Polarization and Related Antenna Parameters

Size: px
Start display at page:

Download "Polarization and Related Antenna Parameters"

Transcription

1 ANTENTOP , # 009 Polarization and Related Antenna Parameters Feel Yourself a Student! Dear friends, I would like to give to ou an interesting and reliable antenna theor. Hours searching in the web gave me lots theoretical information about antennas. Reall, at first I did not know what information to chose for ANTENTOP. Finall, I stopped on lectures Modern Antennas in Wireless Telecommunications written b Prof. Natalia K. Nikolova from McMaster Universit, Hamilton, Canada. You ask me: Wh? Well, I have read man tetbooks on Antennas, both, as in Russian as in English. So, I have the possibilit to compare different tetbook, and I think, that the lectures give knowledge in antenna field in great wa. Here first lecture Introduction into Antenna Stud is here. Net issues of ANTENTOP will contain some other lectures. So, feel ourself a student! Go to Antenna Studies! I.G. M Friends, the above placed Intro was given at ANTENTOP to Antennas ectures. Now I know, that the ecture is one of popular topics of ANTENTOP. Ever Antenna ecture was downloaded more than 1000 times! Now I want to present to ou one more ver interesting ecture - it is a ecture Polarization and Related Antenna Parameters. I believe, ou cannot find such info anwhere for free! Ver interesting and ver useful info for ever ham, for ever radio- engineer. So, feel ourself a student! Go to Antenna Studies! I.G. McMaster Universit Hall Prof. Natalia K. Nikolova Polarization and Related Antenna Parameters Polarization of EM fields revision. Polarization vector. Antenna polarization. Polarization loss factor and polarization efficienc. b Prof. Natalia K. Nikolova mirror: Page-5

2 ecture 5: Polarization and Related Antenna Parameters (Polarization of EM fields revision. Polarization vector. Antenna polarization. Polarization loss factor and polarization efficienc.) 1. Polarization of EM fields. The polarization of the EM field describes the time variations of the field vectors at a given point. In other words, it describes the wa the direction and magnitude the field vectors (usuall E ) change in time. The polarization is the figure traced b the etremit of the timevaring field vector at a given point. According to the shape of the trace, three tpes of polarization eist for harmonic fields: linear, circular and elliptical: E z ω z E z E (a) linear polarization (b) circular polarization (c) elliptical polarization An tpe of polarization can be represented b two orthogonal linear polarizations, ( E, E )or(, E H E V ), whose fields are out of phase b an angle of δ. If δ = 0 or nπ, then a linear polarization results. If δ = π / (90 ) and E = E, then a circular polarization results. In the most general case, elliptical polarization is defined. 6

3 It is also true that an tpe of polarization can be represented b a right-hand circular and a left-hand circular polarizations ( E, E ). We shall revise the above statements and definitions, while introducing the new concept of polarization vector.. Field polarization in terms of two orthogonal linearl polarized components. The polarization of an field can be represented b a suitable set of two orthogonal linearl polarized fields. Assume that locall a far field propagates along the z-ais, and the field vectors have onl transverse components. Then, the set of two orthogonal linearl polarized fields along the -ais and along the -ais, is sufficient to represent an TEM z field. We shall use this arrangement to demonstrate the idea of polarization vector. The field (time-dependent vector or phasor vector) is decomposed into two orthogonal components: e = e + e E = E + E, (5.1) e = Ecos( ωt βz) ˆ E = Eˆ (5.) jδ e = Ecos( ωt βz+ δ) ˆ E = Ee ˆ At a fied position (assume z = 0), equation (5.1) can be written as: et () = ˆ Ecosωt+ ˆ Ecos( ωt+ δ) (5.3) j E = ˆ E + ˆ E e δ R Case 1: inear polarization: δ = nπ, n= 0,1,, et ( ) = ˆ Ecos( ωt) + ˆ Ecos( ωt± nπ) E = ˆ E ± ˆ E (5.) 7

4 δ = kπ τ > 0 δ = (k + 1) π τ < 0 E τ E E E τ E E E τ =± arctan E (a) Case : Circular polarization: (b) π E = E = Em and δ =± + nπ, n= 0,1,, et () = ˆ Ecos( ωt) + ˆ Ecos[ ωt± ( π / + nπ)] E = E ( ˆ± ˆ j) m (5.5) 8

5 E = E ( ˆ+ jˆ) m π δ =+ + nπ 3π 5π 7π E = E ( ˆ jˆ) m π δ = nπ π 3π π ωt = π z 0 ωt = π z 0 3π π π If ( zˆ) is the direction of propagation: clockwise (CW) or right-hand polarization 5π 3π 7π If ( zˆ) is the direction of propagation: counterclockwise (CCW) or left-hand polarization 9

6 A picture of the field vector (at a particular moment of time) along the direction of propagation (left-hand circularl polarized wave): β z β z 10

7 Case 3: Elliptical polarization The field vector at a given point traces an ellipse as a function of time. This is the most general tpe of polarization of time-harmonic fields, obtained for an phase difference δ and an ratio ( E/ E ). Mathematicall, the linear and the circular polarizations are special cases of the elliptical polarization. In practice, however, the term elliptical polarization is used to indicate polarizations other than linear or circular. et ( ) = ˆ Ecosωt+ ˆ Ecos( ωt+ δ) j E = ˆ E + ˆ E e δ Show that the trace of the time-dependent vector is an ellipse: e () t = E (cosωt cosδ sinωt sin δ ) where: e cos () t E and e sin 1 ( t) ωt = E (5.6) () () e() t e() t e t e t sin δ = cosδ E E + E E or 1 = () t () t ()cos t δ + () t, (5.7) e () t cos t t () = ω Esinδ = sinδ ; e () t cos( ωt + δ ) t () = = E sinδ sinδ Equation (5.7) is the parametric equation of an ellipse centered in the plane. It describes the motion of a point of coordinates e( t) and e( t) along an ellipse with a frequenc ω. The elliptical polarization can also be right-hand and left-hand polarization, depending on the relation between the direction of propagation and the direction of rotation. 11

8 e( t) E major ais ( OA) E ω minor ais ( OB) τ E e () t The parameters of the polarization ellipse are given below. Their derivation is given in Appendi I. a) major ais ( OA ) OA = 1 E + E + E + E + EE cos( δ ) (5.8) b) minor ais ( OB) OB = 1 E + E E + E + EE cos( δ ) (5.9) c) tilt angle τ 1 EE τ = arctan cos δ E E (5.10) d) aial ratio AR = major ais OA minor ais OB (5.11) Note: The linear and circular polarizations can be considered as special cases of the elliptical polarization. π If δ =± + nπ and E = E,thenOA= OB= E = E; the ellipse becomes a circle. 1

