Join 60,000+ competitive exam aspirants
What is the relationship between permeability and viscosity of water?
Directly proportional
Inversely proportional
Both are equal
None of the mentioned
Inversely proportional
Permeability (k) in soil is inversely proportional to the dynamic viscosity (╬╝) of the permeating fluid. According to Darcy's Law and Kozeny-Carman equations, as the viscosity of water increases (usually due to a decrease in temperature), the resistance to flow increases, resulting in a lower coefficient of permeability.
Permeability (k) in soil is inversely proportional to the dynamic viscosity (╬╝) of the permeating fluid. According to Darcy's Law and Kozeny-Carman equations, as the viscosity of water increases (usually due to a decrease in temperature), the resistance to flow increases, resulting in a lower coefficient of permeability.
k=KiтАЛтЛЕ╬╝╬│тАЛ тАФ Darcy's hydraulic conductivity formula
kтИЭ╬╝1тАЛ тАФ Inverse relationship between permeability and viscosity
Permeability is defined as the ability of soil to allow fluid to flow through its pores. The intrinsic permeability (KiтАЛ) is a property of the soil structure, while the hydraulic conductivity (k) depends on both the medium and the fluid. The relationship is expressed as k=KiтАЛтЛЕ╬╝╬│тАЛ, where ╬│ is the unit weight of fluid and ╬╝ is dynamic viscosity. Thus, for a fixed medium, kтИЭ╬╝1тАЛ.
Permeability is highly sensitive to temperature because water viscosity decreases as temperature increases.
As temperature increases, water becomes less viscous, leading to higher permeability.
Intrinsic permeability (KiтАЛ) is purely a function of soil pore geometry (size and distribution of voids).
Darcy's Law assumes laminar flow, which is sensitive to fluid viscosity.
Accurate prediction of seepage rates in dams and embankments.
Better understanding of ground water flow behavior under varying climate conditions.
Does not account for non-laminar flow conditions.
Requires precise measurement of fluid temperature for accurate analysis.
Dewatering of construction sites.
Designing seepage control measures for earthen dams.
Groundwater hydrology studies.
The viscosity of water is approximately 0.001┬аPaтЛЕs at 20┬░C.
Option A is incorrect because permeability decreases as viscosity increases, confirming an inverse relationship rather than a direct one.
B is correct тАФ Permeability is inversely proportional to the viscosity of water, meaning that as the fluid becomes more viscous, its flow through the soil pores is restricted.
Always remember that in soil mechanics, an increase in temperature lowers water viscosity, which in turn causes an increase in the measured coefficient of permeability (k).