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Gradually-Varied Flow Profiles in Open Channels: Analytical Solutions by Using Gaussian Hypergeometric Function (2014)

Gradually-varied Flow Profiles in Open Channels

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"Gradually-varied Flow Profiles in Open Channels" by Chyan-Deng Jan is a physics book focused on Dynamics. Best for students, educators, and scientifically curious readers.

This book shows how to solve GVF profiles using direct integration and Gaussian hypergeometric function. Lays groundwork for computing at one sweep the GVF profiles in a series of sustaining and adverse channels, which may have horizontal slopes between them.

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Best For: Students and professionals studying fluid mechanics and open channel hydraulics.
Focus: Analytical methods for solving gradually-varied flow profiles using Gaussian hypergeometric functions.
Covers: Direct integration techniques and computation of flow profiles in channels with varying slopes.
Why It Matters: Provides a mathematical foundation for efficiently computing flow profiles in complex channel conditions, aiding in hydraulic analysis and design.

"Gradually-varied Flow Profiles in Open Channels" by Chyan-Deng Jan is a physics book focused on Dynamics. Best for students, educators, and scientifically curious readers.

Topic: Dynamics

Author: Chyan-Deng Jan

Who this is for:

  • Physics students
  • Science-minded readers
  • Readers building technical understanding

Why this book matters: It provides structured coverage of physics concepts in a way that supports deeper understanding and continued study.

This book shows how to solve GVF profiles using direct integration and Gaussian hypergeometric function. Lays groundwork for computing at one sweep the GVF profiles in a series of sustaining and adverse channels, which may have horizontal slopes between them.

AuthorChyan-Deng Jan
PublisherSpringer
Published2014-02-07
ISBN-139783642352416
BindingHardcover
LanguageEnglish
SubjectsScience
TopicDynamics
SeriesAdvances in Geophysical and Environmental Mechanics and Math

Format: Hardcover

Language: English

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