Journal
JOURNAL OF PHYSICAL CHEMISTRY B
Volume 105, Issue 22, Pages 5353-5357Publisher
AMER CHEMICAL SOC
DOI: 10.1021/jp004505n
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The self-motion of a camphor grain was investigated on a linear water route. The oscillatory motion along the water route was maintained for ca. 15 cycles. The driving force is discussed in relation to a rhythmic change in the surface tension, which depends on the surface concentration of the camphor layer. The essential features of the self-motion were reproduced by a numerical calculation in relation to the spatial distribution of the camphor layer at the air-water interface.
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