4.8 Article

Sublimation-driven morphogenesis of Zen stones on ice surfaces

出版社

NATL ACAD SCIENCES
DOI: 10.1073/pnas.2109107118

关键词

morphogenesis; sublimation; differential ablation

资金

  1. Fdration de Recherche Marie Andre Ampere at the ENS de Lyon
  2. Laboratoire de Physique at the ENS de Lyon

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This article examines the formation of Zen stones on frozen lakes and the subsequent pedestal shape, providing a physical explanation for the process involving slow surface sublimation due to the shade created by the stone. Laboratory experiments confirm that the stone acts as an umbrella, hindering sublimation and protecting the ice beneath, leading to the pedestal formation. Numerical simulations show that the stone's shape influences the ice foot formation, with the stone's infrared radiation leading to the depression surrounding the pedestal.
In this article, the formation of Zen stones on frozen lakes and the shape of the resulting pedestal are elucidated. Zen stones are natural structures in which a stone, initially resting on an ice surface, ends up balanced atop a narrow ice pedestal. We provide a physical explanation for their formation, sometimes believed to be caused by the melting of the ice. Instead, we show that slow surface sublimation is indeed the physical mechanism responsible for the differential ablation. Far from the stone, the sublimation rate is governed by the diffuse sunlight, while in its vicinity, the shade it creates inhibits the sublimation process. We reproduced the phenomenon in laboratory-scale experiments conducted in a lyophilizer and studied the dynamics of the morphogenesis. In this apparatus, which imposes controlled constant sublimation rate, a variety of model stones consisting of metal disks was used, which allows us to rule out the possible influence of the thermal conduction in the morphogenesis process. Instead, we show that the stone only acts as an umbrella whose shade hinders the sublimation, hence protecting the ice underneath, which leads to the formation of the pedestal. Numerical simulations, in which the local ablation rate of the surface depends solely on the visible portion of the sky, allow us to study the influence of the shape of the stone on the formation of the ice foot. Finally, we show that the far-infrared black-body irradiance of the stone itself leads to the formation of a depression surrounding the pedestal.

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