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单词 Convection cooling
释义

Convection cooling

中文百科

对流 Convection

(重定向自Convection cooling)
一个火炉的热对流示意图

对流是指流体内部的分子运动,是热传与质传的主要模式之一。热对流(亦称为对流传热)是三种主要热传方式中的其中一种(另外两种分别是热传导与热辐射)

英语百科

Convection 对流

(重定向自Convection cooling)
This figure shows a calculation for thermal convection in the Earth's mantle. Colors closer to red are hot areas and colors closer to blue are cold areas. A hot, less-dense lower boundary layer sends plumes of hot material upwards, and likewise, cold material from the top moves downwards.
A heat sink provides a large surface area for convection to efficiently carry away heat.
Convection cells in a gravity field
Idealised depiction of the global circulation on Earth

Convection is the concerted, collective movement of groups or aggregates of molecules within fluids (e.g., liquids, gases) and rheids, through advection or through diffusion or as a combination of both of them. Convection of mass cannot take place in solids, since neither bulk current flows nor significant diffusion can take place in solids. Diffusion of heat can take place in solids, but that is called heat conduction. Convection can be demonstrated by placing a heat source (e.g. a Bunsen burner) at the side of a glass full of a liquid, and observing the changes in temperature in the glass caused by the warmer ghost fluid moving into cooler areas.

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更新时间:2025/6/18 7:59:05