Fine-grained magma-graph representation conjecture for Lie algebras

Let g\mathfrak{g} be a complex finite-dimensional Lie algebra, and let (M,δ)(\mathcal{M},\delta) be an abelian magma such that g\mathfrak{g} is M\mathcal{M}-magma-graded, with the M\mathcal{M}-gradation having the finest granularity. Let Gg(V,E)G_{\mathfrak{g}}(V,E) be the graph associated with this pair by the modified graph-construction algorithm. Fine-grained magma-graph conjecture. The graph faithfully represents the internal structure of g\mathfrak{g}: g\mathfrak{g} is non-solvable if and only if the graph contains a self-contained subgraph induced by a closed directed walk; the derived-series and lower-central-series graph sequences yield the corresponding Lie algebras; ideal-graph-property subsets span ideals; simplicity implies a closed directed walk inducing the whole vertex set; and semisimplicity implies that every vertex lies on a closed directed walk inducing a self-contained subgraph. The source presents this as a stronger version of an earlier conjecture and leaves it open.

References

Primary source

Tim Heib and David Edward Bruschi, “On the structural properties of Lie algebras via associated labeled directed graphs”, arXiv:2601.16161 (2026).

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