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The calculations of physicists are fundamental, but they will be useful for metallurgists.
Photo Credit: Rodion Narudinov
Scientific Frontline: Extended "At a Glance" Summary
The Core Concept: A physical model demonstrating that snowflakes (ice dendrites) formed under terrestrial conditions possess complex, non-smooth, and asymmetrical shapes, refuting the popular notion of perfect geometric symmetry.
Key Distinction/Mechanism: Unlike the idealized growth observed in microgravity where crystals form symmetrically in a stationary environment, terrestrial snowflake formation is heavily influenced by gravity and convection (heat transfer). These external forces disrupt the stationary environment, causing the crystal to grow imperfectly and unevenly.
Origin/History: Published by physicists at Ural Federal University (UrFU) in the journal Acta Materialia on February 12, 2026, following a comprehensive analysis of experimental data on ice crystal growth accumulated over several decades.
Major Frameworks/Components:
- Convection & Gravity: The primary environmental variables identified as the cause of asymmetry in terrestrial crystal growth.
- Supercooling Dynamics: The relationship between water supercooling and the growth speed/curvature radius of dendrite tips.
- Microgravity Comparison: The use of space-based experimental data to contrast "ideal" stationary growth with "real-world" terrestrial growth.
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