Tilted S-O bonds on a CaSO4(100) surface exhibit asymmetry under frictional
force microscopic observation. The detection mechanism of the directional
bonds was explained as being an interaction between the probe surface and a
n array of tilted mass-spring systems at the sample surface. When the scan
speed of the probe was changed in the range of 5-91 mu m/s under 40% relati
ve humidity, the asymmetric component of friction increased linearly with t
he speed, while the total friction signal remained constant at speeds highe
r than 25 mu m/s. A higher scan speed is more suitable fur the detection of
the tilted bonds. At lower scan speeds, the total friction signal decrease
d in intensity and the asymmetry signal became unstable. This is due to the
condensation of water beneath the tip, A similar experiment under 60-65% r
elative humidity yielded much smaller signals for both the total friction a
nd the asymmetry component.