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Knowledge Based Cloud FE Simulation of Sheet Metal Forming Processes
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Modelling and simulation of brinicle formation.

Felipe Gómez-Lozada1, Carlos Andrés Del Valle1, Julián David Jiménez-Paz1

  • 1Departamento de Física, Universidad Nacional de Colombia, Carrera 45 No. 26-85, Edificio Uriel Gutiérrez, Bogotá D.C., Colombia.

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Summary

Researchers modeled icy brine flows under Arctic sea ice, forming unique ice stalactites called brinicles. The mathematical model successfully simulated brinicle formation and structure, advancing our understanding of this oceanographic phenomenon.

Keywords:
chemical gardenfinite-element methodmultiphysicsnonlinear dynamicsocean dynamicsphase change

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Area of Science:

  • Oceanography
  • Fluid Dynamics
  • Mathematical Modeling

Background:

  • Brinicles, or ice stalactites, form from supercooled brine flowing beneath Arctic sea ice.
  • This phenomenon involves complex fluid dynamics and heat/salt transport under extreme conditions.

Purpose of the Study:

  • To develop a comprehensive mathematical model for brinicle formation.
  • To simulate the physical processes governing the growth of ice stalactites in the ocean.

Main Methods:

  • Developed a mathematical model with cylindrical symmetry for viscous, quasi-stationary fluid flow.
  • Incorporated coupled heat and salt transport equations, considering diffusive and convective effects.
  • Utilized finite-element discretization to solve the partial differential equations.

Main Results:

  • The model successfully captured the general behavior of brinicle formation.
  • Generated brinicle-like structures and recovered expected dendrite composition.
  • The model aligns with previous experimental findings on ice stalactites.

Conclusions:

  • This study presents the first complete model of the global structure of brinicle formation.
  • The model provides valuable insights into the physics of these unique underwater ice structures.
  • Acknowledged discrepancies, such as brine accumulation, require further investigation.