Convection
Heat Transfer Methods

Heat Transfer Problem

Heat transfer occurs only within a solid or fluid

Heat transfer occurs between multiple, separate, layers

Heat transfer occurs within a solid and into a liquid

Heat transfer only occurs between a solid and fluid

Conduction

Conduction is the transfer of heat through collisions between atoms/molecules and the diffusion of atoms/molecules of high energy. It is mainly defined by Fourier's Law.

It can occur inside a fluid or a solid. See ME3304 S24 Lecture Note (1) Introduction for more info.

One Dimensional

For one-dimensional (x direction only), steady-state, heat diffusion we find that depends on the temperature difference across the solid, the area perpendicular to the flow - , and a material property (which we will call for now).

Thus we can calculate the heat transfer rate as the following:

Again, is a material property referred to as the thermal conductivity coefficient. The minus sign is due to heat always being transferred from hot to cold.

We can convert this to heat flux by moving the area over.

Two Dimensional

With Heat Generation

conduction

Convection

Convection is heat transfer from a solid to a liquid or vise-versa. It is driven by diffusion.

It is given by the following equation:

Where is heat flux, is the convection heat transfer coefficient and is the temperature of the fluid.

Fluid Flow

Chapter 6 reviews convection in depth, fluid flow concepts are heavily involved in this chapter.

convection

Finite Difference Analysis

Finite Difference Analysis, also known as finite-element or boundary-element, is a method of analysis that use finite values rather than the continuous ones of other methods.

It is an approximation rather than an exact result.

This method makes use of a nodal network to break a solid up into finite elements.

See the following for examples and more information:

finite-difference-analysis

Fourier's Law

Fourier's Law essentially states that heat flux is always normal to a cross sectional area of constant temperature.

See ME3304 S24 Lecture Note (1) Introduction for more information.

fouriers-law

Radiation

Covered in Chapter 12 and 13, radiation is heat transfer due to changes in election configuration, it takes the form of electromagnetic waves.

Radiation exists on electromagnetic radiation spectrum (Figure 12.3 below), a subset of this spectrum is thermal radiation which is what this course focuses on. Thermal radiation is an electromagnetic wave.

Thermal radiation is measured via four different radiation heat fluxes defined in table 12.1:

Tip

When working with radiation, Dr. Paul recommends to always convert to Kelvin.

radiation

Extended Surfaces (Fins)

Extended Surfaces or Fins are sections of an object that extend out into a fluid used for heat dissipation. They are covered in Section 3.6.

General form of energy dissipation equation for a fin (Eq. 3.66):

In the above image the cross section does not change along the length of the fin, thus the general equation can be reduced to the following (Eq. 3.67):

The following two definitions (Eq. 3.68 & 3.70):

allow us to reduce our equation (Eq. 3.69):

Now that it is in this form we can find it's general solution to be (Eq. 3.71):

We generally refer to as a temperature difference.

A derivation for a rod fin can be found in 4E - Class 2 - Fins Cont. 2024-02-13 00_10_36

Hyperbolic tribometry functions (namely ) appears frequently. This is due to it's definition:

See extended-surface-equation-table for equations related to extended surfaces.

extended-surfaces

Energy Balance

Heat Transfer lives as a subcategory of thermodynamics and is based off its ideas. Energy balance is one of thermodynamics' defining characteristics and is true for heat transfer.

Starting with the a basic energy balance about a control volume we have:

Where is the rate of energy in and is the rate of energy out.

We can develop this further by accounting for energy stored within a control-volume and energy generated by a control volume using the following equation:

See Section 1.3 of the textbook for more information.

This concept is applied to systems using conduction by the heat diffusion equation.

energy-balance

Heat Diffusion Equation

Equation 2.19 (below) is the general form of the heat diffusion equation in cartesian coordinates.

Cylindrical Coordinates (Eq. 2.26 - Pg. 65)::

Spherical Coordinates (Eq. 2.29 - Pg. 67):

heat-diffusion-equation

Thermal Circuits

In many cases heat flow can be analyzed using thermal 'circuits'. When using this approach heat transfer rate becomes current, temperature difference becomes voltage, and resistance is the material's resistance to the heat flow.

Thermal circuits are covered in chapter 3.

Resistance for conduction:

Where is heat transfer rate in the x direction, is the thermal conductivity coefficient, and is the cross-sectional area (see also Fourier's Law).

Resistance for convection:

Where is convection heat transfer coefficient and is the temperature of the fluid.

Contact Resistance

Section 3.1.4

Equation 3.20:

Thermal Capacitance

Thermal capacitance is an idea that builds upon the foundations laid down in thermal circuits. It is explained in its own page.

thermal-circuits

Problem is a function of only time (not space/location)

Lumped Capacitance Method

Lumped Capacitance really means that heat transfer is a function of time only.

- Dr. Paul

Lumped Capacitance Method is a continuation of the ideas laid down in thermal circuits. As the name suggests we now have a thermal capacitance, .

This method is an approximation and it only works is there is no temperature gradient across the object. This can be quantified by checking to make sure the biot number is much smaller than 1. See ME3304 S24 Lecture Note (2) Conduction.

Given a solid of a high temperature that is in an environment that rapidly changes temperature (for example heat treating metal) we imagine that the solid is a capacitor (or battery). As soon as our solid changes environment it will start to discharge its energy as heat.

Equation 5.4 (temperature difference):

Equation 5.5:

Where is density, is volume, is specific heat, is convection heat transfer coefficient, is cross-sectional area, and is time. The component in front of the natural log () is used frequently and is called the thermal time constant.

