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Scaling, self-similarity, and intermediate asymptotics / Grigory Isaakovich Barenblatt.

By: Material type: TextTextLanguage: English Original language: Russian Series: Cambridge texts in applied mathematics ; 14.Publisher: Cambridge : Cambridge University Press, 1996Description: 1 online resource (xv, 386 pages) : digital, PDF file(s)Content type:
  • text
Media type:
  • computer
Carrier type:
  • online resource
ISBN:
  • 9781107050242 (ebook)
Other title:
  • Scaling, Self-similarity, & Intermediate Asymptotics
Uniform titles:
  • Podobie, avtomodel'nost', promezhutochnai︠a︡ asimptotika. English
Subject(s): Additional physical formats: Print version: : No titleDDC classification:
  • 530.1/5 20
LOC classification:
  • QA401 .B3713 1996
Online resources: Summary: Scaling laws reveal the fundamental property of phenomena, namely self-similarity - repeating in time and/or space - which substantially simplifies the mathematical modelling of the phenomena themselves. This book begins from a non-traditional exposition of dimensional analysis, physical similarity theory, and general theory of scaling phenomena, using classical examples to demonstrate that the onset of scaling is not until the influence of initial and/or boundary conditions has disappeared but when the system is still far from equilibrium. Numerous examples from a diverse range of fields, including theoretical biology, fracture mechanics, atmospheric and oceanic phenomena, and flame propagation, are presented for which the ideas of scaling, intermediate asymptotics, self-similarity, and renormalisation were of decisive value in modelling.
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Title from publisher's bibliographic system (viewed on 05 Oct 2015).

Scaling laws reveal the fundamental property of phenomena, namely self-similarity - repeating in time and/or space - which substantially simplifies the mathematical modelling of the phenomena themselves. This book begins from a non-traditional exposition of dimensional analysis, physical similarity theory, and general theory of scaling phenomena, using classical examples to demonstrate that the onset of scaling is not until the influence of initial and/or boundary conditions has disappeared but when the system is still far from equilibrium. Numerous examples from a diverse range of fields, including theoretical biology, fracture mechanics, atmospheric and oceanic phenomena, and flame propagation, are presented for which the ideas of scaling, intermediate asymptotics, self-similarity, and renormalisation were of decisive value in modelling.

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