The Lamй and Metric Coefficients for Curvilinear Coordinates in R
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Appendix a Orthogonal Curvilinear Coordinates
Appendix A Orthogonal Curvilinear Coordinates Given a symmetry for a system under study, the calculations can be simplified by choosing, instead of a Cartesian coordinate system, another set of coordinates which takes advantage of that symmetry. For example calculations in spherical coordinates result easier for systems with spherical symmetry. In this chapter we will write the general form of the differential operators used in electrodynamics and then give their expressions in spherical and cylindrical coordi- nates.1 A.1 Orthogonal curvilinear coordinates A system of coordinates u1, u2, u3, can be defined so that the Cartesian coordinates x, y and z are known functions of the new coordinates: x = x(u1, u2, u3) y = y(u1, u2, u3) z = z(u1, u2, u3) (A.1) Systems of orthogonal curvilinear coordinates are defined as systems for which locally, nearby each point P(u1, u2, u3), the surfaces u1 = const, u2 = const, u3 = const are mutually orthogonal. An elementary cube, bounded by the surfaces u1 = const, u2 = const, u3 = const, as shown in Fig. A.1, will have its edges with lengths h1du1, h2du2, h3du3 where h1, h2, h3 are in general functions of u1, u2, u3. The length ds of the line- element OG, one diagonal of the cube, in Cartesian coordinates is: ds = (dx)2 + (dy)2 + (dz)2 1The orthogonal coordinates are presented with more details in J.A. Stratton, Electromagnetic The- ory, McGraw-Hill, 1941, where many other useful coordinate systems (elliptic, parabolic, bipolar, spheroidal, paraboloidal, ellipsoidal) are given. © Springer International Publishing Switzerland 2016 189 F. Lacava, Classical Electrodynamics, Undergraduate Lecture Notes in Physics, DOI 10.1007/978-3-319-39474-9 190 Appendix A: Orthogonal Curvilinear Coordinates Fig. -
A Scaling Technique for the Design Of
A SCALING TECHNIQUE FOR THE DESIGN OF IDEALIZED ELECTROMAGNETIC LENSES Tj:lesis by Carl E. Baum Capt . , USAF In Partial Fulfillment of the Requi rements For the Degree of Doctor of Philosophy California Institute of Technology Pasadena, California 1969 (Submitte d August 22 , 1968) -ii- ACKNOWLEDGEMENT We would like to thank Professor C. H. Papas for his guidance and encouragement and Mrs. R. Stratton for typing the text. -iii- ABSTRACT A technique is developed for the design of lenses for transi tioning TEM waves between conical and/or cylindrical transmission lines, ideally with no reflection or distortion of the waves. These lenses utilize isotropic but inhomogeneous media and are based on a soluti on of Maxwell's equations instead of just geometrical optics. The technique employs the expression of the constitutive parameters, £ and µ , plus Maxwell's equations, in a general orthogonal curvilinear coordinate system in tensor form, giving what we term as formal quantities. Solving the problem for certain types of formal constitutive parameters, these are transformed to give £ and µ as functions of position. Several examples of such l enses are considered in detail. -iv- TABLE OF CONTENTS I. Introduction l II. Formal Vectors and Operators 5 III. Formal Electromagnetic Quantities lO IV. Restriction of Constitutive Parameters to Scalars l4 V. General Case with Field Components in All Three 16 Coordinate Directions VI . Three- Dimensional TEM Waves 19 VII. Three-Dimensional TEM Lenses 29 A. Modified Spherical Coordinates 29 B. Mo dif i ed Bispherical Coordinates 33 c. Modified Toroidal Coordinates 47 D. Modified Cylindrical Coordinates 57 VIII. -
Computer Facilitated Generalized Coordinate Transformations of Partial Differential Equations with Engineering Applications
