Coordinate Systems.

Slides:



Advertisements
Similar presentations
Differential Calculus (revisited):
Advertisements

Dr. Charles Patterson 2.48 Lloyd Building
Chapter 9: Vector Differential Calculus Vector Functions of One Variable -- a vector, each component of which is a function of the same variable.
VECTOR CALCULUS 1.10 GRADIENT OF A SCALAR 1.11 DIVERGENCE OF A VECTOR
ENTC 3331 RF Fundamentals Dr. Hugh Blanton ENTC 3331.
EEE 340Lecture Curl of a vector It is an axial vector whose magnitude is the maximum circulation of per unit area as the area tends to zero and.
EE3321 ELECTROMAGENTIC FIELD THEORY
ELEC 3600 T UTORIAL 2 V ECTOR C ALCULUS Alwin Tam Rm. 3121A.
ENE 206 Matlab 4 Coordinate systems. Vector and scalar quantities Vector scalar A.
EE2030: Electromagnetics (I)
Fundamentals of Applied Electromagnetics
2-7 Divergence of a Vector Field
For each point (x,y,z) in R3, the cylindrical coordinates (r,,z) are defined by the polar coordinates r and  (for x and y) together with z. Example Find.
1 Lecture 4 Coordinate Systems: Rectangular, Cylindrical, Spherical.
Chapter 1 Vector analysis
Mathematics Review A.1 Vectors A.1.1 Definitions
Lecture 14 Today Orthogonal coordinate systems 1.The Cartesian (rectangular) coordinate system 2.The cylindrical coordinate system 3.The spherical.
Coordinate System VECTOR REPRESENTATION 3 PRIMARY COORDINATE SYSTEMS: RECTANGULAR CYLINDRICAL SPHERICAL Choice is based on symmetry of problem Examples:
1-1 Engineering Electromagnetics Chapter 1: Vector Analysis.
Lecture 13 Basic Laws of Vector Algebra Scalars: e.g. 2 gallons, $1,000, 35ºC Vectors: e.g. velocity: 35mph heading south 3N force toward center.
Z x y Cylindrical Coordinates But, first, let’s go back to 2D.
Darryl Michael/GE CRD Fields and Waves Lesson 2.1 VECTORS and VECTOR CALCULUS.
Vector calculus 1)Differential length, area and volume
ELEN 3371 Electromagnetics Fall Lecture 2: Review of Vector Calculus Instructor: Dr. Gleb V. Tcheslavski Contact:
EED 2008: Electromagnetic Theory Özgür TAMER Vectors Divergence and Stokes Theorem.
MAGNETOSTATIC FIELD (STEADY MAGNETIC)
Why Study Electromagnetics? What is Electromagnetics?
UNIVERSITI MALAYSIA PERLIS
Chapter 10 Vector Calculus
PHYSICS-II (PHY C132) ELECTRICITY & MAGNETISM
Review of Vector Analysis
1 Chapter 2 Vector Calculus 1.Elementary 2.Vector Product 3.Differentiation of Vectors 4.Integration of Vectors 5.Del Operator or Nabla (Symbol  ) 6.Polar.
Ch. 10 Vector Integral Calculus.
EE 543 Theory and Principles of Remote Sensing
Chapter 1 - Vector Analysis. Scalars and Vectors Scalar Fields (temperature) Vector Fields (gravitational, magnetic) Vector Algebra.
EEE241: Fundamentals of Electromagnetics
1 ENE 325 Electromagnetic Fields and Waves Lecture 1 Electrostatics.
1 ENE 325 Electromagnetic Fields and Waves Lecture 1 Electrostatics.
ENE 325 Electromagnetic Fields and Waves Lecture 3 Gauss’s law and applications, Divergence, and Point Form of Gauss’s law 1.
§1.2 Differential Calculus
Dr. Hugh Blanton ENTC 3331 Dr. Blanton - ENTC Orthogonal Coordinate Systems 2 Fields and Waves VECTORS and VECTOR CALCULUS.
§1.2 Differential Calculus Christopher Crawford PHY 416G
Mathematics Review A.1 Vectors A.1.1 Definitions
Angular Velocity: Sect Overview only. For details, see text! Consider a particle moving on arbitrary path in space: –At a given instant, it can.
1 Vector Calculus. Copyright © 2007 Oxford University Press Elements of Electromagnetics Fourth Edition Sadiku2 Figure 3.1 Differential elements in the.
Wave Dispersion EM radiation Maxwell’s Equations 1.
Multiplication of vectors Two different interactions (what’s the difference?)  Scalar or dot product : the calculation giving the work done by a force.
مفردات منهج الكهرومغناطيسية CH 1: vector analysis Change in Cartesian coordinates systems. Change of axis (Rotation Matrices). Field and differential operators.
ELECTROMAGNETICS THEORY (SEE 2523).  An orthogonal system is one in which the coordinates are mutually perpendicular.  Examples of orthogonal coordinate.
ENE 325 Electromagnetic Fields and Waves Lecture 2 Static Electric Fields and Electric Flux density.
Chapter 2 Vector Calculus
ECE 305 Electromagnetic Theory
Soh Ping Jack, Azremi Abdullah Al-Hadi, Ruzelita Ngadiran
Second Derivatives The gradient, the divergence and the curl are the only first derivatives we can make with , by applying twice we can construct.
Chapter 3 Overview.
Chapter 3. Gauss’ law, Divergence
PROVIDED BY BRAINZORP.
Vector & Coordinate systems
ENE 325 Electromagnetic Fields and Waves
Electromagnetics II.
EEE 161 Applied Electromagnetics
Fields and Waves I Lecture 8 K. A. Connor Y. Maréchal
ENE/EIE 325 Electromagnetic Fields and Waves
Vector Calculus for Measurements in Thermofluids
ENE 325 Electromagnetic Fields and Waves
Chapter 3 1. Line Integral Volume Integral Surface Integral
EEE 161 Applied Electromagnetics
Reference W.H. Hayt and J.A. Buck , Engineering Electromagnetics, McGraw-Hill, 8th Ed., J. Edminister, Schaum's Outline of Electromagnetics, McGraw-Hill,
Electricity and Magnetism I
Fundamentals of Applied Electromagnetics
Presentation transcript:

