High-frequency dynamics of v-GeO 2The effect of <strong>di</strong>sorder on the density fluctuations is atopic with so many unsolved aspects that measuringthe dynamics at THz frequencies in simple glassesremains a class of deman<strong>di</strong>ng experiments. Severalattempts have been made to experimentally identifythe nature of the excitations in the mesoscopic region,as well as the origin of the excess of states in thedensity of states (DOS) which gives rise to the BosonPeak (BP). Inelastic x-ray scattering (IXS) experimentsat THz frequency were carried out in several glassesand evidence for the existence of phonon-likeexcitations was found [1,2]. A recent contribution camefrom the observation of two excitations in the currentspectra of v-SiO 2 on IXS data and the persistence ofpropagating sound waves up to Q values close thepseudo-Brillouin-zone edge [2]. The experimentalfin<strong>di</strong>ngs were complemented by the results of MolecularDynamics Simulations (MD) [3]. This work [4] isde<strong>di</strong>cated to the investigation of the high frequencydynamics of v-GeO 2 carried out by exploiting four INSspectrometers operated over complementarykinematics ranges with <strong>di</strong>fferent energy resolutions. Insuch a way, access to a wide kinematics range with aresolution adequate to resolve the inelastic featuresunder investigation was obtained. Brillouin peaks, welldefined and resolved from the tails of the elastic peak,are clearly apparent from the spectra independently ofany model or data treatment. Increasing Q, the peakposition shifts towards higher which reveals, beyondany doubt, the propagating character of this excitation.At low Q, besides the inelastic peak associated to thesound mode, both theoretical and numerical stu<strong>di</strong>espre<strong>di</strong>ct a second <strong>di</strong>spersing excitation in the dynamicresponse function, suggesting the existence of atransverse-like dynamics (Fig. 1).1000 IN1 0.3 Å -1The whole set of the present neutron data in v-GeO 2 isconsistent with the picture of propagating vibrationalexcitations, namely a first mode which shows aremarkable <strong>di</strong>spersion, beyond which it merges into abroad inelastic bump roughly centred at ∼30 meV, anda second mode characterized by much lower excitationenergies and a much less pronounced <strong>di</strong>spersion. Weassign a longitu<strong>di</strong>nal acoustic character to the firstmode and a transverse acoustic nature to the secondmode, whose flattening at large Q could contribute tothe excess of vibrational states typical of the high-Q BP.The visibility of a transverse excitation in theintrinsically longitu<strong>di</strong>nal density fluctuation spectra of a<strong>di</strong>sordered system can be justified by the mixingphenomenon: the polarization character of thevibrations, which is well defined at low Q, becomesmore and more ill-defined at larger Q. At highfrequency the transverse dynamics acquires alongitu<strong>di</strong>nal symmetry component, observable by INSmeasurements. To give further ground to the presentinterpretation, we carried out a MD simulation on v-GeO 2 using 680 molecules in a cubic box correspon<strong>di</strong>ngto the density ρ=3.6 g cm -3 , interacting through a VanBeest-type potential. Longitu<strong>di</strong>nal and transversecurrent spectra were obtained from the simulations andthey reproduce the vibrational features observed in theexperimental spectra. The <strong>di</strong>spersion relationsassociated to the <strong>di</strong>fferent modes are shown in fig 2together with the results of MD. In conclusion we foundclear presence of two well defined peaks with anassociated <strong>di</strong>spersion, which were assigned to the highfrequency counterpart of the LA and TA modes. Thecomparison between experimental and simulated<strong>di</strong>spersion curves supported the hypothesis that thequasi-transverse acoustic modes contribute to the BP.60500S(Q, ω) [a.u.]01000 0.5 Å -15001000 IN8 0.65 Å -1500010000-30 -20 -10 0 10 20 305000-30 -20 -10 0 10 20 3080 IN3 0.75 Å -1604020080 2.0 Å -16040200-10 -5 0 5 10ω [meV]0.8 Å -1Fig. 1 Selection of INS spectra of v-GeO 2 at 300 K.Spectra show a well defined high frequency-peak<strong>di</strong>spersing in q. the low two panels show a lowfrequencyexcitation, masked in the upper spectra.Dashed lines represent the spectrometer resolutions.ω [meV]402000 2 4Q [Å -1 ]Fig. 2. Dispersion relations of v-GeO 2 as resulted fromthe fitting of the neutron data are compared with themain maximum of the simulated L (higher branch) andT (lower branch) current spectra (open triangles). Thedashed lines are the L and T sound velocity.References[1] O. Pilla et al. Phys. Rev. Lett.85, 2136 (2000).[2] B. Ruzicka et al. Phys. Rev. B 69, 100201(2004).[3] O. Pilla et al., J. Phys. Cond. Mat. 16, 8519 (2004).[4] L. E. Bove, Europhys. Lett., 71 (4), 563 (2005).Authors:S. Caponi (a), A. Fontana (a), L. E. Bove (b)(a) <strong>Dipartimento</strong> <strong>di</strong> <strong>Fisica</strong> and INFM-CRS <strong>Soft</strong>,Università <strong>di</strong> Trento, Trento, Italy; (b) CRS-SOFT Unità<strong>di</strong> Perugia.63SOFT Scientific <strong>Report</strong> 2004-06
