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Sow-Hsin Chen
Sow-Hsin Chen
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Rain water flux from a canopy. Among the forces that govern drop formation: surface tension, cohesion, Van der Waals force, Plateau–Rayleigh instabili
Rain water flux from a canopy. Among the forces that govern drop formation: surface tension, cohesion, Van der Waals force, Plateau–Rayleigh instability.
Water droplet lying on a damask. Surface tension is high enough to prevent seeping through the textile
Water droplet lying on a damask. Surface tension is high enough to prevent seeping through the textile
A. Water beading on a leaf
A. Water beading on a leaf
C. Water striders stay at the top of liquid because of surface tension
C. Water striders stay at the top of liquid because of surface tension