Flexural vibrations of geometrically nonlinear composite beams with interlayer slip
- Standort
-
Deutsche Nationalbibliothek Frankfurt am Main
- ISSN
-
1619-6937
- Umfang
-
Online-Ressource
- Sprache
-
Englisch
- Anmerkungen
-
online resource.
- Erschienen in
-
Flexural vibrations of geometrically nonlinear composite beams with interlayer slip ; volume:231 ; number:1 ; day:25 ; month:10 ; year:2019 ; pages:251-271 ; date:1.2020
Acta mechanica ; 231, Heft 1 (25.10.2019), 251-271, 1.2020
- Urheber
-
Adam, Christoph
Furtmüller, Thomas
- Beteiligte Personen und Organisationen
-
SpringerLink (Online service)
- DOI
-
10.1007/s00707-019-02528-2
- URN
-
urn:nbn:de:101:1-2020042720225323125174
- Rechteinformation
-
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Letzte Aktualisierung
-
14.08.2025, 10:54 MESZ
Datenpartner
Dieses Objekt wird bereitgestellt von:
Deutsche Nationalbibliothek. Bei Fragen zum Objekt wenden Sie sich bitte an den Datenpartner.
Deutsche Nationalbibliothek. Bei Fragen zum Objekt wenden Sie sich bitte an den Datenpartner.
Beteiligte
- Adam, Christoph
- Furtmüller, Thomas
- SpringerLink (Online service)
Ähnliche Objekte (12)
Powder interlayer bonding of geometrically complex Ti-6Al-4V parts
Spatial Modulation of Nonlinear Flexural Vibrations of Membrane Resonators
Coupled mechanical oscillator enables precise detection of nanowire flexural vibrations
Free flexural vibrations of homogeneous beams with symmetrically variable depths
Curved composite beam with interlayer slip loaded by radial load
In-plane instability of shallow layered arches with interlayer slip
Moderately large deflection of slightly curved layered beams with interlayer slip
Static response of a slightly precurved layered beam with interlayer slip
Ultrafast acousto-optic modulation at the near-infrared spectral range by interlayer vibrations
The nonlocal elasticity theory for geometrically nonlinear vibrations of double-layer nanoplate systems in magnetic field
Lithospheric folding by flexural slip in subduction zones as source for reverse fault intraslab earthquakes
Effects of Incident Nearfield Waves on the Reflection Coefficients for Flexural Vibrations with a Nonlinear Boundary
Powder interlayer bonding of geometrically complex Ti-6Al-4V parts
Spatial Modulation of Nonlinear Flexural Vibrations of Membrane Resonators
Coupled mechanical oscillator enables precise detection of nanowire flexural vibrations
Free flexural vibrations of homogeneous beams with symmetrically variable depths
Curved composite beam with interlayer slip loaded by radial load
In-plane instability of shallow layered arches with interlayer slip
Moderately large deflection of slightly curved layered beams with interlayer slip
Static response of a slightly precurved layered beam with interlayer slip
Ultrafast acousto-optic modulation at the near-infrared spectral range by interlayer vibrations
The nonlocal elasticity theory for geometrically nonlinear vibrations of double-layer nanoplate systems in magnetic field
Lithospheric folding by flexural slip in subduction zones as source for reverse fault intraslab earthquakes
Effects of Incident Nearfield Waves on the Reflection Coefficients for Flexural Vibrations with a Nonlinear Boundary
Powder interlayer bonding of geometrically complex Ti-6Al-4V parts
Spatial Modulation of Nonlinear Flexural Vibrations of Membrane Resonators
Coupled mechanical oscillator enables precise detection of nanowire flexural vibrations
Free flexural vibrations of homogeneous beams with symmetrically variable depths
Curved composite beam with interlayer slip loaded by radial load
In-plane instability of shallow layered arches with interlayer slip
Moderately large deflection of slightly curved layered beams with interlayer slip
Static response of a slightly precurved layered beam with interlayer slip
Ultrafast acousto-optic modulation at the near-infrared spectral range by interlayer vibrations
The nonlocal elasticity theory for geometrically nonlinear vibrations of double-layer nanoplate systems in magnetic field
Lithospheric folding by flexural slip in subduction zones as source for reverse fault intraslab earthquakes