Effects of Temperature on Flow Rate

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Discussion Overview

The discussion focuses on the effects of temperature on flow rate and pressure in a water cycling experiment involving filter media. Participants explore the relationship between flow rate, differential pressure, and temperature, particularly how temperature variations may influence viscosity and flow characteristics.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested

Main Points Raised

  • One participant describes an experiment where water is cycled through filter media, noting that while differential pressure changes linearly with flow rate, the slopes of these relationships do not overlap as expected.
  • Another participant points out that the viscosity of water is temperature dependent and can change significantly (up to 20%) over a temperature range of 10 degrees Celsius.
  • A subsequent reply asks how to apply viscosity values to correct flow rate or pressure measurements.
  • Another participant suggests that the pressure drop should be proportional to the product of flow rate and viscosity, and questions whether the geometry of the porous media has been considered, referencing the Ergun equation and Darcy's law.

Areas of Agreement / Disagreement

Participants express differing views on the factors affecting the slopes of the pressure-flow rate relationship, particularly regarding the role of viscosity and geometry. There is no consensus on how to correct for temperature changes in the flow or pressure measurements.

Contextual Notes

Participants acknowledge the influence of temperature on viscosity but do not resolve how to account for these effects in their experimental setup. The discussion includes assumptions about the negligible thermal expansion of materials and the need for further exploration of flow dynamics through porous media.

Who May Find This Useful

Researchers and practitioners involved in fluid dynamics, experimental physics, and engineering applications related to flow through porous media may find this discussion relevant.

Abe Rosenberg
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Using a pump we are cycling water through a capsule with filter media inside; while measuring the flow rate (l/min) and the pressure (psi) going in and the pressure going out. The water is cycled back into the same storage tank. As the flow rate increases the differential pressure should change linearly, which has been the case.

We have three separate sized canisters with the same filter media inside and each plot of Diff Pressure by flow rate has a R^2 over .995 for each trial we complete. The problem is that the slopes do not overlap as they should. We are adjusting the flow rate to a flux to ensure that the flow rates correspond to the same flux for each size. We believe that since we cannot regulate temperature (although we are monitoring it for each test) that the expansion of water, thus letting the density decrease is causing water to flow slightly faster and thus messing up our slopes, this is the case for even capsules of the same size since we are running trials in triplicate each capsule of the same size is even having a problem having slopes overlap.

We believe thermal expansion of the plastic and media is negligible since the greatest temperature change we observe is ~10*C.

How should we go about correcting for a temperature change in our flow/pressure?
 
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Henryk said:
The slopes depend on geometry and viscosity of water.
The viscosity is temperature dependent and can change 20 % over 10 degrees C.
https://wiki.anton-paar.com/en/water/
Thanks, how can we use these values to correct either our flow rate or pressure?
 
If you measure the temperature of each test, then the pressure drop should be proportional to the product of flow rate Tims viscosity. Are you taking into account the different lengths and cross sections of the porous media? Are you familiar with the Ergun equation or Darcy's law for flow through porous media?
 

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