Geodetic Roman Dominating Functions in a Graph

Rona Jane Gamayot Fortosa, Sergio Canoy
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引用次数: 0

Abstract

Let $G$ be a connected graph. A function $f: V(G)\rightarrow \{0,1,2\}$ is a \textit{geodetic Roman dominating function} (or GRDF) if every vertex $u$ for which $f(u)=0$ is adjacent to at least one vertex $v$ for which $f(v)=2$ and $V_1 \cup V_2$ is a geodetic set in $G$. The weight of a geodetic Roman dominating function $f$, denoted by $\omega_{G}^{gR}(f)$, is given by $\omega_{G}^{gR}(f)=\sum_{v \in V(G)}f(v)$. The minimum weight of a GRDF on $G$, denoted by $\gamma_{gR}(G)$, is called the \textit{geodetic Roman domination number} of $G$. In this paper, we give some properties of geodetic Roman domination and determine the geodetic Roman domination number of some graphs.
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图中的测地罗马支配函数
让 $G$ 做一个连通图。函数 $f: V(G)\rightarrow \{0,1,2\}$ 是? \textit{罗马大地测量的支配作用} (或GRDF),如果每个顶点 $u$ 为了什么? $f(u)=0$ 至少与一个顶点相邻 $v$ 为了什么? $f(v)=2$ 和 $V_1 \cup V_2$ 大地测量仪设置好了吗 $G$. 罗马大地测量法的主导功能的重量 $f$,表示为 $\omega_{G}^{gR}(f)$,由 $\omega_{G}^{gR}(f)=\sum_{v \in V(G)}f(v)$. GRDF的最小重量 $G$,表示为 $\gamma_{gR}(G)$,叫做 \textit{大地测量罗马统治数} 的 $G$. 本文给出了测地罗马支配的一些性质,并确定了一些图的测地罗马支配数。
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CiteScore
1.30
自引率
28.60%
发文量
156
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