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GPS-X Technical Reference

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101 Suspended Growth Models<br />

In the case of user-defined standard air (see Entering Airflow section below), the airflow<br />

is calculated using Equation 6.15.<br />

Equation 6.15<br />

where:<br />

molfr O2<br />

MW O2<br />

= mole fraction of O 2 in user-defined air (mole/mole)<br />

= molecular weight of O 2 (32 g/mole)<br />

P user = density of user-defined air (g/m 3 )<br />

MW user<br />

= average molecular weight of user-defined air (g/mole)<br />

The airflow at either U.S. or European standard conditions is converted to field<br />

conditions using the ideal gas law:<br />

Equation 6.16<br />

where:<br />

T standard<br />

T field<br />

= air temperature at standard conditions (°C)<br />

= air temperature at field conditions (°C)<br />

Equation 6.16 assumes that the field air has the same humidity as the standard air. If the<br />

humidity of the field air is different than for the standard air, the user can multiply the<br />

<strong>GPS</strong>-X calculated field air by the ratio of the mole fraction of oxygen in the field air by<br />

the mole fraction of air in the standard air.<br />

No conversion to field conditions is undertaken for user-defined standard air.<br />

<strong>GPS</strong>-X <strong>Technical</strong> <strong>Reference</strong>

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