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Geodetic metrizations of graphs

โœ Scribed by Frank Rhodes; Robert A. Melter


Publisher
Elsevier Science
Year
1999
Tongue
English
Weight
665 KB
Volume
194
Category
Article
ISSN
0012-365X

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โœฆ Synopsis


A graph can be metrized by assigning a length to each of its edges. Such a graph is said to be geodetic if for each pair of vertices there is a unique geodesic joining them. It is said to be normally geodetic if each of these unique geodesics is one of the geodesics in the usual metrization of the graph in which each edge is given unit length. It is shown that every graph admits a normally geodetic metrization.

Geodetic metrizations of the four-and eight-connection graphs of the digital plane which can be processed easily on a computer are investigated. Examples are given of normally geodetic integral metrizations of arbitrarily large rectangular blocks of these planes. However, it is proved that there are no normally geodetic metrizations of the whole of these planes which are periodic in each variable. @


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We study the graphs in which the number of geodesics between any two vertices depends only on their distance. We consider also a connection between some of these graphs and geodetic graphs.

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Let G = ( y E) be a graph with vertex set V of size n and edge set E of size m. A vertex LJ E V is called a hinge vertex if the distance of any two vertices becomes longer after u is removed. A graph without hinge vertex is called a hinge-free graph. In general, a graph G is k-geodetically connected

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A graph G is k-geodetically connected (k-GC) if it is connected and the removal of at least k vertices is required to increase the distance between at least one pair of vertices or reduce G to a single vertex. We completely characterize the class of minimum 3-GC graphs that have the fewest edges for