Title: AOE 5104 Class 3 9/2/08
1AOE 5104 Class 3 9/2/08
- Online presentations for todays class
- Vector Algebra and Calculus 1 and 2
- Vector Algebra and Calculus Crib
- Homework 1 due 9/4
- Study group assignments have been made and are
online. - Recitations will be
- Mondays _at_ 530pm (with Nathan Alexander)
- Tuesdays _at_ 5pm (with Chris Rock)
- Locations TBA
- Which recitation you attend depends on which
study group you belong to and is listed with the
study group assignments
2Unnumbered slides contain comments that I
inserted and are not part of Professors
Devenports original presentation.
3 Last Class
- Vectors, inherent property of direction
- Algebra
- Volumetric flow rate through an area
- Taking components, eqn. of a streamline
- Triple products, A.BxC, Ax(BxC)
- Coordinate systems
4Cylindrical Coordinates
- Coordinates r, ? , z
- Unit vectors er, e?, ez (in directions of
increasing coordinates) - Position vector
- R r er z ez
- Vector components
- F Fr erF? e?Fz ez
- Components not constant, even if vector is
constant
z
F
ez
e?
er
R
z
r
?
y
x
5Spherical Coordinates
Errors on this slide in online presentation
- Coordinates r, ? , ?
- Unit vectors er, e?, e? (in directions of
increasing coordinates) - Position vector
- r r er
- Vector components
- F Fr erF? e?F? e?
z
er
e?
F
r
e?
?
r
?
y
x
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7LOW REYNOLDS NUMBER AXISYMMETRIC JET
J. KURIMA, N. KASAGI and M. HIRATA
(1983) Turbulence and Heat Transfer Laboratory,
University of Tokyo
8Class ExerciseUsing cylindrical coordinates (r,
?, z)
- Gravity exerts a force per unit mass of 9.8m/s2
on the flow which at (1,0,1) is in the radial
direction. Write down the component
representation of this force at - (1,0,1) b) (1,?,1) c) (1,?/2,0) d)
(0,?/2,0)
z
- (9.8,0,0)
- (-9.8,0,0)
- (0,-9.8,0)
- (9.8,0,0)
ez
e?
er
9.8m/s2
R
z
r
?
y
x
9Vector Algebra in Components
B
n
A
103. Vector Calculus
- Fluid particle Differentially Small Piece of the
Fluid Material
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12Concept of Differential Change In a Vector. The
Vector Field.
???(r,t)
Scalar field
VV(r,t)
Vector field
V
dV
VdV
- Differential change in vector
- Change in direction
- Change in magnitude
13Change in Unit Vectors Cylindrical System
de?
erder
e?
ez
e?de?
der
er
P'
e?
P
z
er
r
d?
?
14Change in Unit Vectors Spherical System
er
e?
r
e?
?
r
See Formulae for Vector Algebra and Calculus
?
15Example
Fluid particle Differentially small piece of the
fluid material
The position of fluid particle moving in a flow
varies with time. Working in different coordinate
systems write down expressions for the position
and, by differentiation, the velocity vectors.
VV(t)
RR(t)
Cartesian System
O
Cylindrical System
... This is an example of the calculus of vectors
with respect to time.
16Vector Calculus w.r.t. Time
- Since any vector may be decomposed into scalar
components, calculus w.r.t. time, only involves
scalar calculus of the components
17High Speed Flow Past an Axisymmetric Object
Finned body of revolution fired from a gun into a
supersonic wind tunnel flow for a net Mach number
of 2. The plastic shell casing is seen
separating. Vincenti, NASA
Shadowgraph picture is from An Album of Fluid
Motion by Van Dyke
18Line integrals
19Integral Calculus With Respect to Space
D(r)
D(r)
O
n
B
r
DD(r), ? ?(r)
ds
dS
d?
Surface S Volume R
A
Line Integrals
For closed loops, e.g. Circulation
20For closed loops, e.g. Circulation
Mach approximately 2.0
Picture is from An Album of Fluid Motion by Van
Dyke
21Integral Calculus With Respect to Space
D(r)
D(r)
O
n
B
r
DD(r), ? ?(r)
ds
dS
d?
Surface S Volume R
A
Surface Integrals
For closed surfaces
e.g. Volumetric Flow Rate through surface S
Volume Integrals
22n
dS
Mach approximately 2.0
Picture is from An Album of Fluid Motion by Van
Dyke
23Differential Calculus w.r.t. Space Definitions of
div, grad and curl
In 1-D
In 3-D
24Alternative to the Integral Definition of
Grad We want the generalization of
continued
25Alternative to the Integral Definition of
Grad Cylindrical coordinates
continued
26Alternative to the Integral Definition of
Grad Spherical coordinates
27Gradient
? high
?ndS (medium)
?ndS (large)
n
Resulting ?ndS
? low
dS
?ndS (small)
Elemental volume ?? with surface ?S
?ndS (medium)
magnitude and direction of the slope in the
scalar field at a point
28Gradient
- Component of gradient is the partial derivative
in the direction of that component - Fouriers Law of Heat Conduction
29The integral definition given on a previous slide
can also be used to obtain the formulas for the
gradient. On the next four slides, the form of
GradF in Cartesian coordinates is worked out
directly from the integral definition.
30Differential form of the Gradient
Cartesian system
Evaluate integral by expanding the variation in ?
about a point P at the center of an elemental
Cartesian volume. Consider the two x faces
? ?(x,y,z)
dz
k
i
j
P
adding these gives
Face 2
Proceeding in the same way for y and z
and
we get
, so
dx
Face 1
dy
31An element of volume with a local Cartesian
coordinate system having its origin at the
centroid of the corners, O
Point M is at the centroid of the face
perpendicular to the y-axis with coordinates (0,
?y/2, 0) Other points in this face have the
coordinates (x, ?y/2, z)
.
O
Gradient of a Differentiable Function, F
continued
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34Differential Forms of the Gradient
Cartesian
Cylindrical
Spherical
These differential forms define the vector
operator ?
35Divergence
Fluid particle, coincident with ?? at time t,
after time ?t has elapsed.
n
dS
Elemental volume ?? with surface ?S
proportionate rate of change of volume of a
fluid particle
36Differential Forms of the Divergence
Cartesian
Cylindrical
Spherical
37Differential Forms of the Curl
Cartesian
Cylindrical
Spherical
- Curl of the velocity vector ??V
- twice the circumferentially averaged angular
velocity of - the flow around a point, or
- a fluid particle
- Vorticity ?
Pure rotation
No rotation
Rotation
38Curl
Elemental volume ?? with surface ?S
e
n
dS
Perimeter Ce
Area ??
ds
?h
n
dSds?h
radius a
v? avg. tangential velocity
twice the avg. angular velocity about e