Wetting
of solid surfaces occurs when the intervening air film
between a water droplet and a solid surface ruptures. Although this
rupturing phenomenon is well known, the underlying mechanism has not
yet been well understood. In this work, the rupture of intervening
air films is systematically studied by measuring the spatiotemporal
thickness profiles of the air films between droplets of deionized
water and flat solid surfaces using a synchronized triwavelength reflection
interferometry microscope. It has been shown that the critical rupture
thickness of the air film (hc) depends
on the surface hydrophobicity of solid surfaces. The hc value was increased from 50 nm on a hydrophobic surface
having an equilibrium water contact angle (θw) of
96° to 1.42 μm on a hydrophilic surface having a θw of 25°. In addition, an increase in the critical rupture
thickness with decreasing surface hydrophobicity was found to be applicable
not only to chemically treated quartz surfaces but also to a variety
of natural mineral surfaces. By determining the pressure within the
air films, we have shown that a strong attractive force is present
between water droplets and hydrophilic surfaces, thereby accelerating
the draining of air films. The measured forces might be of electrostatic
origin, and the forces become less attractive with increasing hydrophobicity
of solid surfaces. The present result provides a fundamental insight
into the rupture of air films from the perspective of surface forces.