On two conjectures about the sum of element orders
Canadian mathematical bulletin, Tome 65 (2022) no. 1, pp. 30-38
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Let G be a finite group and $\psi (G) = \sum _{g \in G} o(g)$, where $o(g)$ denotes the order of $g \in G$. There are many results on the influence of this function on the structure of a finite group G.In this paper, as the main result, we answer a conjecture of Tărnăuceanu. In fact, we prove that if G is a group of order n and $\psi (G)>31\psi (C_n)/77$, where $C_n$ is the cyclic group of order n, then G is supersolvable. Also, we prove that if G is not a supersolvable group of order n and $\psi (G) = 31\psi (C_n)/77$, then $G\cong A_4 \times C_m$, where $(m, 6)=1$.Finally, Herzog et al. in (2018, J. Algebra, 511, 215–226) posed the following conjecture: If $H\leq G$, then $\psi (G) \unicode[stix]{x02A7D} \psi (H) |G:H|^2$. By an example, we show that this conjecture is not satisfied in general.
Mots-clés :
Sum of element orders, supersolvable group, element orders
Azad, Morteza Baniasad; Khosravi, Behrooz. On two conjectures about the sum of element orders. Canadian mathematical bulletin, Tome 65 (2022) no. 1, pp. 30-38. doi: 10.4153/S0008439521000047
@article{10_4153_S0008439521000047,
author = {Azad, Morteza Baniasad and Khosravi, Behrooz},
title = {On two conjectures about the sum of element orders},
journal = {Canadian mathematical bulletin},
pages = {30--38},
year = {2022},
volume = {65},
number = {1},
doi = {10.4153/S0008439521000047},
url = {http://geodesic.mathdoc.fr/articles/10.4153/S0008439521000047/}
}
TY - JOUR AU - Azad, Morteza Baniasad AU - Khosravi, Behrooz TI - On two conjectures about the sum of element orders JO - Canadian mathematical bulletin PY - 2022 SP - 30 EP - 38 VL - 65 IS - 1 UR - http://geodesic.mathdoc.fr/articles/10.4153/S0008439521000047/ DO - 10.4153/S0008439521000047 ID - 10_4153_S0008439521000047 ER -
%0 Journal Article %A Azad, Morteza Baniasad %A Khosravi, Behrooz %T On two conjectures about the sum of element orders %J Canadian mathematical bulletin %D 2022 %P 30-38 %V 65 %N 1 %U http://geodesic.mathdoc.fr/articles/10.4153/S0008439521000047/ %R 10.4153/S0008439521000047 %F 10_4153_S0008439521000047
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