13 Current Sheet, Solenoid, Vector Potential and Current Loops

Total Page:16

File Type:pdf, Size:1020Kb

13 Current Sheet, Solenoid, Vector Potential and Current Loops 13 Current sheet, solenoid, vector potential and current loops Js =ˆzJs z In the following examples we will calculate the magnetic fields B = µoH established by some simple current configurations by using the integral form y of static Ampere’s law. B L C B =ˆyB(x) W x Example 1: Consider a uniform surface current density Js = Jszˆ A/m flowing on µ J B(x)= o s x =0plane (see figure in the margin) — the current sheet extends infinitely in 2 y and z directions. Determine B and H. Solution: Since the current sheet extends infinitely in y and z directions we expect B As shown in Example 1 mag- to depend only on coordinate x.Also,thefieldshouldbethesuperpositionofthe netic field of a current sheet fields of an infinite number of current filaments, which suggests, by right-hand- rule, B =ˆyB(x),whereB(x) is an odd function of x.TodetermineB(x),such is independent of distance that B( x)= B(x),weapplyAmpere’slawbycomputingthecirculationof x from the current sheet. − − | | B around the rectangular path C shown in the figure in the margin. We expand Also H changes discontinu- B dl = µ I ously across the current sheet · o C !C by an amount Js. as B(x)L +0 B( x)L +0=µ J L, − − o s from which we obtain µoJs µoJs Js B(x)= B =ˆy sgn(x) and H =ˆy sgn(x). 2 ⇒ 2 2 1 Example 2: Consider a slab of thickness W over W <x<W which extends in- − 2 2 finitely in y and z directions and conducts a uniform current density of J =ˆzJo A/m2.DetermineH if the current density is zero outside the slab. Solution: Given the geometric similarities between this problem and Example 1, we postulate that B =ˆyB(x),whereB(x) is an odd function of x,thatisB( x)= − B(x).TodetermineB(x) we apply Ampere’s law by computing the circulation − of B around the rectangular path C shown in the figure in the margin. For W x< 2 ,weexpand B dl = µ I · o C !C as B(x)L +0 B( x)L +0=µ J 2xL B(x)=µ J x. z − − o o ⇒ o o W y For x 2 ,theexpansiongives ≥ Jozˆ W B(x)L +0 B( x)L +0=µoJoWL B(x)=µoJo . B L B =ˆyB(x) − − ⇒ 2 C Hence, we find that W x W W W yJˆ ox, x < 2 − 2 2 H = W | | "yJˆ o 2 sgn(x), otherwise. By(x) µoJoW 2 Note that the solution plotted in the margin shows no discontinuity at x = W ± 2 or elsewhere. W W x − 2 2 The figure in the margin depicts a finite section of an infinite solenoid. Asolenoidcanbeconstructedinpracticebywindingalongwireintoa 2 multi loop coil as depicted. A solenoid with its loop carrying a current I B =ˆzB in φˆ direction (as shown), produces effectively a surface current density of Js = INφˆ A/m, where N is the number density (1/m) of current loops in C the solenoid. In Example 3 we compute the magnetic field of the infinite solenoid using Ampere’s law. L I Example 3: An infinite solenoid having N loops per unit length is stacked in z- direction, each loop carrying a current of I Aincounter-clockwisedirectionwhen Infinite solenoid viewed from the top (see margin). Determine H. with N loops per unit length carrying I amps per loop Solution: Assuming that B =0outside the solenoid, and also B is independent of z within the solenoid, we find that Ampere’s law indicates for the circulation C B = µoIN shown in the margin B dl = µ I LB = µ INL. · o C ⇒ o !C This leads to B = µoIN and H =ˆzIN for the field within the solenoid. The assumption of zero magnetic flux density B =0for the exterior region is justified because: (a) if the exterior field is non-zero, then it must be independent of x and y (follows from Ampere’s law applied to any exterior path C with IC =0), and 2 (b) the finite interior flux Ψ=µoINπa can only be matched with the flux of the infinitely extended exterior region when the constant exterior flux density (because of (a)) is vanishingly small. 