5. Lattice Vibrations Solid State Physics 355 Introduction Unlike the static lattice model, which deals with average positions of atoms in a crystal, lattice dynamics extends the concept of crystal lattice to an array of atoms with finite masses that are capable of motion. This motion is not random but is a superposition of vibrations of atoms around their equilibrium sites due to interactions with neighboring atoms. A collective vibration of atoms in the crystal forms a wave of allowed wavelengths and amplitudes. Applications • • • • • Lattice contribution to specific heat Lattice contribution to thermal conductivity Elastic properties Structural phase transitions Particle Scattering Effects: electrons, photons, neutrons, etc. • BCS theory of superconductivity Normal Modes x1 x2 u1 x3 u2 x4 u3 x5 u4 u5 Check this out... http://www-users.york.ac.uk/~dmh8/cymatic/PhysicalModelling.htm Consider this simplified system... x1 x2 u1 x3 u2 u3 Suppose that only nearest-neighbor interactions are significant, then the force of atom 2 on atom 1 is proportional to the difference in the displacements of those atoms from their equilibrium positions. F21 C1 (u1 u2 ) and F12 C1 (u2 u1 ) F32 C2 (u3 u2 ) and F23 C2 (u2 u3 ) Net Forces on these atoms... F1 C1 (u1 u2 ) F2 C1 (u2 u1 ) C2 (u2 u3 ) F3 C2 (u3 u2 ) Normal Modes Mr. Newton... m d 2u1 m dt d 2 u2 m dt d 2u3 dt 2 C1 (u1 u2 ) 2 C1 (u2 u1 ) C2 (u2 u3 ) 2 C2 (u3 u2 ) To find normal mode solutions, assume that each displacement has the same sinusoidal dependence in time. ui ui 0e it Normal Modes (C1 m 2 )u1 C1u2 0 C1u1 (C1 C2 m 2 )u2 C2u3 0 C2u2 (C2 m 2 )u3 0 C1 m 2 C1 0 C1 C1 C2 m 2 C2 0 C2 0 C2 m 2 m 2 m2 4 2(C1 C2 )m 2 3C1C2 u1 0 Normal Modes 1 0 1 2 2 1/ 2 1/ 2 2 (C1 C2 ) (C1 C2 C1C2 ) m 1 2 2 1/ 2 1/ 2 3 (C1 C2 ) (C1 C2 C1C2 ) m Brillouin Zones The value of the Brillouin Zone is that it gives a vivid geometrical interpretation of the diffraction condition: D k2 2 k G G 2 k1 1G 2 D O 1G 2 C We divide both sides by 4 to get, C k 12 G 2 1 2G Brillouin Zones The first Brillouin zone is defined to be the Wigner-Seitz primitive cell of the reciprocal lattice. Or, it could be defined as the set of points in k space that can be reached from the origin without crossing any Bragg plane. The second Brillouin zone is the set of points that can be reached from the first zone by crossing only one Bragg plane. The n th Brillouin zone can be defined as the set of points that can be reached from the origin by crossing n - 1 Bragg planes, but no fewer. Wigner-Seitz Primitive Cell How can we choose primitive cells? One algorithm is the Wigner-Seitz cell. Steps: (1) Draw lines to connect a given lattice point to all nearby lattice points (2) At the midpoint and normal to these lines, draw new lines (or planes in 3D) (3) The smallest area (or volume in 3D) enclosed in this way is the Wigner-Seitz primitive cell Wigner-Seitz Primitive Cells Brillouin Zones BCC Brillouin Zones Brillouin Zones Back to Normal Modes q Longitudinal Wave q Transverse Wave Back to Normal Modes m d 2 u2 dt 2 C (un 1 un ) C (un 1 un ) C (un 1 un 1 2un ) ui ui 0e it inqa iqa un1 ue e Traveling wave solutions m 2ueinqa C [ei ( n 1) qa ei ( n 1) qa 2einqa ] m 2 C [eiqa e iqa 2] 2cos qa 2C 1 cos qa m 2 Dispersion Relation Dispersion Relation 0.6 4C / m 4C / m q sin 12 qa First Brillouin Zone What range of q’s is physically significant for elastic waves? un1 ue iqa i ( n 1) qa un 1 ue iqa e inqa un ue The range to + for the phase qa covers all possible values of the exponential. So, only values in the first Brillouin zone are significant. First Brillouin Zone There is no point in saying that two adjacent atoms are out of phase by more than . A relative phase of 1.2 is physically the same as a phase of 0.8 . First Brillouin Zone At the boundaries q = ± /a, the solution u n ue inqa Does not represent a traveling wave, but rather a standing wave. At the zone boundaries, we have un ue in (1) n Alternate atoms oscillate in opposite phases and the wave can move neither left nor right. Group Velocity The transmission velocity of a wave packet is the group velocity, defined as 2C [1 cos qa] m 2 d vg dq or v g q (q) d Ca 2 vg [cos 12 qa] 4C dq m 1 [sin qa] m 2 Group Velocity d Ca 2 vg [cos 12 qa] dq m q Phase Velocity The phase velocity of a wave is the rate at which the phase of the wave propagates in space. This is the velocity at which the phase of any one frequency component of the wave will propagate. You could pick one particular phase of the wave (for example the crest) and it would appear to travel at the phase velocity. The phase velocity is given in terms of the wave's angular frequency ω and wave vector k by vP k Note that the phase velocity is not necessarily the same as the group velocity of the wave, which is the rate that changes in amplitude (known as the envelope of the wave) will propagate. Long Wavelength Limit 1 ( qa) 2 cos qa 1 When qa << 1, we can expand 2 so the dispersion relation becomes C 2 [qa] m 2 The result is that the frequency is directly proportional to the wavevector in the long wavelength limit. This means that the velocity of sound in the solid is independent of frequency. v ωq Force Constants 2 m 2 cos rqa m a a 2 C p [1 cos pqa] p cos(rqa ) dq 2 a C p a [1 cos pqa] cos(rqa) dq p 0 and integrate C 2 a The integral vanishes except for p = r. So, the force constant at range pa is ma Cp 2π a a 2 cos( pqa) dq for a structure that has a monatomic basis. Diatomic Coupled Harmonic Oscillators q m1 m2 d 2 un 2 C ( vn vn 1 2un ) 2 C (un un 1 2vn ) dt d 2 vn dt Diatomic Coupled Harmonic Oscillators m m2 2 C 1 C m1m2 2 m1 m2 2 1 cos qa m1m2 m1m2 For each q value there are two values of ω. These “branches” are referred to as “acoustic” and “optical” branches. Only one branch behaves like sound waves ( ω/q → const. For q→0). For the optical branch, the atoms are oscillating in antiphase. In an ionic crystal, these charge oscillations (magnetic dipole moment) couple to electromagnetic radiation (optical waves). Definition: All branches that have a frequency at q = 0 are optical. q