Appendix A. Curvilinear coordinates. A.1 Lamé coefficients. Consider set of equations. ξ i = ξ i (x 1,x 2,x 3 ), i = 1,2,3

Σχετικά έγγραφα
Spherical Coordinates

Integrals in cylindrical, spherical coordinates (Sect. 15.7)

b. Use the parametrization from (a) to compute the area of S a as S a ds. Be sure to substitute for ds!

CURVILINEAR COORDINATES

Answer sheet: Third Midterm for Math 2339

1. (a) (5 points) Find the unit tangent and unit normal vectors T and N to the curve. r(t) = 3cost, 4t, 3sint

Geodesic Equations for the Wormhole Metric

Problem 3.1 Vector A starts at point (1, 1, 3) and ends at point (2, 1,0). Find a unit vector in the direction of A. Solution: A = 1+9 = 3.

Homework 8 Model Solution Section

Lecture 2: Dirac notation and a review of linear algebra Read Sakurai chapter 1, Baym chatper 3

Second Order Partial Differential Equations

Parametrized Surfaces

Problem 3.16 Given B = ˆx(z 3y) +ŷ(2x 3z) ẑ(x+y), find a unit vector parallel. Solution: At P = (1,0, 1), ˆb = B

Topic 4. Linear Wire and Small Circular Loop Antennas. Tamer Abuelfadl

Exercise 1.1. Verify that if we apply GS to the coordinate basis Gauss form ds 2 = E(u, v)du 2 + 2F (u, v)dudv + G(u, v)dv 2

derivation of the Laplacian from rectangular to spherical coordinates

CHAPTER (2) Electric Charges, Electric Charge Densities and Electric Field Intensity

D Alembert s Solution to the Wave Equation

Orbital angular momentum and the spherical harmonics

Problem Set 9 Solutions. θ + 1. θ 2 + cotθ ( ) sinθ e iφ is an eigenfunction of the ˆ L 2 operator. / θ 2. φ 2. sin 2 θ φ 2. ( ) = e iφ. = e iφ cosθ.

Notes 6 Coordinate Systems

28.3. Orthogonal Curvilinear Coordinates. Introduction. Prerequisites. Learning Outcomes

Areas and Lengths in Polar Coordinates

ECE 468: Digital Image Processing. Lecture 8

Physics 554: HW#1 Solutions

(As on April 16, 2002 no changes since Dec 24.)

Graded Refractive-Index

Variational Wavefunction for the Helium Atom

Dr. D. Dinev, Department of Structural Mechanics, UACEG

Space Physics (I) [AP-3044] Lecture 1 by Ling-Hsiao Lyu Oct Lecture 1. Dipole Magnetic Field and Equations of Magnetic Field Lines

A Introduction to Cartesian Tensors

Tutorial problem set 6,

Partial Differential Equations in Biology The boundary element method. March 26, 2013

VEKTORANALYS. CURVILINEAR COORDINATES (kroklinjiga koordinatsytem) Kursvecka 4. Kapitel 10 Sidor

Chapter 6: Systems of Linear Differential. be continuous functions on the interval

SCHOOL OF MATHEMATICAL SCIENCES G11LMA Linear Mathematics Examination Solutions

Approximation of distance between locations on earth given by latitude and longitude

Geometry of the 2-sphere

3.5 - Boundary Conditions for Potential Flow

Space-Time Symmetries

You may not start to read the questions printed on the subsequent pages until instructed to do so by the Invigilator.

The kinetic and potential energies as T = 1 2. (m i η2 i k(η i+1 η i ) 2 ). (3) The Hooke s law F = Y ξ, (6) with a discrete analog

28.3. Orthogonal Curvilinear Coordinates. Introduction. Prerequisites. Learning Outcomes

SPECIAL FUNCTIONS and POLYNOMIALS

e t e r Cylindrical and Spherical Coordinate Representation of grad, div, curl and 2

Symmetry. March 31, 2013

A Summary Of Linear Continuum Mechanics 1. a b = a i b i = a b cos θ. det A = ɛ ijk A 1i A 2j A 3k. e 1 e 2 e 3 a b = ɛ ijk a j b k e i =

Areas and Lengths in Polar Coordinates

[Note] Geodesic equation for scalar, vector and tensor perturbations

Lifting Entry (continued)

Chapter 3: Vector Analysis

Sixth lecture September 21, 2006

Lifting Entry 2. Basic planar dynamics of motion, again Yet another equilibrium glide Hypersonic phugoid motion MARYLAND U N I V E R S I T Y O F

Parallel transport and geodesics

ECE Spring Prof. David R. Jackson ECE Dept. Notes 2

Section 9.2 Polar Equations and Graphs

Reminders: linear functions

CORDIC Background (2A)

( y) Partial Differential Equations

Written Examination. Antennas and Propagation (AA ) April 26, 2017.

