Quantity of water in air at saturation

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    Air Saturation Water
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Discussion Overview

The discussion centers on calculating the quantity of water in air at saturation, specifically in grams per cubic meter (g/m³). Participants explore various equations and methods for determining saturation vapor density, the validity of the ideal gas law under different humidity conditions, and alternative approaches to obtain the necessary data.

Discussion Character

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

Main Points Raised

  • One participant seeks a correlation for calculating the quantity of water in air at saturation, noting the existence of equations for saturation pressure as a function of temperature.
  • Another participant mentions mixing humidity and provides links to resources on saturation points.
  • A participant identifies the desired quantity as saturation vapor density and questions the validity of using the ideal gas law in their specific case.
  • One response outlines the ideal gas law and how to derive density from it, asserting that calculations would be correct if no errors were made.
  • Another participant expresses doubt about the ideal gas law's applicability at 100% relative humidity, suggesting that it may not be valid in this scenario.
  • A participant discusses the dependence of saturation pressure on temperature and the amount of water in the air, proposing the use of Raoult's law for calculations.
  • Alternative methods are suggested, including using psychrometric charts and published relations for thermodynamic properties of water.
  • One participant recommends consulting engineering handbooks for tabulated values instead of functional forms.

Areas of Agreement / Disagreement

Participants express differing views on the validity of the ideal gas law at high humidity levels, with some asserting it is applicable while others argue against it. Multiple approaches and models for calculating saturation vapor density are discussed, indicating no consensus on a single method.

Contextual Notes

Participants highlight the limitations of the ideal gas law under certain conditions, particularly at 100% relative humidity, and the need for more complex models or empirical data for accurate calculations.

lesy1
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Hi,
I would like to know if somebod knows where I could find a corelation to calculate the quantity of water in air at saturation in g/m3.
I know that many equations exist to calculate saturation pressure of water vapor in air as a function of temperature. Using one of these equations and an ideal gas law the quantity of water in air (in kg/m3) could be calculated, but I think that the asumptions for ideal gas law are not valid in my case.
Regards
 
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Jeff, thank you for the answer, although I did not find out anything new. The quantity I am looking for is also called saturation vapor density, but I cannot find any suitable model to calculate it. Can anybody please comment validity of using ideal gas law in my case.
Regards
 
If you assume it's an ideal gas then
PV = nRT where n is the number of moles, T is in kelvin

You can get the density from number of moles,
n = M/m = mass of water / molar mass of water (18 g/mole)

P* m / (R*T) = M/V = density
 
lesy1 said:
Hi,
I would like to know if somebod knows where I could find a corelation to calculate the quantity of water in air at saturation in g/m3.
I know that many equations exist to calculate saturation pressure of water vapor in air as a function of temperature. Using one of these equations and an ideal gas law the quantity of water in air (in kg/m3) could be calculated, but I think that the asumptions for ideal gas law are not valid in my case.
Regards
The ideal gas law is valid. So your calculations would be correct, assuming no errors were made of course.
 
Redbelly, Y,
I am sure that ideal gas law could be used if humidity of air would be low, but because I have air with 100% relative humidity, something says to me, that I cannot use ideal gas law in this case.
 
lesy1 said:
I know that many equations exist to calculate saturation pressure of water vapor in air as a function of temperature.
What equations are these? The saturation pressure is dependent on more than just temperature - it will change depending on the amount of water in the air. If you meant the saturation pressure of pure water vapor, then, yes, you can determine it from just temperature.

To solve your problem, a simple way is to assume that the air and water form and ideal binary mixture. You can then apply Raoult's law:

P=P^{*}_{w}\ x_{w}+P^{*}_{a}\ x_{a}

where P is the total apparent pressure, x is the mole fraction, P superscript * denotes the pure fluid pressure, and subscripts w and a are for water and air. For the water you would use the pure saturation pressure and for air I would just assume that the pressure is roughly the total pressure. You can then determine the number of moles and therefore the mass fractions and specific volume ratios using the ideal gas law. Doing a quick calc this returned a value with about a 3% error.

Another option would be to find a psychrometric chart at the pressure in question, though this may be difficult if your pressure is far from atmospheric pressure.

Finally, you can use published relations such as from “Formulations for the Thermodynamic Properties of the Saturated Phases of H2O from 173.15 K to 473.15 K", ASHRAE Transactions, Part 2A,Paper 2793 (RP-216), (1983), or you can use more complicated (i.e. non-ideal) binary mixture relations.
 
Best approach IMHO would be to take some engineering handbook and read values from tables - unless you really need them in functional form.
 

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