The entire wiki reimagined as a visual magazine with video discovery · Watch your interests come alive
The entire wiki reimagined as a visual magazine with video discovery · Watch your interests come alive
Rain water flux from a canopy. Among the forces that govern drop formation: surface tension by cohesion, Van der Waals force, Plateau–Rayleigh instabi
Rain water flux from a canopy. Among the forces that govern drop formation: surface tension by 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
Water drop in equilibrium of cohesion and gravity
Water drop in equilibrium of cohesion and gravity