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Magnetism I. History of Magnetism Studies A. 13th Century B.C. – Chinese are using compasses with magnetic needles that were probably invented in Arabia or India B. 500 B.C. – Greeks are using magnetite (Fe3O4) to attract iron filings. The name of the stone was probably derived from the mythical shepherd Magnes whose shoes and the tip of whose staff stuck to magnetite C. 1269 A.D. – Frenchman Pierre de Maricourt mapped out magnetic field lines and magnetic poles 1. poles were named north and south because when freely suspended, they lined up with those directions on Earth 2. magnetic poles are always found in pairs – magnetic monopoles have never been isolated D. 1600 – William Gilbert proposes that Earth is itself a magnet with a magnetic field E. 1750 – Experiments show that like magnetic poles repel; unlike magnetic poles attract; and magnetic force is inversely proportional to the square of the distance between interacting poles. F. 1819 – Oersted discovers the relationship between electricity and magnetism during a lecture demonstration (Romognosi actually observed this in 1802 but failed to publish his results!) G. 1820’s – André Ampère formulated quantitative laws for calculating the magnetic force between current-carrying wires. He also suggests that on an atomic level, electric current loops produce all magnetism H. 1820’s - Michael Faraday and Joseph Henry showed that moving magnets could produce electric currents I. 1880’s James Clerk Maxwell showed that changing electric fields create magnetic fields J. Common Electromagnetic Phenomena 1. auroras 2. magnetic conduction (magnetizing unmagnetized material with a magnet) 3. magnetic induction (moving a magnet to produce a changing electric field which in turn induces another magnetic field) 4. electromagnets II. Magnetic Field A. Exists due to the presence of magnetic poles B. Definitions 1. Given the symbol B 2. Direction is specified by the orientation of the magnetic poles 3. lines always leave N poles and terminate on S poles 4. magnetic field demo with iron filings tracing out magnetic fields (see Figure 32.1) C. Magnetic Force 1. proportional to magnitude of moving charge q 2. proportional to particle velocity v 3. proportional to magnitude of B 4. depends upon direction of v and B 5. FB = 0 when v is parallel to B 6. FB is perpendicular to both v and B 7. + and – charges produce magnetic forces in opposite directions 8. proportional to sin 9. FB = qv x B a. || FB ||=|q|vB sin b. direction of force is direction of v x B if q is + and oppositely directed if q is negative c. direction is given by right-hand rule. Point fingers of right hand in the direction of v, curl them in the direction of B, and then thumb points in direction of FB for + charges. Reverse thumb direction for – charges. d. Fmax = |q|vB D. Differences between Electric and Magnetic Forces 1. FE is parallel to E; FB is perpendicular to B 2. FE acts on any charges whether the charges are stationary or moving; FB acts only on moving charges 3. FE does work in displacing a charged particle; FB does no work in displacing a charged particle E. Magnetic Field and Kinetic Energy 1. B cannot change speed of charged particle (||v||), but it can change the direction of v 1 1 2 2. KE m(v v) mv which is a scalar 2 2 3. W = KE = 0 so B does no work F. Units of B F N N B has units of 1. B qv C(m/s) Am N 2. 