolever. This suggests that also the elastic com-
pliance of the contact contributes to the total
spring constant. The effective spring constant can
be obtained directly from the slope of those parts
of the measured force loops where the contact
sticks [29,30]. To understand this, one can view
the measurement system as a set of springs in ser-
ies. The effective spring constant is constituted of
dF latX
dx¼ ðkTriboleverÞ�1 þ ðkcontactÞ�1
h i�1
; ð3Þ
where kTriboleverx ¼ kTribolever
y ¼ kTribolever is the known
spring constant of the Tribolever and kcontact is
called ‘‘contact stiffness’’ [29]. This contact stiffness
can be separated further in
kcontact ¼ ðkaddÞ�1
þ ðkinterfaceÞ�1
h i�1
; ð4Þ
where kinterface ¼ o2V =ox2 ¼ 2p
a
� � 2V 0 is the spring
formed by the local curvature in the wells of the
potential energy landscape of the substrate as
experienced by the tip, where the last step assumes
a sinusoidal potential with period a and amplitude
V0. The spring formed by additional elastic com-
pliances, such as the elastic compliance of the tip
and that of the sample, is symbolized by kadd.
Since we cannot distinguish between the compli-
ances introduced by the tip and those introduced
by the surface, we will take these together.
Using Eq. (3) we find a contact stiffness in Fig.
1c of 2.3 ± 0.3 N/m. Because the curvature of a cor-
rugated potential energy landscape acts also in the
Tomlinson model as a spring that contributes to
the contact stiffness, also the calculated friction
loop possesses an effective stiffness that differs from
kTribolever, but since kadd = 1 in the model, we sim-
ply have kcontact ¼ kinterface ¼ 2pa
� � 2V 0 in the model
calculation. The force at which the slip events take
place is largely determined by the amplitude of the
potential and the sum of 1/kTribolever + 1/kadd. We
obtain a simultaneous fit of the effective stiffness
and the maximum lateral force for a potential cor-
rugation of V0 = 0.08 eV and a ‘‘potential spring
constant’’ of kinterface = 15.9 N/m. Since kTribolever
is known with an accuracy of 2.3%, we can now
estimate the additional stiffness to be kadd =
2.7 N/m. The effect of the tip compliance is to lower
the effective spring constant of the Tribolever
to kTribolevereff ¼
�
ðkTriboleverÞ�1
þ ðkaddÞ�1��1
¼ 1:8 N/m.
With this value, we find indeed good agreement be-
tween the experimental force loops and the calcu-
lated one. The precise origin of the additional
elastic compliance cannot be determined from
these measurements, but it seems likely that the
elastic compliance of the tip dominates.
A clear difference between the simulated friction
loop and the experimental one, is that the posi-
tions where the slip occurs in the experimental
data display variations in the order of 25% of the
lattice spacing. In the parts of the friction loop
where the tip is sticking, the lateral force fluctua-
tions are much too small to account for these vari-
ations. This is clearly seen also in all lateral force
images, which ‘‘look’’ noisy, despite good lateral
force resolution. We believe that these fluctua-
tions, which can be seen also in other FFM exper-
iments with comparable effective spring constants
and normal loads (e.g. [31]), are thermally induced.
Using a modified Tomlinson model that included a
term representing the effect of random thermal
fluctuations, Sang et al. [32] have studied thermal
effects on atomic friction by adding a Langevin
term to the Tomlinson model. Dudko et al. [33]
used a Fokker–Planck approach, and showed that
it is equivalent with the solution of the Langevin
equation. With an effective spring constant of
keff = 0.86 N/m to fit the data from Gnecco et al.
[31], they have found that the distribution function
of the maximum lateral force in the friction trace,
which is equivalent to the slip position, had a full
M. Dienwiebel et al. / Surface Science 576 (2005) 197–211 201
width at half maximum (FWHM) of approxi-
mately 17%. In order to evaluate thermal fluctua-
tions in our experiment, we simulated them in
the Tomlinson model calculations using a simple
Monte-Carlo approach. At every time step Dt,
where Dt = Dxt/v, we calculated the transition rate
C, which is an inverse measure of the time needed
before a thermally induced jump over the energy
barrier takes place,
C ¼ f0 exp �DV ðxtÞ
kBT
� �
; ð5Þ
where f0 is the eigenfrequency of the Tribolever,
DV(xt) is the remaining energy barrier with respect
to the momentary tip position, kB is the Boltz-
mann constant and T is the temperature. The
‘‘probability’’ CDt for a thermally induced jump
over the barrier was then compared with a number
R 2 [0,1] obtained from a random number genera-
tor and, if R was lower than CDt, a jump at posi-
tion xt was induced.
