We present a method to quantify kinematic stretching in incompressible, unsteady, isoviscous, three-dimensional flows. We extend the method of Kellogg and Turcotte (J. Geophys. Res. 95:421–432, 1990) to compute the axial stretching/thinning experienced by infinitesimal ellipsoidal strain markers in arbitrary three-dimensional incompressible flows and discuss the differences between our method and the computation of Finite Time Lyapunov Exponent (FTLE). We use the cellular flow model developed in Solomon and Mezic (Nature 425:376–380, 2003) to study the statistics of stretching in a three-dimensional unsteady cellular flow. We find that the probability density function of the logarithm of normalised cumulative stretching (log S) for a global...
We present a new closure for the mean rate of stretching of a dissolved polymer by homogeneous isotr...
Hyperbolic points and their unsteady generalization – hyperbolic trajectories – drive the exponentia...
The topological complexity inherent to all porous media can impart complicated transport dynamics un...
The present note deals with large time properties of the Lagrangian trajectories of a turbulent flow...
The deformation of elementary fluid volumes by velocity gradients is a key process for scalar mixing...
The deformation of elementary fluid volumes by velocity gradients is a key process for scalar mixing...
International audienceStretching and compression of material fluid elements is key for the understan...
International audienceWe study the deformation of flexible polymers whose contour length lies in the...
We study the relation between flow structure and fluid deformation in steady flows through two-dimen...
International audienceUsing index matching and particle tracking, we measure the three-dimensional v...
We observe that high-stretch tails of finite-time Lyapunov exponent distributions associated with in...
PACS. 47.27.Gs – Isotropic turbulence; homogeneous turbulence. PACS. 47.52.+j – Chaos in fluid dynam...
International audienceFluid stretching and deformation as quantified by the fluid deformation gradie...
"Passive lines in a statistically stationary isotropic incompressible turbulent flow are tracked num...
In this article we analyze the invariant geometric properties of three-dimensional (3-D) chaotic flo...
We present a new closure for the mean rate of stretching of a dissolved polymer by homogeneous isotr...
Hyperbolic points and their unsteady generalization – hyperbolic trajectories – drive the exponentia...
The topological complexity inherent to all porous media can impart complicated transport dynamics un...
The present note deals with large time properties of the Lagrangian trajectories of a turbulent flow...
The deformation of elementary fluid volumes by velocity gradients is a key process for scalar mixing...
The deformation of elementary fluid volumes by velocity gradients is a key process for scalar mixing...
International audienceStretching and compression of material fluid elements is key for the understan...
International audienceWe study the deformation of flexible polymers whose contour length lies in the...
We study the relation between flow structure and fluid deformation in steady flows through two-dimen...
International audienceUsing index matching and particle tracking, we measure the three-dimensional v...
We observe that high-stretch tails of finite-time Lyapunov exponent distributions associated with in...
PACS. 47.27.Gs – Isotropic turbulence; homogeneous turbulence. PACS. 47.52.+j – Chaos in fluid dynam...
International audienceFluid stretching and deformation as quantified by the fluid deformation gradie...
"Passive lines in a statistically stationary isotropic incompressible turbulent flow are tracked num...
In this article we analyze the invariant geometric properties of three-dimensional (3-D) chaotic flo...
We present a new closure for the mean rate of stretching of a dissolved polymer by homogeneous isotr...
Hyperbolic points and their unsteady generalization – hyperbolic trajectories – drive the exponentia...
The topological complexity inherent to all porous media can impart complicated transport dynamics un...