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AerE 546 Lecture 17 Finite volume method

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Finite volume method Natural for unstructured meshed. Also, working with fluxes leads into hyperbolic equations. A. Recall origin of p.d.e.ʼs Donʼt take second step: apply discretization to the integral balance. Control volume is polyline (polyhedron in 3-D). Divergence theorem (Gaussʼ) is used in f.v. method. Rationale: f = ∫df/dx dx but now f ! ∫F·dS and df/dx dx ! ∫ ∇·F dV =∫ ∇·F dS dxn =∫ dF/dxn dxn dS = ∫n·FdS Divergence theorem - fundamental theorem of calculus: Sometimes useful to start with p.d.e. (see below) 1. Control volumes are defined by mesh: ∂t ! CV qdV = − ! CS F · ndS (without sources). The integrals are This is exact. In 2-D, V = area and S = length: ∂t ∫ q dA= -Σ ∫ F·n dℓ The integrals must be discretized. What is F? Convective uT ; diffusive -κ∇T --- How does one compute the gradient? ∂t ! CV qdV = − ! CS F · ndS + ! CV Sources dV = − ! CV ∇ · FdV + ! CV Sources dV ⇒ ∂tq = −∇ · F + Sources ∂q/∂t F Source ∂t ∫ q dV = -Σ ∫ F·n dS S2 S3 S1 V S4 S6 S5 A

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Institution
AERE 546
Course
AERE 546

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AerE 546 ' Lecture 17




Finite volume method
Natural for unstructured meshed. Also, working with fluxes leads into hyperbolic equations.

A. Recall origin of p.d.e.ʼs
� � �
∂t qdV = − F · ndS + Sources dV
CV CS CV
� �
∂q/∂t F =− ∇ · F dV + Sources dV
CV CV
Source ⇒ ∂t q = −∇ · F + Sources


Donʼt take second step: apply discretization to the integral balance. Control volume is polyline
(polyhedron in 3-D).


Divergence theorem (Gaussʼ) is used in f.v. method. Rationale:

f = ∫df/dx dx but now f ! ∫F·dS and df/dx dx !

∫ ∇·F dV =∫ ∇·F dS dxn =∫ dF/dxn dxn dS = ∫n·FdS
Divergence theorem <-> fundamental theorem of calculus:
Sometimes useful to start with p.d.e. (see below)

1. Control volumes are defined by mesh:
� �
∂t qdV = − F · ndS
CV CS
(without sources). The integrals are
S2 S3


∂t ∫ q dV = -Σ ∫ F·n dS S1 V S4


S6 S5
This is exact. In 2-D, V = area and S = length: ∂t ∫ q dA= -Σ ∫ F·n dℓ

The integrals must be discretized.
What is F? Convective uT ; diffusive -κ∇T --- How does one compute the gradient?




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, AerE 546 ' Lecture 17


2. Sometimes have to think of starting with diff eq. E.g., down gradient heat flux:
∫-∇T dV = - ∫∇·(I T) dV = - ∫T (n·I) dS = - ∫T ndS n = outward normal
Temperature gradient is computed from face temperatures: ∫-∇T dV = -Σ ∫ n T dS

B. Control volumes
1. Order of accuracy determined by `reconstructionʼ.
2. Natural approach for unstructured grids (vs. finite difference)
3. Can derive by integrating diff. eqs. over control volume = mesh cell
4. Centers and vertices define dual grids

' ' ' ' ' ' Data can be stored on grid (vertex)
' ' ' ' ' ' ' ' or on dual (cell center)


g rid
al
Du


c.v.
Grid




Mesh = set of control volumes. ∂t ∫ q dV = -Σ ∫ F·n dS
Note flux out of one cell = flux into neighbor.

Xʼs can be computational nodes of triangular c.v.s. Or vertices can be nodes and
dual defines c.v.ʼs
control
surface
x dual created
x
x from cell centers
x control
x volume
x




This study source was downloaded by 100000899610689 from CourseHero.com on 09-06-2025 01:33:36 GMT -05:00
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