Coordinate Systems

COORDINATE SYSTEMS Examples: RECTANGULAR or Cartesian To understand the Electromagnetics, we must know basic vector algebra and coordinate systems. So let us start the coordinate systems. COORDINATE SYSTEMS Choice is based on symmetry of problem RECTANGULAR or Cartesian CYLINDRICAL SPHERICAL Examples: Sheets - RECTANGULAR Wires/Cables - CYLINDRICAL Spheres - SPHERICAL

Visualization (Animation) Cylindrical Symmetry Spherical Symmetry Visualization (Animation)

Orthogonal Coordinate Systems: 1. Cartesian Coordinates z P(x,y,z) Or y Rectangular Coordinates P (x, y, z) x z z P(r, Φ, z) 2. Cylindrical Coordinates P (r, Φ, z) r y x Φ X=r cos Φ, Y=r sin Φ, Z=z z 3. Spherical Coordinates P(r, θ, Φ) θ r P (r, θ, Φ) X=r sin θ cos Φ, Y=r sin θ sin Φ, Z=z cos θ y x Φ

Cartesian Coordinates Cylindrical Coordinates Spherical Coordinates z z Cartesian Coordinates P(x, y, z) P(x,y,z) P(r, θ, Φ) θ r y y x x Φ Cylindrical Coordinates P(r, Φ, z) Spherical Coordinates P(r, θ, Φ) z z P(r, Φ, z) r y x Φ

Cartesian coordinate system dx, dy, dz are infinitesimal displacements along X,Y,Z. Volume element is given by dv = dx dy dz Area element is da = dx dy or dy dz or dxdz Line element is dx or dy or dz Ex: Show that volume of a cube of edge a is a3. dz Z dy dx P(x,y,z) Y X

Cartesian Coordinates Differential quantities: Length: Area: Volume:

AREA INTEGRALS integration over 2 “delta” distances Example: AREA = dx dy Example: x y 2 6 3 7 AREA = = 16 Note that: z = constant

