Results 91 to 100 of about 856 (202)
Non-linear anelasticity of several Cu-based $\beta_1\,'$ martensitic alloys, exhibiting different stabilization properties, has been studied over wide temperature (8 to 300 K) and strain amplitude (2*10$^{-7}$ to 2*10$^{-4}$) ranges.
S. Golyandin +4 more
core +1 more source
A Nanoindentation Study of Attenuation in Geological Materials
The dissipation of elastic strain energy, or attenuation, in Earth materials contributes to a range of geophysical phenomena, such as the damping of seismic waves and tidal heating of planetary bodies. We present a new method for measuring attenuation in
Nir Z. Badt, Ron Maor, David L. Goldsby
doaj +1 more source
Room-temperature oxygen vacancy migration induced reversible phase transformation during the anelastic deformation in CuO. [PDF]
Li L +10 more
europepmc +1 more source
Ti-15Zr and Ti-15Zr-5Mo Biomaterials Alloys: An Analysis of Corrosion and Tribocorrosion Behavior in Phosphate-Buffered Saline Solution. [PDF]
Santos AA +5 more
europepmc +1 more source
19th International Conference on Internal Friction and Mechanical Spectroscopy. [PDF]
Golovin IS, Cordero F.
europepmc +1 more source
Anelasticity in freestanding aluminum thin films.
Anelastic deformation is present in all metals, but it is generally negligible in bulk form and at low homologous temperatures. In thin films, anelastic deformation contributes a great deal to the overall mechanical properties.
core
The Anelasticity of the Mantle [PDF]
The attenuation of seismic waves provides the most direct data regarding the non-elastic properties of the Earth. Recent experimental results from body waves, surface waves and free oscillations provide estimates of the anelasticity in various regions of
Anderson, Don L.
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Structural Relaxation, Rejuvenation and Plasticity of Metallic Glasses: Microscopic Details from Anelastic Relaxation Spectra. [PDF]
Atzmon M, Ju JD, Lei T.
europepmc +1 more source
Viscoelastic behaviour of basaltic lavas. [PDF]
The rheological properties of basaltic lavas from Etna, Hawai′i and Vesuvius have been investigated at temperatures between 500 and 1150°C using a small-strain oscillatory shear. The viscoelastic response of the lavas to small, forced, sinusoidal torques
James, M R +3 more
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