1 Tesla (T) = 1 Am 3. I T = 104 G where 1 G = 1 Gauss G. Table 29.1 contains typical magnetic field values 1. superconducting magnet = 30 T 2. conventional magnet = 2 T 3. MRI unit = 1.5 T 4. bar magnet = 10-2 T 5. surface of the sun = 10-2 T 6. surface of Earth = 0.5 x 10-4 T 7. human brain = 10-13 T H. Example 29.1 in class I. Magnetic Field of Earth 1. N magnetic pole coincides with S rotational pole and vice-versa. Magnetic field lines saturated with radiation produce Van Allen radiation belts 2. Horizontal component of Earth’s magnetic field currently points toward Hudson Bay in Canada 3. At Hudson Bay, compass needles point straight down 4. The difference between the magnetic pole and the rotational pole is called the magnetic declination. The magnetic declination varies with time; but its average position coincides with the rotational poles over long time scales (see Figure 32.4). 5. Convection currents in Earth’s outer core generate magnetic fields. Due to high temperatures, the magnet is not permanent. 6. Strength of magnetic field depends upon rotation rate which partially explains Jupiter’s strong field and Venus’ absent field 7. Magnetic field reverses polarity ~100,000 years as recorded by magnetic stripes on the seafloor III. Magnetic Force Acting on Current-Carrying Conductors A. A magnetic force is exerted on a charge when it passes through a magnetic field. The magnetic force on a current-carrying wire is the vector sum of the magnetic force on all of the individual charges. B. Let n = # charge carriers/volume and let q = avg charge per charge carrier in straight wire 1. FB qv d B 2. FB FB N FB FB (nAL) FB FB nAL(qv d B) 3. Recall that I (nqA) v d 4. FB L(I B) or FB I (L B) where L and I are defined to be in the same direction. C. Arbitrary Shape 1. dFB I (ds B) b 2. FB I (ds B) a D. Two Special Cases in Uniform B 1. curved wire of length L but displacement L’ b a. vector sum of ds = L’ a b b. FB I ( ds) B a c. FB I (L' B) 2. closed loop of length L but displacement 0 b a. vector sum of ds = 0 a b b. FB I ( ds) B a c. FB 0 d. net magnetic force acting on a closed loop in uniform B field is 0. E. Example 29.6 F. Biot-Savart Law 1. used to define strength of magnetic field 2. experimental observations made by Jean-Baptiste Biot and Felix Savart a. dB ds and dB rˆ 1 b. dB 2 r c. dB I and dB ds dB sin where is the angle between ds and r̂ I ds rˆ 3. dB K m (Biot-Savart law) r2 4. K m 0 where 0 = 4 x 10-7 T m/A is the magnetic permeability of free 4 space I ds rˆ 5. B 0 (Biot-Savart Law in integral form) 4 r2 6. valid for any current either in a wire or flowing through space 7. comparisons between Coulomb’s law and the Biot-Savart law a. current element produces a magnetic field whereas a point charge produces an electric field b. both electric and magnetic fields obey an inverse-square law c. E is radial from a point charge, but B is perpendicular to both r̂ and ds d. E is created by a point charge, but B requires an integration over an extended current distribution composed of many moving (flowing) charges 8. Biot-Savart law is only valid for current-carrying conductors, and it is independent of any external B-fields 9. Examples 30.1 and 30.2 done in class d. 10. Using right-hand rule and Biot-Savart law, direction of B can be determined by grasping a wire with the right hand such that the thumb points in the direction of the current. Then B is composed of concentric circles curling in the direction of the fingers. G. Magnetic Field around an Infinitely Long CurrentCarrying Wire I ds rˆ B 0 4 r2 I ds sin B 0 2 4 ( s R 2 ) I ds R B 0 2 2 4 ( s R ) ( s 2 R 2 ) 12 B 0 IR ds 4 ( s 2 R 2 ) 3 2 IR s B 0 4 R 2 ( s 2 R 2 ) 12 B 0 I 1 4R 1 ( R ) 2 s 0 I [1 (1)] 4R I B 0 2R B H. Magnetic Force between Two Parallel Wires 1. current in wire 1 senses magnetic field from wire 2 (B2) 2. current in wire 2 senses magnetic field from wire 1 (B1) 3. since wire 1 || wire 2, I1 || I2. Because B2 I2, B2 I1 4. F1 L(I1 B 2 ) F1 LI1 B2 (zˆ ) LI1 B2 zˆ 5. F2 L(I 2 B1 ) F2 LI 2 B1 (zˆ ) LI 2 B1 zˆ I 6. B 0 from Biot-Savart Law 2 a I II L 7. F1 LI1 0 2 (zˆ ) 0 1 2 zˆ 2 a 2 a F2 LI 2 0 I1 II L (zˆ ) 0 1 2 zˆ 2 a 2 a 8. F1 = - F2 as required by Newton’s 3rd law 9. Parallel currents in the same direction are attractive. Parallel currents in opposite direction are repulsive. 