Definition

Let 0<ν10<\nu\le 1 and 0<α0<α10<\alpha_0<\alpha_1. A set XRdX\subseteq\mathbb R^d is ν\nu-porous on balls from scales α0\alpha_0 to α1\alpha_1 if every Euclidean ball BB whose diameter RR satisfies α0<R<α1\alpha_0<R<\alpha_1 contains a point xBx\in B such that

BνR(x)X=.B_{\nu R}(x)\cap X=\varnothing.

Thus every admissible observation ball contains a hole whose radius is a fixed fraction of the observation scale.

Scale dependence

Porosity here is explicitly truncated: nothing is required below α0\alpha_0 or above α1\alpha_1. This is the form used in quantitative , where the smallest scale is tied to a semiclassical parameter.

Relation to other notions

tests every line segment and is stronger in dimensions at least two. In one dimension the two definitions agree up to the harmless convention of using radius or diameter as the scale. Porosity also forces quantitative decay of through the .

References
  1. Alex Cohen, “Fractal uncertainty in higher dimensions,” 2024. arXiv record. Relevant: §§1.2 and A.2.