Abstract
AbstractWe consider a random field $$\phi ({\textbf{r}})$$
ϕ
(
r
)
in d dimensions which is largely concentrated around small ‘hotspots’, with ‘weights’, $$w_i$$
w
i
. These weights may have a very broad distribution, such that their mean does not exist, or is dominated by unusually large values, thus not being a useful estimate. In such cases, the median $${\overline{W}}$$
W
¯
of the total weight W in a region of size R is an informative characterisation of the weights. We define the function F by $$\ln {\overline{W}}=F(\ln R)$$
ln
W
¯
=
F
(
ln
R
)
. If $$F'(x)>d$$
F
′
(
x
)
>
d
, the distribution of hotspots is dominated by the largest weights. In the case where $$F'(x)-d$$
F
′
(
x
)
-
d
approaches a constant positive value when $$R\rightarrow \infty $$
R
→
∞
, the hotspots distribution has a type of scale-invariance which is different from that of fractal sets, and which we term ultradimensional. The form of the function F(x) is determined for a model of diffusion in a random potential.
Publisher
Springer Science and Business Media LLC
Reference19 articles.
1. Mandelbrot, B.B.: The Fractal Geometry of Nature, 3rd edn. W. H. Freeman and Comp, New York (1983)
2. Falconer, K.: Fractal Geometry-Mathematical Foundations and Applications. Wiley, New York (1990)
3. Scheidegger, A.E.: On the topology of river nets. Water Resour. Res. 3, 103–106 (1967)
4. Huber, G.: Scheidegger’s rivers, Takayasu’s aggregates and continued fractions. Phys. A 170, 463–470 (1991)
5. Kawagoe, K., Huber, G., Pradas, M., Wilkinson, M., Pumir, A., Ben-Naim, E.: Aggregation-fragmentation-diffusion model for trail dynamics. Phys. Rev. E 96, 012142 (2017)