10. units of Amperes and Coulombs are defined by the force between two parallel wires F 2 x 10-7 N/m a. current in each wire = 1 A if L b. current balances like those used in lab can be used to calculate magnetic forces and electric currents c. 1 C = (1A) x (1 sec) 11. edge effects have been neglected, so at least one wire must have L >> a for this to be valid IV. Torque on a current Loop in a Uniform B-Field A. FB 0 on a current loop in a B-field B. τ r F on a wire 1. F L(I B i ) a. F1 L1 IBi sin F1 bIBi sin b. F2 L2 IBi sin( 90 ) Θ F2 aIBi cos Θ c. F3 L3 IBi sin Θ F3 bIBi sin Θ d. F4 L4 IBi sin( 90 ) F4 aIBi cos e. F F F F F F bIB sin aIB cos F 0 1 2 3 i 2. τ r F where r F a. τ1 r1F1rˆ2 a τ 1 ( )(bIBi sin ) rˆ2 2 τ1 12 abIBi sin rˆ2 b. τ 2 r2 F2 r̂1 b τ 2 ( )( aIBi cos ) rˆ1 2 1 τ 2 2 abIBi cos rˆ1 4 i Θ + bIBi sin Θ + aIBi cos c. τ 3 r3 F3rˆ2 a τ 3 ( )(bIBi sin ) rˆ2 2 1 τ 3 2 abIBi sin rˆ2 d. τ 4 r4 F4 r̂1 b τ 4 ( )( aIBi sin ) rˆ1 2 τ 4 12 abIBi sin rˆ1 3. τ τ τ τ τ τ abIB sin rˆ abiB cos rˆ 1 2 i 3 2 4 i 1 τ IabBi IABi 4. B B i B j B k B j 0 by definition B B i B k B is in the ik-plane A is defined in the k̂ direction since loop is in the ij-plane Bi B sin τ IabBi IAB sin 5. τ IA B a. Define μ IA to be the magnetic dipole moment of the loop b. τ IA B μ B c. τ E p E = torque on an electric dipole τ B μ B = torque on a magnetic dipole d. For N loops τ B Nμ loop B C. D. E. F. τ B μ coil B where coil = Nloop In an E-field, U E p E ; and by analogy, in a B-field, U B μ B Loop at some angle to B will rotate such that points in same direction as B to minimize PE Current-carrying loop is basis for galvanometer Examples 29.7 and 29.8 V. Motion of a Charged Particle in Uniform B-Field A. F v work done on a charged particle by a magnetic field is zero B. FB = qv x B 1. FB = centripetal force (circular motion) 2. If v B, FB = qvB 3. If v B, then v produces circular motion and v|| causes helical progression a. v v cos vˆ || v sin vˆ b. FB = q (v sin )B c. v|| v cos and v v sin x v|| t and v v y2 v z2 C. Fc = mar mv2 r 2. Fc FB qv B 1. Fc mv2 3. qv B r mv 4. r qB v qB 5. r m q q B where the quantity is called the charge to mass ratio. is m m called the cyclotron frequency. 2 2 m 6. T qB 7. Examples 29.3 and 29.4 D. If B is non-uniform, the motion of a particle can be quite complex and would involve calculus of variations or even numerical techniques to solve the problem. 1. A magnetic bottle is a B-field that is strong at the ends and weak in the middle. The strong B-fields at the end can redirect the particle’s motion back to the center, effectively trapping the particle. 2. charged plasmas can be trapped in magnetic bottles until magnetic fields are saturated. 3. Van Allen radiation belts trap cosmic rays and solar wind particles producing auroras at the poles and at lower latitudes during solar flares E. Applications of Moving Charges in E and B fields 1. Ftot FE FB qE qv B 2. velocity selector (+q) a. E is uniform and directed downward in a plane b. B is applied to E and is directed into the page. c. When qv B balances qE, then particles move in a straight line. d. The velocity at which particles move in a straight line is determined E from v B E E e. If v , particles are deflected upwards. If v , particles are B B deflected downwards. f. Gravity can be neglected because it is very much weaker than the electric and the magnetic forces. 