| THEORY & FORMULAE |
Soil samples consists of three phases: solids (soil particles), water and air. Soil properties are measured in situ in the field or in the laboratory. Typically, the measurements include wet volume, wet weight and oven-dried weight. A variety of properties can be defined or derived as shown in the inter-relationships below:
    
where
     V = total volume of wet sample
     W = total weight of wet sample
     subscripts s,w,a,v = solids, water, air, void respectively
     Vv = Vw + Va
     G = specific gravity of soil solids
     e = voids ratio
     n = porosity
     S = degree of water saturation
     m = moisture content
     a = air content
     γ = density
     γ d = dry density
     γ sat = saturated density
     γ bouyant = density when submerged in water
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EXAMPLE Of Input/Output
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