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引用次数: 0
摘要
我们考虑的是\(\mathbb{Z}^{2}\)上的第一通道渗流,其权重是独立且同分布的,其共同分布是绝对连续的,具有有限的指数矩。在极限形状有超过 32 个极值点的假设下,我们证明了起点和终点相近的大地线具有显著的重叠性,除了端点附近的一小部分外,其他部分都会聚合在一起。该声明是量化的,相关量与测地线长度呈幂律关系。最后,与 1965 年的哈默斯利-韦尔什高速公路和支路问题相关,我们证明了从原点开始的无限大地线所覆盖的正方形{-n,. ...,n}2 的预期分数最多是 n 的反幂。这一结果的得出无需明确的极限形状假设。
Coalescence of Geodesics and the BKS Midpoint Problem in Planar First-Passage Percolation
We consider first-passage percolation on \(\mathbb{Z}^{2}\) with independent and identically distributed weights whose common distribution is absolutely continuous with a finite exponential moment. Under the assumption that the limit shape has more than 32 extreme points, we prove that geodesics with nearby starting and ending points have significant overlap, coalescing on all but small portions near their endpoints. The statement is quantified, with power-law dependence of the involved quantities on the length of the geodesics.
The result leads to a quantitative resolution of the Benjamini–Kalai–Schramm midpoint problem. It is shown that the probability that the geodesic between two given points passes through a given edge is smaller than a power of the distance between the points and the edge.
We further prove that the limit shape assumption is satisfied for a specific family of distributions.
Lastly, related to the 1965 Hammersley–Welsh highways and byways problem, we prove that the expected fraction of the square {−n,…,n}2 which is covered by infinite geodesics starting at the origin is at most an inverse power of n. This result is obtained without explicit limit shape assumptions.
期刊介绍:
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