Japan Geoscience Union Meeting 2022

Presentation information

[J] Oral

S (Solid Earth Sciences ) » S-CG Complex & General

[S-CG49] Rheology, fracture and friction in Earth and planetary sciences

Wed. May 25, 2022 3:30 PM - 5:00 PM 304 (International Conference Hall, Makuhari Messe)

convener:Shintaro Azuma(Department of Earth and Planetary Sciences, School of Science, Tokyo Institute of Technology), convener:Miki Tasaka(Shizuoka University), Ichiko Shimizu(Division of Earth and Planetary Sciences, Graduate School of Science, Kyoto University), convener:Osamu Kuwano(Japan Agency for Marine-Earth Science and Technology), Chairperson:Miki Tasaka(Shizuoka University)

3:30 PM - 3:45 PM

[SCG49-01] Transition properties in dynamical and statistical features of shrinkage-induced crack patterns

*Shin-ichi Ito1, Akio Nakahara3, Satoshi Yukawa2 (1.The University of Tokyo, 2.Osaka University, 3.Nihon University)

Keywords:Surface crack patterns, Shrinkage-induced cracks, Statistical properties

We investigate dynamical and statistical properties of shrinkage-induced crack patterns, which are observed such as on the surfaces of cooling lava and drying soil. Since the surface crack patterns evolve slowly in accordance with shrinkage, the statistical properties of the patterns, for example, fragment size distributions are also time-dependent. Understanding such time-dependency of the statistical properties is an important task to estimate the environment history the materials experienced from the current patterns. In this study, we investigated experimentally and theoretically time-dependent properties of fragment size distributions on surface crack patterns of a thin layer of drying dense colloidal suspension.
As a result, we found that the time series of fragment size distributions converged with a single master curve by scaling the fragment sizes with its average, i.e., the statistics had a dynamical scaling law. Although this has been already predicted in numerical simulations by previous studies, the confirmation in real experiments is the first time. To understand the scaling law, we constructed a statistical model of the fragmentation process and succeeded in reproducing the scaling law. In addition, a detailed analysis of the model predicts that there is a transition in the classes of functional forms of the fragment size distributions. To verify the existence of this transition, we applied a Bayesian model selection analysis to the time series of the fragment size data and confirmed the existence of the transition. This result says that investigating the functional form of the fragment size distribution in the current patterns provides the information of shrinkage history the material experienced.