Network and geometric characterization of three-dimensional fluid transport between two layers
arXiv:2108.11191 · doi:10.1103/PhysRevE.104.065111
Abstract
We consider transport in a fluid flow of arbitrary complexity but with a dominant flow direction. This is the situation encountered, for example, when analyzing the dynamics of sufficiently small particles immersed in a turbulent fluid and vertically sinking because of their weight. We develop a formalism characterizing the dynamics of particles released from one layer of fluid and arriving in a second one after traveling along the dominant direction. The main ingredient in our study is the definition of a two-layer map that describes the Lagrangian transport between both layers. We combine geometric approaches and probabilistic network descriptions to analyze the two-layer map. From the geometric point of view, we express the properties of lines, surfaces and densities transported by the flow in terms of singular values related to Lyapunov exponents, and define a new quantifier, the Finite Depth Lyapunov Exponent. Within the network approach, degrees and an entropy are introduced to characterize transport. We also provide relationships between both methodologies. The formalism is illustrated with numerical results for a modification of the ABC flow, a model commonly studied to characterize three-dimensional chaotic advection.
References in corpus (14)
- Predictability in the large: an extension of the concept of Lyapunov exponent
- Flow networks: A characterization of geophysical fluid transport
- Boundaries of the Peruvian Oxygen Minimum Zone shaped by coherent mesoscale dynamics
- Most probable paths in temporal weighted networks: An application to ocean transport
- Sinking microplastics in the water column: simulations in the Mediterranean Sea
- Modeling the dynamical sinking of biogenic particles in oceanic flow
- Dominant transport pathways in an atmospheric blocking event
- Lagrangian betweenness as a measure of bottlenecks in dynamical systems with oceanographic examples
- Characterization of coherent structures in three-dimensional flows using the finite-size Lyapunov exponent
- Characterization of the structure and cross-shore transport properties of a coastal upwelling filament using three-dimensional finite-size Lyapunov exponents
- Lagrangian Flow Network approach to an open flow model
- Inhomogeneities and caustics in the sedimentation of noninertial particles in incompressible flows
- Spatial inhomogeneities in the sedimentation of biogenic particles in ocean flows: analysis in the Benguela region
- Accumulated densities of sedimenting particles in turbulent flows