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Maxwell’s microscopic equations (gaussian units): Classical theory: Quantum theory:
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Maxwell’s macroscopic equations Macroscopic charge density and current averaged over a volume ΔV, where a 0 3 << ΔV << (2πc/ω) 3 Gauss: Ampère: Faraday: Gauss' law for magnetism:
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Purely transversal Currents and charge densities: External sources + internal sources We can distinguish three types of macroscopic internal sources: Conduction by free charges, polarization (‘bound charge) and magnetization
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Gauss: Ampère: Magnetic field strength Gauss: Ampère: External field
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Properties of the Medium, Linear Response to an externally applied electric field in homogeneous matter: Plane waves External currents are zero inside sample, Homogeneous sample: Ampère’s law:
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Induced current: free charges+polarization+magnetization
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Current response to an externally applied electric field in homogeneous matter:
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Kramers Kronig Relations
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Transverse EM+matter waves: Polaritons Polaritons: Transverse polarized waves of Matter & EM field Wave equation Substituton of this solution in the wave equation provides the dispersion relation:
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It is often convenient to use the optical constant in this expression, which has a real and imaginary part: Note, that n>0 and k>0. Also Im(ε)>0, but it is possible to have Re(ε)<0. If Im(ε)=0 and Re(ε) 0, but there is no dissipation! The polariton solitions in the solid have the form
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Case study: The Drude model
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Optical techniques Polarizer Sample Au evaporator Polarizer Sample Analyzer ellipsometry reflection Optical conductivity 1 ( i sample transmission
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1) In most cases only information can be obtained for q << 1/a 0 Experimental ways to measure 2) can be found by means of optical refraction, reflection, absorption, and polarization analysis.
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Transverse EM+matter waves: Unless specified otherwise, we will from now on assume that
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Reflection and transmission at a vacuum-sample interface EiEi ErEr EtEt
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Often the experiment provides the reflected intensity instead of the amplitude, and the phase of the reflected signal is in general difficult to measure. The reflection coefficient is: Kramers Kronig Relations are often used to get the phase of the reflectivity
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Example I : pure Bi
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306090 E (meV) 0
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Reflectivity at an oblique angle P-polarization: E p is Parallel to the plane of reflection b c a EpEp HsHs HsHs EpEp
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Reflectivity at an oblique angle S-polarization: E s is Senkrecht to the plane of reflection b c a HpHp EsEs EsEs HpHp Senkrecht (german) = Perpendicular
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NbN Optically isotropic Normal incidence grazing incidence. Angle = 80 0 p-polarized light
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Grazing incidence. Angle = 80 0 p-polarized light
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Josephson Coupled Planes d d C C L L Josephson Plasma Resonance at
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Re 0 1 Reflection normal to ac-plane 0 1 Grazing incidence reflection of ab-plane
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La 2-x Sr x CuO 4 Tl 2 Ba 2 CuO 6
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Spectroscopic ellipsometry: Measurement of |r p /r s | and p - s ( ) i ( ) - self normalizing technique (no reference is required) - measures directly both real and imaginary parts of the dielectric function
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Spectroscopic ellipsometry b c a P A0A0
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I) II) polariseranalyser Ellipsometrie A0A0 2γ Ellipsometry technique
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polariseranalyser Ellipsometrie A0A0 2γ Ellipsometry technique I) II)
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Spectroscopic ellipsometry Aspnes theorem b c a P A0A0 Aspnes theorem:
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Bi2212
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Pseudo ab-plane dielectric function ab-plane dielectric function corrected for c-axis admixture
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Experiment and ab-initio calculations
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Thick wedged films:
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M.U. Gruninger, 1999 PhD Thesis YBa 2 Cu 3 O 6 Weakly absorbing excitations in insulating YBa 2 Cu 3 O 6 No absorbtive features in R( ) Absorbtive features in T( )
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Optical Transmission
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Thin films:
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NbN d=400 nm 9 K 13 K 9 K 13 K 18 K
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Fused quartz KRS5 NdGaO 3
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SrTiO 3 Sr 010 30 20 4050 Transmission
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THz time domain measurements Fabry-Perot etalon source detector
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THz time domain measurements Fabry-Perot etalon source detector
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THz transmission of SrTiO 3 3132 34 33 3536 37 delay line (mm) intensity (a.u.) Time domain
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THz transmission of SrTiO 3 3132 34 33 3536 wavenumber (cm -1 ) 010 30 20 4050 37 delay line (mm) intensity (a.u.) 0.1 10 -5 10 -3 transmission Time domain Frequency domain Fourier transformation
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Drude-Lorentz fit with RefFIT http://optics.unige.ch/alexey/reffit.html
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010 30 20 40 Transmission 50 Direct measurement of the polariton (q) relation
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