Geodesic clustering of zeros of Eisenstein series for congruence groups

We consider a set of generators for the space of Eisenstein series of even weight $k$ for any congruence group $Γ$ and study the set of all of their zeros taken for $Γ(1)$-conjugates of $Γ$ in the standard fundamental domain for $Γ(1)$. We describe (a) an upper bound $κ_Γ+ O(1/k)$ for their imaginary part; (b) a finite configuration of geodesics segments to which all zeros converge in Hausdorff distance as $k \rightarrow \infty$; (c) a finite set containing all algebraic zeros for all weights. The bound in (a) depends on the (non-)vanishing of a new generalization of Ramanujan sums. The proof of (b) originates in a method used to study phase transitions in statistical physics. The proof of (c) relies on the theory of complex multiplication. The results can be made quantitative for specific groups. For $Γ=Γ(N)$ with $4 \nmid N$, $κ_Γ=1$ and the zeros tend to the unit circle, whereas if $4 \mid N$, $κ_Γ=2$ and the limit configuration includes parts of vertical geodesics and circles of radius $2$. In both cases, the only algebraic zeros are at $\mathrm{i}$ and $\exp(2π\mathrm{i}/3)$ for sufficiently large $k$. For $Γ(N)$ with $N$ odd, we use finer estimates to prove a trichotomy for the exact `convergence speed' of the zeros to the unit circle, as well as angular equidistribution of the zeros as $k \rightarrow \infty$.

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ArXiv.org
Published
2025-09-19
Primary Topic
Geochemistry and Geologic Mapping
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article
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article

Geodesic clustering of zeros of Eisenstein series for congruence groups

ArXiv.org
Geochemistry and Geologic Mapping
article

Geodesic clustering of zeros of Eisenstein series for congruence groups

article en

Abstract

We consider a set of generators for the space of Eisenstein series of even weight $k$ for any congruence group $Γ$ and study the set of all of their zeros taken for $Γ(1)$-conjugates of $Γ$ in the standard fundamental domain for $Γ(1)$. We describe (a) an upper bound $κ_Γ+ O(1/k)$ for their imaginary part; (b) a finite configuration of geodesics segments to which all zeros converge in Hausdorff distance as $k \rightarrow \infty$; (c) a finite set containing all algebraic zeros for all weights. The bound in (a) depends on the (non-)vanishing of a new generalization of Ramanujan sums. The proof of (b) originates in a method used to study phase transitions in statistical physics. The proof of (c) relies on the theory of complex multiplication. The results can be made quantitative for specific groups. For $Γ=Γ(N)$ with $4 \nmid N$, $κ_Γ=1$ and the zeros tend to the unit circle, whereas if $4 \mid N$, $κ_Γ=2$ and the limit configuration includes parts of vertical geodesics and circles of radius $2$. In both cases, the only algebraic zeros are at $\mathrm{i}$ and $\exp(2π\mathrm{i}/3)$ for sufficiently large $k$. For $Γ(N)$ with $N$ odd, we use finer estimates to prove a trichotomy for the exact `convergence speed' of the zeros to the unit circle, as well as angular equidistribution of the zeros as $k \rightarrow \infty$.

ArXiv.org
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Geochemistry and Geologic Mapping
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