Electron, spin-wave, hyperfine, and phonon contributions to the low-temperature specific heat of La0.65Ca0.35MnO3: Effects of magnetic fields and O-16/O-18 exchange - art. no. 134425

Citation
Ra. Fisher et al., Electron, spin-wave, hyperfine, and phonon contributions to the low-temperature specific heat of La0.65Ca0.35MnO3: Effects of magnetic fields and O-16/O-18 exchange - art. no. 134425, PHYS REV B, 6413(13), 2001, pp. 4425
Citations number
42
Categorie Soggetti
Apllied Physucs/Condensed Matter/Materiales Science
Journal title
PHYSICAL REVIEW B
ISSN journal
01631829 → ACNP
Volume
6413
Issue
13
Year of publication
2001
Database
ISI
SICI code
0163-1829(20011001)6413:13<4425:ESHAPC>2.0.ZU;2-Z
Abstract
The field-dependent low-temperature specific heat of an optimally doped pol ycrystalline sample of La0.65Ca0.35MnO3 (T-C=265 K), 1 less than or equal t oT less than or equal to 32 K and 0 less than or equal toH less than or equ al to9 T was analyzed by a global least-square fit to separate the hyperfin e, electronic, spin-wave, and lattice contributions. The hyperfine and spin -wave contributions are in quantitative agreement with nuclear magnetic res onance and inelastic neutron-scattering results, respectively, This agreeme nt supports the validity of both the data and their analysis. The calculate d bandstructure electron density of states is enhanced by a factor of 1.25. Specific heat was measured for two pieces cut from the O-16 parent sample and processed in parallel to produce an O-18 and a reference O-16 sample. T he parallel-processed samples have very much larger lattice contributions ( similar to 50% at low temperatures) than the parent sample, and a somewhat larger electronic contribution. Evidently, the many processing cycles neede d for O-18 homogeneity produced modifications to both the long-wavelength p honons and the electron density of states. The spin-wave contribution has a small shift-nearly within the experimental accuracy-expected for the O-18/ O-16 exchange, while the hyperfine contribution is independent of isotope c omposition.