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Percentage air voids (na) is defined as
VvтАЛVaтАЛтАЛ
VsтАЛVaтАЛтАЛ
VwтАЛVaтАЛтАЛ
VVaтАЛтАЛ
VVaтАЛтАЛ
Percentage air voids (naтАЛ) is defined as the ratio of the volume of air voids (VaтАЛ) to the total volume (V) of the given soil mass. It represents the proportion of the total volume occupied by air, which is a critical index property for understanding soil compaction and permeability.
Percentage air voids (naтАЛ) is defined as the ratio of the volume of air voids (VaтАЛ) to the total volume (V) of the given soil mass. It represents the proportion of the total volume occupied by air, which is a critical index property for understanding soil compaction and permeability.
naтАЛ=VVaтАЛтАЛ├Ч100 тАФ Expression for percentage air voids
naтАЛ=n├ЧSaтАЛ тАФ Relationship where n is porosity and SaтАЛ is air content
In a soil mass, the total volume V is the sum of volume of solids (VsтАЛ), volume of water (VwтАЛ), and volume of air (VaтАЛ). The percentage air voids naтАЛ measures the air-filled space relative to the entire soil structure, providing insight into the degree of aeration within the soil matrix.
It is always expressed as a percentage.
Unlike porosity (n=VvтАЛ/V), which considers all voids, naтАЛ focuses specifically on the air-filled portion.
It is a vital parameter in soil compaction control in engineering projects.
Helps in determining the efficiency of soil compaction.
Useful for calculating the degree of saturation.
Earthwork construction and embankment stability.
Analysis of soil permeability in geotechnical engineering.
Note that naтАЛ=n(1тИТSrтАЛ), where SrтАЛ is the degree of saturation.
Option A (VaтАЛ/VvтАЛ) defines the air content (AcтАЛ or SaтАЛ), not the percentage air voids (naтАЛ).
D is correct тАФ The percentage air voids (naтАЛ) is defined as the ratio of the volume of air voids (VaтАЛ) to the total volume of the soil mass (V).
Remember the difference between Air Content (AcтАЛ=VaтАЛ/VvтАЛ) and Percentage Air Voids (naтАЛ=VaтАЛ/V). Confusing these is a very common error in competitive examinations.