Diffusion Equation

A fundamental partial differential equation that describes how the density of a substance changes over time due to random molecular motion.

Diffusion Equation

The diffusion equation, also known as the heat equation in thermal contexts, is a cornerstone of mathematical physics that describes how a quantity spreads out over time through random motion at the molecular level.

Mathematical Form

The classical diffusion equation in one dimension is:

∂φ/∂t = D ∂²φ/∂x²

where:

Physical Significance

The equation emerges from two fundamental principles:

  1. Fick's Laws of Diffusion
  2. Conservation of Mass

It describes numerous natural phenomena, including:

Solution Methods

Several approaches exist for solving the diffusion equation:

Analytical Methods

Numerical Approaches

Applications

The equation finds applications across multiple fields:

  1. Physics

  2. Chemistry

  3. Biology

  4. Engineering

Historical Development

The equation was first derived by Joseph Fourier in the context of heat conduction, but its universality was later recognized through the work of Adolf Fick and Albert Einstein in their studies of diffusion and Brownian motion.

Modern Extensions

Contemporary research has expanded the classical diffusion equation to include:

The diffusion equation continues to be a active area of research, particularly in its application to new fields such as financial mathematics and social dynamics.