A Cusp-Like Free-Surface Flow due to a Submerged Source or Sink.
Abstract
We consider the steady flow induced by a line source placed at a given depth beneath the undisturbed level of a free-surface. We assume that the flow bifurcates at a definite point somewhere between the source and the undisturbed free-surface level. The free-surface at this point is cusp-like, the tip of the cusp pointing toward the source. The model is motivated by hydraulic problems of water entry or extraction from a reservoir. The problem is solved numerically by collocation. A unique solution is obtained whose cusp lies at 74.938% of the depth of the source. (Author)
Document Details
- Document Type
- Technical Report
- Publication Date
- Sep 01, 1982
- Accession Number
- ADA120985
Entities
People
- E. O. Tuck
- J.-m. Vanden-broeck
Organizations
- University of Wisconsin–Madison