Laplace Transform for PDEs
we know
\( t \) is integrated away
replaced w/ \( s \)
now let's do the same for \( u(x, t) \)
we know
\( t \) is integrated away
replaced w/ \( s \)
now let's do the same for \( u(x, t) \)
let's do a simple heat eq.
find complementary solution: \( U'' - sU = 0 \) \( s \) is "constant"
to find \( C_1, C_2 \), use the BCs
w/ those we get
using undetermined coeff: \( U_p = A \cos x + B \sin x \)
plug into \( U'' - sU = -\sin(x) \)
solution is \( s \)-domain
we often want the solution in \( t \)-domain
Laplace transform is particularly effective w/ infinite domains and time-vary boundary conditions
\( \rightarrow \) separation of variables can't handle these easily
\[ u_t = u_{xx} \quad 0 < x < \infty \]
\( u(0, t) = \sin(t) \) (left end temp = \( \sin(t) \))
\( u(x, 0) = 0 \) initially frozen
\[ \mathcal{L} \{ u_t \} = \mathcal{L} \{ u_{xx} \} \]
\[ sU - u(x, 0) = U'' \rightarrow U'' - sU = 0 \]
\[ U = C_1 e^{\sqrt{s}x} + C_2 e^{-\sqrt{s}x} \]
"hidden" BC at \( \infty \): temp must be bounded at \( \infty \)
\( \rightarrow C_1 = 0 \)
\[ U = C_2 e^{-\sqrt{s}x} \]
BC at \( x = 0 \) : \( u(0, t) = \sin(t) \)
\[ U(x=0) = \frac{1}{s^2 + 1} \]
so, \( C_2 = \frac{1}{s^2 + 1} \)
\[ U(x, s) = \frac{1}{s^2 + 1} e^{-\sqrt{s}x} \]
Solution in S-domain
\[ \mathcal{L} \left\{ \int_0^t f(t-\tau) g(\tau) d\tau \right\} = FG \]
\[ \mathcal{L}^{-1} \left\{ \frac{1}{s^2 + 1} \right\} = f(t) = \sin(t) \]
\[ \mathcal{L}^{-1} \left\{ e^{-\sqrt{s}x} \right\} = \frac{x}{2\sqrt{\pi t^3}} e^{-x^2/4t} = g(t) \]
\[ u(x, t) = \int_0^t \sin(t-\tau) \frac{x}{2\sqrt{\pi \tau^3}} e^{-x^2/4\tau} d\tau \]
\( \sin(t) \): the heat we put in
\[ \frac{x}{2\sqrt{\pi t^3}} e^{-x^2/4t} \]
: how heat moves in this rod
(heat kernel)
Heat kernel is also the impulse response in reaction to an impulse of heat.
What is measured is the sum (integral) of all those.
The visualization above illustrates how heat waves propagate through a rod over time, showing the spatial and temporal distribution of temperature \( u(x,t) \).
The following graph illustrates the temperature distribution \( u(x, t) \) as a function of distance \( x \) for various time steps \( t \). The boundary condition at \( x = 0 \) is driven by a sinusoidal oscillation, causing waves of temperature to propagate into the medium and decay as distance increases.