Porosity and
Water Content of Soil
Porosity - volume of voids divided by total volume
n = Vv/VVoid Ratio - volume of voids divided by volume of solidswhere Vv = volume of void space
V = volume of sample
e = Vv/VsGravimetric Water Content - ratio of weight of water to weight of solid grainswhere Vs = volume of solids
Note:
V = Vv + Vs
Volumetric Water Content - volume of water divided by total volume![]()
where Ww = mass of water in soil
Ws = mass of solid particles
Saturation Ratio - volume of water divided by volume of voids![]()
where Vw = volume of water
Rs = Vw/VvDry Bulk Density - weight of solids divided by total volume
Particle Density - weight of
solids divided by volume of soilds
Capillary Forces
Attraction (surface tension) between
liquid and solid causes fluid to be pulled upward against gravity. How
high the fluid rises depends on pore throat radius
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