Equation 677 Database

Magma 70e5572af795…

magma 70e5572af795
Size
121
Isomorphism class hash
70e5572af7954a2ea2993e55013acaa29f420c8b1bbb8322ca4b43c7902939fe
Satisfies Equation 255
yes
Right-cancellative
yes
Idempotent
yes
Submitted by
b-reinke
Submitted at
2026-05-17 12:41:20
Display reorder
0,2,85,75,107,108,67,39,77,16,57,1,44,23,90,43,21,115,103,69,49,98,81,70,28,14,116,33,45,76,117,83,12,47,56,68,59,120,74,53,71,62,65,50,32,95,60,118,31,17,10,55,100,15,102,54,84,30,3,113,86,5,114,19,79,64,96,109,52,38,37,94,104,20,18,72,13,112,7,27,101,40,58,93,63,29,91,41,92,99,97,4,34,66,35,24,46,26,106,61,6,105,51,119,22,78,80,88,36,8,11,48,89,73,110,82,9,25,42,111,87 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#873c2695, magma#58669675, magma#af70b7bb, 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 17:20:07 · history