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CivilSoil Mechanics
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What is the relationship between permeability and viscosity of water?

A

Directly proportional

B

Inversely proportional

C

Both are equal

D

None of the mentioned

Correct Answer

тЪЩя╕П TE тАв Technical Concept & PrincipleCivilSoil Mechanics
Option B

Inversely proportional

Quick Summary:

Permeability (kkk) in soil is inversely proportional to the dynamic viscosity (╬╝\mu╬╝) 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.

тЪЩя╕ПTETechnical SolutionConcept & Principle
ЁЯТб Explanation

Permeability (kkk) in soil is inversely proportional to the dynamic viscosity (╬╝\mu╬╝) 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.

ЁЯФв Key Formulas

k=KiтЛЕ╬│╬╝k = K_i \cdot \frac{\gamma}{\mu}k=KiтАЛтЛЕ╬╝╬│тАЛ тАФ Darcy's hydraulic conductivity formula

kтИЭ1╬╝k \propto \frac{1}{\mu}kтИЭ╬╝1тАЛ тАФ Inverse relationship between permeability and viscosity

тЪЩя╕П Working Principle

Permeability is defined as the ability of soil to allow fluid to flow through its pores. The intrinsic permeability (KiK_iKiтАЛ) is a property of the soil structure, while the hydraulic conductivity (kkk) depends on both the medium and the fluid. The relationship is expressed as k=KiтЛЕ╬│╬╝k = K_i \cdot \frac{\gamma}{\mu}k=KiтАЛтЛЕ╬╝╬│тАЛ, where ╬│\gamma╬│ is the unit weight of fluid and ╬╝\mu╬╝ is dynamic viscosity. Thus, for a fixed medium, kтИЭ1╬╝k \propto \frac{1}{\mu}kтИЭ╬╝1тАЛ.

ЁЯУМ Key Points
  • тЦ╕

    Permeability is highly sensitive to temperature because water viscosity decreases as temperature increases.

  • тЦ╕

    As temperature increases, water becomes less viscous, leading to higher permeability.

  • тЦ╕

    Intrinsic permeability (KiK_iKiтАЛ) is purely a function of soil pore geometry (size and distribution of voids).

  • тЦ╕

    Darcy's Law assumes laminar flow, which is sensitive to fluid viscosity.

тЬЕ Advantages
  • тЦ╕

    Accurate prediction of seepage rates in dams and embankments.

  • тЦ╕

    Better understanding of ground water flow behavior under varying climate conditions.

тЭМ Disadvantages / Limitations
  • тЦ╕

    Does not account for non-laminar flow conditions.

  • тЦ╕

    Requires precise measurement of fluid temperature for accurate analysis.

ЁЯЫая╕П Applications / Uses
  • тЦ╕

    Dewatering of construction sites.

  • тЦ╕

    Designing seepage control measures for earthen dams.

  • тЦ╕

    Groundwater hydrology studies.

ЁЯУД Additional Information
  • тЦ╕

    The viscosity of water is approximately 0.001┬аPaтЛЕs0.001 \text{ Pa}\cdot\text{s}0.001┬аPaтЛЕs at 20┬░C20┬░\text{C}20┬░C.

  • тЦ╕

    Option A is incorrect because permeability decreases as viscosity increases, confirming an inverse relationship rather than a direct one.

ЁЯУК Diagram / Illustration
Permeability Relationshipk = Kс╡в (╬│ / ╬╝)As ╬╝ increases, k decreasesRelationship: Inversely Proportional
тЬЕ

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.

Core Concepts Used
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Darcy's Law Hydraulic Conductivity Fluid Dynamics in Porous Media
ЁЯТб EXAM TIP

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 (kkk).

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