Abstract
Suppose that, under the action of gravity, liquid drains through the unit d-cube via a minimal-length network of channels constrained to pass through random sites and to now with nonnegative component in one of the canonical orthogonal basis directions of R-d, d >= 2. The resulting network is a version of the so-called minimal directed spanning tree. We give laws of large numbers and convergence in distribution results on the large-sample asymptotic behaviour of the total power-weighted edge length of the network on uniform random points in (0, 1)(d). The distributional results exhibit a weight-dependent phase transition between Gaussian and boundary-effect-derived distributions. These boundary contributions are characterized in terms of limits of the so-called on-line nearest-neighbour graph, a natural model of spatial network evolution, for which we also present some new results. Also, we give a convergence in distribution result for the length of the longest edge in the drainage network; when d = 2, the limit is expressed in terms of Dickman-type variables.
| Original language | English |
|---|---|
| Pages (from-to) | 659-688 |
| Number of pages | 30 |
| Journal | Advances in Applied Probability |
| Volume | 42 |
| Issue number | 3 |
| DOIs | |
| Publication status | Published - Sept 2010 |
Keywords
- distributional fixed-point equation
- Dickman distribution
- random spatial graph
- nearest-neighbour graph
- spanning tree
- phase transition
- weak convergence