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Surfaces of positive curvature whose characteristic lines constitute two families of geodesic parallels - MaRDI portal

Surfaces of positive curvature whose characteristic lines constitute two families of geodesic parallels (Q1201925)

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scientific article; zbMATH DE number 98735
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English
Surfaces of positive curvature whose characteristic lines constitute two families of geodesic parallels
scientific article; zbMATH DE number 98735

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    Surfaces of positive curvature whose characteristic lines constitute two families of geodesic parallels (English)
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    17 January 1993
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    Upon a surface of positive curvature there is a unique conjugate system for which the angle between the directions at any point is the minimum angle between conjugate directions at the point; it is the only conjugate system whose directions are symmetric with respect to the directions of the lines of curvature. In this paper the authors prove: Theorem 1. Surfaces of positive curvature in \(E_ 3\) on which the five families of characteristic lines are geodesic parallels are isometric with rotation surfaces. Theorem 2. A necessary condition for the characteristic lines of a surface \(S\) of positive curvature to be geodesic parallels is that its lines of curvature form an isothermal-conjugate net or, equivalently, its characteristic lines and the lines of curvature form a hexagonal 4- web.
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    surfaces of positive curvature
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    rotation surfaces
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    isothermal-conjugate net
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    hexagonal four-web
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