z-logo
open-access-imgOpen Access
Subsystems and Automorphisms of Some Finite Magmas of Order k + k2
Author(s) -
A. V. Litavrin
Publication year - 2020
Publication title -
izvestiya of saratov university mathematics mechanics informatics
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.255
H-Index - 4
eISSN - 2541-9005
pISSN - 1816-9791
DOI - 10.18500/1816-9791-2020-20-4-457-467
Subject(s) - automorphism , order (exchange) , permutation (music) , magma , permutation group , group (periodic table) , mathematics , idempotence , element (criminal law) , pure mathematics , class (philosophy) , set (abstract data type) , finite group , inner automorphism , automorphism group , algebra over a field , computer science , geology , physics , volcano , geochemistry , business , political science , artificial intelligence , law , acoustics , quantum mechanics , programming language , finance
This work is devoted to the study of subsystems of some finite magmas S = (V, ∗) with a generating set of k elements and order k + k2. For k > 1, the magmas S are not semigroups and quasigroups. An element-by-element description of all magmas S subsystems is given. It was found that all the magmas S have subsystems that are semigroups. For k > 1, subsystems that are idempotent nonunit semigroups are explicitly indicated. Previously, a description of an automorphism group was obtained for magmas S. In particular, every symmetric permutation group Sk is isomorphic to the group of all automorphisms of a suitable magma S. In this paper, a general form of automorphism for a wider class of finite magmas of order k + k2 is obtained.

The content you want is available to Zendy users.

Already have an account? Click here to sign in.
Having issues? You can contact us here
Accelerating Research

Address

John Eccles House
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom