Windable Quasi-Geodesic Paths on Surfaces of Revolution.
Abstract
If r is the profile or radius function for a surface of revolution and ro is the polar radius function, a quasi-geodesic path on the surface can be defined by the generalized Clairaut relation rSin(w)=ro, where w is the meridional angle. An inequality involving r,r',rn,ro,and ro', is derived. The global satisfaction of this inequality guarantees the windability of the path on a convex (rn<0) surface by a filament winding machine. If the surface is concave anywhere (rn>0) and a more well known clinging inequality is also satisfied, windability is also guaranteed. By windable, we mean that the winding data produced from the path represents a single-valued function and that the wound filament does not bridge. In addition to this new windability criterion, simplified methods for generating quasi-geodesic paths and properly scaled winding data are also presented. (AN)
Document Details
- Document Type
- Technical Report
- Publication Date
- Feb 01, 1995
- Accession Number
- ADA294025
Entities
People
- Royce W. Soanes
Organizations
- United States Army Armament Research, Development and Engineering Center