9 E If δ = nπ,thenob= 0and τ =± arctan ; the ellipse collapses into E a line. 3. Field polarization in terms of two circularl polarized components The representation of a comple vector field in terms of circularl polarized components is somewhat less eas to perceive but it is actuall more useful in the calculation of the polarization ellipse parameters. E = E R( ˆ+ jˆ) + E ( ˆ jˆ) (5.1) Assuming a relative phase difference of δc = ϕ ϕr, one can write (5.1) as: jδc E = ER( ˆ + jˆ) + Ee ( ˆ jˆ) (5.13) The relation between the linear-component and the circular-component representations of the field polarization is easil found as: E = ˆ( E R + E ) + ˆ j( E R E ) (5.1) E E. Polarization vector and polarization ratio The polarization vector is the normalized phasor of the electric field vector. It is a comple-number vector of unit magnitude and direction coinciding with the direction of the electric field vector. E E E ˆ ρ = = ˆ + ˆ e, E = E + E jδ m Em Em Em (5.15) The polarization vector takes the following forms in some special cases: Case 1: inear polarization ˆ ρ = E E ˆ ˆ, Em E E E ± m E = + (5.16) m Case : Circular polarization 13

10 1 ˆ ρ = ( ˆ± ˆ j), Em = E = E (5.17) The polarization ratio is the ratio of the phasors of the two orthogonal polarization components. It is a comple number. j E δ E e E δ r = re = = or r = E E E V H (5.18) Point of interest: In the case of circular polarization, the polarization ratio is defined as: jδ E C R r C = rce = (5.19) E The circular polarization ratio r C is of particular interest since the aial ratio of the polarization ellipse AR can be epressed as: rc + 1 AR = (5.0) r 1 Besides, its tilt angle is: δ τ = C (5.1) Comparing (5.10) and (5.1) readil shows the relation between the phase difference of the circular-polarization representation and the linear polarization j ratio r = re δ : r δc = arctan cosδ (5.) 1 r One can calculate r C from the linear polarization ratio r making use of (5.11) and (5.0): C δ δ rc r + 1+ r + r cos( ) = rc 1 1+ r 1+ r + r cos( ) (5.3) 1

11 Using (5.) and (5.3) allows eas switching between the representation of the wave polarization in terms of linear and circular components. 5. Antenna polarization The polarization of a radiated wave (polarization of a radiating antenna) at a specific point in the far zone is the polarization of the locall plane wave. The polarization of a received wave (polarization of a receiving antenna) is the polarization of a plane wave, incident from a given direction, and having given power flu densit, which results in maimum available power at the antenna terminals. 6. Polarization loss factor and polarization efficienc Generall, the polarization of the receiving antenna is not the same as the polarization of the incident wave. This is called polarization mismatch. The polarization loss factor (PF) characterizes the loss of EM power because of polarization mismatch. PF ˆ ˆ The above definition is based on the representation of the incident field and the antenna polarization b their polarization vectors. If the incident field is i i E = Em ˆ ρi, then the field of the same magnitude that would produce maimum received power at the antenna terminals is i E = E ˆ ρ. = ρi ρa (5.) a m a 15

12 If the antenna is polarization matched, then PF = 1, and there is no polarization power loss. If PF = 0, then the antenna is incapable of receiving the signal. 0 PF 1 (5.5) The polarization efficienc has the same phsical meaning as the PF. Eamples Eample 5.1. The electric field of a linearl polarized EM wave is i j z E = ˆ Em(, ) e β It is incident upon a linearl polarized antenna whose polarization is: Ea = ( ˆ+ ˆ) E( r, θ, ϕ) Find the PF. 16

13 1 1 PF = ˆ ( ˆ+ ˆ) = PF = 10log 0.5 = 3 [db] 10 Eample 5.. A transmitting antenna produces a far-zone field, which is right-circularl polarized. This field impinges upon a receiving antenna, whose polarization (in transmitting mode) is also right-circular. Determine the PF. Both antennas (the transmitting one and the receiving one) are rightcircularl polarized in transmitting mode. et s assume that a transmitting antenna is located at the center of a spherical coordinate sstem. The farzone field it would produce is described as: far E = E ˆ m θ cosωt+ ˆ ϕ cos ( ωt π / ) It is a right-circularl polarized field with respect to the outward radial direction. Its polarization vector is: ˆ θ j ˆ ϕ ˆ ρ = According to the definitions in Section, this is eactl the polarization vector of a transmitting antenna. 17

14 z E ϕ ϕ θ r E θ far This same field E is incident upon a receiving antenna, which has the ˆ θa j ˆ ϕa polarization vector ˆ ρa = in its own coordinate sstem ( ra, θa, ϕ a). However, this field propagates along r a in the ( ra, θa, ϕa) coordinate sstem, and, therefore, its polarization vector becomes: ˆ θa + j ˆ ϕa ˆ ρi = The PF is calculated as: ˆ ˆ ( θa + jˆ ϕa)( θa jˆ ϕa) PF = ˆ ρi ˆ ρa = = 1, PF[dB] = 10log101 = 0 There are no polarization losses. 18

15 Eercise: Show that an antenna of right-circular polarization (in transmitting mode) cannot receive left-circularl polarized incident wave (or a wave emitted b a left-circularl polarized antenna). Appendi I Find the tilt angle τ, the length of the major ais OA, and the length of the minor ais OB of the ellipse described b the equation: e () () ( ) ( ) t e t e t e t sin δ = cosδ E E + (A-1) E E e( t) E major ais ( OA) E ω minor ais ( OB) τ E e( t) Equation (A-1) can be written as: a b + c = 1, (A-) where: = e( t) and = e( t) are the coordinates of a point of the ellipse centeredinthe plane; 1 a E sin δ cosδ b = ; EE sin δ 19

