4. Potential Flows Flashcards

1
Q

Irrotational Flows

A

-flows with no vorticity, i.e. such that:

|ω = ∇x|u = 0

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2
Q

Velocity Potential

A

-if a velocity field |u is irrotational, i.e. if ∇x|u = 0, then there exists a velocity potential Φ(|x,t) such that:
|u = ∇Φ

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3
Q

Flows that are irrotational and incompressible

A

-if a flow is irrotational then it can be written in terms of a velocity potential:
|u = ∇Φ
-if in addition it is incompressible then the velocity potential Φ satisfies Laplace’s equation:
∇²Φ = 0
-hence, incompressible irrotational flows can be computed by solving Laplace’s equation and imposing appropriate boundary conditions on the solution

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4
Q

2D Incompressible Irrotational Flows

A

-both velocity potential Φ, and stream function ψ are solutions to Laplace’s equation;
∇²ψ = -ω = 0
AND
∇²Φ = 0
-however the boundary condition on ψ and Φ are different

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5
Q

Kinematic Boundary Conditions

A

-consider a flow past a solid body moving at velocity |U
-if ^n is the unit normal to the surface of the solid then, locally, the surface advances (moves in direction ^n) at the velocity:
(|U . ^n) ^n
-since the fluid cannot penetrate into the solid body, its velocity normal to the surface (|u.^n)^n must locally equal that of the solid;
|u . ^n = |U . ^n
-so since |u=∇Φ (for incompressible irrotational flow)
^n.∇Φ = ∂Φ/∂n = |U.^n
-the velocity satisfies Neumann boundary conditions at the solid body surface

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6
Q

Line Source / Sink

A

-consider an axisymmetric potential Φ=Φ(r)
-from Laplace’s equation in plane polar coordinates:
∇²Φ = 1/r d/dr(rdΦ/dr) = 0
<=>
dΦ/dr = m/r
-where m is a constant:
Φ(r) = m
ln(r) + C
-this potential produces the planar radial velocity:
|u = ∇Φ = m/r * ^er
-corresponding to a source for m>0 and a sink for m<0
-the constant C is arbitrary and doesn’t effect |u
-by convention m=Q/2π where Q is the flow rate
-this flow could be produced approximately using a perforated hose

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7
Q

Point Source / Sink

A

-consider a spherically symmetric potential Φ=Φ(r)
-from Laplace’s equation in spherical polar coordinates:
∇²Φ = 1/r² d/dr(r²*dΦ/dr)=0
<=>
dΦ/dr = m/r²
=>
Φ(r) = - m/r + C
-where m and C are integration constants
-this potential produces the 3D radial velocity:
|u = ∇Φ = m/r² * ^er
-corresponding to a source for m>0 and a sink for m<0
-by convention m=Q/4π where Q is the flow rate or volume flux

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8
Q

Line Vortex

A

-consider the potential Φ(θ) = kθ
-the solution to the Laplace equation in plane polar coordinates is:
ur = ∂Φ/∂r = 0
and
uθ = 1/r * ∂Φ/∂θ = k/r
-where the strength of flow k is a constant
-by convention k=Γ/2π where Γ is the circulation of the flow
-this represents a rotating fluid around a line vortex at r=0, it has zero vorticity but is singular at the origin

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9
Q

Uniform Stream

A

-for a uniform flow along the z axis, |u = (0,0,U) the velocity potential:
Φ(z) = Uz (+C)

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10
Q

Dipole (Doublet Flow)

Description

A
  • since Laplace’s equation is linear, we can add two solutions together to form a new one
  • a dipole is the superposition of a sink and a source of equal but opposite strength next to each other
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11
Q

Dipole (Doublet Flow)

3D Flow

A

-consider a point sink of strength -m at the origin and a point source of strength m at the positioni (0,0,𝛿)
-the velocity potential of the flow is formed by adding the potentials of the source and sink
-taking the limit as 𝛿->0 leads to the potential of a dipole:
Φ = - |μ .|r / r³
= |μ . ∇ (1/r)
-where |μ = μ ^ez is the dipole strength and |r=|x is the vector position
-fluid velocity for a dipole is then found using:
|u = ∇Φ

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12
Q

Dipole (Doublet Flow)

Planar Flow

A

-combining a line sink at the origin with a line source of equal but opposite strength at (𝛿,0) gives:
Φ = -m/2 * [ ln(x²+y²) - ln((x-𝛿)²+y²)]
-as in the 3D case, take the limit as 𝛿->0
-the expression for a 2D dipole of strength μ :
Φ = - |μ .|r / r²
= - |μ . ∇ (ln(r))
-where |μ= μ*^ex and |r=|x is the vector position

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13
Q

Uniqueness of Solutions to Laplace’s Equation

A

-given the value of the normal component of the fluid velocity, |u.|n on the surface S (i.e. the boundary condition), there exists a unique flow satisfying both ∇.|u=0 and ∇x|u=0 (i.e. incompressible and irrotational)

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14
Q

Properties of Laplace’s Equation

Identity From Vector Calculus

A
-let f(|x) be a function defined in a simply connected domain V with boundary S:
∇.(f∇f) = f∇²f + |∇f|²
=>
∫ ∇.(f∇f) dV = ∫ f∇²f dV + ∫ |∇f|²dV
-where integrals are over volume V
-using divergence theorem:
∫ (f∇f) dS = ∫ f∇²f dV + ∫ |∇f|²dV
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15
Q

Kelvin’s Minimum Energy Theorem

A

-of all possible fluid motions satisfying the boundary conditions for |u.|n on the surface S and ∇.|u in domain V, the potential flow is the flow with the smallest kinetic energy;
K = 1/2 ∫ρ ||u|² dV

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16
Q

Flow Past an Obstacle

A
  • since the solution to Laplace’s Equation for given boundary conditions is unique, if we find A solution we have found THE solution
  • this is only true if the domain is simply connected, if it is multiply connected, multiple solutions become possible
  • one technique to calculate non-elementary potential flows involves adding together simple known solutions to Laplace’s equation to get the solution that satisfies the boundary conditions
17
Q

Flow Around a Sphere

A

-velocity potential:
φ(r,z) = Uz [1 + a³/2(r²+z²)^(3/2)]
-corresponding Stoke’s streamfunction:
Ψ(r,z) = Ur²/2 [1 - a³/2(r²+z²)^(3/2)]
-outside the sphere Ψ>0, but we also obtain a solution inside the sphere with Ψ<0
-this flow is not real, it is a ‘virtual flow’ that allows for fluid velocity to be consistent with the boundary condition on a solid sphere

18
Q

Method of Images

A
  • to calculate the flow produced by a singularity near a boundary we can introduce flow singularities (i.e. sources an dipoles) outside of the domain of fluid flow in order to satisfy boundary conditions at a solid surface
  • usually the virtual source/sink will be in a symmetrical position to the real one, but on the other side of the barrier
19
Q

Method of Separation of Variables

A

-standard method for solving linear partial differential equations with compatible boundary conditions
-we shall seek separable solutions of the form:
φ(x,y) = f(x)g(y)
-in Cartesian coordinates or :
φ(r,θ) = f(r)g(θ)
-in polar coordinates
1) sub in the separable form of φ
2) separate variables to each side, this implies that each side is just equal to a constant
3) solve for each function separately and then sub back in for φ