Fig. 2 shows the normalized distribution for
15,000 simulated slip events using kTribolevereff ¼
1:8 N/m, V0 = 0.08 eV, v = 30 nm/s and an effective
mass of the Tribolever of 10 lg. The distribution
possesses a FWHM of 30 pm, which is 12.3% of
the graphite unit cell. In addition, the jumps oc-
curred on average 44 pm before the static case,
recovered in the Tomlinson model at T = 0.
3.2. Friction versus load
The friction versus load data strongly suggests
that the sliding has been taking place between
two graphite surfaces, one being the HOPG sub-
strate, and the other being a small piece of graph-
ite, i.e. a graphite flake, that was attached to the
tungsten tip.
Fig. 3a–f shows three lateral force maps and
friction loops measured in the forward X-direction
at different normal loads. Again, the x-direction
was aligned with the X-direction of the Tribolever.
Fig. 3g–i displays the average waveform of the lat-
eral force variations over one lattice period, ob-
tained by averaging the lateral force variations
over three lattice periods. Already at a negative
load of �3.4 nN, variations in the lateral force
with lattice periodicity are faintly visible. How-
ever, these variations do not have a ‘‘saw tooth’’
shape, typical for stick-slip motion, but a continu-
ous shape (Fig. 3g). At this normal force, the area
enclosed inside each friction loop (Fig. 3d) is very
small. In other words, the energy dissipated during
one sliding cycle is nearly negligible. Correspond-
ingly, the average friction force obtained from
the complete lateral force map, according to the
procedure described in Section 2 (Eqs. (1) and
(2)) is as low as 1:8þ16�1:8 pN. At a higher normal
load of 11.6 nN, the variations in the lateral force
increased, and the lattice can be seen more clearly
in the force map, but the average friction force did
not increase significantly, as can be seen from the
force loop in Fig. 3e.
Note, that the waveform of the lateral force
variations changed and appears ‘‘saw tooth’’-like
(Fig. 3h). At a still higher normal load of 41 nN
we observed clearly ‘‘saw tooth’’-like lateral force
variations (Fig. 3i) and an increase in the average
friction force to 62 ± 19 pN, (Fig. 3f).
Complete friction versus load curves were ob-
tained from friction force spectroscopy measure-
ments (see Section 2 for procedure). Fig. 4a
shows an example for a contact that behaved sim-
ilarly to the one shown in Fig. 3. The normal force
was reduced from 45 nN until the tip lost contact
with the surface at �24 nN, at which point the
tip was fully retracted by the feedback electronics.
The data in Fig. 4a are representative for a large
Fig. 2. Normalized distribution of the slip position at temper-
ature T = 293 K. The origin of the x-axis lies at the slip position
of xt without thermal fluctuations. The calculation was
performed using V0 = 0.08 eV and kx,y = 1.8 N/m.
202 M. Dienwiebel et al. / Surface Science 576 (2005) 197–211
number of measurements. In the normal force
range from �24 to approximately +30 nN the fric-
tion force stayed almost constant at a very low
value of 28 ± 16 pN. The frictional behavior as a
function of normal load obtained from the friction
force spectroscopy experiment shown in Fig. 4a is
in agreement with the friction forces obtained
from individual lateral force images at different,
constant normal loads. As in Fig. 3, we see very
low energy dissipation up to about FN = 40 nN.
For normal loads above 40 nN we observe a slight
increase. A smaller number of measurements pro-
duced entirely different friction versus load curves.
An example is shown in Fig. 4b. The curve was
measured under similar conditions as the one in
Fig. 4a. Now, the friction force between �11 and
+24 nN normal load is on average 453 ± 16 pN,
which is a factor 16 higher than in the measure-
ment shown in 4a. The friction force remained at
a high and almost constant level until the tip lost
contact at FN = �16 nN. In these ‘‘high-friction’’
measurements, the typical increase in friction be-
tween loads of 0 and 25 nN was as low as 0.05–
0.4%. For other substrates, FFM measurements
Fig. 3. Lateral force images in the forward x-direction (a–c) and force loops (d–f) for different normal loads. Graphs (g–i) show the
typical waveform obtained from the forward scan lines shown in (d–f) by averaging over three lattice spacings. (a,d,g) FN = �3.4 nN,
(b,e,h) FN = 11.6 nN, (c,f,i) FN = 42.6 nN; Image size 3 nm · 3 nm.