Cylindrical coordinate system (r,φ,z) X Y Z r φ

Spherical polar coordinate system Cylindrical coordinate system (r,φ,z) dr is infinitesimal displacement along r, r dφ is along φ and dz is along z direction. Volume element is given by dv = dr r dφ dz Limits of integration of r, θ, φ are 0<r<∞ , 0<z <∞ , o<φ <2π Ex: Show that Volume of a Cylinder of radius ‘R’ and height ‘H’ is π R2H . Z dz r dφ dr Y dφ φ r r dφ dr X φ is azimuth angle

Volume of a Cylinder of radius ‘R’ and Height ‘H’ Try yourself: Surface Area of Cylinder = 2πRH . Base Area of Cylinder (Disc)=πR2.

Cylindrical Coordinates: Visualization of Volume element Differential quantities: Length element: Area element: Volume element: Limits of integration of r, θ, φ are 0<r<∞ , 0<z <∞ , o<φ <2π

Spherically Symmetric problem (r,θ,φ) Z θ r Y φ X

Spherical polar coordinate system (r,θ,φ) dr is infinitesimal displacement along r, r dθ is along θ and r sinθ dφ is along φ direction. Volume element is given by dv = dr r dθ r sinθ dφ Limits of integration of r, θ, φ are 0<r<∞ , 0<θ <π , o<φ <2π Ex: Show that Volume of a sphere of radius R is 4/3 π R3 . P(r, θ, φ) Z dr r cos θ P r dθ θ r Y φ r sinθ r sinθ dφ X θ is zenith angle( starts from +Z reaches up to –Z) , φ is azimuth angle (starts from +X direction and lies in x-y plane only)

Volume of a sphere of radius ‘R’ Try Yourself: 1)Surface area of the sphere= 4πR2 .

Spherical Coordinates: Volume element in space

Points to remember Cartesian x,y,z dx dy dz System Coordinates dl1 dl2 dl3 Cartesian x,y,z dx dy dz Cylindrical r, φ,z dr rdφ dz Spherical r,θ, φ dr rdθ r sinθdφ Volume element : dv = dl1 dl2 dl3 If Volume charge density ‘ρ’ depends only on ‘r’: Ex: For Circular plate: NOTE Area element da=r dr dφ in both the coordinate systems (because θ=900)

b) Volume covered by these surfaces. Quiz: Determine a) Areas S1, S2 and S3. b) Volume covered by these surfaces. S3 Z Radius is r, Height is h, r S2 S1 Y dφ X

Vector Analysis What about A.B=?, AxB=? and AB=? Scalar and Vector product: A.B=ABcosθ Scalar or (Axi+Ayj+Azk).(Bxi+Byj+Bzk)=AxBx+AyBy+AzBz AxB=ABSinθ n Vector (Result of cross product is always perpendicular(normal) to the plane of A and B n B A

Scalar and Vector Fields A scalar field is a function that gives us a single value of some variable for every point in space. voltage, current, energy, temperature A vector is a quantity which has both a magnitude and a direction in space. velocity, momentum, acceleration and force

Gradient, Divergence and Curl The Del Operator Gradient of a scalar function is a vector quantity. Divergence of a vector is a scalar quantity. Curl of a vector is a vector quantity. Vector

Fundamental theorem for divergence and curl Gauss divergence theorem: Stokes curl theorem Conversion of volume integral to surface integral and vice verse. Conversion of surface integral to line integral and vice verse.

Operator in Cartesian Coordinate System Gradient: gradT: points the direction of maximum increase of the function T. Divergence: Curl: as where

Operator in Cylindrical Coordinate System Volume Element: Gradient: Divergence: Curl:

Operator In Spherical Coordinate System Gradient : Divergence: Curl:

Divergence or Gauss’ Theorem Basic Vector Calculus Divergence or Gauss’ Theorem The divergence theorem states that the total outward flux of a vector field F through the closed surface S is the same as the volume integral of the divergence of F. Closed surface S, volume V, outward pointing normal

Stokes’ Theorem Stokes’s theorem states that the circulation of a vector field F around a closed path L is equal to the surface integral of the curl of F over the open surface S bounded by L Oriented boundary L