Relationship between turbulence and freezing?

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Discussion Overview

The discussion revolves around the relationship between turbulence in water flow and the freezing point of water, particularly in the context of pumping water through aluminum pipes in cold ambient temperatures. Participants explore the effects of turbulence, environmental conditions, and the physical properties of water on freezing.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested

Main Points Raised

  • One participant queries the necessary water flow rate in a 10" aluminum pipe to prevent freezing under varying ambient temperatures.
  • Another participant emphasizes that the freezing point is critical, noting that even a small amount of heat loss can lead to freezing, especially in uninsulated pipes.
  • A different participant argues that moving water can freeze, citing personal experience in Michigan where water freezes below 0°C regardless of movement.
  • One participant suggests that turbulence may affect the freezing point, referencing observations of fast-moving streams and ocean water being harder to freeze.
  • Another participant counters that turbulence has no effect on freezing, explaining that mixing in large bodies of water can maintain a liquid state while surface layers may freeze.
  • There is a discussion about the temperature of arctic ocean water, with participants noting that surface temperatures can be below freezing due to salinity effects.
  • One participant clarifies that colder waters rise to the surface in polar regions, remaining liquid until reaching the freezing point, which varies with salinity.

Areas of Agreement / Disagreement

Participants express differing views on the impact of turbulence on freezing, with some asserting it has no effect while others propose that it may play a role. The discussion remains unresolved regarding the influence of turbulence and the specific conditions under which water freezes.

Contextual Notes

Participants highlight various environmental factors, such as wind and insulation, that may influence freezing, but these factors are not fully explored or quantified in the discussion.

johnnykatz
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How fast do i need to pump water in a 10" aluminum pipe to prevent freezing? Assume 32*F inlet temp and 0*F ambient . For my conditions, the temps will vary and T ambient easily gets down to -20*F or more.
 
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The conditions you gave are just at singularity: 32F is a freezing point, so even smallest amount of heat lost to environment causes freezing.

But even if you ask about inlet water at +1C - the situation still depends on environmental conditions (esp. wind, but also if your pipe gets covered by frost).

Practical answer is: never use uninsulated aluminum pipes to pump cold water if ambient temperature is likely to drop much below 0C :frown:
 
johnnykatz said:
How fast do i need to pump water in a 10" aluminum pipe to prevent freezing? Assume 32*F inlet temp and 0*F ambient . For my conditions, the temps will vary and T ambient easily gets down to -20*F or more.

Why do you think that moving water does not freeze. As a native of Michigan, I can tell you that it freezes quite readily whenever temperature drop below 0°C and icing nuclei are present--moving or not moving.
 
I understand the practical answer and the additional heat loss concepts.
My question aims at how the nature of turbulence affects the freezing point. From my observations, it is much harder to freeze turbulent water (fast moving streams in sub zero temps, ocean water, etc)
Couldn't the concept of supercooling apply here?
 
Last edited:
Turbulence has no effect at all.

Effect on fast rivers and ocean is only such, that if they mix, they just drop some temperature in the whole volume, which is large enough to keep them liquid, while still rivers freeze on their surfaces, while close to bottom the water remain at +3C or so.

But even dramatically turbulent water (like waterfalls) freeze - you may see that in northern mountain regions.
 
xts said:
Turbulence has no effect at all.

Effect on fast rivers and ocean is only such, that if they mix, they just drop some temperature in the whole volume, which is large enough to keep them liquid, while still rivers freeze on their surfaces, while close to bottom the water remain at +3C or so.

But even dramatically turbulent water (like waterfalls) freeze - you may see that in northern mountain regions.

Are you saying that arctic ocean water is warmer than 0C?
 
johnnykatz said:
Are you saying that arctic ocean water is warmer than 0C?
Its surface temperature is usually about -2C (but it is still a bit above freezing point of salted water), while at some depth it is about +4C
 
Last edited:
xts said:
Its surface temperature is usually about -2C (but it is still a bit above freezing point of salted water), while at some depth it is about +4C

Yes. Water density decreases as temperatures decrease below 3.9°C, so that the colder waters rise to the surface. There, depending upon salinity, they remain liquid until the freezing point is reached.

Since these waters never get much colder than -2°C, they are the warmest environments around in the polar areas. That is why the vast majority of polar life forms are either marine or aquatic.
 

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