Saturday, April 13, 2024

HP Prime: Hagen-Poiseuille Law

HP Prime: Hagen-Poiseuille Law


The Hagen-Poiseuille Law relates flow of water with the change in pressure in the pipe:


Q = K × D^4 × ΔP / (μ × L) where:


K = constant = π / 128 (dependent on the pipe’s diameter)

D = diameter of the pipe (in m)

L = length of the pipe (in m)

ΔP = change in pressure (in Pa)

Q = flow rate (in m^3/s)

μ = viscosity of water (Pa a)



Short Table of Viscosity of Water


Temperature

Viscosity of Water (mPa s)

5 °C (41 °F)

1.5182

10 °C (50 °F)

1.3059

15 °C (59 °F)

1.1375

20 °C (68 °F)

1.0016

25 °C (77 °F)

0.89

30 °C (86 °F)

0.7972


Note that 1 Pa s = 1,000 mPa s


The program references the above table for certain temperatures. The program asks for temperature in degrees Celsius (°C). If any other temperature is entered, the empirical formula known as the Vogel-Fulcher-Tammann Equation is used:


μ = 0.02939 × e^( 507.88 K ÷ (T K – 149.3 K))

= 0.02939 × e^( 507.88 K ÷ ((T °C + 273.15) K – 149.3 K))

= 0.02939 × e^( 507.88 ÷ (T + 123.85))


Equations


Calculating flow:

Q = (π × D^4 × ΔP)/(128 × μ × L)



Calculating Pressure Change:

ΔP = Q × μ × L × 128/(D^4 × π)


HP Prime Code: Hagen-Poiseuille Law


EXPORT HAGEN()

BEGIN

// 2024-02-22 EWS



// local variables

LOCAL ch1;

LOCAL u,t,d,l,p,q;

LOCAL t1,t2,t3;



// list of temps

t1:={"5°C","10°C","15°C",

"20°C","25°C","30°C","Other"};

t2:={1.5182,1.3059,1.1375,

1.0016,0.89,0.7972};

t3:={5,10,15,20,25,30};

// inputs

INPUT({{t,t1},d,l,{ch1,{"ΔPressure",

"Flow Rate"}}},

"Hagen-Poisuelle Law",

{"t:","d:","l:","Solve for:"},

{"Temp of water (ºC)","Pipe Diameter (m)",

"Pipe Length (m)"});



// temp to viscosity

// from table

IF t≤6 THEN

u:=t2(t)/1000;

t:=t3(t);

ELSE

// empirical formula

INPUT(t,"Enter temp in °C","t:");

u:=0.02939*e^(507.88/(t+123.85))/1000;

END;



PRINT();

PRINT("RESULTS:");

PRINT("Temperature: "+STRING(t)+" °C");

PRINT("Viscosity = "+STRING(1000*u)+" mPa s");



// solve for pressure

IF ch1==1 THEN

INPUT(q,"Enter flow rate","q:","m^3/s");

p:=q*u*l*128/(d^4*π);

PRINT("ΔPressure = "+STRING(p)+" Pa");

RETURN {t,u,p};

END;



// solve for flow rate

IF ch1==2 THEN

INPUT(p,"ΔPressure:","Δp:","Pa");

q:=(π*d^4*p)/(128*u*l);

PRINT("Flow Rate = "+STRING(q)+" m^3/s");

RETURN {t,u,q};

END;

END;



Examples


Example 1:

Temp = t = 20°C

Flow = q = 0.5 m^3/s

Solve for Δp

Results:

Viscosity = μ = 1.0016 mPa s

Pressure Change = Δp = 199.261988751 Pa


Example 2:

Temp = t = 10°C

Pressure Change = Δp = 150 Pa

Result:

Viscosity = μ = 1.3059 mPa s

Flow = q = 0.28868299137 m^3/s


Example 3:

Temp = t = 33°C

Flow = q = 0.36 m^3/s

Solve for Δp

Results:

Viscosity = μ = 0.748935277403 mPa s

Pressure Change = Δp = 107.277076309 Pa



Sources


Lauga, Eric. Fluid Mechanics: A Very Short Introduction. Oxford University Press: Oxford, UK 2022. pp. 36-37


“Fluid of Viscosity” Wikipedia. https://en.wikipedia.org/wiki/Viscosity Retrieved February 5, 2024.


“Viscosity of Liquids and Gases” and “Viscosity of Water” HyperPhysics. http://hyperphysics.phy-astr.gsu.edu/hbase/Tables/viscosity.html Retrieved February 8, 2024.


Until next time,


Eddie


All original content copyright, © 2011-2024. Edward Shore. Unauthorized use and/or unauthorized distribution for commercial purposes without express and written permission from the author is strictly prohibited. This blog entry may be distributed for noncommercial purposes, provided that full credit is given to the author.

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