About Heat Equation Visualiser
The heat equation, ∂u/∂t = α∇²u, is one of the most fundamental partial differential equations in mathematical physics. It describes how a quantity — originally temperature, but also concentration in diffusion problems — evolves over time under the influence of its spatial Laplacian. Joseph Fourier derived it in 1822 while studying heat flow in solids.
Solutions to the heat equation exhibit characteristic smoothing behaviour: sharp discontinuities in the initial temperature distribution are immediately smoothed out, and the solution converges to a steady state determined by the boundary conditions. Analytical solutions exist for simple geometries using Fourier series, while complex domains require numerical methods.
Beyond thermodynamics, the heat equation describes Brownian motion, option pricing in finance (the Black–Scholes equation is a transformed heat equation), diffusion of chemicals in tissue, and the spread of electrical signals in neurons. Its versatility makes it one of the most studied equations in applied mathematics.
Frequently Asked Questions
What does the Laplacian operator represent in the heat equation?
The Laplacian ∇²u measures the difference between the value of u at a point and its average in a surrounding neighbourhood. Where ∇²u > 0 (a local minimum), heat flows in and temperature rises; where ∇²u < 0 (a local maximum), heat flows out and temperature drops.
What is the steady-state solution of the heat equation?
As t → ∞, the time derivative vanishes and the heat equation reduces to Laplace's equation ∇²u = 0. The steady-state temperature distribution is harmonic — smooth, with no local maxima or minima inside the domain.
How does the heat equation relate to random walks?
The heat equation is the continuum limit of a random walk on a lattice. If particles diffuse randomly in equal steps, the probability density of finding a particle at position x and time t satisfies the same equation as the temperature field, connecting diffusion, probability theory, and heat transfer.
What numerical methods solve the heat equation?
Common methods include explicit finite differences (forward Euler, simple but conditionally stable), implicit methods (backward Euler, unconditionally stable), and the Crank–Nicolson scheme (second-order accurate and unconditionally stable). Finite element methods handle irregular domains.
Can the heat equation model cooling of the Earth?
Yes. Geophysicists use the heat equation to model how primordial heat escapes through the Earth's crust and mantle. Lord Kelvin famously used it to estimate Earth's age at 20–100 million years, though he was unaware of radioactive heating, which is the main source of internal heat today.