Calculating Viscosity from Acceleration: Is it Possible?

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Discussion Overview

The discussion revolves around the possibility of calculating the viscosity of liquids using the falling sphere method, particularly when the sphere does not reach terminal velocity. Participants explore the implications of using acceleration data instead of terminal velocity measurements, and the applicability of Stokes' law under various conditions.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested
  • Mathematical reasoning

Main Points Raised

  • One participant describes their experiment measuring viscosity using the falling sphere method and questions if viscosity can be calculated from acceleration data alone.
  • Another participant suggests that while it is possible to estimate viscosity from acceleration, it would be an approximation and involves plotting velocity as a function of time to fit experimental data.
  • A participant emphasizes that Stokes' law applies strictly at constant velocity, which is only achieved at terminal velocity, raising concerns about its application during acceleration.
  • Some participants note that Stokes' law is valid only under conditions of low Reynolds numbers, which may not be met in the discussed experiments.
  • There are mentions of the need to verify that the Reynolds number is sufficiently low for Stokes' law to be applicable, highlighting the importance of understanding the limitations of the method.
  • One participant shares specific details about their experimental setup, including the use of Rhenium spheres and a silicate melt, and seeks clarification on cases where the sphere did not reach terminal velocity.

Areas of Agreement / Disagreement

Participants express differing views on the applicability of Stokes' law and the conditions under which it can be used. There is no consensus on whether viscosity can be accurately calculated from acceleration data without reaching terminal velocity, and the discussion remains unresolved regarding the specific conditions of the experiments.

Contextual Notes

Participants highlight the dependence on Reynolds number and the specific characteristics of the fluids and spheres used in the experiments, indicating that the applicability of the discussed methods may vary significantly based on these factors.

Polyamorph
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Hello,

I have recently conducted an experiment to measure the viscosity of some liquids using the falling sphere method and a high speed camera. For most of the measurements this is fine since the spheres reach terminal velocity and so it is easy to calculate the viscosity from:

v = \frac{2}{9}\frac{r^2 g (\rho_p - \rho_f)}{\mu},

where:
v is the particles' terminal velocity velocity (m/s),
r is the radius of the sphere,
g is the gravitational acceleration,
\rho_p is the density of the falling sphere,
\rho_f is the density of the liquid,
and μ is the viscosity.

However, in one or two of the measurements the sphere didn't reach terminal velocity, though it is possible to calculate the acceleration.

My question is, is it possible to calculate the viscosity from knowing only the acceleration of the sphere (by perhaps comparing it to the gravitational acceleration in a particular medium for example)?

Thanks in advance for your help.
 
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Polyamorph said:
Hello,

I have recently conducted an experiment to measure the viscosity of some liquids using the falling sphere method and a high speed camera. For most of the measurements this is fine since the spheres reach terminal velocity and so it is easy to calculate the viscosity from:

v = \frac{2}{9}\frac{r^2 g (\rho_p - \rho_f)}{\mu},

where:
v is the particles' terminal velocity velocity (m/s),
r is the radius of the sphere,
g is the gravitational acceleration,
\rho_p is the density of the falling sphere,
\rho_f is the density of the liquid,
and μ is the viscosity.

However, in one or two of the measurements the sphere didn't reach terminal velocity, though it is possible to calculate the acceleration.

My question is, is it possible to calculate the viscosity from knowing only the acceleration of the sphere (by perhaps comparing it to the gravitational acceleration in a particular medium for example)?

Thanks in advance for your help.

Yes, but it's an approximation. From your equation above, you can show that the drag force on the sphere is given by F = 6πrμv. This applies to a sphere moving at a constant velocity. But, if you assume that, to a first approximation, it also describes the drag force during the final stages of the deceleration, then you can write a force balance on the sphere, and use Newton's second law to solve for the velocity as a function of time. This velocity variation will depend on the viscosity. You can plot the velocity as a function of time for various values of the viscosity, and find the curve that best matches your data.
 
Chestermiller said:
Yes, but it's an approximation. From your equation above, you can show that the drag force on the sphere is given by F = 6πrμv. This applies to a sphere moving at a constant velocity. But, if you assume that, to a first approximation, it also describes the drag force during the final stages of the deceleration, then you can write a force balance on the sphere, and use Newton's second law to solve for the velocity as a function of time. This velocity variation will depend on the viscosity. You can plot the velocity as a function of time for various values of the viscosity, and find the curve that best matches your data.