3 Static electric fields: Curl-free and are governed by • E =0, D = ρ where D = $E ∇× ∇· with $ = $r$o. Static magnetic fields: Divergence-free and are governed by • B =0, H = J where B = µH ∇· ∇× with µ = µrµo —relativepermeabilities µr other than unity (for free space) will be explained later on. Mathematically, we can generate a divergence-free vector field B(x, y, z) as B = A ∇× by taking the curl of any vector field A = A(x, y, z) (just like we can generate acurl-freeE by taking the gradient of any scalar field V (x, y, z)). − Verification: Notice that ∂ ∂ ∂ ∂x ∂y ∂z ∂ ∂ ∂ ∂ ∂ ∂ A = ( A)x + ( A)y + ( A)z = # ∂x ∂y ∂z # ∇·∇× ∂x ∇× ∂y ∇× ∂z ∇× # # # Ax Ay Az # # # ∂ ∂A ∂A ∂ ∂A ∂A ∂ ∂A # ∂A # = ( z y ) ( z x )+ ( y# x )=0.# ∂x ∂y − ∂z − ∂y ∂x − ∂z ∂z ∂x #− ∂y # If B = A represents a magnetostatic field, then A is called mag- • ∇× netostatic potential or vector potential. 4 – Vector potential A can be used in magnetostatics in similar ways to how electrostatic potential V is used in electrostatics. In electrostatics we can assign V =0to any point in space ◦ that is convenient in a given problem. In magnetostatics we can assign A to any scalar that is ◦ ∇· convenient in a given problem. – For example, if we make the assignment1 A =0, ∇· then we find that B = A = ( A) 2A = 2A. ∇× ∇×∇× ∇ ∇· −∇ −∇ This is a nice and convenient outcome, because, when combined with H = J B = µ J, ∇× ⇒∇× o it produces 2A = µ J, ∇ − o which is the magnetostatic version of Poisson’s equation ρ 2V = . ∇ −$o 1With this assignment — known as Coulomb gauge — A acquires the physical meaning of “potential momentum per unit charge”, just as scalar potential V is “potential enegy per unit charge” (see Konopinski, Am. J. Phys., 46,499,1978). 5 – In analogy with solution ρ(r') 3 V (r)= d r' z J(r") 4π$o r r' r r" $ | − | − of Poisson’s equation, it has a solution r r" µoJ(r') 3 A(r)= d r'. 4π r r' $ | − | y 2 Given any static current density J(r),theaboveequationcanbeusedto O obtain the corresponding vector potential A that simultaneously satisfies x A =0 and A = B. ∇· ∇× Once A is available, obtaining B = A is then just a matter of taking a ∇× curl. Magnetic flux density B of a single current loop I can be calculated • after determining its vector potential as follows: z y – For a loop of radius a on z =0plane, we can express the corresponding current density as 2 2 ( y',x', 0) J(r')=Iδ(z')δ( x' + y' a) − a − 2 2 x x' + y' I % ˆ where the ratio on the right is the unit vector φ'.% – Inserting this into the general solution for vector potential, and performing 2 2 Jφ = Iδ(z)δ( x + y a) the integration over z',weobtain & − 2 Also, in quasi-statics we use J(r!,t) to obtain A(r,t) and B = A over regions small compared to ∇× λ = c/f,withf the highest frequency in J(r!,t). 