1 String with massive end-points

CRASH COURSE IN PRECALCULUS

3.4 SUM AND DIFFERENCE FORMULAS. NOTE: cos(α+β) cos α + cos β cos(α-β) cos α -cos β

CYLINDRICAL & SPHERICAL COORDINATES

Double Integrals, Iterated Integrals, Cross-sections

4.6 Autoregressive Moving Average Model ARMA(1,1)

Ó³ Ÿ , º 1(130).. 7Ä ±μ. Ñ Ò É ÉÊÉ Ö ÒÌ ² μ, Ê

Empirical best prediction under area-level Poisson mixed models

Chapter 6: Systems of Linear Differential. be continuous functions on the interval

Computing Gradient. Hung-yi Lee 李宏毅

On the Galois Group of Linear Difference-Differential Equations

Fourier Series. MATH 211, Calculus II. J. Robert Buchanan. Spring Department of Mathematics

Srednicki Chapter 55

Cosmological Space-Times

Matrices and Determinants

11.4 Graphing in Polar Coordinates Polar Symmetries

Review-2 and Practice problems. sin 2 (x) cos 2 (x)(sin(x)dx) (1 cos 2 (x)) cos 2 (x)(sin(x)dx) let u = cos(x), du = sin(x)dx. = (1 u 2 )u 2 ( du)

6.1. Dirac Equation. Hamiltonian. Dirac Eq.

The Jordan Form of Complex Tridiagonal Matrices

arxiv: v1 [math.dg] 31 Jan 2009

DiracDelta. Notations. Primary definition. Specific values. General characteristics. Traditional name. Traditional notation

UNIVERSITETET I OSLO Det matematisk-naturvitenskapelige fakultet

Section 8.2 Graphs of Polar Equations

Concrete Mathematics Exercises from 30 September 2016

Mock Exam 7. 1 Hong Kong Educational Publishing Company. Section A 1. Reference: HKDSE Math M Q2 (a) (1 + kx) n 1M + 1A = (1) =

A Short Introduction to Tensors

Numerical Analysis FMN011

Laplace s Equation on a Sphere

2 Composition. Invertible Mappings

Equations. BSU Math 275 sec 002,003 Fall 2018 (Ultman) Final Exam Notes 1. du dv. FTLI : f (B) f (A) = f dr. F dr = Green s Theorem : y da

Lecture 21: Scattering and FGR

Phys460.nb Solution for the t-dependent Schrodinger s equation How did we find the solution? (not required)

Practice Exam 2. Conceptual Questions. 1. State a Basic identity and then verify it. (a) Identity: Solution: One identity is csc(θ) = 1

Π Ο Λ Ι Τ Ι Κ Α Κ Α Ι Σ Τ Ρ Α Τ Ι Ω Τ Ι Κ Α Γ Ε Γ Ο Ν Ο Τ Α

forms This gives Remark 1. How to remember the above formulas: Substituting these into the equation we obtain with

ExpIntegralE. Notations. Primary definition. Specific values. Traditional name. Traditional notation. Mathematica StandardForm notation

Governing equations for a new compressible Navier-Stokes solver in general cylindrical coordinates

General 2 2 PT -Symmetric Matrices and Jordan Blocks 1

Απόκριση σε Μοναδιαία Ωστική Δύναμη (Unit Impulse) Απόκριση σε Δυνάμεις Αυθαίρετα Μεταβαλλόμενες με το Χρόνο. Απόστολος Σ.

Solutions to Exercise Sheet 5

Transcript:

Appendix A Curvilinear coordinates A. Lamé coefficients Consider set of equations ξ i = ξ i x,x 2,x 3, i =,2,3 where ξ,ξ 2,ξ 3 independent, single-valued and continuous x,x 2,x 3 : coordinates of point P in Cartesian system with radius-vector x ξ,ξ 2,ξ 3 : coordinates of point P in curvilinear system e,e 2,e 3 : base unit vectors in Cartesian coordinates e ξ,e ξ2,e ξ3 : base unit vectors in curvilinear system we restrict ourselves to orthogonal curvilinear coordinates systems e ξi e ξj = δ ij Consider x = xx i ξ j and take the total differential summation over double appearing indices understood dx = x ξ j dξ j x ξ partial derivative keeping ξ 2,ξ 3 fixed: vector tangential to coordinate line ξ in general x ξ = h e ξ dx = h dξ e ξ +h 2 dξ 2 e ξ2 +h 3 dξ 3 e ξ3 h i Lamé coefficients Those coefficients might depend on the coordinates ξ i h i = h i ξ,ξ 2,ξ 3 57

