Fluid Dynamics

💨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.

Key Concepts and Definitions

  • 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\psi is a scalar function whose contours represent streamlines in a 2D incompressible flow
  • Velocity potential ϕ\phi is a scalar function whose gradient gives the velocity field in a potential flow

Governing Equations

  • Conservation of mass for incompressible flow: u=0\nabla \cdot \mathbf{u} = 0, where u\mathbf{u} is the velocity vector
    • This equation is also known as the continuity equation
  • Euler's equation for inviscid flow: ρ(ut+uu)=p+ρg\rho \left(\frac{\partial \mathbf{u}}{\partial t} + \mathbf{u} \cdot \nabla \mathbf{u}\right) = -\nabla p + \rho \mathbf{g}, where ρ\rho is density, pp is pressure, and g\mathbf{g} is the gravitational acceleration vector
  • For steady, irrotational, inviscid flow, Euler's equation simplifies to the Bernoulli equation: 12ρu2+p+ρgz=constant\frac{1}{2}\rho |\mathbf{u}|^2 + p + \rho g z = \text{constant}, where zz is the vertical coordinate
  • Vorticity equation for inviscid flow: DωDt=ωu\frac{D \boldsymbol{\omega}}{Dt} = \boldsymbol{\omega} \cdot \nabla \mathbf{u}, where ω=×u\boldsymbol{\omega} = \nabla \times \mathbf{u} is the vorticity vector and DDt\frac{D}{Dt} is the material derivative
    • For irrotational flow, ω=0\boldsymbol{\omega} = 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\mathbf{u} = \nabla \phi
  • The continuity equation for incompressible potential flow reduces to Laplace's equation: 2ϕ=0\nabla^2 \phi = 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\phi and streamfunction ψ\psi are related by the Cauchy-Riemann equations in 2D: ϕx=ψy\frac{\partial \phi}{\partial x} = \frac{\partial \psi}{\partial y} and ϕy=ψx\frac{\partial \phi}{\partial y} = -\frac{\partial \psi}{\partial x}
    • This relationship allows for the use of complex potential w(z)=ϕ+iψw(z) = \phi + i\psi, where z=x+iyz = 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\psi is a scalar function whose contours represent streamlines in a 2D incompressible flow
    • The velocity components are related to the streamfunction by u=ψyu = \frac{\partial \psi}{\partial y} and v=ψxv = -\frac{\partial \psi}{\partial x}
  • In 2D polar coordinates (r,θ)(r, \theta), the velocity components are ur=1rψθu_r = \frac{1}{r}\frac{\partial \psi}{\partial \theta} and uθ=ψru_\theta = -\frac{\partial \psi}{\partial r}
  • 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\phi is a scalar function whose gradient gives the velocity field in a potential flow: u=ϕ\mathbf{u} = \nabla \phi
  • For incompressible potential flow, the continuity equation reduces to Laplace's equation: 2ϕ=0\nabla^2 \phi = 0
    • In 2D Cartesian coordinates, Laplace's equation is 2ϕx2+2ϕy2=0\frac{\partial^2 \phi}{\partial x^2} + \frac{\partial^2 \phi}{\partial y^2} = 0
    • In 2D polar coordinates, Laplace's equation is 1rr(rϕr)+1r22ϕθ2=0\frac{1}{r}\frac{\partial}{\partial r}\left(r\frac{\partial \phi}{\partial r}\right) + \frac{1}{r^2}\frac{\partial^2 \phi}{\partial \theta^2} = 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: 12ρϕ2+p+ρgz=constant\frac{1}{2}\rho |\nabla \phi|^2 + p + \rho g z = \text{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: un=0\mathbf{u} \cdot \mathbf{n} = 0, where n\mathbf{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\Gamma around a closed contour is defined as the line integral of the velocity: Γ=Cudl\Gamma = \oint_C \mathbf{u} \cdot d\mathbf{l}
    • In potential flow, circulation is related to the jump in velocity potential: Γ=Δϕ\Gamma = \Delta \phi
  • Lift on an airfoil is directly proportional to the circulation around it (Kutta-Joukowski theorem): L=ρVΓL = \rho_\infty V_\infty \Gamma, where ρ\rho_\infty and VV_\infty 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)


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AP® and SAT® are trademarks registered by the College Board, which is not affiliated with, and does not endorse this website.
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