16 1 c = E sin δ. After dividing both sides of (A-) b ( ), one obtains 1 a b+ c = () Introducing ξ = e t = e() t, one obtains that 1 = cξ bξ + a (1 + ξ ) ρ ( ξ) = + = (1 + ξ ) = (A-) cξ bξ + a Here, ρ is the distance of the ellipse point from the center of the coordinate sstem. We want to know at what ξ values the maimum and the minimum of ρ occur. This will produce the tilt angle τ. We also want to know what are the values of ρma and ρ min. Then, we have to solve d( ρ ) = 0,or dξ ( a c) ξ ξ 1 = 0 (A-5) b (A-5) is better solved for the angle α, such that π ξ = tan α = ; α = τ (A-6) Substituting (A-6) in (A-5) ields: sinα sinα C 1= 0 cos α cosα cosα a c E E where C = =. b E E cosδ The solution of (A-7) is: (A-3) (A-7) 0

17 1 EE cos 1 arctan δ π α = ; α = α1+ E E τ = α 1, 1, Substituting α 1 and α back in ρ ields the epressions for OA and OB. (A-8) 1

ECE 6340 Intermediate EM Waves. Fall 2016 Prof. David R. Jackson Dept. of ECE. Notes 16

ECE 6340 Intermediate EM Waves. Fall 2016 Prof. David R. Jackson Dept. of ECE. Notes 16 C 6340 Intermediate M Waves Fall 2016 Prof. David R. Jackson Dept. of C Notes 16 1 Polarization of Waves Consider a plane wave with both and components (,, z) = ( ˆ + ˆ ) e jkz Assume j0 = ae = a = j be

More information

Mathematics 309 Conic sections and their applicationsn. Chapter 2. Quadric figures. ai,j x i x j + b i x i + c =0. 1. Coordinate changes

Mathematics 309 Conic sections and their applicationsn. Chapter 2. Quadric figures. ai,j x i x j + b i x i + c =0. 1. Coordinate changes Mathematics 309 Conic sections and their applicationsn Chapter 2. Quadric figures In this chapter want to outline quickl how to decide what figure associated in 2D and 3D to quadratic equations look like.

More information

15. Polarization. Linear, circular, and elliptical polarization. Mathematics of polarization. Uniaxial crystals. Birefringence.

15. Polarization. Linear, circular, and elliptical polarization. Mathematics of polarization. Uniaxial crystals. Birefringence. 15. Polarization Linear, circular, and elliptical polarization Mathematics of polarization Uniaial crstals Birefringence Polarizers Notation: polarization near an interface Parallel ("p") polarization

More information

Strain Transformation and Rosette Gage Theory

Strain Transformation and Rosette Gage Theory Strain Transformation and Rosette Gage Theor It is often desired to measure the full state of strain on the surface of a part, that is to measure not onl the two etensional strains, and, but also the shear

More information

Systems of Linear Equations: Solving by Graphing

Systems of Linear Equations: Solving by Graphing 8.1 Sstems of Linear Equations: Solving b Graphing 8.1 OBJECTIVE 1. Find the solution(s) for a set of linear equations b graphing NOTE There is no other ordered pair that satisfies both equations. From

More information

Physics Gravitational force. 2. Strong or color force. 3. Electroweak force

Physics Gravitational force. 2. Strong or color force. 3. Electroweak force Phsics 360 Notes on Griffths - pluses and minuses No tetbook is perfect, and Griffithsisnoeception. Themajorplusisthat it is prett readable. For minuses, see below. Much of what G sas about the del operator

More information

Math 123 Summary of Important Algebra & Trigonometry Concepts Chapter 1 & Appendix D, Stewart, Calculus Early Transcendentals

Math 123 Summary of Important Algebra & Trigonometry Concepts Chapter 1 & Appendix D, Stewart, Calculus Early Transcendentals Math Summar of Important Algebra & Trigonometr Concepts Chapter & Appendi D, Stewart, Calculus Earl Transcendentals Function a rule that assigns to each element in a set D eactl one element, called f (

More information

Chapter 14 Matrix Treatment of Polarization

Chapter 14 Matrix Treatment of Polarization Chapter 4 Matri Treatment of Polarization Lecture Notes for Modern Optics based on Pedrotti & Pedrotti & Pedrotti Instructor: Naer Eradat Spring 29 5//29 Matri Treatment of Polarization Polarization Polarization

More information

x y plane is the plane in which the stresses act, yy xy xy Figure 3.5.1: non-zero stress components acting in the x y plane

x y plane is the plane in which the stresses act, yy xy xy Figure 3.5.1: non-zero stress components acting in the x y plane 3.5 Plane Stress This section is concerned with a special two-dimensional state of stress called plane stress. It is important for two reasons: () it arises in real components (particularl in thin components

More information

APPENDIX D Rotation and the General Second-Degree Equation

APPENDIX D Rotation and the General Second-Degree Equation APPENDIX D Rotation and the General Second-Degree Equation Rotation of Aes Invariants Under Rotation After rotation of the - and -aes counterclockwise through an angle, the rotated aes are denoted as the

More information

Symmetry Arguments and the Role They Play in Using Gauss Law

Symmetry Arguments and the Role They Play in Using Gauss Law Smmetr Arguments and the Role The la in Using Gauss Law K. M. Westerberg (9/2005) Smmetr plas a ver important role in science in general, and phsics in particular. Arguments based on smmetr can often simplif

More information

y R T However, the calculations are easier, when carried out using the polar set of co-ordinates ϕ,r. The relations between the co-ordinates are:

y R T However, the calculations are easier, when carried out using the polar set of co-ordinates ϕ,r. The relations between the co-ordinates are: Curved beams. Introduction Curved beams also called arches were invented about ears ago. he purpose was to form such a structure that would transfer loads, mainl the dead weight, to the ground b the elements

More information

Electromagnetic Waves

Electromagnetic Waves May 7, 2008 1 1 J.D.Jackson, Classical Electrodynamics, 2nd Edition, Section 7 Maxwell Equations In a region of space where there are no free sources (ρ = 0, J = 0), Maxwell s equations reduce to a simple

More information

Triple Integrals in Cartesian Coordinates. Triple Integrals in Cylindrical Coordinates. Triple Integrals in Spherical Coordinates

Triple Integrals in Cartesian Coordinates. Triple Integrals in Cylindrical Coordinates. Triple Integrals in Spherical Coordinates Chapter 3 Multiple Integral 3. Double Integrals 3. Iterated Integrals 3.3 Double Integrals in Polar Coordinates 3.4 Triple Integrals Triple Integrals in Cartesian Coordinates Triple Integrals in Clindrical

More information

11.4 Polar Coordinates

11.4 Polar Coordinates 11. Polar Coordinates 917 11. Polar Coordinates In Section 1.1, we introduced the Cartesian coordinates of a point in the plane as a means of assigning ordered pairs of numbers to points in the plane.

