Capillary Action

Earth
Moon

Readout

γ surface tension—
ρ density—
θ contact angle—
r tube radius—
g gravity—
h rise (Jurin)—
verify 2γcosθ/ρgr—
Jurin's law: h = 2γ·cosθ / (ρ·g·r). Surface tension pulls a wetting liquid (θ<90°) up the tube; a non-wetting liquid like mercury (θ>90°) is pushed down. Rise scales as 1/r — halve the radius and the column doubles.