6 µoI 2 2 ( y',x', 0) A(r)= δ( x' + y' a) − dx'dy' 2 2 2 2 2 4π − (x x') +(y y') + z x' + y' $ % − − µoI ( y',x', 0) = δ(r' a) %− r'dr'dφ%' 2 2 2 4π − (x x') +(y y') + z r' $ π − − µoI ( a sin φ',acos φ', 0) = %− dφ' xAˆ x(r)+ˆyAy(r). 2 2 2 4π π (x a cos φ') +(y a sin φ') + z ≡ $− − − % – Given that Az =0,itcanbeshownthatB = A leads to ∇× ∂A ∂A ∂A ∂A B = y ,B= x ,B= y x . x − ∂z y ∂z z ∂x − ∂y – From the expected azimuthal symmetry of B about the z-axis, it is sufficient to evaluate these on, say, y =0plane — after some algebra, and dropping the primes, we find, on y =0plane, π µoaI z cos φ Bx = 2 2 2 3/2 dφ, 4π π (x + a + z 2ax cos φ) $− − π µoaI z sin φ By = 2 2 2 3/2 dφ, 4π π (x + a + z 2ax cos φ) $− − and π µoaI a x cos φ Bz = 2 2 −2 3/2 dφ. 4π π (x + a + z 2ax cos φ) $− − – We note that By =0since the By integrand above is odd in φ and the integration limits are centered about the origin. Hence, the field on y =0 plane is given as B =ˆxBx +ˆzBz with Bx and Bz defined above. – There are no closed form expressions for the Bx and Bz integrals above for an arbitrary (x, z). 7 However, it can be easily seen that if x =0(i.e., along the z-axis), Bx =0 ◦ (as symmetry would dictate) and π 2 µoaI a µoIa Bz = 2 2 3/2 dφ = 2 2 3/2 . 4π π (a + z ) 2(a + z ) 3 $− For z a, 2 | |) 2 µoIa 1 Bz 3 , ≈ 2 z z | | 0 which is positive and varies with the inverse third power of distance z . | | !1 I B B – Also, x and z integrals can be performed numerically. Figure !2 in the margin depicts the pattern of Bˆ on y =0plane for a loop !3 !3 !2 !1 0 1 2 3 of radius a =1computed using Mathematica.
Recommended publications
  • Electromagnetic Fields and Energy
    MIT OpenCourseWare http://ocw.mit.edu Haus, Hermann A., and James R. Melcher. Electromagnetic Fields and Energy. Englewood Cliffs, NJ: Prentice-Hall, 1989. ISBN: 9780132490207. Please use the following citation format: Haus, Hermann A., and James R. Melcher, Electromagnetic Fields and Energy. (Massachusetts Institute of Technology: MIT OpenCourseWare). http://ocw.mit.edu (accessed [Date]). License: Creative Commons Attribution-NonCommercial-Share Alike. Also available from Prentice-Hall: Englewood Cliffs, NJ, 1989. ISBN: 9780132490207. Note: Please use the actual date you accessed this material in your citation. For more information about citing these materials or our Terms of Use, visit: http://ocw.mit.edu/terms 8 MAGNETOQUASISTATIC FIELDS: SUPERPOSITION INTEGRAL AND BOUNDARY VALUE POINTS OF VIEW 8.0 INTRODUCTION MQS Fields: Superposition Integral and Boundary Value Views We now follow the study of electroquasistatics with that of magnetoquasistat­ ics. In terms of the flow of ideas summarized in Fig. 1.0.1, we have completed the EQS column to the left. Starting from the top of the MQS column on the right, recall from Chap. 3 that the laws of primary interest are Amp`ere’s law (with the displacement current density neglected) and the magnetic flux continuity law (Table 3.6.1). � × H = J (1) � · µoH = 0 (2) These laws have associated with them continuity conditions at interfaces. If the in­ terface carries a surface current density K, then the continuity condition associated with (1) is (1.4.16) n × (Ha − Hb) = K (3) and the continuity condition associated with (2) is (1.7.6). a b n · (µoH − µoH ) = 0 (4) In the absence of magnetizable materials, these laws determine the magnetic field intensity H given its source, the current density J.
