The tropical prime form conjecture

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Let Σ\Sigma be a Riemann surface with period matrix Ω\Omega, and let X,YX,Y be points on a tropical graph obtained as the limit of points xα′,yα′x_{\alpha'},y_{\alpha'} on a family of curves with period matrices Ωα′\Omega_{\alpha'}. Define the tropical prime form by

Etrop(X,Y):=−lim⁡α′→0(α′ln⁡∣E(xα′,yα′∣Ωα′)∣).E^{\mathrm{trop}}(X,Y):=-\lim_{\alpha'\to0}\left(\alpha'\ln\left|E(x_{\alpha'},y_{\alpha'}\mid\Omega_{\alpha'})\right|\right).

Tropical prime form conjecture. At any loop order, the tropical prime form equals the scalar ss of Dai, namely the graph distance dγ(X,Y)d_\gamma(X,Y) between XX and YY along a path γ\gamma:

Etrop(X,Y)=dγ(X,Y).E^{\mathrm{trop}}(X,Y)=d_\gamma(X,Y).

This identifies the tropical limit of the string-theoretic prime form with the graph-theoretic distance entering tropical amplitudes. The source presents the statement as conjectural, and no resolution is supplied here.

References

Primary source

Piotr Tourkine, “Tropical Amplitudes”, arXiv:1309.3551 (2017).

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