3. Bainbridge Mass Spectrometer a. velocity selector is attached to a region where E = 0 and a new magnetic field (different in strength from the one in the velocity selector) of B0 is present. b. In the region where E = 0, mv 2 qvB0 r mv mv qB0 d r 2 q 2v m B0 d E c. v from the velocity solution, so B E q 2( B) 2E m B0 d BB0 d d. J. J. Thompson used a technique similar to this to determine the mass of the electron 4. Cyclotrons a. accelerators push charge at very high speeds b. E and B are manipulated to produce helical motion in a set of concentric cylinders c. q V gives additional energy to the particle so that 1 KE mv 2 2 qBR v where v is the ejection velocity from the cylinder and R is m the max. radius of the cylinder 2 1 qBR 1 q2B2R2 KE m 2 m 2 m d. KE expression is valid to 20 MeV before relativistic effects come into play e. Example 29.5 F. Hall Effect 1. current-carrying conductor in magnetic field has V I and V B. 2. gives info about sign of charge carriers and their density 3. Let I be in the + î direction, B in the + ĵ direction, then vd of electrons is in the – î direction and electrons are deflected by FB = qvd x B toward the + k̂ direction. 4. accumulation of electrons on upper surface causes accumulation of + charge on lower surface. This creates an E-field that produces an FE opposed to deflection. 5. Hall voltage is VH EH d where d = conductor height FB FE qv d B qE H E H vd B 6. 7. 8. 9. V H v d Bd From conduction model, I where A is the cross-sectional area of the conductor. vd nqA IBd d VH RH IB nqA A 1 RH = Hall coefficient = nq a. sign of RH gives sign of charge carriers b. magnitude gives # density works well for Li, Na, Cu, and Ag; but not for Fe, Bi, Cd, or superconductors Example 29.2 VI. Ampere’s Law A. When no current flows through a wire, compasses point in direction of B . When current flows, compasses point in direction of B. B. B I 1 B r B || ds everywhere on path so B ds B ds B cnst o I 2 r o I B ds B ds 2 r (2 r ) o I C. For any constant current, Ampere’s Law says that B ds o I , but it is only useful for highly symmetric situations. D. Example 30.3 in class E. General Form of Ampere’s Law dq is conduction current carried by the wire dt 2. If E varies in time, a new Binduced is created that produces a displacement current Id. Ampere’s Law ( B ds o I ) is only valid if E is constant. 1. currents are time-varying so I 3. E E dA qd 0 E qd 0 Electric Flux (Gauss’ Law) dq d d E 0 dt dt d E Id 0 dt d E (Ampere-Maxwell Law) dt 5. Magnetic fields are thus produced by both conduction currents and by timevarying E-fields. 6. Examples 32.3 and 32.4 F. Magnetic Field of a Solenoid 1. A solenoid is a long wire wound in a helix. 2. interior of a solenoid contains an approximately uniform B-field if wire carries a steady I 3. closely-spaced turns can be approximated as circular loops, and the net magnetic field is the vector sum of fields from all turns. 4. interior field lines are parallel and closely-spaced indicating a uniform field. External fields are weak because current elements on right side of turn cancel fields from the left sides of turn. 5. with more and closely-spaced turns, a solenoid becomes more ideal and approaches that of a bar magnet. For a perfectly ideal solenoid, the interior field is uniform over a great volume (changing only as you get near the turns of wire or the end of the solenoid), and the external field is zero. 6. B ds B ds B ds B ds B ds 0 IN 4. B ds loop o 1 ( I I d ) o I o 0 2 3 B ds BL 0 0 0 BL loop 4 0 IN B ds B ds 0 because B ds 2 4 B = 0 along wire 3 so B ds 0 3 7. BL = 0NI N B 0 I L B 0 nI # turns length 8. This equation is only truly valid for B near the middle of the solenoid; at the ends and at the walls, edge effects and proximity to the wire come into play. 1 9. At the end of a long solenoid, B end B center 2 10. Example 30.4 n VII. Magnetic Flux & Gauss’ Law for Magnetism A. Magnetic Flux 1. similar to electric flux 2. B B dA 3. B BA cos for uniform B 4. the unit of magnetic flux is the weber where 1 Wb = 1 T-m2 5. B 0 if B dA 6. B BA if B || dA B. Gauss’ Law for Magnetism 1. Gauss’ Law for E works because # lines through a surface is proportional to the enclosed charge 2. situation is very different for magnetism because magnetic fields are continuous and form closed loops 3. B dA 0 because any magnetic field lines that enter a closed surface also closed surface leave a closed surface! Electric field lines do not necessarily return to a surface that they leave. 