CAPILLARY RISE ON SURFACE OF EARTH
INTRODUCTION
Capillarity
or capillary action is the ability of a liquid to flow in narrow spaces without
the assistance of external forces. When a capillary tube is inserted into a
beaker containing liquid, the level of liquid in the capillary tend to rise or
fall depending on the angle of contact between liquid and the tube wall. We
intend to study only the rise of liquid in a capillary tube. Since the liquid
rises against gravity, the extent to which it can rise also directly depends on
the local acceleration due to gravity. We thus intend to determine the extent
of capillary rise by a liquid on the surface of Earth.
ASSUMPTIONS
1. The
local acceleration due to gravity is constant and not varying continuously
2. The
angle of contact is always acute
3. The
liquid is free from impurities
4. Temperature
of the liquid is constant
CALCULATION
Consider
a liquid [pure water] of density ‘ρ’ in a glass beaker with an inverted glass capillary
tube inserted in a beaker as shown in figure.1. Let ‘r’ be the radius of the
capillary tube, ‘θ’ be the angle of contact between pure water and the wall of
capillary tube and ‘T’ be the surface tension of water.
Fig .1 Capillary rise |
The equation for capillary rise ‘h’ in the tube is given by,
h
– Capillary rise in the tube (m)
T
– Surface tension of water [T = 7.28*10-2 N/m]
θ
– Angle of contact between pure water and glass tube [θ = 0°]
ρ
– Density of water [ρ = 1000 Kg/m3]
r
– Radius of capillary tube [r = 1.5 *10-3 m]
g
– Acceleration due to gravity on Earth [g = 9.8 m/s2]
Substituting
the constants in equation (1),
Hence
the capillary rise for the given configuration is 9.9mm
CONCLUSION
We
thus determined the capillary rise of water on the surface of Earth. It is
interesting to note that the capillary rise does not depend on the length of
the capillary tube.
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