Computer Facilitated Generalized Coordinate Transformations of Partial Differential Equations With Engineering Applications A. ELKAMEL,1 F.H. BELLAMINE,1,2 V.R. SUBRAMANIAN3 1Department of Chemical Engineering, University of Waterloo, 200 University Avenue West, Waterloo, Ontario, Canada N2L 3G1 2National Institute of Applied Science and Technology in Tunis, Centre Urbain Nord, B.P. No. 676, 1080 Tunis Cedex, Tunisia 3Department of Chemical Engineering, Tennessee Technological University, Cookeville, Tennessee 38505 Received 16 February 2008; accepted 2 December 2008 ABSTRACT: Partial differential equations (PDEs) play an important role in describing many physical, industrial, and biological processes. Their solutions could be considerably facilitated by using appropriate coordinate transformations. There are many coordinate systems besides the well-known Cartesian, polar, and spherical coordinates. In this article, we illustrate how to make such transformations using Maple. Such a use has the advantage of easing the manipulation and derivation of analytical expressions. We illustrate this by considering a number of engineering problems governed by PDEs in different coordinate systems such as the bipolar, elliptic cylindrical, and prolate spheroidal. In our opinion, the use of Maple or similar computer algebraic systems (e.g. Mathematica, Reduce, etc.) will help researchers and students use uncommon transformations more frequently at the very least for situations where the transformations provide smarter and easier solutions. ß2009 Wiley Periodicals, Inc. Comput Appl Eng Educ 19: 365À376, 2011; View this article online at wileyonlinelibrary.com; DOI 10.1002/cae.20318 Keywords: partial differential equations; symbolic computation; Maple; coordinate transformations INTRODUCTION usual Cartesian, polar, and spherical coordinates. For example, Figure 1 shows two identical pipes imbedded in a concrete slab. -
In George Warner Swenson, Jr. B.S., Michigan College of Mining And
SOLUTION OF LAPLACE'S EQUATION in INVERTED COORDINATE SYSTEMS by George Warner Swenson, Jr. B.S., Michigan College of Mining and Technology (1944) Submitted in Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE at the MASSACHUSETTS INSTITUTE OF TECHNOLOGY 1948 Signature of Author ..0 Q .........0 .. .. Department of Electrical Engineering Certified by .. S....uper. ... .... .. Thesis Supervisor Chairman, Departmental Committee on Graduate Students ACKNOWLEDGMENT The author wishes to express his sincerest apprecia- tion to Professor Parry Moon, of the Department of Electrical Engineering, who suggested the general topic of this thesis. His lectures in electrostatic field theory have provided the essential background for the investigation and his interest in the problem has prompted many helpful suggestions. In addition, the author is indebted to Dr. R. M. Redheffer, of the Department of Mathematics, without whose patient interpretation of his Doctorate thesis and frequent assistance in overcoming mathematical difficulties the present work could hardly have been accomplished. 2982i19 ii CONTENTS ABSTRACT.............................................. iv I ORIENTATION .............. ,............ *,*.*..*** 1 II THE GEOMETRICAL PROPERTIES OF INVERTED SYSTEMS.... 7 A. The Process of Inversion ..................... 7 B. Practical Methods of Inversion................ 8 (1' Graphical Method ... ................... 8 2 Optical Method ......... ................. 10 C. The Inverted Coordinate Systems .............. 19 1) Inverse Rectangular Coordinates ......... 19 2) Inverse Spheroidal Coordinates .......... 19 3) Inverse Parabolic CooDrdinates ........... 21 III LAPLACE'S EQUATION IN INVERTED COORDINATE SYSTEMS. 30 A. The Form of the Equation ..................... 30 B. Separation of Variables ...................... 30 C. Tabulation of the Separated Equations for the Inverted Coordinate Systems *..........*......35 IV TBE APPLICATION OF THE INVERTED COORDINATE SYSTEMS TO BOUNDARY VALUE PROBLEMS ...................... -
Del in Cylindrical and Spherical Coordinates - Wikipedia, the Free Encycl
Del in cylindrical and spherical coordinates - Wikipedia, the free encycl... http://en.wikipedia.org/wiki/Nabla_in_cylindrical_and_spherical_coordi... Make a donation to Wikipedia and give the gift of knowledge! Del in cylindrical and spherical coordinates From Wikipedia, the free encyclopedia (Redirected from Nabla in cylindrical and spherical coordinates) This is a list of some vector calculus formulae of general use in working with standard coordinate systems. Table with the del operator in cylindrical and spherical coordinates Operation Cartesian coordinates (x,y,z) Cylindrical coordinates (ρ,φ,z) Spherical coordinates (r,θ,φ) Definition of coordinates A vector field Gradient Divergence Curl Laplace operator or Differential displacement Differential normal area Differential volume Non-trivial calculation rules: 1. (Laplacian) 2. 