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These equivalence properties indicate that, to make day-to-day flows evolve to equilibrium flows, it is not necessary for travelers to choose their routes based on actual travel costs of the previous day.
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On the other hand, macroscopic gravity-driven motion of landslides and debris flows evolves over a characteristic time scale (L/g)1/2, where g is the magnitude of gravitational acceleration and L is the characteristic length of the moving mass.
Renewed interest in speciation mechanisms has revealed that divergent natural selection can be a powerful promoter of mating isolation, such that stronger pre-zygotic barriers to gene flow evolve between populations from more divergent environments, i.e. "ecological speciation" [1], [2].
The flow evolves from Newtonian to non-Newtonian behavior with increasing pressure gradient.
As the flow evolved, widened and thickened, laminar flow conditions prevailed.
Results are obtained for a Rayleigh-Taylor flow evolving by the action of gravity on a finite temperature gradient.
With further increase of G s (such as G s > 350.0 kg m−2 s−1), the gas-particle flow evolved into dense conveying flow.
Results show that for Re≤100 the flow is segregated with poor mixing; for Re≥150 the flow evolves to an oscillation regime with strong mixing.
It is possible that the sediment-gravity flow evolved, due to a decrease in flow density, into simple settling from suspension, or that the unit represents two (or more) events (or pulses).
The governing equations for a single phase flow evolves from a combination of fundamental concepts i.e., the conversation of mass, conservation of momentum and an equation of state for the porous medium when considered as a control volume.
The flow patterns of the no-control case exhibit an open-top, single-ring vortex sitting on the blockage disc with a jetlike swirling flow evolving from the central disc face toward the downstream area.
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CEO of Professional Science Editing for Scientists @ prosciediting.com