💨Fluid Dynamics Unit 4 – Incompressible inviscid flows
Incompressible inviscid flows are a crucial foundation in fluid dynamics. They simplify complex fluid behavior by assuming constant density and neglecting viscosity, allowing for elegant mathematical solutions to many flow problems.
This unit covers key concepts like potential flow, streamlines, and governing equations. It explores applications such as flow around cylinders and airfoils, providing essential tools for analyzing and solving real-world fluid dynamics challenges.
Incompressible flow assumes fluid density remains constant throughout the flow field
Inviscid flow neglects the effects of viscosity, assuming no friction between fluid particles or between the fluid and solid boundaries
Potential flow is a type of inviscid flow where the velocity field can be expressed as the gradient of a scalar potential function
Irrotational flow has zero vorticity, meaning fluid particles do not rotate about their own axes as they move along streamlines
Potential flows are always irrotational, but not all irrotational flows are potential flows
Streamlines are curves tangent to the velocity vector at every point in a steady flow field
Streamfunction ψ is a scalar function whose contours represent streamlines in a 2D incompressible flow
Velocity potential ϕ is a scalar function whose gradient gives the velocity field in a potential flow
Governing Equations
Conservation of mass for incompressible flow: ∇⋅u=0, where u is the velocity vector
This equation is also known as the continuity equation
Euler's equation for inviscid flow: ρ(∂t∂u+u⋅∇u)=−∇p+ρg, where ρ is density, p is pressure, and g is the gravitational acceleration vector
For steady, irrotational, inviscid flow, Euler's equation simplifies to the Bernoulli equation: 21ρ∣u∣2+p+ρgz=constant, where z is the vertical coordinate
Vorticity equation for inviscid flow: DtDω=ω⋅∇u, where ω=∇×u is the vorticity vector and DtD is the material derivative
For irrotational flow, ω=0 everywhere in the flow field
Potential Flow Theory
Potential flow assumes the velocity field can be expressed as the gradient of a scalar potential function: u=∇ϕ
The continuity equation for incompressible potential flow reduces to Laplace's equation: ∇2ϕ=0
Potential flow theory allows for the superposition of elementary flow solutions (uniform flow, source/sink, doublet, vortex) to construct more complex flow patterns
The velocity potential ϕ and streamfunction ψ are related by the Cauchy-Riemann equations in 2D: ∂x∂ϕ=∂y∂ψ and ∂y∂ϕ=−∂x∂ψ
This relationship allows for the use of complex potential w(z)=ϕ+iψ, where z=x+iy is the complex coordinate
Potential flow theory is particularly useful for analyzing flows around simple geometries (cylinders, spheres, airfoils) and for understanding the basic features of more complex flows
Streamlines and Streamfunctions
Streamlines are curves that are everywhere tangent to the velocity vector at a given instant in time
In steady flow, fluid particles follow streamlines, while in unsteady flow, streamlines and particle paths may differ
The streamfunction ψ is a scalar function whose contours represent streamlines in a 2D incompressible flow
The velocity components are related to the streamfunction by u=∂y∂ψ and v=−∂x∂ψ
In 2D polar coordinates (r,θ), the velocity components are ur=r1∂θ∂ψ and uθ=−∂r∂ψ
The difference in streamfunction values between two points gives the volume flow rate per unit depth between the corresponding streamlines
Streamlines cannot cross each other in steady flow, as this would imply multiple velocity vectors at the point of intersection
Stagnation points occur where the velocity is zero, and the streamfunction has a local maximum, minimum, or saddle point
Velocity Potential and Laplace's Equation
The velocity potential ϕ is a scalar function whose gradient gives the velocity field in a potential flow: u=∇ϕ
For incompressible potential flow, the continuity equation reduces to Laplace's equation: ∇2ϕ=0
In 2D Cartesian coordinates, Laplace's equation is ∂x2∂2ϕ+∂y2∂2ϕ=0
In 2D polar coordinates, Laplace's equation is r1∂r∂(r∂r∂ϕ)+r21∂θ2∂2ϕ=0
Solutions to Laplace's equation are called harmonic functions and have important mathematical properties (e.g., uniqueness, maximum principle)
Elementary potential flow solutions (uniform flow, source/sink, doublet, vortex) are building blocks for more complex potential flows and can be superposed due to the linearity of Laplace's equation
The velocity potential is related to the pressure through the Bernoulli equation in steady, irrotational, inviscid flow: 21ρ∣∇ϕ∣2+p+ρgz=constant
Boundary Conditions and Flow Patterns
To solve for the velocity potential or streamfunction, appropriate boundary conditions must be specified
The no-penetration condition states that the velocity normal to a solid boundary must be zero: u⋅n=0, where n is the unit normal vector to the boundary
This condition is satisfied by setting the streamfunction to a constant value along the boundary
The no-slip condition, which states that the tangential velocity at a solid boundary must be zero, is not applicable to inviscid flows
Far-field boundary conditions specify the behavior of the flow at large distances from the object of interest (e.g., uniform flow, quiescent fluid)
Kutta condition is applied at sharp trailing edges (airfoils) to ensure smooth flow separation and uniqueness of the solution
Circulation Γ around a closed contour is defined as the line integral of the velocity: Γ=∮Cu⋅dl
In potential flow, circulation is related to the jump in velocity potential: Γ=Δϕ
Lift on an airfoil is directly proportional to the circulation around it (Kutta-Joukowski theorem): L=ρ∞V∞Γ, where ρ∞ and V∞ are the freestream density and velocity, respectively
Applications and Examples
Flow around a circular cylinder can be modeled using a doublet and a uniform flow, with the doublet strength adjusted to satisfy the no-penetration condition
Flow around a sphere can be modeled using a point source and a uniform flow, with the source strength determined by the sphere's radius and the freestream velocity
Rankine oval is a simple model for flow around a bluff body, constructed by superposing a uniform flow and a source-sink pair
Flow around a Joukowski airfoil can be obtained by conformal mapping of the flow around a cylinder using the Joukowski transformation
The Kutta condition is applied at the trailing edge to determine the circulation and lift
Potential flow theory can be used to analyze the flow in a 90-degree bend by superposing a uniform flow and a doublet
Wind tunnel contraction and diffuser sections can be designed using potential flow theory to minimize flow non-uniformity and separation
Potential flow solutions serve as a starting point for more advanced numerical methods (panel methods, vortex methods) that can handle more complex geometries and flow conditions
Problem-Solving Techniques
Identify the key features of the problem (geometry, boundary conditions, far-field behavior) and select appropriate elementary potential flow solutions
Use the principle of superposition to combine elementary solutions and satisfy the boundary conditions
Apply conformal mapping techniques to transform the flow around simple geometries (circles, polygons) into the desired flow around more complex shapes (airfoils, ducts)
Exploit the symmetry of the problem, if present, to simplify the analysis and reduce the computational domain
Use the Kutta condition to determine the circulation and lift for flows around airfoils and other lifting bodies
Employ complex potential and complex velocity to streamline the analysis of 2D potential flows
Verify that the solution satisfies the governing equations (Laplace's equation) and the specified boundary conditions
Validate the potential flow solution against experimental data or higher-fidelity numerical simulations, and be aware of the limitations of the potential flow assumptions (inviscid, irrotational)