Topological phase transition in the Scheidegger model of river networks

被引:0
|
作者
Oppenheim, Jacob N. [1 ]
Magnasco, Marcelo O. [1 ]
机构
[1] Rockefeller Univ, Phys Math Lab, New York, NY 10065 USA
来源
PHYSICAL REVIEW E | 2012年 / 86卷 / 02期
基金
美国国家科学基金会;
关键词
SCALING LAWS; PRINCIPLE; STABILITY; MASS;
D O I
10.1103/PhysRevE.86.021134
中图分类号
O35 [流体力学]; O53 [等离子体物理学];
学科分类号
070204 ; 080103 ; 080704 ;
摘要
Transport networks are found at the heart of myriad natural systems, yet are poorly understood, except for the case of river networks. The Scheidegger model, in which rivers are convergent random walks, has been studied only in the case of flat topography, ignoring the variety of curved geometries found in nature. Embedding this model on a cone, we find a convergent and a divergent phase, corresponding to few, long basins and many, short basins, respectively, separated by a singularity, indicating a phase transition. Quantifying basin shape using Hacks law l similar to a(h) gives distinct values for h, providing a method of testing our hypotheses. The generality of our model suggests implications for vascular morphology, in particular, differing number and shapes of arterial and venous trees.
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页数:5
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