4. A result of gauss’ Law for magnetism is that isolated magnetic monopoles cannot theoretically exist. 5. Experimentally, magnetic monopoles have never been detected, but many other physical theories suggest their possible existence. This is a fundamental area of new research. VIII. Magnetism in Matter A. Every current loop has both a magnetic field and a dipole moment. B. Magnetism in matter arises from currents at the atomic level due to an atomic property called “magnetic spin.” C. Magnetic Moments of Atoms 1. model atom as a positive nucleus by a negative electron q q qv 2. if e- has speed v and orbital radius r, then I T 2 2 r qv 1 )( r 2 ) qvr 3. magnetic moment is IA I ( r 2 ) ( 2 r 2 4. for most atoms are randomly oriented so net = 0 5. orbital angular momentum a. L r mv L rmv sin( 90) L L rm e v v rm e orb 1 1 L qvr q ( )r 2 2 rm e orb 1 q L 2 me h = 1.05 x 10-34 J s is Planck’s constant 2 c. can only measure quantized component of L along one axis Lorb, z ml where ml = 0, 1, 2, is the orbital magnetic b. quantum number 1 q L d. orb 2 me 1 (e) orb ml 2 me e orb ml 2me e. U orb μ orb B ext is potential energy of orbiting electron in an external B field f. magnetic moment of e- is proportional to L and oppositely directed because e- is negative. Both L and are perpendicular to plane of electron’s orbit. 6. Spin angular momentum e S a. μ s me b. μ s cannot be measured directly. Only its quantized component along one axis can be determined. S z ms where ms = 12 is the spin magnetic quantum number. Positive values of spin are considered to be spin “up” and negative values of spin are considered to be spin “down.” e Sz c. μ s , z me e μs,z ms me 1 e μs,z 2 me d. B = Bohr magneton = 9.27 x 10-24 J/T e. U spin μ s B ext is potential energy of spinning electron in an external B field 7. In most atoms, electrons usually pair up to cancel spin, but some atoms have an odd # of electrons. Thus, some atoms have net = 0 while others have net = angular momentum + spin. 8. magnetic moments of protons and neutrons are ~1000 times smaller than those of electrons and can generally be neglected. 9. Loop Model for Electron Orbits a. orb IA q orb (r 2 ) t e orb (r 2 ) 2 r ( ) v orb 12 evr b. L orb r (me v) Lorb me vr sin 90 Lorb me vr c. orb 12 evr Lorb me vr Take the ratio of the magnetic moment and the angular momentum orb 12 evr Lorb me vr 1 e μ orb L orb 2m d. In a non-uniform field, dF I (dL B) and sensitivity of atomic orbital angular momentum to the external magnetic field determines the magnetic properties of a material. D. Magnetization Vector and Magnetic Field Strength μ 1. magnetization vector = M = volume 2. B = Bint + B0 where B0 is the external magnetic field Bint = 0M (0 is the magnetic permeability, not the magnetic moment) B = B0 + 0M 3. magnetic field strength (H) represents the effects of conduction currents. H = magnetic field strength and B is referred to as the magnetic flux density or magnetic induction B B 4. H 0 M 0 0 B 0 ( H M) H has units of A/m 5. Example of torus in vacuum a. M = 0 in vacuum because no substance is present b. B = Bint + B0 B = B0 = 0nI B H 0 nI μ0 c. H depends only upon current and # turns of wire E. Classification of magnetic Substances 1. paramagnetic substances display permanent but weak magnetic moments 2. diamagnetic