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14. Die Rauheit beweglicher Sedimentsohlen

  • 2019
  • OriginalPaper
  • Chapter
Published in:
Author
Andreas Malcherek
Published in
Fließgewässer
Publisher
Springer Fachmedien Wiesbaden

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Zusammenfassung

Sobald die Sohlschubspannung die kritische Schubspannung des Bewegungsbeginns überschreitet, beginnen die Sedimente an einer Flusssohle Strukturen auszubilden, die man je nach Größe als Riffel oder Dünen bezeichnet.

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previous chapter Die Grenzschichttheorie für Fließgewässer
next chapter Der gegliederte Querschnitt
Title
Die Rauheit beweglicher Sedimentsohlen
Author
Andreas Malcherek
Copyright Year
2019
Book
Fließgewässer

Print ISBN: 978-3-658-26999-9

Electronic ISBN: 978-3-658-27000-1

Copyright Year: 2019

DOI
https://doi.org/10.1007/978-3-658-27000-1_14
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