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GPS-X Technical Reference

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95 Suspended Growth Models<br />

where:<br />

V = reactor volume (m 3 )<br />

C L<br />

Q<br />

C in<br />

K La<br />

C * ∞<br />

r<br />

= concentration of dissolved oxygen (DO) in the reactor (mg/L)<br />

= influent flow rate (m 3 /d)<br />

= concentration of DO entering reactor (mg/L)<br />

= oxygen mass transfer coefficient at field conditions (1/day)<br />

= DO saturation concentration at field conditions (mg/L)<br />

= rate of use of DO by biomass (g/day), the respiration rate<br />

The volume flows, and reaction rates are known from specifications or other modelling<br />

equations leaving two terms that must be calculated in order to solve the dissolved<br />

oxygen mass balance over time for the DO concentration in the reactor, C L:<br />

1. DO saturation concentration at field conditions, C * ∞, and,<br />

2. Oxygen mass transfer coefficient at field conditions, K La<br />

Calculation of DO Saturation Concentration at Field Conditions<br />

The DO saturation concentration at field conditions is calculated as follows:<br />

Equation 6.2<br />

where:<br />

τ<br />

β<br />

Ω<br />

C * ∞20<br />

= temperature correction factor (unitless)<br />

= correction factor for salts, particulates, and surface-active substances<br />

(unitless)<br />

= pressure correction factor (unitless)<br />

= DO saturation concentration at 20°C and 1 atm (mg/L)<br />

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

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