Topological phase transition in the Scheidegger model of river networks

Jacob N. Oppenheim and Marcelo O. Magnasco
Phys. Rev. E 86, 021134 – Published 29 August 2012

Abstract

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 lah 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.

  • Figure
  • Figure
  • Figure
  • Figure
  • Received 31 May 2012

DOI:https://doi.org/10.1103/PhysRevE.86.021134

©2012 American Physical Society

Authors & Affiliations

Jacob N. Oppenheim* and Marcelo O. Magnasco

  • Laboratory of Mathematical Physics, Rockefeller University, New York, New York 10065, USA

  • *joppenheim@rockefeller.edu

Article Text (Subscription Required)

Click to Expand

References (Subscription Required)

Click to Expand
Issue

Vol. 86, Iss. 2 — August 2012

Reuse & Permissions
Access Options
CHORUS

Article Available via CHORUS

Download Accepted Manuscript
Author publication services for translation and copyediting assistance advertisement

Authorization Required


×
×

Images

×

Sign up to receive regular email alerts from Physical Review E

Log In

Cancel
×

Search


Article Lookup

Paste a citation or DOI

Enter a citation
×