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Updated: Apr 3, 2026

A Microfluidic Approach for the Study of Ice and Clathrate Hydrate Crystallization
Published on: August 18, 2022
Abrupt eruptive instability of ice adhered to solid surfaces
Lei Wang1,2, Kai Wu3, Huijie Zhang1,4
1Beijing National Laboratory for Molecular Science, Key Laboratory of Green Printing, Institute of Chemistry, Chinese Academy of Sciences, Beijing 100190, P. R. China.
Sudden ice fracture events, like frost quakes, are now explained by a new eruptive fracture model. This discovery reveals ice
Area of Science:
- Cryospheric science
- Materials science
- Geophysics
Background:
- Violent ice fracture events can cause significant climatic and geomorphic changes.
- Current models fail to explain the explosive nature of natural ice fracture events.
Purpose of the Study:
- To uncover the mechanism behind explosive ice fracture.
- To investigate the role of internal grain size in ice fracture behavior.
- To determine the tensile strength of adhered ice.
Main Methods:
- Investigated ice fracture on solid surfaces under quasistatic cooling.
- Analyzed the dependence of fracture mode on internal grain size.
- Measured the apparent tensile strength of adhered ice.
Main Results:
- Identified a novel eruptive fracture mechanism in adhered ice.
- Fracture mode transitions from progressive to abrupt based on grain size.
- Adhered ice exhibits significantly higher tensile strength (39-58 MPa) than typical ice (0.7-3.1 MPa).
Conclusions:
- The study provides a mechanistic framework for predicting abrupt cryospheric fracture.
- Findings can inform the design of self-actuating deicing systems exploiting thermomechanical instabilities.
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