(a) (b)
Fig. 4. Friction force FF versus normal load curves for two different contacts. Notice that in both curves the friction force varies little,
but the average friction force in (b) is about a factor of 16 higher than in (a).
M. Dienwiebel et al. / Surface Science 576 (2005) 197–211 203
usually show a substantial load dependence,
which, for modest loads, can be attributed to the
elastic variation in the contact area with the load
(e.g. [34]). Load-independent friction has also been
observed in FFM experiments on thermally oxi-
dized MoS2, and it was proposed that MoO3 nano-
crystals, that grew during the oxidation process on
the MoS2 surface [35], acted as a spacer between
the tip and the sample, such that the contact area
remained unchanged upon loading. In the present
case, the contact area would be completely deter-
mined by the flake size, which would be indepen-
dent of the loading force. Hence, the friction
would only increase slightly with normal load as
the result of the increase in contact pressure.
Each friction versus load measurement on the
polycrystalline HOPG surface resulted in a curve
of one of the two types shown in Fig. 4, but with
different precise values of the average friction
force. The measured friction force curves switched
back and forth between the two types (Fig. 4a and
b) randomly in intervals ranging from days to sev-
eral weeks. Subsequent measurements that were
performed within a short period of several hours
were highly reproducible. The switching in the
average friction force could not be attributed to
changes in the ambient conditions such as the
humidity inside the FFM chamber, e.g. we did
not observe systematic changes in friction when
we varied the humidity from 9% to 42% RH dur-
ing one experiment. Also, no systematic differences
were found between the friction force on freshly
cleaved HOPG and on surfaces that had been ex-
posed to ambient conditions for several days.
The possibility of dissipationless motion was
probably first mentioned by Prandtl already in
1928 [36] who developed what is now referred to
as the Tomlinson model in order to explain
stress–strain curves of metals. However, he also
pointed out the application of the model towards
dry friction. Much later, it has been pointed out
by Tomanek et al. [37] that it is possible to obtain
frictionless sliding in with a FFM when a single-
atom tip is moving over the surface without insta-
bilities, i.e. without the familiar stick-slip motion
and this has very recently been demonstrated
experimentally by Socoliuc et al. [38]. This can oc-
cur when the tip is moving through a potential en-
ergy landscape with a corrugation amplitude that
is small with respect to the stiffness of the measure-
ment system. However, in our case, this would re-
quire a spectacularly low potential corrugation
and an unrealistically high yield strength of the
tip to maintain a single-atom contact at a normal
load of 30 nN. Here, the difference between the
high- and low-friction force loops is attributed to
the difference in commensurability between the
flake and the substrate, the high friction corre-
sponding to a fully commensurate contact and
the low friction to an incommensurate contact.
Within the context of superlubricity it is possible
for a sliding contact to remain in the frictionless
regime also at much higher loads.
The seemingly random selection of either low or
high friction states can be explained easily by the
slow drift of the FFM or the irreproducibility of
the mounting procedure of the HOPG sample
holder after cleaving. This results in a change of
the measurement location from one grain of the
ZYH-quality polycrystalline HOPG substrate to
the next, differently oriented grain. We will return
to this point in Section 3.5.
3.3. Friction versus sample rotation
In order to obtain further evidence for our
interpretation, we rotated the graphite sample in
small steps with respect to the tip, using the U-
motor of our FFM. Because the U-motor does
not rotate perfectly concentrically around the tip,
the tip did not stay at the same location on the
sample during rotation. Therefore, we used the
single crystalline HOPG sample (ZYA-grade) to
make sure that the lattice orientation of the sample
would not change because the tip would land on a
different grain after a few rotational steps. For
each orientation, we performed a complete friction
force spectroscopy measurement for loading forces
between +25 nN and pull-off (�22 nN). We re-
corded the lateral forces in the X- and the Y-direc-
tion of the sensor and calculated the average
friction force in the sliding direction of the tip
according to Eqs. (1) and (2).
