$$ T_{m,n,k}^i $$
We sum up heat transfer to/from volume element:
$$ \small \left( \begin{array}{ccc} \text{Sum of heat}\\ \text{transfer rate}\\ \text{across surfaces}\\ \text{of volume element} \end{array} \right) + \left( \begin{array}{ccc} \text{Rate of heat}\\ \text{generation}\\ \text{inside the}\\ \text{element} \end{array} \right) = \left( \begin{array}{ccc} \text{Rate of change}\\ \text{of the energy}\\ \text{content of}\\ \text{the element} \end{array} \right) $$
$$ \small \sum_\text{all surfaces} \dot{Q} + \dot{G}_\text{element} = \frac{\Delta E_\text{element}}{\Delta t} $$
$$ \small \sum_\text{all surfaces} \dot{Q} + \dot{G}_\text{element} = m c_p \frac{\Delta T_\text{element}}{\Delta t} $$
$$ \small \sum_\text{all surfaces} \dot{Q} + \dot{G}_\text{element} = V_\text{element} \rho c_p \frac{\Delta T_\text{element}}{\Delta t} $$
Question is: How do we advance from time $t$ (timestep $i$) to timestep $t+\Delta t$ (timestep $i+1$)?
Explicit method
\(\displaystyle \sum_\text{all surfaces} \textcolor{#008000}{Q^i} + \textcolor{#008000}{\dot{G}_\text{element}^i} \) \(\displaystyle =\) \(\displaystyle \frac{\rho V_\text{element} c_p (T_m^{i+1}-T_m^i)}{\Delta t} \)
Implicit method
\(\displaystyle \sum_\text{all surfaces} Q^{i+1} + \dot{G}_\text{element}^{i+1} \) \(\displaystyle =\) \(\displaystyle \frac{\rho V_\text{element} c_p (T_m^{i+1}-T_m^i)}{\Delta t} \)
Explicit: Use data from current time step $i$ (all known temperatures)
Implicit: Use data from next time step $i+1$ (unknown temperatures)
Energy balance at interior node:
Energy balance for boundary node with convection:
Consider a large uranium plate of thickness $L=4$ cm, thermal conductivity $k=28$ W/(m·K), and thermal
diffusivity
$a=12.5 \times 10^{-6}$ m$^2$/s that is initially at a uniform temperature of 200°C.
Heat is generated uniformly in the plate at a constant rate of
$\dot{g}=5 \times 10^6$ W/m$^3$.
At time $t = 0$ s, one side of the plate is brought into contact with iced water and is maintained
at 0°C at all times, while the other side is subjected to convection to an environment at
$T_\infty=30$°C with a heat transfer coefficient of $h=45$ W/(m$^2$·K).
Estimate the exposed surface temperature of the plate 2.5 min after start of cooling. Use three equally spaced nodes in the medium, two at the boundaries and one at the middle.
Observation: Explicit solution method may diverge if time step size is too large!
Stability criterion: When looking at node $m$, the coefficient in front of $T_m^i$ should be larger than zero
\( \displaystyle T_m^{i+1} = \tau(T_{m-1}^i+T_{m+1}^i) \) \(+ \) \( \displaystyle (1-2\tau) \) \( \displaystyle T_m^i+\tau\frac{\dot{g}_m^i (\Delta x)^2}{k}\)
\( \displaystyle T_0^{i+1} \) \( \displaystyle = \) \( \displaystyle \left(1-2\tau-2\tau \frac{h \Delta x}{k}\right) \) \( \displaystyle T_0^i + \) \( \displaystyle (2\tau) \) \( \displaystyle T_1^i \) \( \displaystyle + 2\tau\frac{h\Delta x}{k}T_\infty+\frac{\tau\dot{g}_0^i(\Delta x)^2}{k} \)
Energy balance at interior node:
Energy balance at boundary node with convection:
Consider a large uranium plate of thickness $L=4$ cm, thermal conductivity $k=28$ W/(m·K), and thermal
diffusivity
$a=12.5 \times 10^{-6}$ m$^2$/s that is initially at a uniform temperature of 200°C.
Heat is generated uniformly in the plate at a constant rate of
$\dot{g}=5 \times 10^6$ W/m$^3$.
At time $t = 0$ s, one side of the plate is brought into contact with iced water and is maintained
at 0°C at all times, while the other side is subjected to convection to an environment at
$T_\infty=30$°C with a heat transfer coefficient of $h=45$ W/(m$^2$·K).
Estimate the exposed surface temperature of the plate 2.5 min after start of cooling. Use three equally spaced nodes in the medium, two at the boundaries and one at the middle.