More information

All parabolas through three non-collinear points

All parabolas through three non-collinear points ALL PARABOLAS THROUGH THREE NON-COLLINEAR POINTS 03 All parabolas through three non-collinear points STANLEY R. HUDDY and MICHAEL A. JONES If no two of three non-collinear points share the same -coordinate,

More information

MATH Line integrals III Fall The fundamental theorem of line integrals. In general C

MATH Line integrals III Fall The fundamental theorem of line integrals. In general C MATH 255 Line integrals III Fall 216 In general 1. The fundamental theorem of line integrals v T ds depends on the curve between the starting point and the ending point. onsider two was to get from (1,

More information

Section 8.5 Parametric Equations

Section 8.5 Parametric Equations 504 Chapter 8 Section 8.5 Parametric Equations Man shapes, even ones as simple as circles, cannot be represented as an equation where is a function of. Consider, for eample, the path a moon follows as

More information

The Force Table Introduction: Theory:

The Force Table Introduction: Theory: 1 The Force Table Introduction: "The Force Table" is a simple tool for demonstrating Newton s First Law and the vector nature of forces. This tool is based on the principle of equilibrium. An object is

More information

4 The Cartesian Coordinate System- Pictures of Equations

4 The Cartesian Coordinate System- Pictures of Equations The Cartesian Coordinate Sstem- Pictures of Equations Concepts: The Cartesian Coordinate Sstem Graphs of Equations in Two Variables -intercepts and -intercepts Distance in Two Dimensions and the Pthagorean

More information

Exact Differential Equations. The general solution of the equation is f x, y C. If f has continuous second partials, then M y 2 f

Exact Differential Equations. The general solution of the equation is f x, y C. If f has continuous second partials, then M y 2 f APPENDIX C Additional Topics in Differential Equations APPENDIX C. Eact First-Order Equations Eact Differential Equations Integrating Factors Eact Differential Equations In Chapter 6, ou studied applications

More information

Phys 322 Lecture 21. Chapter 8 Polarization

Phys 322 Lecture 21. Chapter 8 Polarization Phs 3 Lecture 1 Chapter 8 Polarization Plane of polarization Transverse M wave B Plane of polarization - plane defined b vector and k: Plane of polarization z: z t ˆi z, t ˆi coskz t, z Linearl (plane)

More information

17.3. Parametric Curves. Introduction. Prerequisites. Learning Outcomes

17.3. Parametric Curves. Introduction. Prerequisites. Learning Outcomes Parametric Curves 7.3 Introduction In this Section we eamine et another wa of defining curves - the parametric description. We shall see that this is, in some was, far more useful than either the Cartesian

More information

Separation of Variables in Cartesian Coordinates

Separation of Variables in Cartesian Coordinates Lecture 9 Separation of Variables in Cartesian Coordinates Phs 3750 Overview and Motivation: Toda we begin a more in-depth loo at the 3D wave euation. We introduce a techniue for finding solutions to partial

More information

LESSON #42 - INVERSES OF FUNCTIONS AND FUNCTION NOTATION PART 2 COMMON CORE ALGEBRA II

LESSON #42 - INVERSES OF FUNCTIONS AND FUNCTION NOTATION PART 2 COMMON CORE ALGEBRA II LESSON #4 - INVERSES OF FUNCTIONS AND FUNCTION NOTATION PART COMMON CORE ALGEBRA II You will recall from unit 1 that in order to find the inverse of a function, ou must switch and and solve for. Also,

More information

Chapter 3. Theory of measurement

Chapter 3. Theory of measurement Chapter. Introduction An energetic He + -ion beam is incident on thermal sodium atoms. Figure. shows the configuration in which the interaction one is determined b the crossing of the laser-, sodium- and

More information

10.2 The Unit Circle: Cosine and Sine

10.2 The Unit Circle: Cosine and Sine 0. The Unit Circle: Cosine and Sine 77 0. The Unit Circle: Cosine and Sine In Section 0.., we introduced circular motion and derived a formula which describes the linear velocit of an object moving on

More information

And similarly in the other directions, so the overall result is expressed compactly as,

And similarly in the other directions, so the overall result is expressed compactly as, SQEP Tutorial Session 5: T7S0 Relates to Knowledge & Skills.5,.8 Last Update: //3 Force on an element of area; Definition of principal stresses and strains; Definition of Tresca and Mises equivalent stresses;

More information

Lab 9: Polarization Phy208 Spring 2008

Lab 9: Polarization Phy208 Spring 2008 Lab 9: Polarization Ph208 Spring 2008 Name Section This sheet is the lab document our TA will use to score our lab. It is to be turned in at the end of lab. To receive full credit ou must use complete

More information

14.1 Systems of Linear Equations in Two Variables

14.1 Systems of Linear Equations in Two Variables 86 Chapter 1 Sstems of Equations and Matrices 1.1 Sstems of Linear Equations in Two Variables Use the method of substitution to solve sstems of equations in two variables. Use the method of elimination

More information

The details of the derivation of the equations of conics are com-

The details of the derivation of the equations of conics are com- Part 6 Conic sections Introduction Consider the double cone shown in the diagram, joined at the verte. These cones are right circular cones in the sense that slicing the double cones with planes at right-angles

More information

VECTORS IN THREE DIMENSIONS

VECTORS IN THREE DIMENSIONS 1 CHAPTER 2. BASIC TRIGONOMETRY 1 INSTITIÚID TEICNEOLAÍOCHTA CHEATHARLACH INSTITUTE OF TECHNOLOGY CARLOW VECTORS IN THREE DIMENSIONS 1 Vectors in Two Dimensions A vector is an object which has magnitude

More information

( ) ( ) ( ) ( ) TNM046: Datorgrafik. Transformations. Linear Algebra. Linear Algebra. Sasan Gooran VT Transposition. Scalar (dot) product:

( ) ( ) ( ) ( ) TNM046: Datorgrafik. Transformations. Linear Algebra. Linear Algebra. Sasan Gooran VT Transposition. Scalar (dot) product: TNM046: Datorgrafik Transformations Sasan Gooran VT 04 Linear Algebra ( ) ( ) =,, 3 =,, 3 Transposition t = 3 t = 3 Scalar (dot) product: Length (Norm): = t = + + 3 3 = = + + 3 Normaliation: ˆ = Linear