Fig. 5 shows lateral force maps and force loops
measured in the X-direction for different rotational
orientations. Note that the X- and x-direction are
204 M. Dienwiebel et al. / Surface Science 576 (2005) 197–211
not aligned here, because the scan piezo rotates to-
gether with the sample. A typical force loop is
shown in Fig. 5d, which was measured at a normal
force of 18 nN. The lateral force in Fig. 5d displays
clearly resolved atomic-scale stick-slip sliding and
the average friction force parallel to the sliding
direction is 203.3 ± 20 pN. Fig. 5b,e and c,f show
FFM measurement measured with the graphite
substrate rotated +12� and �22� with respect to
5a,d around an axis normal to the surface, and
parallel to the tip. The rotation by 12� has caused
the average friction force to reduce by more than
one order of magnitude, to 15 ± 15 pN. Rotating
22� away from the first measurement in the oppo-
site direction also has caused a reduction to
8þ16�8 pN, which is equal to zero friction within
the detection limit of our instrument. This varia-
tion of the friction force with angle U was com-
pletely reversible. Notice that the ultra-low
lateral forces in Fig. 5e and f still exhibit regular
variations with the periodicity of the graphite
substrate.
Fig. 6 displays the average friction forces mea-
sured over a 100� range of substrate rotation an-
gles. We recognize two narrow angular regions
with high friction, separated by a wide angular
interval with nearly zero friction. The distance be-
tween the two friction peaks is 61 ± 2�, which cor-
responds well with the 60� symmetry of individual
atomic layers in the graphite lattice. This result
corresponds precisely with the expectation within
the scenario of superlubricity. After every 60�
Fig. 5. Lateral force images (forward direction) and friction loops measured in the X-direction at 60� (a,d), 72� (b,e) and 38� (c,f)
rotation angle U. Normal force (a,d,c,f) FN = 18 nN; (b,e) FN = 30.1 nN. Grey scale (a) 590 pN, (b) 270 pN, (c) 265 pN. Image size
3 nm · 3 nm.
Fig. 6. Average friction force versus rotation angle U of the
graphite sample around an axis normal to the sample surface.
Two narrow peaks of high friction are observed at 0� and 61�,
respectively. Between these peaks a wide angular range with
ultra-low friction, close the detection limit of the instrument, is
found. The first peak has a maximum friction force of 306 ±
40 pN, and the second peak has a maximum of 203 ± 20 pN.
The curve through the data points shows results from a
Tomlinson model for a symmetric 96-atom graphite flake
sliding over the graphite surface (for details about the calcu-
lation see [39]).
M. Dienwiebel et al. / Surface Science 576 (2005) 197–211 205
rotation, the lattices of the substrate and the
graphite flake align and the friction is high. For
intermediate angles, the lattices are incommensu-
rate and the friction force is close to zero.
The maximum friction forces of the two peaks
were found to differ by 103 pN. This possibly re-
flects the fact that due the AB stacking, graphite
does not really possess a 60� symmetry but rather
a 120� symmetry, which should have an influence
in case the flake is more than one layer thick.
Unfortunately, we could not measure a third peak
in the present experiment, so that we have not been
able to test this hypothesis experimentally.
We can use the peak width in Fig. 6 to estimate
the flake diameter. As an illustration, a single-
atom tip should show high friction for all orienta-
tions, while an infinitely large contact would be
completely superlubric, except for infinitely nar-
row angular ranges around perfect registry, if we
assume that no energy can be dissipated via elastic
deformations within the contact. For finite-size
contacts, the cancellation of lateral forces, which
causes superlubricity, can be considered complete
when the mismatch between the two lattices adds
up to one lattice spacing over the diameter of the
contact. The mismatch condition provides us with
the estimate that tan(DU) = 1/D, where DU is the
full width at half maximum of the friction peak,
and D is the flake diameter, expressed in lattice
spacings. From the widths of the two peaks in
Fig. 6, of 5.4 ± 1.0� for the first peak and 6.5 ±
0.8� for the second, we estimate that the flake
diameter is between 7 and 12 lattice spacings.
The solid curve in Fig. 6 is the result obtained from
a modified Tomlinson model calculation in which
we moved various rigid graphite flakes, connected
to the Tribolever springs, in a rigid hexagonal po-
tential, reflecting the periodicity of the graphite
surface. More details on this calculation are pre-
sented in a recent publication by Verhoeven et al.