3. 4. (using Lagrange's formula for the cross product) 5. Remarks 1 of 2 10/20/2007 7:08 PM Del in cylindrical and spherical coordinates - Wikipedia, the free encycl... http://en.wikipedia.org/wiki/Nabla_in_cylindrical_and_spherical_coordi... This page uses standard physics notation; some (American mathematics) sources define φ as the angle from the z-axis instead of θ. The function atan2(y, x) is used instead of the mathematical function arctan(y/x) due to its domain and image. The classical arctan(y/x) has an image of (-π/2, +π/2), whereas atan2(y, x) is defined to have an image of (-π, π]. See also Orthogonal coordinates Curvilinear coordinates Vector fields in cylindrical and spherical coordinates Retrieved from "http://en.wikipedia.org/wiki/Del_in_cylindrical_and_spherical_coordinates" Categories: Vector calculus | Coordinate systems This page was last modified 11:17, 11 October 2007. All text is available under the terms of the GNU Free Documentation License. -
Divergence and Curl Operators in Skew Coordinates
International Journal of Modeling and Optimization, Vol. 5, No. 3, June 2015 Divergence and Curl Operators in Skew Coordinates Rajai S. Alassar and Mohammed A. Abushoshah where r is the position vector in any three dimensional space, Abstract—The divergence and curl operators appear in i.e. r r(,,) u1 u 2 u 3 . numerous differential equations governing engineering and physics problems. These operators, whose forms are well r Note that is a tangent vector to the ui curve where known in general orthogonal coordinates systems, assume ui different casts in different systems. In certain instances, one the other two coordinates variables remain constant. A unit needs to custom-make a coordinates system that my turn out to be skew (i.e. not orthogonal). Of course, the known formulas for tangent vector in this direction, therefore, is the divergence and curl operators in orthogonal coordinates are not useful in such cases, and one needs to derive their rr counterparts in skew systems. In this note, we derive two uuii r formulas for the divergence and curl operators in a general ei or hiei (3) coordinates system, whether orthogonal or not. These formulas r hi ui generalize the well known and widely used relations for ui orthogonal coordinates systems. In the process, we define an orthogonality indicator whose value ranges between zero and unity. The Divergence of a vector field over a control volume V bounded by the surface S , denoted by F , is defined by Index Terms—Coordinates systems, curl, divergence, Laplace, skew systems. F n dS F lim S (4) I. -
Orthogonal Curvilinear Coordinates
AN INTRODUCTION TO CURVILINEAR ORTHOGONAL COORDINATES Overview Throughout the first few weeks of the semester, we have studied vector calculus using almost exclusively the familiar Cartesian x,y,z coordinate system. In your past math and physics classes, you have encountered other coordinate systems such as cylindri- cal polar coordinates and spherical coordinates. These three coordinate systems (Cartesian, cylindrical, spherical) are actually only a subset of a larger group of coordinate systems we call orthogonal coordinates. We are familiar that the unit vectors in the Cartesian system obey the relationship xi x j dij where d is the Kronecker delta. In other words, the dot product of any two unit vectors is 0 unless they are the same vector (in which case the dot product is one). This is the orthogonality property of vectors, and orthogonal coordinate systems are those in which all the unit vectors obey this property. We will learn general techniques for for translating vector operations into any orthogonal coordinate system, although we will be most concerned with the three systems used most frequently in basic physics (Cartesian, cylindrical polar, and spherical). We will start with very basic geometric properties of coordinate systems, and use those results as the basis for a more detailed analysis. Scale Factors Let' s start by considering a point in the x-y plane. We know we can describe the location of this point by the ordered pair (x,y) if we are using Cartesian coordinates, or by the ordered pair r,f) if we are using polar coordinates. You may also be familiar with the use of the symbols (r,q) for polar coordinates; either usage is fine, but I will try to be consistent in the use of (r,f) for plane polar coordinates, and (r,f,z) for cylindrical polar coordinates. -
