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Titlebook: Introduction to Perturbation Methods; Mark H. Holmes Textbook 2013Latest edition Springer Science+Business Media New York 2013 Asymptotic

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Textbook 2013Latest editionp-to-date research and are drawn from a wide range of application areas..One hundred new pages added including new material on  transcedentally small terms, Kummer‘s function, weakly coupled oscillators and wave interactions..
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Textbook 2013Latest editiontics, engineering sciences, and physics. Each chapter begins with an introductory development involving ordinary differential equations, and goes on to cover such traditional topics as boundary layers and multiple scales. However, it also contains material arising from current research interest, inc
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The Method of Homogenization, not consider them as composites of discrete interacting molecules. Instead, one uses a continuum approximation that assumes the material to be continuously distributed. Using this approximation, material parameters, such as the mass density, are assumed to represent an average.
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Introduction to Bifurcation and Stability,-state bifurcation uses only regular expansions (Chap. .), and the stability arguments will use regular and multiple-scale expansions (Chap. .). On certain examples, such as when studying relaxation dynamics, we will use matched asymptotic expansions (Chap. .).
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0939-2475 duate text is based on a graduate course the author has taught repeatedly over the last ten years to students in applied mathematics, engineering sciences, and physics. Each chapter begins with an introductory development involving ordinary differential equations, and goes on to cover such tradition
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Multiple Scales,ce of this is that what may start out as an ordinary differential equation is transformed into a partial differential equation. Exactly why this helps to solve the problem, rather than make it harder, will be discussed as the method is developed in this chapter.
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The WKB and Related Methods, expectation since many of the problems we studied in Chap. . ended up having an exponential dependence on the boundary-layer coordinate. Also, with this assumption, the work necessary to find an asymptotic approximation of the solution can be reduced significantly.
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