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Overfull graph
In graph theory, an overfull graph is a graph whose size is greater than the product of its maximum degree and half of its order floored, i.e. |E| \Delta (G) \lfloor |V|/2 \rfloor where |E| is the size of G, \displaystyle\Delta(G) is the maximum degree of G, and |V| is the order of G. The concept of an overfull subgraph, an overfull graph that is a subgraph, immediately follows. An alternate, stricter definition of an overfull subgraph S of a graph G requires \displaystyle\Delta (G) = \Delta (S).
Examples
Every odd cycle graph of length three or more is overfull. The product of its degree (two) and half its length (rounded down) is one less than the number of edges in the cycle. More generally, every regular graph with an odd number n of vertices is overfull, because its number of edges, \Delta n/2 (where \Delta is its degree), is larger than \Delta\lfloor n/2\rfloor.
Properties
A few properties of overfull graphs:
- Overfull graphs are of odd order.
- Overfull graphs are class 2. That is, they require at least Δ + 1 colors in any edge coloring.
- A graph G, with an overfull subgraph S such that \displaystyle\Delta (G) = \Delta (S), is of class 2.
Overfull conjecture
In 1986, Amanda Chetwynd and Anthony Hilton posited the following conjecture that is now known as the overfull conjecture.{{citation
:A graph G with \Delta (G) n/3 is class 2 if and only if it has an overfull subgraph S such that \displaystyle \Delta (G) = \Delta (S).
This conjecture, if true, would have numerous implications in graph theory, including the 1-factorization conjecture.{{citation
Algorithms
For graphs in which \Delta \ge n/3, there are at most three induced overfull subgraphs, and it is possible to find an overfull subgraph in polynomial time. When \Delta \ge n/2, there is at most one induced overfull subgraph, and it is possible to find it in linear time.{{citation
References
This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.
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