Calculating Gas Density At Depth
by
Larry "Harris" Taylor, Ph.D.
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This article assumes a basic understanding of the common gas law properties. See A Gas Law Primer for review of these concepts.
Calculating Gas Density At STP
The change in density as a result of change in chemical composition of a gas mix can be easily determined using well-established chemical principles. It is fact that 1 mole (the molecular mass of a substance expressed in grams) of any gas occupies 22.4 liters at STP (standard temperature and pressure: 0 oC (273 K); 1 ata). Tables of molecular weights can be found in any elementary chemical text. These tables tell us that:
molecular mass of O2: 31.998 amu (atomic mass units) molecular mass of N2: 28.014 amu molecular mass of He: 4.00 amu |
Density is defined as mass / volume. Since one mole of dry gas at STP occupies 22.4 liters, the density of a pure substance is easily determined:
Density = Mass
Volume
Density O2 = 31.998 g/mole x 1 mole/22.4 L = 1.428 g/L Density N2 = 28.014 g/mole x 1 mole/22.4 L = 1.251 g/L Density He = 4.00 g/mole x 1 mole/22.4 L = 0.178 g/L |
Oxygen enriched air (EANx or Nitrox) is a binary mixture of nitrogen and oxygen. Thus, the mass for the mix can be determined by simply summing the masses of the individual
components. For example, by choosing a volume of 1 liter, the density, at STP, of 32 % oxygen containing mix (NOAA I) can be calculated:
Mass = Density x Volume
For NOAA I (32 % O2 ) |
For NOAA II (36 % O2 ) |
|
Oxygen mass in 1 liter of mix: 0.32 (1.428 g/L) (1 L) = 0.4569 g Nitrogen mass in 1 liter of mix:: 0.68 (1.251 g/L) (1 L) = 0.8507 g ______________________________________________________ Mass of NOAA I mix occupying 1 liter at STP: 1.3076 g
|
Oxygen mass in 1 liter of mix: 0.36 (1.428 g/L) (1 L) = 0.5141 g Nitrogen mass in 1 liter of mix: 0.64 (1.251 g/L) (1 L) = 0.8507 g _____________________________________________________ Mass of NOAA II mix occupying 1 liter at STP: 1.3648 g
|
This method, as long as components are known, can be applied to any mixture of gases. For example, the density of Tri-mix 21/50 calculates to be 0.75196 g/L. This can be compared to the value of dry air at STP listed in the CRC HANDBOOK OF CHEMISTRY AND PHYSICS of 1.296 g/L.
Density of Dry Gases At STP (g/L) |
|
Air: NOAA I NOAA II Tri-mix 21/50 |
1.2960 1.3076 1.3648 0.75196 |
Calculating Gas Density at Depth
Since the pressure changes associated with scuba diving at recreational depths are relatively small, we may assume ideal gas behavior. With this assumption, the gases will behave according to Boyle's law and density will be directly proportional to absolute pressure. For the direct comparison of air with oxygen enriched air, let's examine a "worst case" scenario: diver breathing dry gas at 0 oC at 132 FSW. (Note that 132 FSW exceeds the recommended depth for NOAA II; also 0 oC is much colder than waters where divers normally play.) These values was chosen, as an illustration, to maximize the density differences observed.
First. determine the absolute pressure at 132 fsw:
Absolute Pressure = Water Column Pressure + Atmospheric Pressure
water pressure = 132 ft / 33 ft/atm = 4 atm absolute pressure = 4 atm + 1 Atm = 5 ata |
Since density is directly proportional to absolute pressure:
Density of Dry Gases At 132 fsw |
|
Air: NOAA I : NOAA II : Tri-mix 21/50 |
1.296 g/L x 5 = 6.48 g/L 1.308 g/L x 5 = 6.54 g/L 1.315 g/L x 5 = 6.58 g/L 0.752 g/L x 5 = 3.76 g/L |
Although the density differences between compressed air and oxygen enriched air are slight, there is some evidence (Israeli Military Divers) that the slight increase in density at depth of the EANx mixtures may lead to CO2 retention. So, divers doing physical labor while diving on EANx should pay particular attention to CO2 buildup.
Conclusion
Assuming ideal gas behavior allows basic chemical principles to be used to estimate gas density of a dry gas at recreational depths. It should be noted that mixes with helium often do not display ideal gas behavior. Also, as depth increases well beyond the recreational limit, gas behavior departs from predictions of ideal relationships and more complex real gas equations must be used. Although this simple method offers a reasonable estimate of gas densities, it should not be considered "gospel" for all mixes at all depths.
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About The
Author:
Larry "Harris" Taylor, Ph.D. is a
biochemist and Diving Safety Coordinator at the University of Michigan. He has
authored more than 200 scuba related articles. His personal dive library (See
Alert Diver, Mar/Apr, 1997, p. 54) is considered one of the best recreational
sources of information In North America.
All rights reserved.
Use of these articles for personal or organizational profit is specifically denied.
These articles may be used for not-for-profit diving education