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Wave Dispersion EM radiation Maxwell’s Equations 1
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2 - Simply stated, a dispersion relation is the function ω(k) for an harmonic wave. - A dispersion relation connects different properties of the wave such as its energy, frequency, wavelength and wavenumber. - From these relations the phase velocity and group velocity of the wave can be found and thereby refractive index of the medium can be determine. Wave Dispersion
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t0t0 t1t1 t2t2 Non dispersive : All colours moving with same speed Dispersive: Red moving faster than blue 3
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Normal dispersion of visible light Shorter (blue) wavelengths refracted more than long (red) wavelengths. Refractive index of blue light > red light.
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A medium in which phase velocity is frequency dependent is known as a dispersive medium, and a dispersion relation expresses the variation of as a function of k. Group velocity If a group contains number of components of frequencies which are nearly equal, then:
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Phase and Group velocity P’ vgvg 6
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Non dispersive waves v p = Constant Signal is propagated without distortion More generally v p is a function of (or k) 7
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Usually, is positive, so that v g < v p Normal Dispersion When, is negative, so that v g > v p Anomalous Dispersion More in electromagnetic waves When, is constant, so that v g = v p Non-Dispersive medium (Ex: Free space)
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Wave packet (without Dispersion) Wave packet (with Dispersion)
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Non-dispersive Dispersive Wikipedia.org
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Wave Packets
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y(t) = Sin t 0 < t < 200 Superposition of waves and wave packet formation 12
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y(t) = [Sin t + Sin (1.08 t)]/2 0 < t < 200 13
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Suppose we have group of many frequency components lying within the narrow frequency range …
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y(t) = [Sin t + Sin(1.04 t) + Sin (1.08 t)]/3 0 < t < 400 15
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y(t) = [Sin t + Sin(1.02 t) + Sin (1.04 t) + Sin(1.06 t) + Sin (1.08 t)]/5 0 < t < 400 16
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y(t) = [Sin t + Sin(1.01 t) + Sin (1.02 t) + Sin(1.03 t) + Sin (1.04 t) + Sin (1.05 t) + Sin (1.06 t) + Sin (1.07 t) + Sin (1.08 t)]/9 0 < t < 800 17
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y(t) = [Sin t + Sin(1.01 t) + Sin (1.02 t) + Sin(1.03 t) + Sin (1.04 t) + Sin (1.05 t) + Sin (1.06 t) + Sin (1.07 t) + Sin (1.08 t)]/9 0 < t < 400 18
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19 http://en.wikipedia.org/wiki/Coherence_%28physics%29
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Electromagnetic Radiation
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Let‘s first develop the understanding by taking the example of oscillating charge and/or dipole oscillator 21
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For stationary charges the electric force field Coulomb’s law © 2005 Pearson Prentice Hall, Inc
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Coulomb’s law What is the electric field produced at a point P by a charge q located at a distance r? where e r is an unit vector from P to the position of the charge
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If a charge moves non-uniformly, it radiates © 2005 Pearson Prentice Hall, Inc
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http://www.cco.caltech.edu/~phys1/java/phys1/MovingCharge/MovingCharge.html The electric field of a moving point charge
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Electric field - P :unit vector directed from q to P at earlier time q
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_ The correct formula for the electric field Important features 1.No information can propagate instantaneously 2. The electric field at the time t is determined by the position of the charge at an earlier time, when the charge was at r’, the retarded position. 3. First two terms falls off as 1/r’ 2 and hence are of no interest at large distances
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Correct Expression (at large distances) This is electro-magnetic radiation or simply radiation. It is also to be noted that only accelerating charges produce radiation.
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Electric Dipole Oscillator © SPK/SB
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Radio-wave transmission
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Car Antenna TV Antenna
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“Let there be electricity and magnetism and there is light” J.C. Maxwell
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Vector Analysis (Refresh)
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- The gradient points in the direction of the greatest rate of increase of the function, - and its magnitude is the slope (rate of increase) of the graph in that direction. GRADIENT For a scalar function T of three variable T(x,y,z), the gradient of T is a vector quantity given by:
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DIVERGENCE For a vector T the divergence of T is given by: It is a measure of how much the vector T diverges / spreads out from the point in question.