More information

roth t dive = 0 (4.2.3) divh = 0 (4.2.4) Chapter 4 Waves in Unbounded Medium Electromagnetic Sources 4.2 Uniform plane waves in free space

roth t dive = 0 (4.2.3) divh = 0 (4.2.4) Chapter 4 Waves in Unbounded Medium Electromagnetic Sources 4.2 Uniform plane waves in free space Chapter 4 Waves in Unbounded Medium 4. lectromagnetic Sources 4. Uniform plane waves in free space Mawell s equation in free space is given b: H rot = (4..) roth = (4..) div = (4..3) divh = (4..4) which

More information

SECTION 8-7 De Moivre s Theorem. De Moivre s Theorem, n a Natural Number nth-roots of z

SECTION 8-7 De Moivre s Theorem. De Moivre s Theorem, n a Natural Number nth-roots of z 8-7 De Moivre s Theorem 635 B eactl; compute the modulus and argument for part C to two decimal places. 9. (A) 3 i (B) 1 i (C) 5 6i 10. (A) 1 i 3 (B) 3i (C) 7 4i 11. (A) i 3 (B) 3 i (C) 8 5i 12. (A) 3

More information

Stress and Strain ( , 3.14) MAE 316 Strength of Mechanical Components NC State University Department of Mechanical & Aerospace Engineering

Stress and Strain ( , 3.14) MAE 316 Strength of Mechanical Components NC State University Department of Mechanical & Aerospace Engineering (3.8-3.1, 3.14) MAE 316 Strength of Mechanical Components NC State Universit Department of Mechanical & Aerospace Engineering 1 Introduction MAE 316 is a continuation of MAE 314 (solid mechanics) Review

More information

MECHANICS OF MATERIALS

MECHANICS OF MATERIALS CHAPTER MECHANICS OF MATERIALS Ferdinand P. Beer E. Russell Johnston, Jr. John T. DeWolf Lecture Notes: J. Walt Oler Teas Tech Universit Transformations of Stress and Strain 006 The McGraw-Hill Companies,

More information

8.7 Systems of Non-Linear Equations and Inequalities

8.7 Systems of Non-Linear Equations and Inequalities 8.7 Sstems of Non-Linear Equations and Inequalities 67 8.7 Sstems of Non-Linear Equations and Inequalities In this section, we stud sstems of non-linear equations and inequalities. Unlike the sstems of

More information

Coordinate geometry. + bx + c. Vertical asymptote. Sketch graphs of hyperbolas (including asymptotic behaviour) from the general

Coordinate geometry. + bx + c. Vertical asymptote. Sketch graphs of hyperbolas (including asymptotic behaviour) from the general A Sketch graphs of = a m b n c where m = or and n = or B Reciprocal graphs C Graphs of circles and ellipses D Graphs of hperbolas E Partial fractions F Sketch graphs using partial fractions Coordinate

More information

ES.1803 Topic 16 Notes Jeremy Orloff

ES.1803 Topic 16 Notes Jeremy Orloff ES803 Topic 6 Notes Jerem Orloff 6 Eigenalues, diagonalization, decoupling This note coers topics that will take us seeral classes to get through We will look almost eclusiel at 2 2 matrices These hae

More information

Effects of birefringence on Fizeau interferometry that uses polarization phase shifting technique

Effects of birefringence on Fizeau interferometry that uses polarization phase shifting technique Effects of birefringence on Fizeau interferometr that uses polarization phase shifting technique Chunu Zhao, Dongel Kang and James H. Burge College of Optical Sciences, the Universit of Arizona 1630 E.

More information

17.3. Parametric Curves. Introduction. Prerequisites. Learning Outcomes

17.3. Parametric Curves. Introduction. Prerequisites. Learning Outcomes Parametric Curves 17.3 Introduction In this section we eamine et another wa of defining curves - the parametric description. We shall see that this is, in some was, far more useful than either the Cartesian

More information

On Range and Reflecting Functions About the Line y = mx

On Range and Reflecting Functions About the Line y = mx On Range and Reflecting Functions About the Line = m Scott J. Beslin Brian K. Heck Jerem J. Becnel Dept.of Mathematics and Dept. of Mathematics and Dept. of Mathematics and Computer Science Computer Science

More information

Section 3.1. ; X = (0, 1]. (i) f : R R R, f (x, y) = x y

Section 3.1. ; X = (0, 1]. (i) f : R R R, f (x, y) = x y Paul J. Bruillard MATH 0.970 Problem Set 6 An Introduction to Abstract Mathematics R. Bond and W. Keane Section 3.1: 3b,c,e,i, 4bd, 6, 9, 15, 16, 18c,e, 19a, 0, 1b Section 3.: 1f,i, e, 6, 1e,f,h, 13e,

More information

Methods of Solving Ordinary Differential Equations (Online)

Methods of Solving Ordinary Differential Equations (Online) 7in 0in Felder c0_online.te V3 - Januar, 05 0:5 A.M. Page CHAPTER 0 Methods of Solving Ordinar Differential Equations (Online) 0.3 Phase Portraits Just as a slope field (Section.4) gives us a wa to visualize

More information

Limits. Calculus Module C06. Copyright This publication The Northern Alberta Institute of Technology All Rights Reserved.

Limits. Calculus Module C06. Copyright This publication The Northern Alberta Institute of Technology All Rights Reserved. e Calculus Module C Limits Copright This publication The Northern Alberta Institute of Technolog. All Rights Reserved. LAST REVISED March, Introduction to Limits Statement of Prerequisite Skills Complete

More information

9.1 VECTORS. A Geometric View of Vectors LEARNING OBJECTIVES. = a, b

9.1 VECTORS. A Geometric View of Vectors LEARNING OBJECTIVES. = a, b vectors and POLAR COORDINATES LEARNING OBJECTIVES In this section, ou will: View vectors geometricall. Find magnitude and direction. Perform vector addition and scalar multiplication. Find the component

More information

x c x c This suggests the following definition.

x c x c This suggests the following definition. 110 Chapter 1 / Limits and Continuit 1.5 CONTINUITY A thrown baseball cannot vanish at some point and reappear someplace else to continue its motion. Thus, we perceive the path of the ball as an unbroken

More information

Plane Wave: Introduction

Plane Wave: Introduction Plane Wave: Introduction According to Mawell s equations a timevarying electric field produces a time-varying magnetic field and conversely a time-varying magnetic field produces an electric field ( i.e.

