Stability analysis and investigation of a magnetoelastic beam subjected to axial compressive load and transverse magnetic field (Q1958827)
From MaRDI portal
| This is the item page for this Wikibase entity, intended for internal use and editing purposes. Please use this page instead for the normal view: Stability analysis and investigation of a magnetoelastic beam subjected to axial compressive load and transverse magnetic field |
scientific article; zbMATH DE number 5793744
| Language | Label | Description | Also known as |
|---|---|---|---|
| English | Stability analysis and investigation of a magnetoelastic beam subjected to axial compressive load and transverse magnetic field |
scientific article; zbMATH DE number 5793744 |
Statements
Stability analysis and investigation of a magnetoelastic beam subjected to axial compressive load and transverse magnetic field (English)
0 references
30 September 2010
0 references
Summary: The interactive behaviors between transverse magnetic fields and axial loads of a magnetoelastic (ME) beam subjected to general boundary conditions are investigated. In particular, the instability criterion for the magneto-mechanical buckling problem is intricately discussed based on the structure characteristics and the initial conditions. The equation of motion for the proposed physical model is introduced according to the Hamilton's principle, and the stability criterion is obtained by using the method of multiple scales implemented on both spatial and time domains. Eventually a so-called Schrodinger equation with cubic nonlinearity (NLS) can be generated by suitably changing the variables; as a result, the stable criterion for the magnetoelastic beam can be acquired after dissecting the nonlinear Schrodinger equation and requiring the imaginary part of the time domain solution to be vanished. Stability criterion curve for the dispersion equation of the ME beam is firstly depicted in order to reveal the magnificent influence of the structure characteristic itself, followed by the instability constraint due to the variation of initial conditions and the observation locations. The results indicate that the prior one actually denotes a parabola, whereas the latter one is sometimes a diamond-like or ellipse-like region spotting along the prior one.
0 references