Sum-difference exponents for boundedly many slopes, and rational complexity
Terence Tao
TL;DR
The paper investigates how the sum-difference exponent ${\operatorname{SD}}(R;s)$, which governs entropy-based bounds on projections and underpins Kakeya-type dimension estimates, behaves when the slope set $R$ is fixed and the target slope $s$ varies. It introduces rational complexity $D(R;s)$ to quantify how efficiently $s$ can be expressed in terms of $R$, and proves that ${\operatorname{SD}}(R;s)$ approaches 2 with a rate controlled by $D(R;s)$ (and related quantities) via a detailed entropic framework. The core contribution is a reduction to an independent-case setting, accomplished through a sequence of steps that produce good configurations, invertible projections, and controlled doubling, culminating in a bound involving the function $f(R;s)$. The results yield precise asymptotics in the single-slope case and general bounds for arbitrary finite $R$, and they illuminate a continuous-limit regime where $s$ approaches a real parameter $\alpha$, characterized by a variational constant $c_\alpha$. This work thus links rational-expression complexity to entropy-based sumset estimates and Kakeya-type dimension bounds, providing a structured path to tighten the arithmetic Kakeya conjecture in the regime of bounded slopes.
Abstract
The dimension of Kakeya sets can be bounded using sum-difference exponents $\SD(R;s)$ for various sets of rational slopes $R$ and output slope $s$; the arithmetic Kakeya conjecture, which implies the Kakeya conjecture in all dimensions, asserts that the infimum of such exponents is $1$. The best upper bound on this infimum currently is $1.67513\dots$. In this note, inspired by numerical explorations from the tool \texttt{AlphaEvolve}, we study the regime where the cardinality of the set of slopes $R$ is bounded. In this regime, we establish that these exponents converge to $2$ at a rate controlled by the \emph{rational complexity} of $s$ relative to $R$, which measures how efficiently $s$ can be expressed as a rational combination of slopes in $R$.
