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.

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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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