[39]. Shown here is the calculation for a symmetric
96-atom flake (diameter of 11 atomic spacings).
It provides an excellent fit to the experimental
friction data.
We have to mention here that reproducible
measurements, such as those in Fig. 6, in which
the same relative orientations always led to the
same friction loops, were rare, the fixed-flake situ-
ation occurring as the exception, rather than the
rule. More often, results were obtained of the type
described in the next section.
3.4. A ‘‘loose’ ’ flake
Fig. 7 shows two lateral force maps, measured
in the X-direction, before (a) and after (b) a delib-
erate, modest misalignment by less than 2� of an
initially aligned contact. While the friction force
in Fig. 7a is as high as 550 ± 21 pN (see also Fig.
7c), the friction force in the upper part of Fig. 7b
is reduced to 27 ± 16 pN (see also Fig. 7d). In
the course of a few scan lines, the friction force
gradually restored back to about 431 ± 17 pN
(Fig. 7e) and at the last scanline of Fig. 7b the fric-
tion was as high as in Fig. 7a. We interpret these
events as the effect of the torque exerted by the sur-
face on a nearly aligned flake, which was attached
to the tungsten tip sufficiently loosely to rotate
back into registry. During the restoration of the
high friction force the lateral force exhibited irreg-
ular sharp peaks, which might have been caused by
the dynamic process of reorientation of the flake.
3.5. Large-scale images on polycrystalline graphite
The effect of a change in commensurability be-
tween a flake and the surface was also observed
on the polycrystalline graphite sample. In Section
3.2 we already ascribed the switching from low fric-
tion to high friction and vice versa to the different
orientations of neighboring grains on the polycrys-
talline substrate. Fig. 8a is a large-scale topo-
graphic image of the polycrystalline grade ZYH
sample. The image shows a grain boundary that
runs across the surface. The height and lateral
dimensions of the boundary are similar to those
for grain boundaries on HOPG that have been ob-
served in STM experiments [40]. Fig. 8c shows the
lateral force image in the forward direction of the
same area. The grain in the upper right corner of
the image exhibits a significantly lower friction
force than the grain in the lower left corner. This
can be also seen from the friction loop shown in
8d, measured in the x-direction, where the friction
force on the left grain was found to be 319 ±
30 pN and on the right grain 222 ± 29 pN. Also
206 M. Dienwiebel et al. / Surface Science 576 (2005) 197–211
Fig. 8. Topography image (a) and lateral force map in the forward x-direction (c), showing a grain boundary running across the
polycrystalline HOPG surface. Graph (b) shows a cross section along the line indicated by the markers in (a). Graph (d) shows a force
loop along the line indicated by the markers in (c); Normal force FN = 5.1 nN. Image size 500 nm · 500 nm.
Fig. 7. Lateral force images (a,b) and friction force loops (c–e) before and after a modest rotation DU of less than 2� of an initially
aligned contact. The three pairs of markers at the sides of the images indicate the positions where the three force loops were taken.
Normal force (a) FN = 23 nN; (b) FN = �0.9 nN; Image size 3 nm · 3 nm.
M. Dienwiebel et al. / Surface Science 576 (2005) 197–211 207
from atomic-scale measurements (3 nm · 3 nm) we
found a change in the friction force in the sliding
direction from 326 ± 33 pN on the left grain to
221 ± 18 pN on the right grain. The height line
(8b) taken from the topographic image shows also
a change in the slope by 0.7� between the two
grains. Ruan et al. [41] have proposed a ‘‘ratchet
mechanism’’, in which the local friction coefficient
in microscale measurements should scale with the
slope h of the sample. Therefore, it might be possi-
ble that the change in friction between the two
grains was slope induced. However, the change in
the friction coefficient, expected due to the change
in slope, is only Dl = 0.05% and cannot explain
the observed large change in the friction. Again
we conclude that the change in the friction from
one grain to another is the effect of a change in com-
mensurability between a flake and the substrate.