More information

Space frames. b) R z φ z. R x. Figure 1 Sign convention: a) Displacements; b) Reactions

Space frames. b) R z φ z. R x. Figure 1 Sign convention: a) Displacements; b) Reactions Lecture notes: Structural Analsis II Space frames I. asic concepts. The design of a building is generall accomplished b considering the structure as an assemblage of planar frames, each of which is designed

More information

Eigenvectors and Eigenvalues 1

Eigenvectors and Eigenvalues 1 Ma 2015 page 1 Eigenvectors and Eigenvalues 1 In this handout, we will eplore eigenvectors and eigenvalues. We will begin with an eploration, then provide some direct eplanation and worked eamples, and

More information

a. plotting points in Cartesian coordinates (Grade 9 and 10), b. using a graphing calculator such as the TI-83 Graphing Calculator,

a. plotting points in Cartesian coordinates (Grade 9 and 10), b. using a graphing calculator such as the TI-83 Graphing Calculator, GRADE PRE-CALCULUS UNIT C: QUADRATIC FUNCTIONS CLASS NOTES FRAME. After linear functions, = m + b, and their graph the Quadratic Functions are the net most important equation or function. The Quadratic

More information

Hurricane Modeling E XPANDING C ALCULUS H ORIZON

Hurricane Modeling E XPANDING C ALCULUS H ORIZON Februar 5, 2009 :4 Hurricane Modeling E XPANDING THE Sheet number Page number can magenta ellow black C ALCULUS H ORIZON Hurricane Modeling... Each ear population centers throughout the world are ravaged

More information

Wave Phenomena Physics 15c

Wave Phenomena Physics 15c Wave Phenomena Phsics 15c Lecture 13 Multi-Dimensional Waves (H&L Chapter 7) Term Paper Topics! Have ou found a topic for the paper?! 2/3 of the class have, or have scheduled a meeting with me! If ou haven

More information

hydrogen atom: center-of-mass and relative

hydrogen atom: center-of-mass and relative hdrogen atom: center-of-mass and relative apple ~ m e e -particle problem (electron & proton) ~ m p p + V ( ~r e ~r p ) (~r e, ~r p )=E (~r e, ~r p ) separation in center-of-mass and relative coordinates

More information

One-Dimensional Wave Propagation (without distortion or attenuation)

One-Dimensional Wave Propagation (without distortion or attenuation) Phsics 306: Waves Lecture 1 1//008 Phsics 306 Spring, 008 Waves and Optics Sllabus To get a good grade: Stud hard Come to class Email: satapal@phsics.gmu.edu Surve of waves One-Dimensional Wave Propagation

More information

14. Matrix treatment of polarization

14. Matrix treatment of polarization 14. Matri treatment of polarization This lecture Polarized Light : linear, circular, elliptical Jones Vectors for Polarized Light Jones Matrices for Polarizers, Phase Retarders, Rotators (Linear) Polarization

More information

Lab 10: Polarization Phy248 Spring 2009

Lab 10: Polarization Phy248 Spring 2009 Lab 10: Polarization Ph248 Spring 2009 Name Section This sheet is the lab document our TA will use to score our lab. It is to be turned in at the end of lab. To receive full credit ou must use complete

More information

MATRIX TRANSFORMATIONS

MATRIX TRANSFORMATIONS CHAPTER 5. MATRIX TRANSFORMATIONS INSTITIÚID TEICNEOLAÍOCHTA CHEATHARLACH INSTITUTE OF TECHNOLOGY CARLOW MATRIX TRANSFORMATIONS Matri Transformations Definition Let A and B be sets. A function f : A B

More information

Lecture 1a. Complex numbers, phasors and vectors. Introduction. Complex numbers. 1a.1

Lecture 1a. Complex numbers, phasors and vectors. Introduction. Complex numbers. 1a.1 1a.1 Lecture 1a Comple numbers, phasors and vectors Introduction This course will require ou to appl several concepts ou learned in our undergraduate math courses. In some cases, such as comple numbers

More information

Lecture 5. Equations of Lines and Planes. Dan Nichols MATH 233, Spring 2018 University of Massachusetts.

Lecture 5. Equations of Lines and Planes. Dan Nichols MATH 233, Spring 2018 University of Massachusetts. Lecture 5 Equations of Lines and Planes Dan Nichols nichols@math.umass.edu MATH 233, Spring 2018 Universit of Massachusetts Februar 6, 2018 (2) Upcoming midterm eam First midterm: Wednesda Feb. 21, 7:00-9:00

More information

Physics Letters A 374 (2010) Contents lists available at ScienceDirect. Physics Letters A.

Physics Letters A 374 (2010) Contents lists available at ScienceDirect. Physics Letters A. Physics Letters A 374 (2010) 1063 1067 Contents lists available at ScienceDirect Physics Letters A www.elsevier.com/locate/pla Macroscopic far-field observation of the sub-wavelength near-field dipole

More information

15. Eigenvalues, Eigenvectors

15. Eigenvalues, Eigenvectors 5 Eigenvalues, Eigenvectors Matri of a Linear Transformation Consider a linear ( transformation ) L : a b R 2 R 2 Suppose we know that L and L Then c d because of linearit, we can determine what L does

More information

Wave Phenomena Physics 15c

Wave Phenomena Physics 15c Wave Phenomena Phsics 15c Lecture 13 Multi-Dimensional Waves (H&L Chapter 7) Term Paper Topics! Have ou found a topic for the paper?! 2/3 of the class have, or have scheduled a meeting with me! If ou haven

More information

University of Waterloo Faculty of Mathematics. MATH 227: Calculus 3 for Honours Physics

University of Waterloo Faculty of Mathematics. MATH 227: Calculus 3 for Honours Physics Universit of Waterloo Facult of Mathematics MATH 227: Calculus 3 for Honours Phsics Fall 2010 Lecture Notes E.R. Vrsca Department of Applied Mathematics c E.R. Vrsca 2010 1 Lecture 1 (Relevant sections

More information

2.5 CONTINUITY. a x. Notice that Definition l implicitly requires three things if f is continuous at a:

2.5 CONTINUITY. a x. Notice that Definition l implicitly requires three things if f is continuous at a: SECTION.5 CONTINUITY 9.5 CONTINUITY We noticed in Section.3 that the it of a function as approaches a can often be found simpl b calculating the value of the function at a. Functions with this propert

