Lattice Dynamics 21 February, 2007 U. Milan Short Course Thermal Expansion • As temperature changes, density changes • Thermodynamics – Relates this change to changes in other properties – Cannot tell the magnitude or even the sign! • • • • Why positive alpha? What value vs. P,T,X? Macroscopic to Microscopic Thermodynamics to Statistical Mechanics Interatomic Forces • Ambient Structure • Bulk Modulus – Curvature • Thermal Expansivity – Beyond harmonic – Molecules – Solids Potential Energy – Minimum Distance One Dimensional Lattice N 2Vn,n p 1 Vn V0 (un p un ) 2 H.O.T. 2 2 pN un N Vn Fn K (u u ) un pN p n p n 2Vn,n p Kp un2 N 2 un m 2 K p (un p un ) t pN un u0 exp inka t pka 4 N K p sin 2 2 m p1 2 2 ka K sin m 2 One Dimensional Lattice • Periodicity reflects that of the lattice • Brillouin zone center, k=0: =0 • Brillouin zone edge, k=/a: =maximum • All information in first Brillouin zone Frequency, 1st Brillouin Zone 2(K/m)1/2 0 Wavevector, k One Dimensional Lattice k=/a=2/; =2a k0; Acoustic Velocities K ka sin m 2 – k0 – w=2(K/m)1/2ka/2 – w/k=dw/dk=a(K/m)1/2 • Acoustic Velocity – v=a(K/m)1/2 • Three dimensions – Wavevector, ki – Polarization vector, pi – For each ki, 3 acoustic branches – ki pi longitudinal (P) wave – kipi transverse (S) waves (2) Frequency 2 0.0 0.2 0.4 0.6 Wavevector (a) 0.8 1.0 Polyatomic Lattice a New Brillouin Zone Frequency • Unit cell doubled • Brillouin Zone Halved • Acoustic Branches folded • New, finite frequency mode at k=0 • Optic Branch 0.0 0.2 0.4 0.6 Wavevector (a) 0.8 1.0 General Lattice Fumagalli et al. (2001) EPSL • Number of modes = 3N organized into 3Z branches – Z= number of atoms in unit cell • 3 Acoustic branches • 3Z-3 optic branches • Experimental Probes – Optic zone center • Raman • Infrared – Acoustic near zone center • Brillouin – Full phonon spectrum • Inelastic neutron scattering Quartz MgSiO3 Perovskite Movie Internal Energy Energy • Sum over all vibrational modes • Energy of each mode depends on n=3 – Frequency – Population • Frequency • Temperature n=2 n=1 1 E n n 2 n=0 Displacement Heat Capacity U vib 3N 1 3N i ni i 2 i1 i1 1 n i exp i 1 kT 3N U vib 3N 1 i 2 i1 i1 i i exp 1 kT High Temperature 3N U vib 3N 1 i kT 2 i1 i1 U CV 3Nk T V • or • CV=3R per mol of atoms (Dulong-Petit) Thermal Pressure 1 3N i 1 3N FTH i kT ln 1 exp kT 2 i1 i1 FTH PTH V T PTH V UTH 3N i i i1 i Energy 3N i i1 ln i ln V • Compression Increases – Vibrational frequencies – Vibrational energy • Thermal pressure Displacement Thermal Pressure 2 Thermal Pressure PTH 3RT Bulk Modulus KTH 1 q Volume dependence of ln q ln Thermal pressure Interatomic Forces • Ambient Structure • Bulk Modulus – Curvature • Thermal Expansivity – Beyond harmonic – Molecules – Solids Potential Energy – Minimum Distance Fundamental Thermodynamic Relation Helmholtz free energy as a function of volume and temperature Complete information of equilibrium states/properties F(V,T) Divide into purely volume dependent “cold” part and a thermal part F(V,T) F0 F(V,T0 ) FTH (V,T) Recall we already have an expression for the “cold” part Cold part • • Start from fundamental relation Helmholtz free energy 140 F=af 120 • Isotherm, fixed composition – F=F(V) • • Taylor series expansion Expansion variable must be V or function of V – F = af2 + bf3 + … • • Pressure (GPa) – F=F(V,T,Ni) f = f(V) Eulerian finite strain a = 9K0V0 2 MgSiO3 Perovskite 300 K 100 80 60 40 20 0 0.70 0.75 0.80 0.85 0.90 0.95 1.00 Volume, V/V 0 Thermal part FTH 3N i 1 3N i kT ln 1 exp 2 i1 kT i1 Not easily evaluated, need to know all vibrational frequencies at all pressures This information not available for ANY mantle mineral! What to do? Frequencies only appear in sums Thermodynamics insensitive to details of distribution of frequencies Assume i=E, all i, where E is a characteristic frequency of the material -1 -1 -1 -1 -1 Anorthite 522 cm-1 Forsterite 562 cm-1 Corundum 647 cm-1 -1 -1 Characteristic (Debye) frequencies -1 -1 CP , (H-H0)/T, S+10 (J mol atom K ) CP , (H-H0)/T, S+10 (J mol atom K ) CP , (H-H0)/T, S+10 (J mol atom K ) Comparison to experiment 70 Anorthite 60 50 S 40 CP 30 20 (H-H0)/T 10 0 0 70 -10 500 1000 1500 2000 Temperature (K) Forsterite 60 50 S 40 30 CP 20 (H-H0)/T 10 0 0 70 500 1000 1500 2000 -10 Temperature (K) Corundum 60 50 S 40 CP 30 20 (H-H0)/T 10 0 -10 0 500 1000 1500 Temperature (K) 2000