Calculate Dynamic Viscosity of Air at 4000m Altitude

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Discussion Overview

The discussion focuses on calculating the dynamic viscosity of air at an altitude of 4000 meters above sea level, specifically at a temperature of 262 Kelvin. Participants explore various methods and formulas relevant to this calculation.

Discussion Character

  • Technical explanation, Mathematical reasoning

Main Points Raised

  • One participant inquires about the method to calculate dynamic viscosity at high altitudes, providing the specific altitude and temperature.
  • Another participant suggests using Sutherland's Formula to calculate viscosity, providing the formula and constants relevant to air.
  • A third participant references a source that includes a formula for viscosity at altitude and mentions kinematic viscosity and its relation to Reynolds Number.
  • A participant asks for clarification on the term "rALT" mentioned in the context of kinematic viscosity calculations.

Areas of Agreement / Disagreement

Participants present different formulas and approaches for calculating dynamic viscosity, indicating multiple competing views on the methodology. The discussion remains unresolved regarding the best approach to take.

Contextual Notes

Some assumptions about temperature and pressure conditions may not be explicitly stated, and the dependence on specific constants and definitions is acknowledged but not fully resolved.

es_joe
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How to calculate the dynamic viscosity of air at high alttitudes,i want to calculate it at height 4000m abovesea level at that height the temp. is 262 kelven degrees.

Any thoughts?
 
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Since viscosity is more or less dependent on temperature, I would start with using Sutherland's Formula:

\mu = \mu_o \left[ \frac{0.555T_o+C}{.555T+C}\right] \left[\frac{T}{T_o}\right]^{1.5}

Where:
\mu_o= .01827 cP for air (or some known value at a different known temperature)
T_o= 524.07°R for air (for the viscosity above, different if using a different value)
C= 120 for air (Sutherland's constant)
T= absolute temperature (°R)

Crane's states that the variation in viscosity is on the order of 10% when going up to 500 psi. Assuming no wierdness goes on at lower (sub atmospheric) pressures, the variation should be very small when deviating less than 15 psi.

You can then go on and calculate the dynamic viscosity through the relation \nu=\frac{\mu}{\rho}
 
Last edited:
According to: http://www.bh.com/companions/034074152X/appendices/data-d/default.htm

Viscosity (kilogram per metre second)

Viscosity is needed to determine kinematic viscosity as shown in the next item.

mALT = (1.458x10-6 x TALT3/2) / TALT + 110.4

where: mALT = viscosity (kg/ms) at altitude (h)

Kinematic Viscosity (square metre per second)

The coefficient of kinematic viscosity is used in determination of Reynolds Number It is evaluated by the ratio:-

nALT = mALT / rALT

where: nALT = coefficient of kinematic viscosity at altitude (m2/s)

It looks like they use a version of Sutherland's method as shown above.
 
Last edited by a moderator:
what is rALT ?
 

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