3.6. TEM analysis of the tip
We have used high-resolution transmission elec-
tron microscopy (TEM) to image the tungsten tip
after our friction experiments. For this purpose,
we glued the central part of the force sensor with
the tip onto a holder that fitted inside the TEM
holder. The TEM analysis showed that the tung-
sten tip had a radius of about 80 nm and was cov-
ered with a smooth amorphous layer of 7 nm thick
tungsten oxide. Unfortunately, thorough TEM
inspection of the tip was not possible due to rapid
removal of the amorphous layer by the electron
beam. Before the tip was modified by the electron
beam, which occurred within minutes, it was not
possible to properly correct for astigmatism. This
is seen in Fig. 9, which displays the tip after
approximately 5 min of exposure to the electron
beam. The amorphous layer has been almost com-
pletely removed by the electron irradiation. In the
image, we find several locations that look like lay-
ered structures similar to graphite sheets (indicated
by circles). At a first glance, one might be tempted
to identify these as graphite flakes. However, at
that point of the TEM observation the tip was al-
ready strongly modified by the electron beam and,
in addition, it is possible that these features merely
appeared like layered structures due to astigma-
tism. Therefore, the present TEM analysis cannot
provide definite evidence for the presence or the
absence of either a multilayer flake or a single layer
of graphite.
3.7. Friction anisotropy
The measurements of the friction force versus
sample rotation, presented in Section 3.3, were
taken for a single sliding direction with respect to
the substrate. Miura et al. found for the sliding of
a 1 mm · 1 mm large MoS2 flake on a MoS2 sur-
face [42], as well as for a 1 mm · 1 mm large graph-
ite flake on HOPG [43], a variation in the friction
force between 0 and 2 nN as a function of sliding
Fig. 9. High-resolution TEM micrographs of the tungsten tip about 5 min after the tip was first exposed to the electron beam. The
circles show areas in which layered structures were observed that are consistent with multilayer graphite flakes. A zoom-in into one of
these regions is shown in the inset.
208 M. Dienwiebel et al. / Surface Science 576 (2005) 197–211
direction. Before we discuss friction anisotropy in
our experiment, we first clarify the terminology.
Often friction anisotropy refers to the variation in
friction as a function of the sliding direction [44],
whereas other authors use this term also for
changes in friction as a function of relative orienta-
tion, i.e. commensurability [45] (superlubricity), or
for both phenomena [42]. To avoid misunderstand-
ings, we will use the term friction anisotropy
strictly for the variation of friction with respect to
the sliding direction. In the measurements of Figs.
5–7, where we recorded the friction force as a func-
tion of the rotation angle U of the sample, the slid-
ing direction did not change with respect to the
substrate lattice because the scan piezo rotated to-
gether with the sample. This is why we can directly
rule out anisotropy as a cause for the observed
peaks. However, if a graphite/graphite contact does
exhibit high friction anisotropy, the dependence of
the friction force on the degree of incommensura-
bility might change dramatically with sliding direc-
tion. In order to investigate this, we measured the
friction force for a number of sample rotation an-
gles U as a function of the sliding direction f. We
invariably observed that the friction force FF var-
ied between high and low simultaneously, for all
sliding directions f. The friction anisotropy was
very modest (at most 25%) and did not interfere
with the commensurability effect. As an example,
Fig. 10 shows the friction force as a function of
sliding angle for a commensurate contact, with
high friction. Whereas the friction forces in the X-
and Y-directions of the sensor strongly varied as
a function of the sliding angle, the total friction
force in the sliding direction remained nearly con-
stant. In our modified Tomlinson model [39], for
a graphite flake sliding over a graphite surface, a
modest anisotropy was found for all sample rota-
tion angles U, as illustrated for the aligned contact
in Fig. 10.
4. Discussion
All measurements presented in this article were
consistent with friction between a graphite flake
and the graphite substrate. In fact, the notion that
graphite flakes adhere frequently to the tip of scan-
ning probe microscopes has originated already
many years ago in order to explain ‘‘unusual’’ con-
trast in scanning tunneling microscopy images (see
e.g. [46,47]). Although we have not been able to
convincingly observe the presence of a graphite
flake with TEM, our friction measurements pro-
vide firm evidence that a flake caused the observed
superlubricity.
A few earlier experiments provided indications
of superlubricity. Hirano et al. [45] found a modest
reduction in friction between two mica sheets from
8 · 10�4 N to 2 · 10�4 N, caused by rotating the
two sheets with respect to each other. In a
modified scanning tunnelling microscope (STM)
experiment [48] the same authors claimed the
observation of superlubricity between a tungsten
tip and a Si(001) sample. However, the evidence
provided in their paper has been rather incomplete.
