Difference between revisions of "Heat transfer module - Fluid Dynamics 2019"

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(Applied Examples of Heat Transfer)
(Applied Examples of Heat Transfer)
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When you flip on the light in a lava lamp, heat from the bulb works slowly to warm up the wax (or ‘lava’). This kind of heat transfer is called conduction, or movement of heat from one place to another. Heat energy flows from high heat (light bulb) to low heat (wax), and the gradient is the driver of conductive heat transfer.  
 
When you flip on the light in a lava lamp, heat from the bulb works slowly to warm up the wax (or ‘lava’). This kind of heat transfer is called conduction, or movement of heat from one place to another. Heat energy flows from high heat (light bulb) to low heat (wax), and the gradient is the driver of conductive heat transfer.  
  
[[File:lava1.png|200px|Image: 200 pixels]] [[File:lava2.png|200px|Image: 200 pixels]] [[File:lava3.png|190px|Image: 190 pixels]]  
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[[File:lava1.png|200px|Image: 200 pixels]] [[File:lava2.png|200px|Image: 200 pixels]] [[File:lava3.png|185px|Image: 185 pixels]]  
  
 
Until things start moving, conduction is the dominant heat transfer process in our lava lamp system.
 
Until things start moving, conduction is the dominant heat transfer process in our lava lamp system.
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The density of the wax is inversely related to temperature, meaning that at higher temperatures, the wax is less dense. When the density becomes lower than the density of the liquid in the lava lamp, the wax will tend to float upward.  
 
The density of the wax is inversely related to temperature, meaning that at higher temperatures, the wax is less dense. When the density becomes lower than the density of the liquid in the lava lamp, the wax will tend to float upward.  
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 +
[[File:lava4.png|200px|Image: 200 pixels]] [[File:lava6.png|190px|Image: 190 pixels]]
  
 
Wax reaches critical density (less than liquid) and tends to float upward. That movement of wax introduces velocity into the system--advection.
 
Wax reaches critical density (less than liquid) and tends to float upward. That movement of wax introduces velocity into the system--advection.
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With the movement of wax in the upward direction away from the heat source at the bottom of the container and into a cooler material the wax density increases again (more than liquid). This wax density increase causes the wax to sink back down to the bottom of the container towards the heat source. This process is called convection.
 
With the movement of wax in the upward direction away from the heat source at the bottom of the container and into a cooler material the wax density increases again (more than liquid). This wax density increase causes the wax to sink back down to the bottom of the container towards the heat source. This process is called convection.
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[[File:lava5.png|200px|Image: 210 pixels]]
  
 
*'''Convection''' depends on driving forces and resisting forces.  
 
*'''Convection''' depends on driving forces and resisting forces.  

Revision as of 01:54, 11 March 2019

Basic Equations to Know

Heat Transfer Equation:

Describes how heat changes through time

 ∂T/∂t = κ∇²T + v∇T + A
 ∂T/∂t = conduction + advection + production


Peclét Number:

Dimensionless number which indicates whether conduction or advection dominates the system

 Pe = uL/κ

where u = flow velocity, L = characteristic length Height of lava lamp, κ = thermal diffusivity

  • Low peclet regime- dominated by heat transport by conduction
  • High peclet regime- dominated by heat transport by advection


Rayleigh Number:

Dimensionless number used to describe whether convection grows or decays

 Ra ≡ (gρΔTαd³)/μκ
  • g = acceleration due to gravity
  • ρ = density
  • κ = thermal diffusivity
  • ΔT = the temperature difference between the bottom and top of the convection cell
  • α = the volume coefficient of thermal expansion
  • d = the height of the convection cell
  • μ = viscosity
  • κ = thermal diffusivity
  • When numerator terms are dominant convection grows
  • When denominator terms are dominant convection decays

Where at some critical Rayleigh (Racr) number (dependent on the system), the convection regime shifts

Applied Examples of Heat Transfer

HEAT TRANSFER IN A LAVA LAMP

Description

When you flip on the light in a lava lamp, heat from the bulb works slowly to warm up the wax (or ‘lava’). This kind of heat transfer is called conduction, or movement of heat from one place to another. Heat energy flows from high heat (light bulb) to low heat (wax), and the gradient is the driver of conductive heat transfer.

Image: 200 pixels Image: 200 pixels Image: 185 pixels

Until things start moving, conduction is the dominant heat transfer process in our lava lamp system.

  • Conduction depends on:
    • thermal diffusivity of the material through which heat is moving
    • thermal gradient

The density of the wax is inversely related to temperature, meaning that at higher temperatures, the wax is less dense. When the density becomes lower than the density of the liquid in the lava lamp, the wax will tend to float upward.

Image: 200 pixels Image: 190 pixels

Wax reaches critical density (less than liquid) and tends to float upward. That movement of wax introduces velocity into the system--advection.

  • Advection depends on:
    • velocity of the fluid
    • thermal gradient

With the movement of wax in the upward direction away from the heat source at the bottom of the container and into a cooler material the wax density increases again (more than liquid). This wax density increase causes the wax to sink back down to the bottom of the container towards the heat source. This process is called convection.

Image: 210 pixels

  • Convection depends on driving forces and resisting forces.
    • Driving forces:
      • Acceleration due to gravity (g)
      • Density (ρ)
      • The temperature difference between the bottom and top of the convection cell (ΔT)
      • The volume coefficient of thermal expansion (α)
      • The height of the convection cell (d)
    • Resisting forces:
      • Viscosity (μ)
      • Thermal diffusivity (κ)


HEAT TRANSFER IN ICE STREAM SHUTDOWN AND START (based on Joughin and Alley, 2011)

Stop and start of ice streams is dependent on:

  • Thinning (steepens basal temperature gradients)
  • Basal freezing (puts on the brakes for a system)
  • Thickening (build up traps geothermal heat)
  • Ice stream activation & the cycle is repeated

See video below to walk through the steps of ice stream shut-down and speed-up.