More information

Time-Frequency Analysis: Fourier Transforms and Wavelets

Time-Frequency Analysis: Fourier Transforms and Wavelets Chapter 4 Time-Frequenc Analsis: Fourier Transforms and Wavelets 4. Basics of Fourier Series 4.. Introduction Joseph Fourier (768-83) who gave his name to Fourier series, was not the first to use Fourier

More information

Polarized sunglasses. Polarization

Polarized sunglasses. Polarization Polarized sunglasses 3 4 : is a propert of the wave of light that can oscillate with certain orientation; the wave ehibits polarization which has onl one possible polarization, namel the direction in which

More information

Parametric Equations for Circles and Ellipses

Parametric Equations for Circles and Ellipses Lesson 5-8 Parametric Equations for Circles and Ellipses BIG IDEA Parametric equations use separate functions to defi ne coordinates and and to produce graphs Vocabular parameter parametric equations equation

More information

Survey of Wave Types and Characteristics

Survey of Wave Types and Characteristics Seminar: Vibrations and Structure-Borne Sound in Civil Engineering Theor and Applications Surve of Wave Tpes and Characteristics Xiuu Gao April 1 st, 2006 Abstract Mechanical waves are waves which propagate

More information

What is Parametric Equation?

What is Parametric Equation? Chapter 13 Parametric Equation and Locus Wh the graph is so strange? Let s investigate a few points. t -5-4 -3 - -1 0 1 3 4 4 15 8 3 0-1 0 3 8 15-4.04-3.4-3.14 -.91-1.84 0 1.84.91 3.14 3.4 B plotting these

More information

nm nm

nm nm The Quantum Mechanical Model of the Atom You have seen how Bohr s model of the atom eplains the emission spectrum of hdrogen. The emission spectra of other atoms, however, posed a problem. A mercur atom,

More information

Triple Integrals. y x

Triple Integrals. y x Triple Integrals. (a) If is an solid (in space), what does the triple integral dv represent? Wh? (b) Suppose the shape of a solid object is described b the solid, and f(,, ) gives the densit of the object

More information

Math 21a: Multivariable calculus. List of Worksheets. Harvard University, Spring 2009

Math 21a: Multivariable calculus. List of Worksheets. Harvard University, Spring 2009 Math 2a: Multivariable calculus Harvard Universit, Spring 2009 List of Worksheets Vectors and the Dot Product Cross Product and Triple Product Lines and Planes Functions and Graphs Quadric Surfaces Vector-Valued

More information

Ch 3 Alg 2 Note Sheet.doc 3.1 Graphing Systems of Equations

Ch 3 Alg 2 Note Sheet.doc 3.1 Graphing Systems of Equations Ch 3 Alg Note Sheet.doc 3.1 Graphing Sstems of Equations Sstems of Linear Equations A sstem of equations is a set of two or more equations that use the same variables. If the graph of each equation =.4

More information

Mechanics Departmental Exam Last updated November 2013

Mechanics Departmental Exam Last updated November 2013 Mechanics Departmental Eam Last updated November 213 1. Two satellites are moving about each other in circular orbits under the influence of their mutual gravitational attractions. The satellites have

More information

Algebra/Pre-calc Review

Algebra/Pre-calc Review Algebra/Pre-calc Review The following pages contain various algebra and pre-calculus topics that are used in the stud of calculus. These pages were designed so that students can refresh their knowledge

More information

STATICS. Equivalent Systems of Forces. Vector Mechanics for Engineers: Statics VECTOR MECHANICS FOR ENGINEERS: Contents & Objectives.

STATICS. Equivalent Systems of Forces. Vector Mechanics for Engineers: Statics VECTOR MECHANICS FOR ENGINEERS: Contents & Objectives. 3 Rigid CHATER VECTOR ECHANICS FOR ENGINEERS: STATICS Ferdinand. Beer E. Russell Johnston, Jr. Lecture Notes: J. Walt Oler Teas Tech Universit Bodies: Equivalent Sstems of Forces Contents & Objectives

More information

Topic 5.2: Introduction to Vector Fields

Topic 5.2: Introduction to Vector Fields Math 75 Notes Topic 5.: Introduction to Vector Fields Tetbook Section: 16.1 From the Toolbo (what you need from previous classes): Know what a vector is. Be able to sketch a vector using its component

More information

Second-Order Linear Differential Equations C 2

Second-Order Linear Differential Equations C 2 C8 APPENDIX C Additional Topics in Differential Equations APPENDIX C. Second-Order Homogeneous Linear Equations Second-Order Linear Differential Equations Higher-Order Linear Differential Equations Application

More information

University of Regina Department of Mathematics and Statistics

University of Regina Department of Mathematics and Statistics u z v 1. Consider the map Universit of Regina Department of Mathematics and Statistics MATH431/831 Differential Geometr Winter 2014 Homework Assignment No. 3 - Solutions ϕ(u, v) = (cosusinv, sin u sin

More information

Physics 1402: Lecture 18 Today s Agenda

Physics 1402: Lecture 18 Today s Agenda Physics 1402: Lecture 18 Today s Agenda Announcements: Midterm 1 distributed available Homework 05 due Friday Magnetism Calculation of Magnetic Field Two ways to calculate the Magnetic Field: iot-savart

More information

Linear Equation Theory - 2

Linear Equation Theory - 2 Algebra Module A46 Linear Equation Theor - Copright This publication The Northern Alberta Institute of Technolog 00. All Rights Reserved. LAST REVISED June., 009 Linear Equation Theor - Statement of Prerequisite

More information

5.1 Angles and Their Measurements

5.1 Angles and Their Measurements Graduate T.A. Department of Mathematics Dnamical Sstems and Chaos San Diego State Universit November 8, 2011 A ra is the set of points which are part of a line which is finite in one direction, but infinite

More information

Unit 3 NOTES Honors Common Core Math 2 1. Day 1: Properties of Exponents

Unit 3 NOTES Honors Common Core Math 2 1. Day 1: Properties of Exponents Unit NOTES Honors Common Core Math Da : Properties of Eponents Warm-Up: Before we begin toda s lesson, how much do ou remember about eponents? Use epanded form to write the rules for the eponents. OBJECTIVE