substances display no permanent magnetization 3. ferromagnetic substances display strong and permanent magnetic dipole moments 4. For paramagnetic and diamagnetic materials, M = H where is defined to be the magnetic susceptibility of a material a. If > 0, M and H lie in the same direction (paramagnetic) b. If < 0, M and H lie in opposite directions (diamagnetic) c. B 0 (H M) 0 (H H) 0 (1 )H d. m 0 (1 ) is the magnetic permeability of the material. = 0 for vacuum m > 0 is paramagnetism m < 0 is diamagnetism e. is very small for both paramagnetic and diamagnetic substances. This implies that a linear relationship exists between M and H, and that m 0. 5. In ferromagnetic substances, is very large and m >> 0. M and H also depend upon the magnetic history of the substance. F. Ferromagnetism 1. Examples include iron, cobalt, nickel, gadolinium, and dysprosium 2. magnetic moments of these materials align in a weak magnetic field and stay aligned after the field is removed 3. magnetic domains are microscopic regions typically 10-12 to 10-8 m3 in volume and containing 1017 to 1021 atoms whose magnetic moments are roughly aligned with each other. 4. domain walls separate magnetic domains of different orientations. 5. magnetic domains are randomly oriented in the absence of an external magnetic field, so average M = 0. 6. In a magnetic field, magnetic domains aligned with B0 grow at the expense of non-aligned domains. When the field is removed, ferromagnetic materials retain their alignment unless they are thermally agitated (heated). Heating will randomize magnetic moments. 7. Seafloor striping occurs because the cooling magma at mid-ocean ridges freezes in the magnetic field direction of Earth at the time. 8. Rowland rings (toroids connected to galvanometers) can measure ferromagnetic properties of a substance by determining B and H. 9. Hysteresis a. magnetic hysteresis is the ability to use a past magnetic state to achieve a new magnetization state of a ferromagnetic material b. hysteresis means “lagging behind,” and this is visible as B lags H on the magnetization curves abc and def. In both cases H reaches 0 before B reaches 0. c. magnetization that remains after B = 0 at points c and f is B = Bm = 0M. This is called remanent magnetization. d. Size of loop represents the work done in the hysteresis cycle. Shape of loop represents the ability to demagnetize a substance with an external magnetic field. Large area implies more work. Thickness of loop is proportional to magnitude of demagnetization field. e. work done goes from transformation of magnetic energy to internal energy. Devices subjected to alternating fields are made of “soft” ferromagnetic materials to minimize loop thickness and energy losses. f. Devices that use hysteresis include floppy disks, audio tapes, and videotapes to store information. G. Paramagnetism 1. Paramagnetic materials align with external B0, but when B0 is removed, magnetic domains compete with thermal agitation for alignment. B 2. Pierre Curie found experimentally that M c 0 (Curie’s Law) where c = T Curie’s constant for a particular material, M is the magnetic moment, and T is the temperature 3. Above a critical temperature (called the Curie temperature, Tc), magnetic domains are randomized. Below Tc, they are aligned with the external magnetic field B0. H. Diamagnetism 1. H and M are in opposite directions 2. diamagnetic materials tend to be repelled by magnets 3. present in all substances, but much weaker than both diamagnetism and ferromagnetism. I. Example 32.2 J. Superconductors and magnets repel each other because superconductors expel applied magnetic fields in order to keep B and E equal to 0 in their interiors. Thus magnets can be levitated above superconductors. This is called the Meissner effect.