    [Show full text]
  • Steady-State Electric and Magnetic Fields
    Steady State Electric and Magnetic Fields 4 Steady-State Electric and Magnetic Fields A knowledge of electric and magnetic field distributions is required to determine the orbits of charged particles in beams. In this chapter, methods are reviewed for the calculation of fields produced by static charge and current distributions on external conductors. Static field calculations appear extensively in accelerator theory. Applications include electric fields in beam extractors and electrostatic accelerators, magnetic fields in bending magnets and spectrometers, and focusing forces of most lenses used for beam transport. Slowly varying fields can be approximated by static field calculations. A criterion for the static approximation is that the time for light to cross a characteristic dimension of the system in question is short compared to the time scale for field variations. This is equivalent to the condition that connected conducting surfaces in the system are at the same potential. Inductive accelerators (such as the betatron) appear to violate this rule, since the accelerating fields (which may rise over many milliseconds) depend on time-varying magnetic flux. The contradiction is removed by noting that the velocity of light may be reduced by a factor of 100 in the inductive media used in these accelerators. Inductive accelerators are treated in Chapters 10 and 11. The study of rapidly varying vacuum electromagnetic fields in geometries appropriate to particle acceleration is deferred to Chapters 14 and 15. The static form of the Maxwell equations in regions without charges or currents is reviewed in Section 4.1. In this case, the electrostatic potential is determined by a second-order differential equation, the Laplace equation.
    [Show full text]
  • On the Helmholtz Theorem and Its Generalization for Multi-Layers
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by DSpace@IZTECH Institutional Repository Electromagnetics ISSN: 0272-6343 (Print) 1532-527X (Online) Journal homepage: http://www.tandfonline.com/loi/uemg20 On the Helmholtz Theorem and Its Generalization for Multi-Layers Alp Kustepeli To cite this article: Alp Kustepeli (2016) On the Helmholtz Theorem and Its Generalization for Multi-Layers, Electromagnetics, 36:3, 135-148, DOI: 10.1080/02726343.2016.1149755 To link to this article: http://dx.doi.org/10.1080/02726343.2016.1149755 Published online: 13 Apr 2016. Submit your article to this journal Article views: 79 View related articles View Crossmark data Full Terms & Conditions of access and use can be found at http://www.tandfonline.com/action/journalInformation?journalCode=uemg20 Download by: [Izmir Yuksek Teknologi Enstitusu] Date: 07 August 2017, At: 07:51 ELECTROMAGNETICS 2016, VOL. 36, NO. 3, 135–148 http://dx.doi.org/10.1080/02726343.2016.1149755 On the Helmholtz Theorem and Its Generalization for Multi-Layers Alp Kustepeli Department of Electrical and Electronics Engineering, Izmir Institute of Technology, Izmir, Turkey ABSTRACT ARTICLE HISTORY The decomposition of a vector field to its curl-free and divergence- Received 31 August 2015 free components in terms of a scalar and a vector potential function, Accepted 18 January 2016 which is also considered as the fundamental theorem of vector KEYWORDS analysis, is known as the Helmholtz theorem or decomposition. In Discontinuities; distribution the literature, it is mentioned that the theorem was previously pre- theory; Helmholtz theorem; sented by Stokes, but it is also mentioned that Stokes did not higher order singularities; introduce any scalar and vector potentials in his expressions, which multi-layers causes a contradiction.
    [Show full text]
  • Lecture 23 Scalar and Vector Potentials
    Lecture 23 Scalar and Vector Potentials 23.1 Scalar and Vector Potentials for Time-Harmonic Fields 23.1.1 Introduction Previously, we have studied the use of scalar potential Φ for electrostatic problems. Then we learnt the use of vector potential A for magnetostatic problems. Now, we will study the combined use of scalar and vector potential for solving time-harmonic (electrodynamic) problems. This is important for bridging the gap between static regime where the frequency is zero or low, and dynamic regime where the frequency is not low. For the dynamic regime, it is important to understand the radiation of electromagnetic fields. Electrodynamic regime is important for studying antennas, communications, sensing, wireless power transfer ap- plications, and many more. Hence, it is imperative that we understand how time-varying electromagnetic fields radiate from sources. It is also important to understand when static or circuit (quasi-static) regimes are impor- tant. The circuit regime solves problems that have fueled the microchip industry, and it is hence imperative to understand when electromagnetic problems can be approximated with simple circuit problems and solved using simple laws such as KCL an KVL. 23.1.2 Scalar and Vector Potentials for Statics, A Review Previously, we have studied scalar and vector potentials for electrostatics and magnetostatics where the frequency ! is identically zero. The four Maxwell's equations for a homogeneous 225 226 Electromagnetic Field Theory medium are then r × E = 0 (23.1.1) r × H = J (23.1.2) r · "E = % (23.1.3) r · µH = 0 (23.1.4) Using the knowledge that r × rΦ = 0, we can construct a solution to (23.1.1) easily.
