Fonction de flux

The stream function is a mathematical tool that simplifies two-dimensional incompressible flow analysis by automatically satisfying the continuity equation for mass conservation. Instead of solving for horizontal and vertical velocity components separately, the stream function allows velocities to be defined as partial derivatives, eliminating tedious calculations and making fluid motion analysis more efficient.

The horizontal velocity equals the partial derivative of the stream function with respect to the vertical direction, while the vertical velocity equals the negative partial derivative with respect to the horizontal direction. These definitions automatically satisfy the continuity equation because the mixed partial derivatives of the stream function cancel out.

Streamlines are the paths that fluid particles follow within a flow field and are tangent to velocity vectors at every point. They can be visualized as contour lines of constant stream function values, providing an intuitive representation of fluid behavior without requiring individual velocity calculations at each location.

The difference in stream function values between two streamlines directly represents the volumetric flow rate per unit depth flowing between them. This property eliminates the need to integrate velocity components separately, making flow rate calculations straightforward and efficient for two-dimensional incompressible flows.

The continuity equation ensures mass conservation by requiring that the net inflow and outflow in any region remain balanced. For incompressible flow where density is constant, this means the divergence of the velocity field must equal zero, guaranteeing that fluid mass is neither created nor destroyed within the flow domain.

The stream function satisfies mass conservation because velocity components are defined as specific partial derivatives of the stream function. When these derivatives are substituted into the continuity equation, the mixed partial derivatives cancel out mathematically, automatically ensuring the divergence condition equals zero without additional constraints.

Using the stream function eliminates the need to solve separate equations for horizontal and vertical velocity components in steady laminar flow between parallel plates or other two-dimensional incompressible flows. This reduces computational complexity while providing direct access to flow rates and streamline patterns through a single scalar function.