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AOE 5104 Class 3 9/2/08 Online presentations for today’s 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 5:30pm (with Nathan Alexander) 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
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Unnumbered slides contain comments that I inserted and are not part of Professor’s Devenport’s original presentation.
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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 Class 3. 8/29/06 Assignments: Online Presentation “Vector Algebra and Calculus 2” Homework 1, due 9/5/06 Vector Algebra and calculus crib on course web site Study groups
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Cylindrical 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 er+F e+Fz ez Components not constant, even if vector is constant z F ez e er R z r y x
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Spherical Coordinates
Errors on this slide in online presentation Spherical Coordinates Coordinates r, , Unit vectors er, e, e (in directions of increasing coordinates) Position vector r = r er Vector components F = Fr er+F e+F e z er e F r e r y x
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LOW REYNOLDS NUMBER AXISYMMETRIC JET
J. KURIMA, N. KASAGI and M. HIRATA (1983) Turbulence and Heat Transfer Laboratory, University of Tokyo
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Class Exercise Using 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) ez e er 9.8m/s2 R z r y x
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Vector Algebra in Components
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Fluid particle: Differentially Small Piece of the Fluid Material
3. Vector Calculus Fluid particle: Differentially Small Piece of the Fluid Material
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Class 3. 8/29/06 Assignments: Online Presentation “Vector Algebra and Calculus 2” Homework 1, due 9/5/06 Vector Algebra and calculus crib on course web site Study groups
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Concept of Differential Change In a Vector. The Vector Field.
Scalar field =(r,t) Vector field V=V(r,t) V dV V+dV Differential change in vector Change in direction Change in magnitude
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Change in Unit Vectors – Cylindrical System
de er+der e ez e+de der P' er e P z er r d
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Change in Unit Vectors – Spherical System
r See “Formulae for Vector Algebra and Calculus”
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Example 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. V=V(t) R=R(t) Cartesian System O Cylindrical System ... This is an example of the calculus of vectors with respect to time.
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Vector 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
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High 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
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Line integrals
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Integral Calculus With Respect to Space
D(r) D(r) O n B r ds D=D(r), = (r) dS d Surface S Volume R A Line Integrals For closed loops, e.g. Circulation
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For closed loops, e.g. Circulation
Mach approximately 2.0 Picture is from “An Album of Fluid Motion” by Van Dyke
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Integral Calculus With Respect to Space
D(r) D(r) O n B r ds D=D(r), = (r) dS d Surface S Volume R A Surface Integrals For closed surfaces e.g. Volumetric Flow Rate through surface S Volume Integrals
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n dS Mach approximately 2.0
Picture is from “An Album of Fluid Motion” by Van Dyke
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Differential Calculus w.r.t. Space Definitions of div, grad and curl
In 1-D Elemental volume with surface S n dS D=D(r), = (r) In 3-D
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Alternative to the Integral Definition of Grad
We want the generalization of continued
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Alternative to the Integral Definition of Grad Cylindrical coordinates
continued
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Alternative to the Integral Definition of Grad
Spherical coordinates
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Gradient = high ndS (medium) ndS (large) n = low Resulting ndS
(small) Elemental volume with surface S ndS (medium) = magnitude and direction of the slope in the scalar field at a point
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Gradient Component of gradient is the partial derivative in the direction of that component Fourier´s Law of Heat Conduction
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The 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.
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Differential 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) k dz i P j adding these gives Face 2 Proceeding in the same way for y and z we get and , so Face 1 dx dy
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. Gradient of a Differentiable Function, F
An element of volume with a local Cartesian coordinate system having its origin at the centroid of the corners, O x y z Δx Δz Δy M Point M is at the centroid of the face perpendicular to the y-axis with coordinates (0, Δy/2, 0) Other points in this face have the coordinates (x, Δy/2, z) . O Gradient of a Differentiable Function, F continued
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Differential Forms of the Gradient
Cartesian Cylindrical Spherical These differential forms define the vector operator
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Divergence 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
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Differential Forms of the Divergence
Cartesian Cylindrical Spherical
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Differential 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 Ω Pure rotation No rotation Rotation
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Curl Elemental volume with surface S e n dS Perimeter Ce Area
dS=dsh radius a v avg. tangential velocity = twice the avg. angular velocity about e
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