More information

Chapter 18 Quadratic Function 2

Chapter 18 Quadratic Function 2 Chapter 18 Quadratic Function Completed Square Form 1 Consider this special set of numbers - the square numbers or the set of perfect squares. 4 = = 9 = 3 = 16 = 4 = 5 = 5 = Numbers like 5, 11, 15 are

More information

10.5. Polar Coordinates. 714 Chapter 10: Conic Sections and Polar Coordinates. Definition of Polar Coordinates

10.5. Polar Coordinates. 714 Chapter 10: Conic Sections and Polar Coordinates. Definition of Polar Coordinates 71 Chapter 1: Conic Sections and Polar Coordinates 1.5 Polar Coordinates rigin (pole) r P(r, ) Initial ra FIGURE 1.5 To define polar coordinates for the plane, we start with an origin, called the pole,

More information

MECHANICS OF MATERIALS

MECHANICS OF MATERIALS 00 The McGraw-Hill Companies, Inc. All rights reserved. T Edition CHAPTER MECHANICS OF MATERIALS Ferdinand P. Beer E. Russell Johnston, Jr. John T. DeWolf Lecture Notes: J. Walt Oler Teas Tech Universit

More information

11.1 Double Riemann Sums and Double Integrals over Rectangles

11.1 Double Riemann Sums and Double Integrals over Rectangles Chapter 11 Multiple Integrals 11.1 ouble Riemann Sums and ouble Integrals over Rectangles Motivating Questions In this section, we strive to understand the ideas generated b the following important questions:

More information

(6, 4, 0) = (3, 2, 0). Find the equation of the sphere that has the line segment from P to Q as a diameter.

(6, 4, 0) = (3, 2, 0). Find the equation of the sphere that has the line segment from P to Q as a diameter. Solutions Review for Eam #1 Math 1260 1. Consider the points P = (2, 5, 1) and Q = (4, 1, 1). (a) Find the distance from P to Q. Solution. dist(p, Q) = (4 2) 2 + (1 + 5) 2 + (1 + 1) 2 = 4 + 36 + 4 = 44

More information

FIRST- AND SECOND-ORDER IVPS The problem given in (1) is also called an nth-order initial-value problem. For example, Solve: Solve:

FIRST- AND SECOND-ORDER IVPS The problem given in (1) is also called an nth-order initial-value problem. For example, Solve: Solve: .2 INITIAL-VALUE PROBLEMS 3.2 INITIAL-VALUE PROBLEMS REVIEW MATERIAL Normal form of a DE Solution of a DE Famil of solutions INTRODUCTION We are often interested in problems in which we seek a solution

More information

Analytic Geometry in Three Dimensions

Analytic Geometry in Three Dimensions Analtic Geometr in Three Dimensions. The Three-Dimensional Coordinate Sstem. Vectors in Space. The Cross Product of Two Vectors. Lines and Planes in Space The three-dimensional coordinate sstem is used

More information

Vibrational Power Flow Considerations Arising From Multi-Dimensional Isolators. Abstract

Vibrational Power Flow Considerations Arising From Multi-Dimensional Isolators. Abstract Vibrational Power Flow Considerations Arising From Multi-Dimensional Isolators Rajendra Singh and Seungbo Kim The Ohio State Universit Columbus, OH 4321-117, USA Abstract Much of the vibration isolation

More information

Math Notes on sections 7.8,9.1, and 9.3. Derivation of a solution in the repeated roots case: 3 4 A = 1 1. x =e t : + e t w 2.

Math Notes on sections 7.8,9.1, and 9.3. Derivation of a solution in the repeated roots case: 3 4 A = 1 1. x =e t : + e t w 2. Math 7 Notes on sections 7.8,9., and 9.3. Derivation of a solution in the repeated roots case We consider the eample = A where 3 4 A = The onl eigenvalue is = ; and there is onl one linearl independent

More information

LATERAL BUCKLING ANALYSIS OF ANGLED FRAMES WITH THIN-WALLED I-BEAMS

LATERAL BUCKLING ANALYSIS OF ANGLED FRAMES WITH THIN-WALLED I-BEAMS Journal of arine Science and J.-D. Technolog, Yau: ateral Vol. Buckling 17, No. Analsis 1, pp. 9-33 of Angled (009) Frames with Thin-Walled I-Beams 9 ATERA BUCKING ANAYSIS OF ANGED FRAES WITH THIN-WAED

More information

APPLIED OPTICS POLARIZATION

APPLIED OPTICS POLARIZATION A. La Rosa Lecture Notes APPLIED OPTICS POLARIZATION Linearly-polarized light Description of linearly polarized light (using Real variables) Alternative description of linearly polarized light using phasors

More information

Linear Programming. Maximize the function. P = Ax + By + C. subject to the constraints. a 1 x + b 1 y < c 1 a 2 x + b 2 y < c 2

Linear Programming. Maximize the function. P = Ax + By + C. subject to the constraints. a 1 x + b 1 y < c 1 a 2 x + b 2 y < c 2 Linear Programming Man real world problems require the optimization of some function subject to a collection of constraints. Note: Think of optimizing as maimizing or minimizing for MATH1010. For eample,

More information

2.4 Orthogonal Coordinate Systems (pp.16-33)

2.4 Orthogonal Coordinate Systems (pp.16-33) 8/26/2004 sec 2_4 blank.doc 1/6 2.4 Orthogonal Coordinate Sstems (pp.16-33) 1) 2) Q: A: 1. 2. 3. Definition: ). 8/26/2004 sec 2_4 blank.doc 2/6 A. Coordinates * * * Point P(0,0,0) is alwas the origin.

More information

Assignment , 7.1, 7.2, 7.5, 7.11, 7.12, 7.15, TIR and FTIR

Assignment , 7.1, 7.2, 7.5, 7.11, 7.12, 7.15, TIR and FTIR LC45-summer, 1 1. 1.1, 7.1, 7., 7.5, 7.11, 7.1, 7.15, 7.1 1.1. TIR and FTIR a) B considering the electric field component in medium B in Figure 1. (b), eplain how ou can adjust the amount of transmitted

More information

ELE 3310 Tutorial 10. Maxwell s Equations & Plane Waves

ELE 3310 Tutorial 10. Maxwell s Equations & Plane Waves ELE 3310 Tutorial 10 Mawell s Equations & Plane Waves Mawell s Equations Differential Form Integral Form Faraday s law Ampere s law Gauss s law No isolated magnetic charge E H D B B D J + ρ 0 C C E r dl

More information