Question:

The Grashof number is the ratio of

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In natural convection, the Grashof number is crucial for determining the flow behavior, especially for buoyancy-driven flows.
Updated On: Jul 6, 2026
  • thermal diffusivity and mass diffusivity
  • inertial force and surface tension force
  • sensible heat and latent heat
  • buoyancy force and viscous force
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The Correct Option is D

Approach Solution - 1

Step 1: Understanding the Grashof number.
The Grashof number (Gr) is used in fluid dynamics and heat transfer to characterize the ratio of buoyancy forces to viscous forces in a fluid. It is an important dimensionless number in natural convection and helps determine the flow regime (laminar or turbulent). It is defined as: \[ Gr = \frac{g \beta \Delta T L^3}{\nu^2} \] Where: - \( g \) is the acceleration due to gravity
- \( \beta \) is the thermal expansion coefficient
- \( \Delta T \) is the temperature difference
- \( L \) is the characteristic length
- \( \nu \) is the kinematic viscosity
Step 2: Conclusion.
The Grashof number compares buoyancy forces (due to temperature difference) and viscous forces. Thus, the correct answer is (4).
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Approach Solution -2

The Grashof number is a dimensionless group used in natural (free) convection heat transfer to compare the relative importance of two competing forces acting on a fluid parcel near a heated or cooled surface. Let's check each option against its actual definition, \( Gr = \dfrac{g \beta \Delta T L^3}{\nu^2} \).

  1. Thermal diffusivity and mass diffusivity: A ratio of these two quantities is actually the Lewis number, not the Grashof number.
  2. Inertial force and surface tension force: This ratio describes the Weber number, used in droplet or bubble formation, not natural convection.
  3. Sensible heat and latent heat: This kind of ratio appears in phase-change heat transfer problems (like the Jakob number), not in the Grashof number's definition.
  4. Buoyancy force and viscous force: The numerator \( g \beta \Delta T L^3 \) in the Grashof number represents the buoyancy force driving fluid motion due to density differences from temperature variation, while \( \nu^2 \) in the denominator represents the retarding effect of viscous forces, exactly matching the Grashof number's physical meaning.

The Grashof number is specifically the ratio that quantifies buoyancy-driven motion against viscous resistance in natural convection.

Therefore, the correct answer is buoyancy force and viscous force.

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