No normal force was measured or controlled, and
the tip was actually only in tunnelling range from
the substrate. The friction force was measured only
for two relative orientations. No typical friction
loops were shown. Ko et al. [49] have shown that
variations in the friction coefficient caused by the
rotation of two (100) metal surfaces with respect
to each other do not necessarily have to be the re-
sult of a change in lattice mismatch.
Fig. 10. Friction as function of the sliding angle f for a
commensurate contact (U = 0).The data points show the friction
FF measured in the sliding direction. The dotted line shows
calculated friction forces, obtained using a Tomlinson model for
a symmetric, 96-atom graphite flake (for details about the
calculation see [39]).
M. Dienwiebel et al. / Surface Science 576 (2005) 197–211 209
Beyond showing the existence of superlubricity
between graphite surfaces on the nanometer scale,
which might explain the ultra-low friction coeffi-
cients as well as the large variations found in
previous FFM experiments on graphite, our obser-
vation might also have important implications for
understanding the macroscopic lubrication prop-
erties of solid lamellar lubricants.
Indications that also in a macroscopic sliding
contact of lamellar solids rotated flakes are cre-
ated, come from transmission electron microscopy
(TEM) observations by Martin et al. [50] on MoS2.
In contrast to our single-contact FFM experiment,
macroscopic-scale friction involves multiple micro-
contacts with different sizes and orientations.
Based on our observations, one may speculate that
in the case of macroscopic lubrication by graphite
a large fraction of the graphite–graphite contacts
will be in the ‘‘superlubric state’’, while only a
small fraction will be in registry. This should lead
to a tremendous reduction in the average friction
force, experienced in the ensemble of micro-con-
tacts, and thus might explain the excellent lubrica-
tion by graphite and similar, layered materials,
such as MoS2 and Ti3SiC2. It was shown by Liu
et al. [51] that under sliding conditions, a graphi-
tized tribolayer is formed on top of diamond-like
carbon (DLC) coatings, which goes hand in hand
with a decrease of the friction coefficient after
run-in. Therefore, also the excellent lubrication
properties of DLC films might be caused by super-
lubric graphitic contacts.
We suppose that for sufficiently large contacts
superlubricity might break down, as the two lat-
tices are not perfectly rigid, and a network of misfit
dislocations should form between the two. There-
fore, to give an estimate to what percentage super-
lubricity contributes to the good lubrication
properties of solid lubricants, more experiments
are needed to find out at which contact size and
normal load superlubricity breaks down and to
find out, how many of the ‘‘loose’’ flakes, which
might form the majority species in a real tribolog-
ical contact, twist back into registry. A first indica-
tion that superlubricity breaks down at higher
contact pressures might be found already in Fig.
4a, where we observed a reversible slight increase
in the friction above 40 nN normal load.
Other graphitic systems have been found that
show remarkable tribological properties, which
might also be attributed to the phenomenon of
superlubricity. TEM observations [52] suggest that
nested carbon nanotubes (CNT) possess very low
inter-wall friction. In most cases, the inner and
outer tubes in a multiwall CNT form an incom-
mensurate graphitic system, similar to a rotated
flake that slides over a graphite surface. Similarly,
Falvo et al. have found that carbon nanotubes that
are pushed sideways over HOPG when they are out
of registry, whereas they can only roll when they
are in registry with the underlying surface [53,54].
5. Conclusions
By measuring atomic-scale friction as a function
of the rotational angle between a tungsten tip and
a graphite surface we have shown that the origin of
the ultra-low friction of graphite in friction force
experiments lies in the incommensurability be-
tween a flake that is attached to the tip and the
graphite surface. The observation of two narrow
peaks in the friction force that are separated by
60� provided clear experimental evidence of super-
lubricity. The width of the two peaks allowed us to
estimate the contact diameter to be 7–12 lattice
spacings. Our conclusions are further substanti-
ated by the calculations presented in [39].
The occurrence of superlubricity in layered
materials might explain why these materials are
good solid lubricants.
Acknowledgments
This work is part of the research program of the
‘‘Stichting voor Fundamenteel Onderzoek der
Materie (FOM)’’ and was made possible by finan-
cial support from the ‘‘Nederlandse Organisatie
voor Wetenschappelijk Onderzoek (NWO)’’.
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