Computation of Steady Gradually-Varied Flows
Oscar Castro-Orgaz () and
Willi H. Hager ()
Additional contact information
Oscar Castro-Orgaz: University of Córdoba
Willi H. Hager: VAW, ETH Zürich
Chapter 3 in Shallow Water Hydraulics, 2019, pp 137-181 from Springer
Abstract:
Abstract Steady open channel flow is generally non-uniform. In gradually-varied flows, the changes of depth and velocity in space are small, so that streamline curvature effects can be neglected. If the channel bottom slope is small, then the hydrostatic vertical pressure distribution prevails.
Date: 2019
References: Add references at CitEc
Citations:
There are no downloads for this item, see the EconPapers FAQ for hints about obtaining it.
Related works:
This item may be available elsewhere in EconPapers: Search for items with the same title.
Export reference: BibTeX
RIS (EndNote, ProCite, RefMan)
HTML/Text
Persistent link: https://EconPapers.repec.org/RePEc:spr:sprchp:978-3-030-13073-2_3
Ordering information: This item can be ordered from
http://www.springer.com/9783030130732
DOI: 10.1007/978-3-030-13073-2_3
Access Statistics for this chapter
More chapters in Springer Books from Springer
Bibliographic data for series maintained by Sonal Shukla () and Springer Nature Abstracting and Indexing ().