Heat Transfer in Water: Convection, Expansion & Conduction

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Discussion Overview

The discussion revolves around heat transfer in water, focusing on convection, expansion, and conduction. Participants explore how water behaves at different temperatures, particularly around 0°C and 4°C, and the implications for heat transfer processes in aquatic environments.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested

Main Points Raised

  • Some participants describe convection as a process where denser molecules move down while lighter molecules rise, questioning how heat is transferred in water at 0°C when it contracts and becomes denser.
  • Others argue that molecules do not possess density in isolation, and that the bulk material density changes with temperature, suggesting a macroscopic view of convection may be more beneficial for understanding.
  • A participant notes that water at the bottom must heat past the temperature of maximum density before convection can occur, highlighting the anomalous expansion of water as a critical factor for aquatic life survival in cold conditions.
  • There is a mention of the slow nature of conduction in water, which is contrasted with convection processes.
  • A later reply introduces a contentious remark about evolution and intelligent design, leading to a debate about the implications of such statements.

Areas of Agreement / Disagreement

Participants express differing views on the nature of convection and the role of molecular density, with no consensus reached on the implications of these processes for heat transfer in water. Additionally, the discussion about evolution and intelligent design introduces further disagreement.

Contextual Notes

Some limitations in the discussion include assumptions about molecular behavior and the definitions of density, as well as unresolved questions regarding the mechanisms of heat transfer in water.

Zaya Bell
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Looking back to heat transfer by convection, which means denser molecules move down, lighter molecules move up.
And then water at 4°C expands when cooled further, and at 0°C it contracts when heated. So if water at 0°C in a container is heated from the bottom, its molecules should contract(becomes denser) and should sit well at the bottom but how then is heat transferred to the top?
If we say by conduction, isn't the time to heat such water be much longer since water is a poor conductor of heat.
 
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Zaya Bell said:
denser molecules move down, lighter molecules move up.
Molecules don't have a density. The space between them will change as the temperature changes so the Bulk Material density changes. You are suffering here because of the way the phenomenon is being presented. Modern teaching likes to dive into the microscopic world of Particles as soon as possible. If you just consider Convection as a Macroscopic process then you have a better chance of overall understanding. Of course, particles are involved but they don't always need to be brought into the explanation. Dense Water sinks and less dense Water is displaced and rises to the top.
Zaya Bell said:
So if water at 0°C in a container is heated from the bottom, its molecules should contract(becomes denser) and should sit well at the bottom but how then is heat transferred to the top?
A very good question. The water on the bottom needs to heat up past the temperature of maximum density before convection starts. The anomalous expansion of water is thought to be the reason that aquatic life survives in very cold conditions. The liquid water under ice is cold but still floats on top of the less cold water beneath. That inhibits convection which, otherwise would take heat from the bottom of the pond and it would all freeze much quicker than it does, just by conduction (as you say, a very slow process for a substance like water).
Weren't we lucky? But for this protection of pond life from freezing to death, we might never have evolved into the splendid PF members you see today.
 
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sophiecentaur said:
Molecules don't have a density. The space between them will change as the temperature changes so the Bulk Material density changes. You are suffering here because of the way the phenomenon is being presented. Modern teaching likes to dive into the microscopic world of Particles as soon as possible. If you just consider Convection as a Macroscopic process then you have a better chance of overall understanding. Of course, particles are involved but they don't always need to be brought into the explanation. Dense Water sinks and less dense Water is displaced and rises to the top.

A very good question. The water on the bottom needs to heat up past the temperature of maximum density before convection starts. The anomalous expansion of water is thought to be the reason that aquatic life survives in very cold conditions. The liquid water under ice is cold but still floats on top of the less cold water beneath. That inhibits convection which, otherwise would take heat from the bottom of the pond and it would all freeze much quicker than it does, just by conduction (as you say, a very slow process for a substance like water).
Weren't we lucky? But for this protection of pond life from freezing to death, we might never have evolved into the splendid PF members you see today.
Thanks for your clarification.
 
sophiecentaur said:
Weren't we lucky? But for this protection of pond life from freezing to death, we might never have evolved into the splendid PF members you see today.
You're implying Creationism/intelligent design, aren't you?
Well, I know we never evolved.
 
Last edited:
Zaya Bell said:
You're implying Creationism/intelligent design, aren't you?
Well, I know we never evolved.
You jest? :wink:
 

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