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Instability of Liquid Surfaces and the Formation of Drops, Vol. 2 (Classic Reprint): A Refined Theory: A Refined Theory (Classic Reprint) - Tapa blanda

Kolodner, Ignace I.

 
9781332090280: Instability of Liquid Surfaces and the Formation of Drops, Vol. 2 (Classic Reprint): A Refined Theory: A Refined Theory (Classic Reprint)

Sinopsis

Explore how thin liquid sheets become unstable and break into filaments or drops. This refined treatment blends theory and calculation to show how small disturbances evolve, slow down or speed up deformation, and shape the final breakup patterns.

This work frames a free boundary problem for a liquid layer, derives the governing equations, and develops a formal method to approximate solutions. It focuses on one- and two-dimensional profiles, analyzes stability, and discusses how thickness, surface tension, and initial disturbances influence the breakup into filaments or drops. The results connect linear instability ideas with nonlinear evolution, offering explicit expressions up to several orders in a small parameter.


  • How instability theory predicts when a sheet will break into filaments and how many filaments may form per wavelength

  • A method to express the evolving sheet profile using Fourier expansion and successive approximations

  • Conditions under which nonlinear effects slow deformation compared to linear predictions

  • Different outcomes for various thickness, surface tension, and disturbance amplitudes



Ideal for readers of advanced fluid dynamics, applied mathematics, and physics who want a rigorous, numbers-driven view of surface instability and drop formation.

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Reseña del editor

Excerpt from Instability of Liquid Surfaces and the Formation of Drops, Vol. 2: A Refined Theory

In an earlier paper [2] we showed how the notion of Taylor instability can be used to explain the break-up of accelerated thin liquid sheets into drops, and how on the basis of this theory the drop sizes can be estimated. The idea underlying the calculation is as follows: One considers a plane layer accelerated in a direction normal to its surface by imposing, e.g., a pressure difference on opposite surfaces. The zero order motion - which incidentally is an exact solution for the plane layer - is a parallel flow with the velocity of bounding surfaces. It is next argued that the flow actually deviates from the zero order solution because either the bounding surfaces are not perfectly plane, or the pressure on the boundary is not exactly constant, or because of some random perturbation that may occur at the outset or during the motion. To see what happens to the bounding surfaces, one considers the first order perturbation which satisfies linear equations and is represented by a series (or integral) of normal modes. Some of these modes are found to be unstable in the sense that their amplitudes grow unrestrictedly with time. Among tries one or more may be called most unstable in the sense that they grow most rapidly. When the acceleration of the layer is constant the unstable modes grow exponentially and the most unstable modes have the largest exponent.

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