Thanks. I've done this, solving Newton's 2nd law to find v as a function of time, taking into account gravitational force, bouyancy and drag force. The resulting function v(t) can then be fitted to the experimental data using a least square fit to find the optimum η. My remaining question the is regarding Stokes law F = 6πrμv, is this really only valid at constant velocity? Because the only time a falling sphere is at constant velocity is when it is at terminal velocity. During its fall it is subject to the velocity dependent drag force. Is this not F = 6πrμv ?
 
Whoa whoa whoa. Keep in mind this is the equation for Stokes flow, meaning that it only applies to flows with \text{Re}_D \ll 1. That is absolutely a problem here since your Reynolds numbers are almost certainly not low enough.
 
boneh3ad said:
Whoa whoa whoa. Keep in mind this is the equation for Stokes flow, meaning that it only applies to flows with \text{Re}_D \ll 1. That is absolutely a problem here since your Reynolds numbers are almost certainly not low enough.

Whoa, whoa, whoa, whoa. A standard viscometer for very viscous fluids is the falling ball viscometer. Yes, it applies when the Reynolds number is very low. Typically, the viscosity of the fluid will be on the order of 100's to 1000's of poise, and the ball will only be on the order of a few mm.
 
Polyamorph said:
Thanks. I've done this, solving Newton's 2nd law to find v as a function of time, taking into account gravitational force, bouyancy and drag force. The resulting function v(t) can then be fitted to the experimental data using a least square fit to find the optimum η. My remaining question the is regarding Stokes law F = 6πrμv, is this really only valid at constant velocity? Because the only time a falling sphere is at constant velocity is when it is at terminal velocity. During its fall it is subject to the velocity dependent drag force. Is this not F = 6πrμv ?

No. Stokes law is only strictly valid at constant velocity, and, in the falling ball viscometer, this is when the ball is at its terminal velocity. But, even when the ball is still accelerating to approach the terminal velocity, Stokes law should still provide an excellent approximation to the drag force. Can you visualize why? It is because, at any time, the far field velocity of the fluid relative to the ball is essentially constant over the length scale of the ball.
 
Chestermiller said:
Whoa, whoa, whoa, whoa. A standard viscometer for very viscous fluids is the falling ball viscometer. Yes, it applies when the Reynolds number is very low. Typically, the viscosity of the fluid will be on the order of 100's to 1000's of poise, and the ball will only be on the order of a few mm.

Yes, a falling ball viscometer is great, but it can't simply use Stokes Law indiscriminately.
 
boneh3ad said:
Yes, a falling ball viscometer is great, but it can't simply use Stokes Law indiscriminately.

Of course not. It is important to verify a postiori that the Reynolds number is sufficiently low.
 
Chestermiller said:
Of course not. It is important to verify a postiori that the Reynolds number is sufficiently low.

The thing is, it takes a quite viscous fluid, a very buoyant ball or else an incredibly tiny sphere for Stokes Law to apply due to the Reynolds number restriction. Without the OP mentioning nothing about the types of velocities he is measuring or size/type of sphere being used, there is basically no information about the Reynolds number and I feel it important to point out the limits of the technique. In my experience, many inexperienced experimenters aren't aware of that restriction and don't even think to consider it.
 
  • #10
boneh3ad said:
The thing is, it takes a quite viscous fluid, a very buoyant ball or else an incredibly tiny sphere for Stokes Law to apply due to the Reynolds number restriction. Without the OP mentioning nothing about the types of velocities he is measuring or size/type of sphere being used, there is basically no information about the Reynolds number and I feel it important to point out the limits of the technique. In my experience, many inexperienced experimenters aren't aware of that restriction and don't even think to consider it.

Your caveat is appropriate. Maybe the OP can provide more details of the experiments.
 
  • #11
Chestermiller said:
Your caveat is appropriate. Maybe the OP can provide more details of the experiments.

I used Rhenium spheres with diameters of 100-150 μm in a silicate melt, which has a viscosity of about 0.05 Pa s using white beam x-ray radiography with a very fast CCD camera. I just wanted to know the special case when the sphere didn't reach terminal velocity, which happened a couple of times due to the process used to make the spheres means they don't always have uniform density - instead of throwing that data away it would be nice to use it. I think the method described by Chestermiller does the trick, it just means the error bars might be a bit larger in those cases. Cheers.
 
  • #12
Yeah looks like you pretty much have your bases covered on the Reynolds number side. I don't know what the density of your silicate melt is, but it seems like your formula will most likely work.
 

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