Rayleigh-Bénard convection

名词 n.
中文释义

英文释义

名词 n.
  1. A type of natural convection, occurring in a planar horizontal layer of fluid heated from below, in which the fluid develops a regular pattern of convection cells known as Bénard cells. countable,uncountable

词形变化

Rayleigh-Bénard convections plural

词源

Named after Henri Bénard and John William Strutt, 3rd Baron Rayleigh.
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