Algorithms and complexity for geodetic sets on planar and chordal graphs
arXiv:2006.16511 · doi:10.1016/j.tcs.2023.114217
Abstract
A set of vertices of a graph is a \emph{geodetic set} if every vertex of lies in a shortest path between some pair of vertices of . The \textsc{Minimum Geodetic Set (MGS)} problem is to find a geodetic set with minimum cardinality of a given graph. A \emph{grid embedding} of a graph is a set of points in two dimensions with integer coordinates such that each point in the set represents a vertex of the graph and, for each edge, the points corresponding to its endpoints are at Euclidean distance~. A graph is a \emph{partial grid} if it has a grid embedding. In this paper, we first prove that \textsc{Minimum Geodetic Set} remains NP-hard even for subcubic partial grids of arbitrary girth. This jointly strengthens three existing hardness results: for bipartite graphs (Dourado et al., Discrete. Math, 2010), subcubic graphs (Bueno et al., Inf. Process. Lett., 2018)~\cite{bueno2018}, and planar graphs (Chakraborty et al., CALDAM, 2020). The \emph{area} of an internal face is the number of integer points lying on the boundary or interior of the face. A graph is a \emph{solid grid} if it has a grid embedding such that all interior faces have area exactly four. To complement the above hardness result, we design a linear-time algorithm for \textsc{Minimum Geodetic Set} on solid grids, improving on a -approximation algorithm by Chakraborty et al. (CALDAM, 2020). Our results hold for \textsc{Edge Geodetic Set} as well. A set of vertices of a graph is a \emph{geodetic set} if every edge of lies in a shortest path between some pair of vertices of . The \textsc{Minimum Edge Geodetic Set (MEGS)} problem is to find an edge geodetic set with minimum cardinality of a given graph. As corollaries, we obtain that \textsc{MEGS} remains NP-hard on partial grids and is linear-time solvable on solid grids.
This manuscript corresponds to one part of the original ISAAC 2020 conference paper (Algorithms and Complexity for Geodetic Sets on Planar and Chordal Graphs). During journal revision, the conference version was split into two independent journal articles. This arXiv version matches the article published in TCS. The second part will be uploaded separately. The author list has also changed