Equation 677 Database

Magma af70b7bb8ac9…

magma af70b7bb8ac9
Size
121
Isomorphism class hash
af70b7bb8ac907715809a347d0dfe8ad9ff48f6a7cd60bc12915c37a36e82d89
Satisfies Equation 255
yes
Right-cancellative
yes
Idempotent
yes
Submitted by
b-reinke
Submitted at
2026-05-17 12:42:11
Display reorder
0,2,89,50,80,14,49,25,98,20,32,1,116,86,72,78,83,103,7,90,36,27,58,37,99,41,54,19,18,34,6,33,39,17,64,13,108,16,38,111,10,79,101,43,57,85,60,22,112,77,106,44,75,73,51,68,31,97,84,61,11,5,82,66,110,40,119,91,42,59,88,92,109,26,70,56,30,94,8,107,24,118,12,105,114,52,115,93,74,69,81,62,35,47,102,117,15,53,28,45,71,4,65,48,46,113,95,23,100,3,104,87,21,96,63,29,9,67,120,76,55 history
Raw table
canonical order · displayed order
Equational Theories
Finite Magma Explorer

Commentary

Size-121 RC idempotent magma on F_121 = F_11² with NO size-11 sub-magmas — an "order-8 multiplier" construction outside the standard Phi_10 family. Size 121, fully idempotent, right-cancellative. Sub-magma count by size: only 0 (singletons) and 121 (the whole magma). Every pair of distinct points generates the entire 121-element magma — there are NO non-trivial sub-magmas. L_0 and R_0 each have cycle structure **1 + 15·8** — the multiplier in the F_121 linear operation has order **8**, not 10. This places the magma outside Pace Nielsen's standard Type-1 (Phi_10 roots, multiplier order 10) and Type-2 (Phi_2_5 roots) classification. Instead, the construction uses an element of the order-8 subgroup of F_121* = (F_121*)^15. The additive structure is F_11² (= F_121 additively). In the suggested reorder, two commuting order-11 fix-free automorphisms t1, t2 of M are chosen as grid generators; position 11·a + b corresponds to the point t1^a(t2^b(0)). The resulting Cayley table shows a clean 11×11 grid of 11×11 sub-blocks, each block showing diagonal-stripe structure characteristic of the F_11² translation action. Family at size 121 sharing this fingerprint (1 + 15·8 cycle): 5 RC idempotent iso classes — magma#70e5572a, magma#873c2695, magma#58669675, magma#fdc7e335. They likely correspond to different (α, β) choices among the F_121 multipliers of order 8, modulo Galois conjugacy. This is one of the "sub-11 = 0" magmas distinct from the F_121 affine line (Phi_10 multiplier, would have sub-11 = 132 if used) and the Zassenhaus near-field (magma#5ebfbb80, multiplier order 30). [text written by Claude]

last edited by dwrensha at 2026-05-18 17:20:08 · history