h i dξ i no summation components of length element along e ξi Without restriction to orthogonal systems the length element ds = dx is defined as Coefficients ds 2 = dx dx = dx j dx j = x j ξ l x j ξ m dξ l dξ m = g lm dξ l dξ m g lm = x j ξ l x j ξ m are called the elements of the metric tensor For an orthogonal curvilinear system the base vectors e ξ,e ξ2,e ξ3 are mutually perpendicular and form a right-handed system We get the length element squared the Lamé coefficients ds 2 = h 2 dξ 2 +h 2 2dξ 2 2 +h 2 3dξ 3 2 g = h 2, g 22 = h 2 2, g 33 = h 2 3, g ik = 0 for i k the volume element elementary rectangular box d 3 x dv = h h 2 h 3 dξ dξ 2 dξ 3 58

A.2 Some special orthogonal coordinates Cartesian coordinates < x <, < x 2 <, < x 3 < h = h 2 = h 3 = ds 2 = dx 2 +dx 2 2 +dx 2 3 d 3 x = dx dx 2 dx 3 Cylindrical coordinates 0 ρ <, 0 ϕ < 2π, < z < x = ρ cosϕ, x 2 = ρ sinϕ, x 3 = z h ρ = h z =, h ϕ = ρ ds 2 = dρ 2 +ρ 2 dϕ 2 +dz 2 d 3 x = ρdρdϕdz Spherical coordinates 0 r <, 0 θ π, 0 ϕ < 2π x = r sinθ cosϕ, x 2 = r sinθ sinϕ, x 3 = r cosθ h r =, h θ = r, h ϕ = r sinθ ds 2 = dr 2 +r 2 dθ 2 +r 2 sinθ 2 dϕ 2 d 3 x = r 2 dr sinθdθdϕ = r 2 drdcosθdϕ r 2 drdω Parabolic cylindrical coordinates parametrization in Mathematica 0 u <, 0 v <, < z < x = 2 u2 v 2, x 2 = uv, x 3 = z h u = h v = u 2 +v 2, h z = ds 2 = u 2 +v 2 du 2 +dv 2 +dz 2 d 3 x = u 2 +v 2 dudvdz parametrization of Arfken 0 ξ <, 0 η <, < z < x x 2, u η, v ξ Parabolic coordinates parametrization of Arfken, Landau/Lifshitz 0 ξ <, 0 η <, 0 ϕ < 2π x = ξη cosϕ, x 2 = ξη sinϕ, x 3 = ξ η 2 59

h ξ = ξ +η, h η = ξ +η, h ϕ = ξη 2 ξ 2 η ds 2 = ξ +η dξ 2 + ξ +η dη 2 +ξηdϕ 2 4 ξ 4 η d 3 x = ξ +ηdξdηdϕ 4 parametrization in Mathematica 0 u <, 0 v <, 0 ϕ < 2π ξ = u 2, η = v 2, x = uv cosϕ, x 2 = uvsinϕ, x 3 = 2 u2 v 2 h u = h v = u 2 +v 2, h ϕ = uv ds 2 = u 2 +v 2 du 2 +dv 2 +uvdϕ 2 d 3 x = uvu 2 +v 2 dudvdϕ 60

A.3 Vector operations in orthogonal coordinates Gradient The length element along coordinate line ξ is h dξ form of the nabla operator e ξ gradψ = e ξ ψ = h ψ ξ ψ = h ψ ξ e ξ + h 2 ψ ξ 2 e ξ2 + h 3 ψ ξ 3 e ξ3 = 3 i= e ξi h i ξ i Divergence and Laplacian Use the divergence definition with A = lim V 0 V S A nda A = A ξ,ξ 2,ξ 3 e ξ +A 2 ξ,ξ 2,ξ 2 e ξ +A 3 ξ,ξ 2,ξ 3 e ξ3 and choose as volume V an elementary rectangular box of sides h ξ h 2 ξ 2 h 3 ξ 3 Analogously to the derivation in Cartesian coordinates compare Chapter.2 we calculate the net outward flux in direction of coordinate line ξ divided by the volume: lim V 0 [ A ξ + ξ,ξ 2,ξ 3 h 2 ξ + ξ,ξ 2,ξ 3 ξ 2 h 3 ξ + ξ,ξ 2,ξ 3 ξ 3 ] A ξ,ξ 2,ξ 3 h 2 ξ,ξ 2,ξ 3 ξ 2 h 3 ξ,ξ 2,ξ 3 ξ 3 /h ξ h 2 ξ 2 h 3 ξ 3 h 2 h 3 A h h 2 h 3 ξ we get for the divergence A = h h 2 h 3 { h 2 h 3 A + h 3 h A 2 + } h h 2 A 3 ξ ξ 2 ξ 3 The Laplacian operator follows 2 = 2 = : = h h 2 h 3 { ξ h2 h 3 h ξ + ξ 2 h3 h h 2 ξ 2 + ξ 3 h h 2 h 3 ξ 3 } 6

