The movement of water in a cup after a sharp turn or wisps of smoke swirling in the air obey equations that calculate every whirl, but still haven't revealed all their secrets.
In practice: Weather forecasts, wing aerodynamics calculations, climate modeling, and ocean current simulations — all are built on these equations.
French engineer Claude-Louis Navier (1821) and British physicist George Stokes (1845) combined into a system equations expressing the conservation of mass and momentum in a viscous fluid. The momentum equation: ρ (∂v/∂t + v·∇v) = -∇p + μ ∇²v + f. The left side is mass times acceleration (including convective transport), the right side includes pressure forces, viscous friction, and external influences. The incompressibility condition ∇·v = 0 is added. Their genius was accounting for internal friction (the term with viscosity μ).
How it works
With them, engineers calculate how air flows around a car, and meteorologists predict cyclone movement. Viscosity (flow resistance) calms the flow, and if viscosity is low, turbulence arises — chaotic mixing.
💡 The Clay Mathematics Institute has announced a $$1 million prize for proving that solutions to the equations always exist and do not 'blow up' (remain smooth) in the three-dimensional case — it is one of the Millennium Prize problems.
The Navier-Stokes equations describe how fluids and gases move. They relate changes in flow velocity to pressure, viscosity (internal friction), and external forces (e.g., gravity). Simply put, it is a mathematical way of saying: 'what flows into a volume minus what flows out, plus everything that pushes or slows down.' The equations are complex because they contain nonlinear interaction: vortices create new vortices.
How it works
With them, engineers calculate how air flows around a car, and meteorologists predict cyclone movement. Viscosity (flow resistance) calms the flow, and if viscosity is low, turbulence arises — chaotic mixing.
💡 Even a small change in initial conditions can radically alter the flow — this is the famous 'butterfly effect,' popularized by Edward Lorenz, who, incidentally, discovered deterministic chaos while working with a simplified model of the Navier-Stokes equations.
The Navier-Stokes equations are a system of nonlinear partial differential equations describing the motion of a viscous Newtonian fluid (with a linear relationship between stress and strain rate). In vector form for an incompressible fluid: ρ (∂v/∂t + v·∇v) = -∇p + μ Δv + f, ∇·v = 0. Here v is velocity, ρ is density, p is pressure, μ is dynamic viscosity, f is external body forces. The equations express Newton's second law for a fluid element and the law of mass conservation.
Discovery
Claude-Louis Navier derived the equations in 1821, introducing a molecular hypothesis about forces between particles. In 1845, George Gabriel Stokes refined the derivation, abandoning molecular notions and formulating the commonly accepted form with a continuum approach. Later, Leonhard Euler derived equations for an ideal (inviscid) fluid, and Navier and Stokes added viscosity.
How it works
The equations are the foundation of hydro- and aerodynamics, meteorology, oceanography, astrophysics (accretion disks, interstellar medium). Depending on the Reynolds number, they describe laminar or turbulent flow. Numerical methods of computational fluid dynamics (CFD) allow modeling everything from blood flow to aircraft aerodynamics, but high turbulence requires supercomputers.
Caveats
The problem of existence and smoothness of solutions in 3D (one of the Millennium Prize problems); Turbulence remains analytically unsolved — semi-empirical models are used; For some initial data, solutions may break down singularly in finite time (neither proven nor disproven)
ρ is fluid density, ∂v/∂t is local acceleration, v·∇v is convective acceleration, ∇p is pressure gradient, μ is dynamic viscosity, ∇²v is the Laplacian of velocity (viscous dissipation), f is external body forces (e.g., gravity)
\nabla \cdot \mathbf{v} = 0
∇·v is the divergence of the velocity vector; for an incompressible fluid, it is zero, meaning no sources or sinks
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