Void ratio refers to the size of voids to the volume of solids. It is indicated
It is expressed as a decimal.
It is the ratio of volume of voids to the total volume. It is indicated by ‘n’
It is usually expressed as a percentage.
1/n= 1+ (1/e) = (1+e)/e
n=e/ (1+e) (a)
1/e= (1/n)-1= (1-n)/n
e=n/ (1-n) (b)
In equations (a) and (b), the porosity should be expressed as a ratio and not percentage.
Degree of saturation
The degree of saturation is the quotient of the volume of water to the volume of voids. It is indicated by ‘S’.
The degree of saturation is normally expressed as a percentage. It is equal to zero when the soil is absolutely dry and 100% when the soil is fully immersed.
Percentage air voids
It is the ratio of volume of air to the total volume.
It is also expressed as a percentage.
Air content is the ratio of the volume of air to the volume of voids
na= n ac
The water content (w) is the quotient of the mass of water to the mass of soilids
It is also known as the moisture content (m). It is articulated as a percentage but used as a decimal in computation.
- BULK MASS DENSITY
The bulk mass density (ρ) is known as the total mass (M) per unit volume (V)
- DRY MASS DENSITY
The dry mass density (ρd) is known as the mass of solids per unit total volume
- SATURATED MASS DENSITY
The saturated mass density (ρsat) refers to the bulk density of the soil when it is fully immersed.
- SUBMERGED MASS DENSITY
When the soil is located under the water, it is known as submerged condition. The submerged mass density (ρ’) of the soil is known as the submerged mass per unit total volume.
- MASS DENSITY OF SOLIDS
The mass density of solids (ρs) is equivalent to quotient of the mass of solids to volume of solids
- BULK UNIT WEIGHT (γ)= W/V
- DRY UNIT WEIGHT (γd)= Ws/V
- SATURATED UNIT WEIGHT (γsat) = Wsat/V
- SUBMERGED UNIT WEIGHT (γsubor γ’) = Wsub/V
- UNIT WEIGHT OF SOIL SOLIDS (γs) = Ws/Vs
PARTICULAR GRAVITY OF SOLIDS
The particular gravity of soil particles (G) is defined as the ratio of weight of a given volume of solids to mass of an equivalent volume of water at 4° C.
G = ρs/ρw
The mass density of water ρw at 4°C is 1gm/ml, 1000 kg/m3 or 1 Mg/m3
|Sl No||Relationship in mass density||Relationship in unit weight|
|1||n = e/(1+e)||n = e/(1+e)|
|2||e = n/(1-n)||e = n/(1-n)|
|3||na = n ac||na = n ac|
|4||ρ= (G+Se)ρw/(1+e)||γ= (G+Se) γ w/(1+e)|
|5||ρd = Gρw/(1+e)||γd = G γ w/(1+e)|
|6||ρsat = (G+e)ρw/(1+e)||γsat = (G+e) γ w/(1+e)|
|7||ρ’ = (G-1)ρw/(1+e)||γ’ = (G-1) γ w/(1+e)|
|8||e = wG/s||e = wG/s|
|9||ρd = ρ/(1+w)||γd = γ/(1+w)|
|10||ρd = (1-na)G ρw/(1+wG)||γd = (1-na)G γ w/(1+wG)|