Results 261 to 270 of about 81,786 (299)
Some of the next articles are maybe not open access.
Iterated Integrals, Gelfand—Leray Residue, and First Return Mapping
Journal of Dynamical and Control Systems, 2006Recently, one of the authors gave an algorithm for calculating the first nonzero Poincaré-Pontryagin function of a small polynomial perturbation of a polynomial Hamiltonian, under a generic hypothesis. We generalize this algorithm and show that any Poincaré-Pontryagin function of order l, denoted by Ml, can be written as a sum of an iterated integral ...
Françoise, Jean-Pierre, Pelletier, M.
openaire +1 more source
Linearization and return mapping algorithms for elastoplasticity models
International Journal for Numerical Methods in Engineering, 2003AbstractThe return mapping algorithm is one of the most efficient procedures to solve elasto‐plastic problems. However, a criticism that may be lodged against this method is the difficulty of the practical computation of the consistent tangent matrix when the return is non‐radial. Much research has been done to handle this matrix.
Asensio, G., Moreno, C.
openaire +1 more source
A stochastic return map for stochastic differential equations
Journal of Statistical Physics, 1990zbMATH Open Web Interface contents unavailable due to conflicting licenses.
Weiss, Jeffrey B., Knobloch, Edgar
openaire +2 more sources
A return mapping algorithm for plane stress elastoplasticity
International Journal for Numerical Methods in Engineering, 1986AbstractAn unconditionally stable algorithm for plane stress elastoplasticity is developed, based upon the notion of elastic predictor‐return mapping (plastic corrector). Enforcement of the consistency condition is shown to reduce to the solution of a simple nonlinear equation. Consistent elastoplastic tangent moduli are obtained by exact linearization
Simo, J. C., Taylor, R. L.
openaire +1 more source
Control Bifurcation Structure of Return Map Control in Chua's Circuit
International Journal of Bifurcation and Chaos, 1997We demonstrate that return map control and adaptive tracking can be used together to locate, stabilize, and track unstable periodic orbits (UPOs). Through bifurcation studies as a function of some control parameters of return map control, we observe the control bifurcation (CB) phenomenon which exhibits another route to chaos.
Lee, Byoung-Cheon +2 more
openaire +1 more source
Estimating Lyapunov Exponents from Approximate Return Maps
1989Phase portrait reconstructions from experimental time series are widely used for the calculation of dimensions, Lyapunov exponents and entropy, all of which can be used to characterise a dynamical system and investigate the effect of varying external parameters (Schuster 1984).
openaire +1 more source
Return maps of folded nodes and folded saddle-nodes
Chaos: An Interdisciplinary Journal of Nonlinear Science, 2008Folded nodes occur in generic slow-fast dynamical systems with two slow variables. Open regions of initial conditions flow into a folded node in an open set of such systems, so folded nodes are an important feature of generic slow-fast systems. Twisting and linking of trajectories in the vicinity of a folded node have been studied previously, but their
openaire +2 more sources
Cascaded Return Map Models a Nonperiodically Clocked CPM Boost Converter
Nonlinear Dynamics, 2006zbMATH Open Web Interface contents unavailable due to conflicting licenses.
Krupar, Jörg, Schwarz, Wolfgang
openaire +2 more sources
Return-Mapping and Consistent Tangent Modulus Tensor
2014Constitutive equations of irreversible deformation, e.g. elastoplastic, viscoelastic and viscoplastic deformations are described in rate forms in which the stress rate and the strain rate are related to each other through the tangent modulus. Therefore, numerical calculations are executed in their incremental forms by the input of load (stress ...
openaire +1 more source
The displacement function and the return map
2011This chapter studies the displacement function dᵧ on X that is associated with a semisimple element γ ∈ G. If φ″, t ∈ R denotes the geodesic flow on the total space X of the tangent bundle of X, the critical set X(γ) ⊂ X of dᵧ can be easily related to the fixed point set Fᵧ ⊂ X of the symplectic transformation γ⁻¹φ₁ of X.
openaire +1 more source

