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Melting of pure ice in an aqueous binary solution.

Fusion de glace pure dans une solution saline.

Author(s) : GEOFFROY S., MERGUI S., BENARD C., et al.

Summary

Thermohaline convection flows are induced by density gradients due to local variations of temperature and concentration. This type of flow, which appears in many natural processes (melting of ice in oceanography), but also industrial applications (material processing), have a direct influence on heat and mass transfers to liquid-solid interfaces. Thus, the understanding of these interfacial conditions is very important.

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Pages: 188-194

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Details

  • Original title: Fusion de glace pure dans une solution saline.
  • Record ID : 2001-1079
  • Languages: French
  • Source: Permafrost and Actions of Natural or Artificial Cooling
  • Publication date: 1998/10/21
  • Document available for consultation in the library of the IIR headquarters only.

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