Scientific <strong>Report</strong> – Non Equilibrium Dynamics and ComplexityBrillouin visible and ultraviolet light scattering measurementsin v-SiO 2 and silica porous systemsIt is known that a planewave excitation can propagatein a <strong>di</strong>sordered structure only when the wavelength ismuch longer than the scale spanned by microscopicinhomogeneities; as the wavelength shortens, the waveis increasingly <strong>di</strong>storted and scattered. The question asto the causes of attenuation far from the longwavelength limit, is unlikely to have a single answer,and <strong>di</strong>fferent mechanisms have been suggested.Depen<strong>di</strong>ng on the physical origin of the acoustic energy<strong>di</strong>ssipation, the attenuation can be stronglytemperature dependent (dynamic) or temperatureindependent (static). In order to clarify the interplaybetween <strong>di</strong>fferent mechanisms, is necessary toinvestigate as thoroughly as possible, besides thetemperature evolution, also the frequency evolution ofthe acoustic attenuation.Brillouin Light Scattering (BLS) and Inelastic X-RayScattering (IXS) experiments do not cover the wholefrequency and q range from GHz to THz, an<strong>di</strong>nvestigations within the frequency gap which separatesthese techniques could be useful to <strong>di</strong>scriminatebetween the <strong>di</strong>fferent hypotheses.With this purpose, thanks to a newly availablespectrometer HIRESUV, Ultraviolet Brillouin lightscattering(BUVS) experiments are possible in anunexplored frequency region. We have investigated twoprototype systems v-SiO 2 and silica porous systems.For v-SiO 2, considered as the prototype strong glass,the comparison of the new data with those obtained byIXS and BLS in<strong>di</strong>cates [1]:1) the existence of a crossover among <strong>di</strong>fferentattenuation mechanisms: from a dynamic onecharacteristic of low frequency region to a static one,which dominates in the high frequency regime.2) necessarily somewhere in the interme<strong>di</strong>ate range,the acoustic attenuation have to grow faster thanquadratically with q (see fig.1).As regard porous systems, investigating the attenuationof phonons with <strong>di</strong>fferent wavelength in homogeneoussystems, is equivalent to investigate the attenuation ata given wavelength varying the size of the microscopicinhomogeneities. We have stu<strong>di</strong>ed samples withdensities between 500 and 2200 kg/m 3 , as aΓ(GHz)1000 BUVS T=300KIXS T=1050KIXS T=300K100 POT T=300KBLS T=300K1010.10.01 0.1 1Q(nm -1 )Fig. 1 Log-log plot of Brillouin widths as a function ofthe exchanged wave vector q, obtained at roomtemperature by BLS, BUVS, IXS, POT. The dashedlines, in<strong>di</strong>cating the q 2 law, are guides for the eye.consequence of a controlled sintering procedure lea<strong>di</strong>ngto mo<strong>di</strong>fications of their “texture” and of the networkconnectivity. A dynamic to static transition in theattenuation has been found by Brillouin light scatteringmeasurements (see Fig.2) [2]. The static or dynamicalorigin of the attenuation is ascribed to the interplaybetween the mean pore sizes of the samples and theprobe wavelength. This hypothesis is confirmed by thebehaviour of attenuation investigated at twowavelength (see insets of fig.2). A crossover length a*related to the pore size has been determined. For themean pore size smaller than a* the largest contributionto the absorption comes from the attenuation due todynamic mechanisms, such as relaxation processes andanharmonic coupling. For pore size larger than a*, therapidly growing sound attenuation can be attributed tothe <strong>di</strong>sorder due to inhomogeneities produced by pores.HWHM (GHz)0.10.01Densified xerogelΓ (MHz)Γ (MHz)3002001000500400300200λ= 514.5 nmα-quarz0 5 10 15a * (UV)a * (BLS)λ= 266.0 nm0 5 10 15L1E-3p(nm)0 200 400 600 800 1000 1200Temperature (K)aerogel1xerogel1v-SiO 2Fig. 2.Temperature behaviours of the half width halfmaximum of the Brillouin peak in systems withgrooving pore size. In the inset HWHMs of visible andultraviolet Brillouin peaks versus the mean pore size.References[1] P.Benassi et al. Phys. Rev. B 71, 172201 (2005).[2] S. Caponi et al. Phys. Rev. B 70, 214204 (2004).[3] S. Caponi Phil. Mag., 84, Nos.13–16,1423 (2004).Authors:S. Caponi (a), P. Benassi (b) R. Eramo (c), A. Fontana(a), A. Giugni (b), M. Nardone (b), M. Sampoli (d), andG. Viliani (a)-(a) <strong>Dipartimento</strong> <strong>di</strong> <strong>Fisica</strong> and INFM-CRS<strong>Soft</strong>, Universita` <strong>di</strong> Trento, Italy; (b) <strong>Dipartimento</strong> <strong>di</strong><strong>Fisica</strong>, and INFM-CRS <strong>Soft</strong>, Università dell’Aquila, Italy;(c) <strong>Dipartimento</strong> <strong>di</strong> <strong>Fisica</strong> and LENS and INFM-CRS <strong>Soft</strong>,Università <strong>di</strong> Firenze, Italy; (d) <strong>Dipartimento</strong> <strong>di</strong>Energetica and INFM-CRS <strong>Soft</strong>, Università <strong>di</strong> Firenze,ItalySOFT Scientific <strong>Report</strong> 2004-0664
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