Equation 5.6:

Relating to thermocouple somehow.

An example of a problem using this method can be found in ME3304 Conduction Previous Test Solution.

Allows you to write energy-stored as the following?

lumped-capacitance-method

Semi Infinite Solid

A method that considers space and time.

- Dr. Paul

In contrast to lumped capacitance method which only works on problems that are a function of time, semi-infinite solid method works on problems that are a function of both location and time.

Semi-Infinite Solid is an analysis method that uses a solid that is of infinite size in all but one direction. It is used to analyze temperature of an object over time.

This method yields an analytical solution rather than an approximation, although you are still making an approximation in the fact that infinite solids do not exist. Unlike the lumped capacitance method it can be used where there is a temperature gradient across the solid we are analyzing (the biot number is not very small).

Below are example transient temperature distribution for constant surface temperature (1), constant surface heat flux (2), and surface convection (3).

Temperature distribution

The derivation for the following equations (and what the error function is and where it came from) can be found in 7A - 2nd Class.

Equation 5.60:

Where is the similarity variable, is the gaussian error function. Under various conditions equation 5.60 reduces to the following equations.

Case 1 Constant Surface Temperature (Eq. 5.61):

Case 2 Constant Surface Heat Flux (Eq. 5.62):

Case 3 Surface Convection (Eq. 5.63):

Python

Equation 5.63 (Case 3 above):

def caseThree(T, Ti, Too, x, alpha, t, h, k):
  coeffOne = erfc(x/(2*sqrt(alpha * t)))
  coeffTwo = exp(((h*x)/k) + ((h**2 * alpha*t)/k**2))
  coeffThr = erfc((x/2*sqrt(alpha*t)) + ((h*sqrt(alpha*t))/k))
  coeffFou = (T-Ti)/(Too-Ti)

  return coeffOne - coeffTwo * coeffThr - coeffFou
semi-infinite-solid

Problem is a function of both time and space (location)

Internal Flow

Chapter 8

Internal fluid flow is fluid flow that occurs within a pipe or other container.

If the flow is laminar (ie. in the fully developed region) the velocity profile is parabolic. See entry-region for how to calculate the distance at which the fully developed region starts.

When dealing with turbulent flow it becomes extremely difficult to find the temperature gradient so instead we use the mean temperature (or mixed bulk temperature).

For internal flow the characteristic length is known has hydraulic diameter.

Mass Flow Rate (Equation 8.5):

Where is density, is velocity, and is cross-sectional area.

See Chapter 8 and ME3304 S24 Lecture Note (3) Convection for more info.

Energy Balance

Section 8.3

As the flow in completely enclosed, an energy balance can be used to find the mean temperature.

Equation (8.34):

Constant Surface Heat Flux

Covered in Section 8.3.2, analyzing internal flow with constant heat flux is greatly simplified as heat flux becomes independent of location. Equation 8.38 gives convection heat transfer rate:

As shown in 7C - 1st Class and section 8.3.2 we can derive an expression for temperature as a function of location (Equation 8.49):

Idk what Figure 8.7 is, its just "very important" or smth

Constant Surface Temperature

Covered in Section 8.3.3, another simplification we can take advantage of is when there is a constant surface temperature.

Equation 8.41b:

Equation 8.42:

Equation 8.45:

internal-flow

Convection heat transfer coefficient is not known

ngl, that sucks

External Flow

external-flow

Cylinder in Cross Flow

Section 7.4

The Hilpert Correlation (Equation 7.52):

Constants and are listed in table-7.2. Constants for non-cylindrical geometries can be found in table-7.3.

Diameter is used as the characteristic length.

cylinder-in-cross-flow

Flow around a Sphere

Section 7.5

Stokes' Law (Equation 7.55):

Equation 7.56:

Equation 7.57:

flow-around-a-sphere

Flow Across Banks of Tubes

Section 7.6

flow-across-banks-of-tubes

Impinging Jets

Section 7.7

impinging-jets

Flat Plate in Parallel Flow

Section 7.2 covers a the convection associated with an isothermal flat plate exposed to flow on one side as shown in the below image.

Using the similarity transformation on the boundary layer equations, the following equations for continuity, momentum, and energy can be found:

Continuity (Eq. 7.4):

Momentum (Eq. 7.5):

Energy (Eq. 7.6):

See ME3304 S24 Lecture Note (3) Convection and Example 7.1 for more information.

Laminar Flow over an Isothermal Plate

Section 7.2.1

Equation 7.29:

Equation 7.30 (temperature):

Equation 7.31 (mass):

Turbulent Flow over an Isothermal Plate

Section 7.2.2

Equation 7.34:

Where is the friction coefficient and is the Reynolds number.

Velocity boundary layer thickness (Equation 7.35):

Equation 7.36 (temperature):

Where is the Nusselt number, is the Stanton number, and is the Prandtl number.

Equation 7.37 (mass):

Where is the Sherwood number, is the Stanton number, and is the Schmidt number.

Mixed Boundary Layer Conditions

Section 7.2.3

Equation 7.38:

Where is the Nusselt number and is the Prandtl number.

Equation 7.40:

Where is the friction coefficient.

Equation 7.41:

Where is the Sherwood number and is the Schmidt number.

Other conditions

Section 7.2.4 covers a unheated starting length
Section 7.2.5 covers Flat Plates with Constant Heat Flux

flat-plate-in-parallel-flow