    [Show full text]
  • Lecture 10: Vector Fields, Curl and Divergence
    Vector Fields, Curl and Divergence Lecture 10: Vector fields, Curl and Divergence Rafikul Alam Department of Mathematics IIT Guwahati Rafikul Alam IITG: MA-102 (2013) Vector Fields, Curl and Divergence Vector fields Definition: A vector field in Rn is a function F : Rn ! Rn that assigns to each x 2 Rn a vector F (x): A vector field in Rn with domain U ⊂ Rn is called a vector field on U: Geometrically, a vector field F on U is interpreted as attaching a vector to each point of U: Thus, there is a subtle difference between a vector field in Rn and a function from Rn to Rn: When a function F : Rn ! Rn is viewed as a vector field, for each x the vector F (x) is identified with the vector that starts at the point x and points to F (x); i.e., F (x) is identified with the vector that is obtained by translating F (x) to the point x: Thus every vector field on U ⊂ Rn is uniquely determined by a function from U ! Rn: Rafikul Alam IITG: MA-102 (2013) Vector Fields, Curl and Divergence Examples of vector fields • The gravitational force field describes the force of attraction of the earth on a mass m and is given by mMG F = − r; r 3 where r := (x; y; z) and r := krk: The vector field F points to the centre of the earth. 2 2 • The vector field F : R ! R given by F (x; y) := (−y; x) is a rotational vector field in R2 which rotates a vector in the anti-clockwise direction by an angle π=2: n 1 • Let x : [0; 1] ! R be C and Γ := x([0; 1]): Then F :Γ ⊂ Rn ! Rn given by F (x(t)) = x0(t) is a tangent vector field on Γ: Rafikul Alam IITG: MA-102 (2013) Vector Fields, Curl and Divergence
    [Show full text]
  • Magnetic Vector Potential When We Derived the Scalar Electric Potential
    Magnetic vector potential When we derived the scalar electric potential we started with the relation ~ E~ = 0 to conclude that E~ could be written as the gradient of a scalar r £ potential. That wonzt work for the magnetic field (except where ~j = 0), because the curl of B~ is not zero in general. Instead, the divergence of B~ is zero. That means that B~ may be written as the curl of a vector that we shall call A~. B~ = ~ A~ ~ B~ = ~ ~ A~ = 0 r £ ) r ¢ r ¢ r £ ³ ´ Then the second equation becomes ~ B~ = ~ ~ A~ = ~ ~ A~ 2A~ = µ ~j r £ r £ r £ r r ¢ ¡ r 0 ³ ´ ³ ´ We had some flexibility in choosing the scalar potential V because E~ = ~ V is ¡r not changed if we add a constant to V, since ~ (constant) = 0. Similarly here, r if we add to A~ the gradient of a scalar function, A~ = A~ + ~ χ, we have 2 1 r B~ = ~ A~ = ~ A~ + ~ χ = ~ A~ = B~ 2 r £ 2 r £ 1 r r £ 1 1 ³ ´ With this flexibility, we may choose ~ A~ = 0. For suppose this is not true. r ¢ Then ~ A~ + ~ χ = ~ A~ + 2χ = 0 r ¢ 1 r r ¢ 1 r So we have an equation fo³r the func´tion χ 2χ = ~ A~ r ¡r ¢ 1 Once we solve this we will have a vector A~2 whose divergence is zero. Once we know that we can do this, we may just set ~ A~ = 0 from the start. This is r ¢ called the Coulomb gauge condition. With this choice, the equation for A~ is 2A~ = µ ~j (1) r ¡ 0 We may look at this equation one component at a time (provided that we use Cartesian components.) Thus, for the x component ¡ 2A = µ j r x ¡ 0 x This equation has the same form as the equation for V ρ 2V = r ¡ ε0 and thus the solution will also have the same form: µ j (~r ) A (~r) = 0 x 0 dτ x 4π R 0 Z 1 and since we have an identical relation for each component, then ~ ¹0 j (~r0) A~ = d¿0 (2) 4¼ R Z Now remember that ~j d¿ corresponds to Id`~, so if the current is confined in wires, the result is µ Id`~ A~ = 0 0 (3) 4π R Z At this point we may stop and consider if there is any rule for magnetic field analagous to our RULE 1 for electric fields.
