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The governing heat equation is derived from an energy balance applied to a differential control volume and Fourier's Law. It includes all possible mechanisms that can contribute to heat transfer in a system, and encapsulates the combined effects of energy storage, conduction, convection, and internal heat generation, and allows the prediction of the temperature profile within the system.
The governing heat equation can be written in Cartesian or radial coordinates. While heat transfer can occur in three dimensions, it is simplified here to be solved with heat flowing only in one direction (x,r).
In practice, many problems involve simplifying assumptions (e.g., system at steady state, no bulk flow in the system, or no internal heat generation), which allow certain terms to be removed. The meaning of each term and the conditions under which it should be retained or dropped are summarized below.
Governing Equation Simplifications
| Term | What is it? | When do I keep it? | When can I drop it? |
|---|---|---|---|
| \( \frac{\partial T}{\partial t} \) | Stored energy | Unsteady state, T changing with time (transient) | Steady state (constant T) |
| \( u\frac{\partial T}{\partial x} \) | Bulk flow (Convection) | Fluid flow | No flow (solid) |
| \( \frac{k}{\rho c_p} \frac{\partial ^2 T}{\partial x^2} \) | Conduction | Almost always | No conduction (no temperature gradient) |
| \( \frac{Q}{\rho c_p} \) | Generation | Conversion of energy in the system | No generation/heat source |
To obtain a particular solution, we must solve the general governing equation utilizing known quantities called boundary conditions (which describe heat transfer at particular surfaces and interfaces) as well as initial conditions (for unsteady state or time-dependent problems).
Temperature at the surface can be specified as a constant or a function of time.
Heat flux at the surface is specified as a constant or a function of time. There are two special cases for this boundary condition:
When there is liquid at the surface, the flow of heat due to conduction can be set equal to the flow due to convection. There is one special case for this boundary condition: