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Many rivers in sub-zero winter temperatures don't freeze (photo). For simplicity let's discuss a (small) water pipe/canal with uniform cross section, inclined by an angle $\theta$.

It seems that:

  • According to the heat equation, $\frac{\partial T}{\partial t} - \alpha \nabla^2 T=0$, the temperature of the water in the canal supposed to change (drop) to meet equilibrium conditions with the environment.
  • According to the incompressible Bernoulli's equation, ${v^2 \over 2}+gz+{p\over\rho}=p_0$, the inclination which causes loss of potential energy causes the flow speed to increase.
  • According to the expression for adiabatic stagnation temperature, $T_0 = T + \frac{v^2}{2C_p}$, the reduction of the stagnation temperature (due to heat loss), will cause the flow velocity to decrease.

So:

  1. What would eventually happen to the running water in the canal?
  2. Is the inclination the only thing that prevents the water from freezing?
  3. Is there a known threshold for flow speed as a function of environment temperature ratio to prevent freezing?
  4. What's the velocity profile in the canal?
  5. Is flow speed the only reason some rivers don't freeze?
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    $\begingroup$ This is interesting, but it's usually best to have one specific question per post. Can you perhaps pare this down and make additional posts for the extra questions? This may not be appropriate, but it usually is. $\endgroup$
    – DanielSank
    Commented Feb 11, 2015 at 19:41
  • $\begingroup$ @DanielSank, the "sub-questions" I listed are meant to describe the main questions -- they are not separate questions but rather different aspects of the same thing, and I believe it would be more beneficial for everyone to have it all "under one roof" in this case. $\endgroup$
    – Sparkler
    Commented Feb 11, 2015 at 20:24
  • $\begingroup$ Ok, makes sense. Perhaps that could be made clearer in the question. $\endgroup$
    – DanielSank
    Commented Feb 11, 2015 at 21:43
  • $\begingroup$ Just to get things started: I don't think that Bernoulli's eqn. is particularly applicable. Rivers are highly lossy (lots of friction and turbulence) so an assumption of inviscid flow seems very questionable.You probably want to use a constant velocity and assume that the potential energy from going down hill goes directly to viscous dissipation. Also, the concept that you've drawn from the heat equation is correct, but the eqn. itself is inadequate for flowing media (needs advection). $\endgroup$ Commented Feb 11, 2015 at 23:47

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It should be noted that the Water freezes on surface, cause the density of the Water is highest at 4 degrees, which makes the 0-degree water to float on the top.

1. What would eventually happen to the running water in the canal?

Typically the running water simply is mixed, which means that the whole water mass must be cooled (and even the earth below it) to zero before it starts to freeze. And if this happens, then the river starts to freezes from bottom or where ever it simply founds a point to build chrystals.

The term is "Frazil ice".

2. Is the inclination the only thing that prevents the water from freezing? No. If the water doesn't find points to build chrystal, it just becomes supercooled. You can actually cool a still distilled water down to - 48 Celcius and still have it liquid.

3. Is there a known threshold for flow speed as a function of environment temperature ratio to prevent freezing?

Froude number is also here practical; FR<1 typically doens't freeze, and Fr>1 freezes. The air temperature doesn't make so much of a difference.

4. What's the velocity profile in the canal?

"Typical", I would say. Means the highest velocity is near the surface in the middle of the flow.

5. Is flow speed the only reason some rivers don't freeze? The velocity is not so relevant as Froude Number. Many other aspects are also explained already.

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  • $\begingroup$ if so then why water supercooling is limited to -48C? $\endgroup$
    – Sparkler
    Commented Jun 21, 2015 at 4:38
  • $\begingroup$ Froude number is related to flow speed. $\endgroup$
    – Sparkler
    Commented Jun 21, 2015 at 4:39
  • $\begingroup$ Well, actually I personally think that it is not limited only there.(Supercooling) $\endgroup$
    – Jokela
    Commented Jun 21, 2015 at 7:26
  • $\begingroup$ About Froude number, yes, It is related to velocity, but a small creek with 5 cm waterdepth flows with Fr=1 with a velocity of 0.7 m/s, and some river with one meter water depth with 4.43 m/s. So as you see, the velocity is not so relevant. The one meter deep river surely builds ice with sudden -20 Celcius night, with 2 m/s, when the small creek still doesnt do it with. 0.5 m/s. $\endgroup$
    – Jokela
    Commented Jun 21, 2015 at 7:33

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