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Why does hot less dense air rise and cold more dense air sink? Also, why is hot air less dense than cold air?
The discussion centers around the phenomenon of why hot air rises and cold air sinks, focusing on the concepts of air density, temperature, and buoyancy. Participants explore theoretical explanations, physical principles, and hypothetical scenarios related to this behavior in gases.
Participants express various viewpoints, and while some explanations align with each other, there is no consensus on the complete understanding of the mechanisms involved. Multiple competing views remain regarding the interactions between temperature, density, and buoyancy.
Some discussions involve assumptions about hydrostatic equilibrium and the effects of temperature mixing, which remain unresolved. The role of viscous forces and pressure gradients in natural convection is also noted but not fully explored.
If the system is not at hydrostatic equilibrium, there are also viscous forces involved, and these need to be taken into account in the momentum balance. With natural convection like this, the pressures are close to being equal, but not quite. The small difference in density results in small differences in vertical pressure gradients between the hot and cold regions, and this gives rise to the buoyant forces. When you get into natural convective heat transfer, all these factors will be taken into account in determining the flow and the heat transfer. For such a detailed analysis, see Bird, Stewart, and Lightfoot, Transport Phenomena.Scheuerf said:But if you had a region of less dense air surrounded by more dense air, why wouldn't the less dense air be filled with air from the more dense area?
As Chestermiller said ... yet in my wording.Scheuerf said:But if you had a region of less dense air surrounded by more dense air, why wouldn't the less dense air be filled with air from the more dense area?