Curl Using a similar derivation as in Cartesian coordinates we get for the curl of vector A A = { h 3 A 3 } h 2 A 2 e ξ + cyclic permutations h 2 h 3 ξ 2 ξ 3 Representation as determinant: A = h h 2 h 3 h e ξ h 2 e ξ2 h 3 e ξ3 ξ ξ 2 ξ 3 h A h 2 A 2 h 3 A 3 62

A.4 Some explicit forms of vector operations Cartesian coordinates x,x 2,x 3 with base vectors e,e 2,e 3 ψ = ψ x e + ψ x 2 e 2 + ψ x 3 e 3 A = A + A 2 + A 3 x x 2 x 3 A3 A = A 2 e + x 2 x 3 ψ = 2 ψ + 2 ψ + 2 ψ x 2 x 2 2 x 2 3 A A 3 A2 e 2 + A e 3 x 3 x x x 2 Cylindrical coordinates ρ,ϕ,z with base vectors e ρ,e ϕ,e z ψ = ψ ρ e ρ + ψ ρ ϕ e ϕ + ψ z e z A = ρ ρ ρa ρ+ A ϕ ρ ϕ + A z z A z A = ρ ϕ A ϕ e ρ + z ψ = ρ ψ + 2 ψ ρ ρ ρ ρ 2 ϕ + 2 ψ 2 z 2 Aρ z A z ρ e ϕ + ρ ρ ρa ϕ A ρ e z ϕ Spherical coordinates r,θ,ϕ with base vectors e r,e θ,e ϕ ψ = ψ r e r + ψ r θ e θ + A = r 2 r r2 A r + r sinθ A = + ψ = r 2 r θ sinθa ϕ A θ ϕ r sinθ A r r sinθ ϕ r r 2 ψ + r ψ r sinθ ϕ e ϕ θ sinθa θ+ r sinθ r ra ϕ r 2 sinθ θ e r A ϕ ϕ e θ + r r ra θ A r θ sinθ ψ 2 ψ + θ r 2 sin 2 θ ϕ 2 e ϕ Note r 2 r r 2 ψ r r 2 r 2 rψ 63

A.5 Relationbetweenunitbasevectorsandtheirtime derivatives Relation between the local unit base vectors of cylindrical coordinates e ρ t,e ϕ t,e z and their time derivatives and the global constant unit base vectors of Cartesian coordinates e,e 2,e 3 eρ = cosϕe +sinϕe2 e = cosϕeρ sinϕeϕ e ϕ = sinϕe +cosϕe 2 e z = e 3 e 2 = sinϕe ρ +cosϕe ϕ e 3 = e z ė ρ = sinϕ ϕe +cosϕ ϕe 2 = ϕe ϕ ė = 0 ė ϕ = ϕe ρ ė 2 = 0 ė z = 0 ė 3 = 0 Same for the local unit base vectors of spherical coordinates e r t,e θ t,e ϕ t and their time derivatives e r = sinθ cosϕe +sinθ sinϕe 2 +cosθe 3 e θ = cosθ cosϕe +cosθ sinϕe 2 sinθe 3 e ϕ = sinϕe +cosϕe 2 e = sinθ cosϕe r +cosθ cosϕe θ sinϕe ϕ e 2 = sinθ sinϕe r +cosθ sinϕe θ +cosϕe ϕ e 3 = cosθe r sinθe θ ė r = θe θ +sinθ ϕe ϕ ė θ = θe r +cosθ ϕe ϕ ė ϕ = ϕ sinθe r +cosθe θ Relation between the local unit base vectors e ρ t,e ϕ t,e z and e r t,e θ t,e ϕ t e ρ = sinθe r +cosθe θ e ϕ = e ϕ e z = cosθe r sinθe θ e r = sinθe ρ +cosθe z e θ = cosθe ρ sinθe z e ϕ = e ϕ 64