Li's slope formula for entropy

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Let (X,L)(X,L) be a polarized variety and let φ∈ENA2(X,L)\varphi\in\mathcal{E}_{\mathrm{NA}}^2(X,L) subordinate to its maximal geodesic ray {ℓφ,t}t∈[0,∞)\{\ell_{\varphi,t}\}_{t\in[0,\infty)}. The entropy slope

lim⁡t→∞t−1∫Xlog⁡MA⁡(ℓφ,t)MA⁡(ℓφ,0)MA⁡(ℓφ,t)\lim_{t\to\infty}t^{-1}\int_X\log\frac{\operatorname{MA}(\ell_{\varphi,t})}{\operatorname{MA}(\ell_{\varphi,0})}\operatorname{MA}(\ell_{\varphi,t})

should equal the non-archimedean entropy

∫XNAAXMA⁡(φ).\int_{X^{\mathrm{NA}}}A_X\operatorname{MA}(\varphi).

This formula would directly identify the ray and non-archimedean Calabi-energy descriptions; the source attributes it to Li and notes it follows from the regularization conjecture, but it remains unproved in the stated generality.

References

Primary source

Eiji Inoue, “Entropies in μ-framework of canonical metrics and K-stability, II – Non-archimedean aspect: non-archimedean μ-entropy and μK-semistability”, arXiv:2202.12168 (2022).

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