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CURL For a vector T the Curl of T is given by: It is a measure of how much the vector T curls around the point in question.
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DIVERGENCE THEOREM / Green’s Theorem / Gauss’s Theorem Integral of a derivative (in this case the divergence) over a volume is equal to the value of the function at the surface that bounds the volume.
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Integral of a derivative (in this case the curl) over a patch of surface is equal to the value of the function at the boundary (perimeter of the patch). STOKES’ THEOREM
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What we know from previous classes? 1)Oscillating magnetic field generates electric field (Faraday´s law) and vice-versa (modified Ampere´s Law). 2)Reciprocal production of electric and magnetic fields leads to the propogation of EM waves with the speed of light. Question: WAVES?????? How do we show that a wave is obtained? 40
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Our Attempt: To derive the relevant wave equation 41
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x y z EyEy BzBz Consider an oscillating electric field E y January 21, 201642 This will generate a magnetic field along the z- axis
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C E y (x) E y (x+ x) x Y Z We know that Faraday´s law in the integral form in given as: where C is the rectangle in the XY plane of length l width x, and S is the open surface spanning the contour C January 21, 201643 Faraday’s Law N: Number of turns B: External magnetic field A: Area of coil The induced electromotive force in any closed circuit is equal to the negative of the time rate of change of the magnetic flux through the circuit.
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Using the Faraday´s law on the contour C, we get: this implies... Keep this in mind... 44
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We know that the Ampere´s law with displacement current term can be written as: EyEy xx C/C/C/C/ x z Y B z (x) B z (x+ x) 45
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Using the Ampere´s law, for the Contour C /, we get: this implies... 46
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Using the eq. obtained earlier i.e., Note: Similar Equation can be derived for B z Form of wave equation 47
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Solution of EM Wave equation
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Electromagnetic waves for E field for B field
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In general, electromagnetic waves Where represents E or B or their components
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# A plane wave satisfies wave equation in Cartesian coordinates # A spherical wave satisfies wave equation in spherical polar coordinates # A cylindrical wave satisfies wave equation in cylindrical coordinates
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Solution of 3D wave equation In Cartesian coordinates Separation of variables
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Substituting for we obtain Variables are separated out Each variable-term independent And must be a constant
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So we may write where we use
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Solutions are then Total Solution is plane wave
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Traveling 3D plane wave
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spherical waves Spherical coordinates (r, θ, φ): radial distance r, polar angle θ (theta), and azimuthal angle φ (phi)
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Spherical waves
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Alternatively The wave equation becomes
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Put Then Hence
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Therefore Wave equation transforms to
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Which follows that Separation of variables Solutions are Total solution is
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outgoingwaves incomingwaves Final form of solution General solution spherical wave
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Cylindrical waves Cylindrical Coordinate Surfaces(ρ, φ, z). The three orthogonal components, ρ (green), φ (red), and z (blue), each increasing at a constant rate. The point is at the intersection between the three coloured surfaces.
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with angular and azimuthal symmetry, the Laplacian simplifies and the wave equation
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The solutions are Bessel functions. For large r, they are approximated as
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Maxwell’s equations
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Use B in Divergence Theorem No magnetic monopoles II
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Use E in Stokes’ Theorem From Faraday’s Law III
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IV Use B in Stokes’ Theorem From Ampere’s Law
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Charge conservation is a fundamental law of Physics which is written as a continuity equation
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IV
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Maxwell’s equations
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Plane EM waves in vacuum
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Wave vector k is perpendicular to E Wave vector k is perpendicular to B
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B is perpendicular to E
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B, k and E make a right handed Cartesian co-ordinate system
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Plane EM waves in vacuum
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