Titlebook: Surface Forces and Surfactant Systems; Conference proceedings 1987 Springer-Verlag Berlin Heidelberg 1987 Migration.aerosol.protein.surfa

决定性

E. Kiss,C. -G. Gölander,J. C. Erikssonave approach and the pattern of shoreline curvature (Lewis, 1937). The empirical nature of this assessment was critically received however, and geomorphologists during the following hundred years or so, e.g. Gulliver (1899) and Wheeler (1902), promoted longshore currents for the formation of curved

jarring

Hla461

Solutions of alkali soaps and water in fatty acids VI. Studies of the refractive index and light sccordance with previously presented studies they show that one, with respect to the role of water, has two main regions, one extending from the water-free phase up to a content of water of about 40% and the other at water contents above about 55%. An intermediate transition region lies between about

钩针织物

jealousy

chronicle

Experimental evidence for repulsive and attractive forces not accounted for by conventional DLVO thticular, experimentally observed attractive and repulsive deviations from force curves, calculated from conventional DLVO theory, are discussed. Such “additional” forces are present in most systems. Even in cases where the measured interaction appears to be well described by conventional DLVO theory

老巫婆

连锁

COLON

Dynamics of wetting on smooth and rough surfaces,recently proposed scaling laws (.. for capillarity driven and .. for gravity driven spreading) when the surface was smooth. However, the crossover between these regimes was not observed at a constant value of the radius. Rough surfaces exhibited at least four spreading regimes which could be rationa

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