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Published November 1, 2015 | Published
Journal Article Open

Reflection thermal diffuse x-ray scattering for quantitative determination of phonon dispersion relations

Abstract

Synchrotron reflection x-ray thermal diffuse scattering (TDS) measurements, rather than previously reported transmission TDS, are carried out at room temperature and analyzed using a formalism based upon second-order interatomic force constants and long-range Coulomb interactions to obtain quantitative determinations of MgO phonon dispersion relations ℏω_j(q), phonon densities of states g(ℏω), and isochoric temperature-dependent vibrational heat capacities c_v(T). We use MgO as a model system for investigating reflection TDS due to its harmonic behavior as well as its mechanical and dynamic stability. Resulting phonon dispersion relations and densities of states are found to be in good agreement with independent reports from inelastic neutron and x-ray scattering experiments. Temperature-dependent isochoric heat capacities c_v(T), computed within the harmonic approximation from ℏω_j(q) values, increase with temperature from 0.4 × 10^(−4) eV/atom K at 100 K to 1.4 × 10^(−4) eV/atom K at 200 K and 1.9 × 10^(−4) eV/atom K at 300 K, in excellent agreement with isobaric heat capacity values c_p(T) between 4 and 300 K. We anticipate that the experimental approach developed here will be valuable for determining vibrational properties of heteroepitaxial thin films since the use of grazing-incidence (θ≲θ_c, where θ_c is the density-dependent critical angle) allows selective tuning of x-ray penetration depths to ≲10nm.

Additional Information

© 2015 American Physical Society. Received 24 August 2015. Revised 1 October 2015. The authors thank Dr. Mauro Sardela for valuable discussions. The financial support of the Swedish Research Council (VR) Grant No. 2014-5790 (Greene) and No. 2013-4018 (Hultman), the Swedish Government Strategic Research Area (SFO) Grant No. 2009-00971 in Materials Science on Advanced Functional Material (MatLiU AFM), and the US Department of Energy (DOE), Office of Science, Office of Basic Energy Sciences (TCC under Grant No. DE-FG02-07ER46383) is greatly appreciated. This research used resources of the Advanced Photon Source, a US DOE Office of Science User Facility operated for the DOE Office of Science by Argonne National Laboratory under Contract No. DE-AC02-06CH11357.

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Published - PhysRevB.92.174301.pdf

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