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GPS-X Technical Reference

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147 Suspended Growth Models<br />

To model this process, two processes are added in MANTIS2.<br />

44. Growth of anammox microorganism: The stoichiometry factors to express<br />

the yield of biomass, NO2-N consumption and N2 and NO3- are expressed in<br />

terms of per unit NH 4+ -N oxidized. The reaction rate expression uses an<br />

oxygen inhibition function and NO 2-N and NH 3-N saturation functions. Total<br />

(ionized + non-ionized) concentration of both substrates is used in the kinetic<br />

expression.<br />

45. Decay of anammox microorganism: Decay of anammox microorganisms is<br />

modelled using first order reaction rate with respect to the biomass<br />

concentration.<br />

Chemical precipitation processes<br />

The precipitation reactions in MANTSI2 are adapted from Musvoto et al. 2000 with<br />

some modifications. In addition to the processes of precipitation of AlPO 4 and FePO 4<br />

which are included in ASM2d, five commonly observed precipitation processes in<br />

wastewater treatment are included in the model. The key differences from<br />

Musvoto et al. 2000 are: 1) the effect of ion-pair is neglected in the calculations; 2) the<br />

kinetic rate equations use the approach suggested in ASM2d with a few modification and<br />

3) the mole based stoichiometry is replaced with mass based stoichiometry for<br />

maintaining model consistency. The kinetic expression for the precipitation reactions<br />

uses the concentration of participating ions, rate of precipitation and solubility product of<br />

the precipitate. The kinetic rate expression is formulated such that the precipitation and<br />

dissolution reactions can be modeled by a single equation.<br />

46. Precipitation/dissolution of CaCO 3: CaCO 3 is assumed to precipitate as<br />

calcite. The calcite precipitation is assumed to take place in the presence of<br />

Ca 2+ and CO 3<br />

2-<br />

ions in the solution. The concentration of CO 3<br />

2-<br />

is estimated<br />

by using the soluble inorganic carbon and the pH of the system.<br />

47. Precipitation/dissolution of MgNH 4PO 4.6H 2O (struvite): Struvite is the<br />

most commonly observed precipitate in the digester supernatant. The<br />

precipitation of struvite takes place if the Mg 2+ , NH 4<br />

+<br />

and PO 4<br />

3-<br />

species are<br />

present in the solution. The concentrations of NH 4<br />

+<br />

and PO 4<br />

3-<br />

are estimated<br />

based on the solution pH.<br />

48. Precipitation/dissolution of MgHPO 4.3H 2O (newberyite): This is another<br />

precipitate of magnesium with phosphate which is normally observed at<br />

lower pH. For this precipitate, Mg 2+ and HPO 4<br />

2-<br />

ionic species are required.<br />

The concentration of HPO 4<br />

2-<br />

ion is estimated based on pH of the solution.<br />

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

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