A Review: Operators Involving ∇In Curvilinear Orthogonal Coordinates
A Review: Operators involving in Curvilinear Orthogonal Coordinates r and Vector Identities and Product Rules r Markus Selmke Student at the Universität Leipzig, IPSP,[email protected] 22.7.2006, updated 15.02.2008 Contents Abstract I 1 The Laplacian in Spherical Coordinates - The Tedious Way 1 2 The Angular Momentum Operators in Spherical Coordinates 4 3 Operators in Arbitrary Orthogonal Cuvilinear Coordinate Systems 5 r Summary of Important Formulas 11 4 Examples using the General Expressions 12 5 Proofs for the Product Rules 16 r 6 Gauss Divergence Theorem variants 18 References 19 Abstract This document provides easily understandable derivations for all important operators applicable to arbitrary orthog- 3 r onal coordinate systems in R (like spherical, cylindrical, elliptic, parabolic, hyperbolic,..). These include the laplacian (of a scalar function and a vector field), the gradient and its absolute value (of a scalar function), the divergence (of a vector field), the curl (of a vector field) and the convective operator (acting on a scalar function and a vector field) (Section 3). For the first two mentioned special coordinate systems the operators are calculated using these expressions along with some remarks on their simplifications in cartesian coordinates (Section 4). Alongside these calculations, some useful derivations are presented, including the volume element and the velocity components. The Laplacian as well as the absolute value of the gradient are also calculated the clumsy way (ab)using the chain-rule (Section 1). Using the same tedious way as in section 1, the angular momentum operators arising in quantum mechanics are derived for spherical coodinates (Section 2) only. -
Tensor Analysis and Curvilinear Coordinates.Pdf
Tensor Analysis and Curvilinear Coordinates Phil Lucht Rimrock Digital Technology, Salt Lake City, Utah 84103 last update: May 19, 2016 Maple code is available upon request. Comments and errata are welcome. The material in this document is copyrighted by the author. The graphics look ratty in Windows Adobe PDF viewers when not scaled up, but look just fine in this excellent freeware viewer: http://www.tracker-software.com/pdf-xchange-products-comparison-chart . The table of contents has live links. Most PDF viewers provide these links as bookmarks on the left. Overview and Summary.........................................................................................................................7 1. The Transformation F: invertibility, coordinate lines, and level surfaces..................................12 Example 1: Polar coordinates (N=2)..................................................................................................13 Example 2: Spherical coordinates (N=3)...........................................................................................14 Cartesian Space and Quasi-Cartesian Space.......................................................................................15 Pictures A,B,C and D..........................................................................................................................16 Coordinate Lines.................................................................................................................................16 Example 1: Polar coordinates, coordinate lines -
IX. ORTHOGONAL SYSTEMS Orthogonal Coordinate Systems
IX. ORTHOGONAL SYSTEMS Orthogonal coordinate systems produce fewer additional terms in transformed partial differential equations, and thus reduce the amount of computation required. Also, as has been noted in Chapter V, severe departure from orthogonality will introduce truncation error in difference expressions. A general discussion of orthogonal systems on planes and curved surfaces is given in Ref. [42], and various generation procedures are surveyed in Ref. [42] and Ref. [1]. In numerical solutions, the concept of numerical orthogonality, i.e., that the off-diagonal metric coefficients vanish when evaluated numerically, is usually more important than strict analytical orthogonality, especially when the equations