    [Show full text]
  • 7-3 the Biot-Savart Law and the Magnetic Vector Potential
    11/14/2004 section 7_3 The Biot-Savart Law blank.doc 1/1 7-3 The Biot-Savart Law and the Magnetic Vector Potential Reading Assignment: pp. 208-218 Q: Given some field B (r ) , how can we determine the source J ()r that created it? A: Easy! Æ JB()rxr= ∇ ( ) µ0 Q: OK, given some source J (r ), how can we determine what field B ()r it creates? A: HO: The Magnetic Vector Potential HO: Solutions to Ampere’s Law HO: The Biot-Savart Law Example: The Uniform, Infinite Line of Current HO: B-field from an Infinite Current Sheet Jim Stiles The Univ. of Kansas Dept. of EECS 11/14/2004 The Magnetic Vector Potential.doc 1/5 The Magnetic Vector Potential From the magnetic form of Gauss’s Law ∇ ⋅=B ()r0, it is evident that the magnetic flux density B (r ) is a solenoidal vector field. Recall that a solenoidal field is the curl of some other vector field, e.g.,: BA(rxr) = ∇ ( ) Q: The magnetic flux density B (r ) is the curl of what vector field ?? A: The magnetic vector potential A (r )! The curl of the magnetic vector potential A (r ) is equal to the magnetic flux density B (r ): ∇xrAB( ) = ( r) where: Jim Stiles The Univ. of Kansas Dept. of EECS 11/14/2004 The Magnetic Vector Potential.doc 2/5 ⎡Webers⎤ magnetic vector potential A ()r ⎣⎢ meter ⎦⎥ Vector field A ()r is called the magnetic vector potential because of its analogous function to the electric scalar potential V ()r . An electric field can be determined by taking the gradient of the electric potential, just as the magnetic flux density can be determined by taking the curl of the magnetic potential: EBA()r=−∇V ( r) (r) =∇ x() r Yikes! We have a big problem! There are actually (infinitely) many vector fields A ()r whose curl will equal an arbitrary magnetic flux density B ()r .
    [Show full text]
  • A Rigorous and Completed Statement on Helmholtz Theorem
    Progress In Electromagnetics Research, PIER 69, 287–304, 2007 A RIGOROUS AND COMPLETED STATEMENT ON HELMHOLTZ THEOREM Y. F. Gui and W. B. Dou State Key Lab of Millimeter Waves Southeast University Nanjing, 210096, China Abstract—There are some limitations on the statement of classic Helmholtz theorem although it has broad applications. Actually, it only applies to simply connected domain with single boundary surface and does not provide any conclusion about the domain where discontinuities of field function exist. However, discontinuity is often encountered in practice, for example, the location of surface sources or interface of two kinds of medium. Meanwhile, most existing versions of Helmholtz theorem are imprecise and imperfect to some extent. This paper not only tries to present a precise statement and rigorous proof on classic Helmholtz theorem with the accuracy of mathematical language and logical strictness, but also generalizes it to the case of multiply connected domain and obtains a generalized Helmholtz theorem in the sense of Lebesgue measure and Lebesgue integral defined on three-dimensional Euclidean space. Meanwhile, our proof and reasoning are more sufficient and perfect. As an important application of the generalized Helmholtz theorem, the concepts of irrotational and solenoidal vector function are emphasized. The generalized Helmholtz theorem and the present conclusion should have important reference value in disciplines including vector analysis such as electromagnetics. 1. INTRODUCTION It is well-known that Helmholtz theorem decomposes an arbitrary vector function into two parts: one is an irrotational component which can be expressed by the gradient of a scalar function and the other is a rotational part which can be expressed by the curl of vector function.
