Mathematical Physicsundergraduategraduate

Heat Equation

Also known as: Diffusion equation · Fourier's heat equation

The temperature at a point rises in proportion to how much colder it is than its neighbors' average (the Laplacian). Heat flows down gradients, smoothing bumps and erasing fine detail irreversibly.

ut=D2u\frac{\partial u}{\partial t} = D\,\nabla^2 u
Live simulation
warming up the physics…

A sharp hot spike on a rod relaxes into an ever-wider, ever-shorter Gaussian. The diffusivity slider sets the pace; the area stays constant (energy conserved) while the peak flattens — and a 'reverse' note reminds you the process can't be undone.

Equivalent forms

ut=Duxxu_t = D u_{xx}
u(x,t)=14πDtex2/4Dt(point-source / heat kernel)u(x,t) = \frac{1}{\sqrt{4\pi D t}}\,e^{-x^2/4Dt}\quad(\text{point-source / heat kernel})
First order in time, so it has an arrow: it smooths forward but is ill-posed backward — the mathematics of irreversibility in one symbol.