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13
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0002000240
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We neglect higher harmonics of the drive frequency as caused by cantilever buckling
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We neglect higher harmonics of the drive frequency as caused by cantilever buckling [G. Y. Chen, R. J. Warmack, P. I. Oden, and T. Thundat, J. Vac. Sci. Technol. B 14, 1313 (1996)]. We also require that the cantilever follows the surface well. This requires a low quality factor such that the time constant for changes in amplitude is short. While this is a severe constraint on tapping in air, in our case it is easily satisfied due to the damping of liquid.
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21544459866
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Digital Instruments, Santa Barbara, CA93117
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Nanoscope IIIa Multimode, Digital Instruments, Santa Barbara, CA93117.
-
Nanoscope IIIa Multimode
-
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22
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21544440118
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Model SR 560, Stanford Research Systems Inc., Sunnyvale, CA94089
-
Model SR 560, Stanford Research Systems Inc., Sunnyvale, CA94089.
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-
-
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23
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21544434611
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Model 3202, Krohn-Hite, Avon, MA02322
-
Model 3202, Krohn-Hite, Avon, MA02322.
-
-
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24
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21544444699
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Model 113, EG&G PARC, Princeton, NJ08543
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Model 113, EG&G PARC, Princeton, NJ08543.
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25
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21544454941
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-
Brasilia, DF, Brazil
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P&S Calcite Export, Brasilia, DF, Brazil.
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P&S Calcite Export
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27
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0031042587
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Hansma, P.K.7
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31
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21544462280
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Although it is possible to slow down the step kinetics by reducing the supersaturation, at low supersaturations surface defects in the calcite substrate cause typically straight steps to become corrugated or pinned. To create straight and continuous steps, higher supersaturations are needed, which, in turn, result in increased step velocities
-
Although it is possible to slow down the step kinetics by reducing the supersaturation, at low supersaturations surface defects in the calcite substrate cause typically straight steps to become corrugated or pinned. To create straight and continuous steps, higher supersaturations are needed, which, in turn, result in increased step velocities.
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32
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21544440893
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eq) was calculated to be 0.57±0.03 under these conditions using data from the Geochemists' Workbench personal communication
-
eq) was calculated to be 0.57±0.03 under these conditions using data from the Geochemists' Workbench (C. Orme, personal communication).
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Orme, C.1
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33
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21544466702
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National Institutes of Health
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W. Rasband, National Institutes of Health, http://rsb.info.nih.gov/NIH-IMAGE.
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Rasband, W.1
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Zaitseva, N.P.7
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