    [Show full text]
  • Vector Fields
    Vector fields Let F = (Fx;Fy;Fz) be a vector field. The divergence of F is @F @F @F r · F = x + y + z ; @x @y @z while the curl of F is @F @F @F @F @F @F r × F = z − y ; x − z ; y − x : @y @z @z @x @x @y A vector field F is conservative if there is a scalar field φ such that F = rφ. Such a φ is called a potential function for F. The potential function is unique up to addition of a constant. 1. Consider r = (x; y; z). (a) Show that r · r = 3 and r × r = 0. (b) Find a potential function φ for which rφ = r. 2. Let a and b be constant vectors. Compute the divergence and curl of a(r · b) and a × r: 3. Define 1 1 φ(r) = = : krk px2 + y2 + z2 (a) Let E = −∇φ. Show that 0x1 r 1 E(r) = = y : krk3 2 2 2 3=2 @ A (x + y + z ) z (b) Compute r · E and r × E. 4. Define A(r) = −2 log(krk) z^ = (0; 0; − log(x2 + y2)): (a) Let B = r × A. Show that 2 2y 2x B(r) = θ^ = − ; ; 0 : krk x2 + y2 x2 + y2 (b) Compute r · B and r × B. 5. A two-dimensional vector field F = (Fx;Fy) can also be regarded as a three-dimensional vector field F = (Fx;Fy; 0) restricted to the xy-plane. In this setting, compute r · F and r × F in terms of Fx and Fy. 1 6.
    [Show full text]
  • BEE304 ELECTRO MAGNETIC THEORY 2ND YEAR 3RD SEM UNIT I ELECTROSTATICS ELECTROSTATICS : Study of Electricity in Which Electric Charges Are Static I.E
    BEE304 ELECTRO MAGNETIC THEORY 2ND YEAR 3RD SEM UNIT I ELECTROSTATICS ELECTROSTATICS : Study of Electricity in which electric charges are static i.e. not moving, is called electrostatics • STATIC CLING • An electrical phenomenon that accompanies dry weather, causes these pieces of papers to stick to one another and to the plastic comb. • Due to this reason our clothes stick to our body. • ELECTRIC CHARGE : Electric charge is characteristic developed in particle of material due to which it exert force on other such particles. It automatically accompanies the particle wherever it goes. • Charge cannot exist without material carrying it • It is possible to develop the charge by rubbing two solids having friction. • Carrying the charges is called electrification. • Electrification due to friction is called frictional electricity. Since these charges are not flowing it is also called static electricity. There are two types of charges. +ve and –ve. • Similar charges repel each other, • Opposite charges attract each other. • Benjamin Franklin made this nomenclature of charges being +ve and –ve for mathematical calculations because adding them together cancel each other. • Any particle has vast amount of charges. • The number of positive and negative charges are equal, hence matter is basically neutral. • Inequality of charges give the material a net charge which is equal to the difference of the two type of charges. Electrostatic series :If two substances are rubbed together the former in series acquires the positive charge and later, the –ve. (i) Glass (ii) Flannel (iii) Wool (iv) Silk (v) Hard Metal (vi) Hard rubber (vii) Sealing wax (viii) Resin (ix) Sulphur Electron theory of Electrification • Nucleus of atom is positively charged.
