Heat Transfer in Water: Convection, Expansion & Conduction

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SUMMARY

This discussion centers on the mechanisms of heat transfer in water, specifically focusing on convection, expansion, and conduction. It highlights that water at 4°C expands when cooled and contracts when heated at 0°C, affecting how heat is transferred. The conversation emphasizes that convection occurs when water at the bottom of a container heats past its maximum density, allowing less dense water to rise. This anomalous behavior of water is crucial for aquatic life, as it prevents rapid freezing in cold conditions.

PREREQUISITES
  • Understanding of heat transfer principles, specifically convection and conduction.
  • Knowledge of water's unique thermal properties, including anomalous expansion.
  • Familiarity with molecular behavior in relation to temperature changes.
  • Basic concepts of density and buoyancy in fluids.
NEXT STEPS
  • Research the principles of heat transfer in fluids, focusing on "Convection in Fluids".
  • Study the thermal properties of water, particularly "Anomalous Expansion of Water".
  • Explore the impact of temperature on density and buoyancy in "Fluid Dynamics".
  • Investigate the ecological implications of water's thermal properties for "Aquatic Life Survival".
USEFUL FOR

Students, educators, and researchers in physics, environmental science, and biology who are interested in understanding heat transfer mechanisms and their implications for aquatic ecosystems.

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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