to be solved on the system are in the conservative law form. There are basically two types of orthogonal generation systems, those based on the construction of an orthogonal system from a non-orthogonal system, and those involving field solutions of partial differential equations. The first approach involves the construction of orthogonal trajectories on a given non-orthogonal system. Here one set of coordinate lines of the non-orthogonal system is retained, while the other set is replaced by lines emanating from a boundary and constructed by integration across the field so as to cross each line of the retained set orthogonally. Control of the line spacing is exercised through the generation of the non-orthogonal system and through the point distribution on the boundary from which the trajectories start. The point distributions on only three of the four boundaries can be specified. Several methods for the construction of orthogonal trajectories are discussed in Ref. [42] and Ref. -
Orthogonal Curvilinear Coordinates 28.3
® Orthogonal Curvilinear Coordinates 28.3 Introduction The derivatives div, grad and curl from Section 28.2 can be carried out using coordinate systems other than the rectangular Cartesian coordinates. This Section shows how to calculate these derivatives in other coordinate systems. Two coordinate systems - cylindrical polar coordinates and spherical polar coordinates - will be illustrated. • be able to find the gradient, divergence and Prerequisites curl of a field in Cartesian coordinates Before starting this Section you should ... • be familiar with polar coordinates • find the divergence, gradient or curl of a Learning Outcomes vector or scalar field expressed in terms of On completion you should be able to ... orthogonal curvilinear coordinates HELM (2008): 37 Section 28.3: Orthogonal Curvilinear Coordinates 1. Orthogonal curvilinear coordinates The results shown in Section 28.2 have been given in terms of the familiar Cartesian (x, y, z) co- ordinate system. However, other coordinate systems can be used to better describe some physical situations. A set of coordinates u = u(x, y, z), v = v(x, y, z) and w = w(x, y, z) where the direc- tions at any point indicated by u, v and w are orthogonal (perpendicular) to each other is referred to as a set of orthogonal curvilinear coordinates. With each coordinate is associated a scale factor q ∂x 2 ∂y 2 ∂z 2 hu, hv or hw respectively where hu = ∂u + ∂u + ∂u (with similar expressions for hv and hw). The scale factor gives a measure of how a change in the coordinate changes the position of a point. Two commonly-used sets of orthogonal curvilinear coordinates are cylindrical polar coordinates and spherical polar coordinates. -
The Charged Bowl in Toroidal Coordinates.Pdf
The Charged Bowl in Toroidal Coordinates Phil Lucht Rimrock Digital Technology, Salt Lake City, Utah 84103 last update: January 5, 2016 Maple code is available upon request. Comments and errata are welcome. The material in this document is copyrighted by the author. The graphics look ratty in Windows Adobe PDF viewers when not scaled up, but look just fine in this excellent freeware viewer: http://www.tracker-software.com/pdf-xchange-products-comparison-chart . Overview and Summary.........................................................................................................................3 1. Bipolar and toroidal coordinates .......................................................................................................7 1.1 Bipolar coordinates .........................................................................................................................7 1.2 Toroidal coordinates .......................................................................................................................9 2. The charged bowl potential in toroidal coordinates ......................................................................16 2.1 Level curves, the charged ellipsoid problem and a dashed hope ..................................................16 2.2 Cartesian, spherical, toroidal and ellipsoidal atomic forms ..........................................................17 2.3 Smythian forms and one for the bowl...........................................................................................18 2.4 Solution