    [Show full text]
  • Vector Field Analysis Other Features Topological Features
    Vector Field Analysis Other Features Topological Features • Flow recurrence and their connectivity • Separation structure that classifies the particle advection Vector Field Gradient Recall • Consider a vector field = = , , = • Its gradient is = It is also called the Jacobian matrix of the vector field. Many feature detection for flow data relies on Jacobian Divergence and Curl • Divergence- measures the magnitude of outward flux through a small volume around a point = = + + = • Curl- describes the infinitesimal rotation around a point = = − − − ( ) = 0 ( ) = 0 Gauss Theorem • Also known as divergence theorem, that relates the vectors on the boundary of a region to the divergence in the region! = " ! # V! = # V n " n being the! outward normal" of the boundary • This leads to a physical interpretation of the divergence. Shrinking to a point in the theorem yields that the divergence! at a point may be treated as the material generated at that point Stoke Theorem • The rotation of vector field on a surface is related to its boundary V . It says that" the curl on equals the" integrated = & field over . " & ' n curl V" = , V " & • This theorem is limited to two dimensional vector fields. Another Useful Theorem about Curl • In the book of Borisenko [BT79] • Suppose with c, an arbitrary but fixed vector, substituted V = V- . into the divergence theorem. Using / , one gets V . = . V- ' curl V-! = ' n V-" ! " • Stoke’s theorem says that the flow around a region determines the curl. • The second theorem says: Shrinking the volume to a point, the curl vector indicates the axis and magnitude of the! rotation of that point. 2D Vector Field Recall • Assume a 2D vector field 0 + 1 + = = , = = + 2 + • Its Jacobian is 0 1 = = 2 • Divergence is 0 + 2 • Curl is b − d Given a vector field defined on a discrete mesh, it is important to compute the coefficients a, b, c, d, e, f for later analysis.
    [Show full text]
  • Semester II, 2015-16 Department of Physics, IIT Kanpur PHY103A: Lecture # 5 Anand Kumar
    Semester II, 2017-18 Department of Physics, IIT Kanpur PHY103A: Lecture # 18 (Text Book: Intro to Electrodynamics by Griffiths, 3rd Ed.) Anand Kumar Jha 09-Feb-2018 Summary of Lecture # 17: • The magnetic field produced by a steady line current × r = 4 r 0 ̂ � 2 ′ • The magnetic field produced by a surface current ( ) × r = 4 r′ 0 ̂ � 2 ′ • The magnetic field produced by a volume current ( ) × r = 4 ′r 0 ̂ � 2 ′ • The magnetic field due to a finite-size wire with current = sin + sin 4 0 2 1 � • The magnetic field above a loop with current = 2 + 2 / 0 2 2 3 2 • The Ampere’s Law × = = 2 0 � ⋅ 0enc Question/Clarification • Current = = • Surface Current = = Density This is per unit transverse length (not area) • Volume Current = = Density This is per unit transverse area (not volume) 3 The Divergence of The magnetic field produced by a volume current ( ) × r = 4 ′r 0 ̂ � 2 ′ r = + + ′ ′ ′ Take the divergence of− the �above magnetic− � field − (with � respect to the unprimed coordinates × r = 4 ′r 0 ̂ ⋅ � ⋅ 2 ′ Using × = × ( × ) ⋅ r⋅ − ⋅ r = × × 4 r 4 r 0 ̂ ′ ′ 0 ′ ̂ ⋅ � 2 ⋅ − � ⋅ 2 ′ × = since does not depend on r ′ ′ × = . (Prob. 1.62 Griffiths, 3rd ed.) r ̂ 2 = 0 The divergence of a magnetic field is zero. 4 ⋅ The Curl of The magnetic field produced by a volume current ( ) × r = 4 ′r 0 ̂ � 2 ′ r = + + ′ ′ ′ Take the curl of the above− magnetic� − field� (with −respect � to the unprimed coordinates × r × = × 4 ′r 0 ̂ � 2 ′ × × = + ( ) ×r r ⋅ −
    [Show full text]