Add-on packages are dedicated process units to cover different technologies or areas such as mobile carrier technologies or detailed sewer network modeling. The chapter provides description about these models.
The addons are available for download on our website.
Mobile carrier can be described as free moving, submerged biofilm carrier which can leave the reactor boundaries with the biofilm attached to it.
Mobile carrier (MC) model is the extension of the SumoBioFilm© model by allowing the carrier and the attached biofilm to move between process units. The model uses Xcarrier variable to calculate the amount of carrier and attached biofilm transported via connections. The sub-model allows the simulation of recirculation, back mixing, media removal and addition.
Biofilm carrier migration model describes reactor performance, Water Science & Technology, 75.12, 2017, Joshua P. Boltz, Bruce R. Johnson, Imre Takács, Glen T. Daigger, Eberhard Morgenroth, Doris Brockmann, Róbert Kovács, Jason M. Calhoun, Jean-Marc Choubert and Nicolas Derlon
The sewer network add-on contains a pipe segment process unit, a service cover and compatible gas flow elements. The pipe segment is consider as a plug flow reactor and can model force main and gravity sewers with fixed biofilm or sediments.
In gravity sewers, the gas phase is allowed to flow both directions – same as sewage and counter direction as well. The service cover predicts fresh air intrusion and gas transfer.
The pipe segment is implemented as a 3-3 input and output ports process unit: one input for sewage, one for gas (same direction as sewage), one for gas (counter direction). Same 3 for outputs.
Pipe segments can be considered as simple plug flow reactors. Sewage flows in one direction, no recirculation is possible. Influent always enters the first segment. The ports with circles are for the liquid phase, the ports with triangles are for the gas phase. The triangles themselves show the direction of gas flow at that port.
The number of segments, length and pipe diameters and fraction of liquid in segments can be modified in parameter inputs.
Gravity sewer pipes are not filled 100% liquid, headspace is accounted. Mass transfer between the sewage and gas phase takes place with a fixed (5 d-1) kLa.
Gas phase is allowed to flow both directions – same as sewage and counter direction as well. This should be implemented in a way that changing flow direction should be possible during simulation, no retranslation should appear.
Based on the influent gas flows from both directions, the process unit calculates the ultimate gas flow. In this implementation, only Q (m3/d) gas is considered. The resultant Qair depend on two cases:
A fixed biomass is modeled as a one-layer biofilm with a fixed thickness. The biofilm cover the wetted surface.
The air flows are summed, and the mass flow is calculated adequately.
The air flow is divided with a fix flow (pump) or proportionally to the input flow and the mass flow is calculated adequately.
Similarly to the pipe segment, the side flow combiner is implemented as a 3-3-3 input and output ports process unit. The liquid flows entrance from the left and the top of the process unit. The liquid flow (input through the circles ports) is represented by the grey lines and its direction is indicated by the arrow below the graphic.
The ports with triangles are for the gas phase and the triangles themselves show the direction of gas flow at that port.
The liquid flow output is the sum of the two liquid flows inputs.
The air flow output depends on two cases:
The service cover mimics an air input (gasventinp) or output (gasventoutp) from or to the outside of the sewer network. The air flows from or to outside the sewer network (gasventoutp and gasventinp) are fixed as parameters. The rest of the service cover is a 3-3 input and output ports process unit as pipe segment, but with no volume and non-reactive.
The air flow outputs to the smallest gas input side and to the gasventoutp (if not null). Two cases may happen:
This add-on includes a Densified sludge separator process unit to simulate the granules selection obtained with a hydrocyclone. A specific model extension is required to simulate separate biological reactions in the flocs and granules: Sumo2 with the granule extension model.
The concept is based on the aerobic granular sludge modeling approach described by Baeten et al. (2018) wherein separate modelling state variable components are assigned for floccular and granular organism groups. The diffusion resistance of substrate into the granules is accounted for using higher “apparent” half-saturation coefficients for granular components. The selective retention and accumulation of granules is predicted by the model as a result of the differential effect on the floccular and granular organism groups of biological selector zones and external selectors, for example wasting from the overflow of hydrocyclones.
The granule fraction is calculated as a function of the relative ratio of granular to total organism groups (granules + flocs) and by assigning portions of influent particulate material to either the floccular or granular groups.
Under normal circumstances, the floccular components of ordinary heterotrophs (XOHO), and PAO and GAO carbon storing organisms (XCASTO) will dominate the growth processes because the model applies a “Diffusion Resistance” parameter to the growth of granular organisms. This diffusion resistance accounts for the reduced access to substrate and oxygen in the inner layers of the granules. It is applied using the “apparent Ks” concept described by Baeten et al. (2018). For example, in the equation below the Monod saturation term for some substrate “S” is defined with the half-saturation coefficient “MsatS” increased proportionally to the diffusion resistance “DR”. The default value of DR is 3 which implies a 300% increase in the half-saturation coefficient.
In fact the term (Ks*DR) acts as the “apparent Ks” investigated by Baeten et al. Table 1 shows how this might be applied in a simplified model matrix. Figure 1 provides a conceptual framework for how modeling direction of influent substrate to growth of floccular and granular organisms in the mixed liquor can then be used to calculate the densified fraction of the mixed liquor.
Table 1 - Gujer matrix presenting separate state components for floccular and granular PAOs, storage products (PHA) as well as “apparent Ks” applied to VFA sequestration and O2 utilization in granules
Because the higher “apparent Ks” has less impact when substrate concentrations are high, the model will simulate the beneficial effects of an internal selector for sludge densification. It is then easy to model the benefits of an external selector to enhancing densification, such as a hydrocyclone, in which granular state variables are selectively retained.
A granular fraction of the following components has been implemented as state variable:
Table 2 - List of Sumo2_granule specific state variables
XB,granule | Slowly biodegradable substrate in granule |
XB,e,granule | Slowly biodegradable substrate from biomass decay - granule |
XU,granule | Particulate unbiodegradable organics in granule |
XPHA,PAO,granule | Polyhydroxyalkanoates (PHA) stored by PAOs in granule |
XPHA,GAO,granule | Polyhydroxyalkanoates (PHA) stored by GAOs in granule |
XE,granule | Endogenous decay products in granule |
XE,ana,granule | Anaerobic endogenous decay products in granule |
XOHO,granule | Ordinary heterotrophic organisms (OHO) in granule |
XCASTO,granule | Carbon storing organisms (CASTO) in granule |
XMEOLO,granule | Anoxic methanol utilizers (MEOLO) in granule |
XAOB,granule | Aerobic ammonia oxidizers (AOB) in granule |
XNOB,granule | Nitrite oxidizers (NOB) in granule |
XN,B,granule | Particulate biodegradable organic N (from XB) in granule |
XN,Be,granule | Particulate biodegradable organic N (from XBe) in granule |
XN,U,granule | Particulate unbiodegradable organic N in granule |
XPP,granule | Stored polyphosphate (PP) in granule |
XP,B,granule | Particulate biodegradable organic P (from XB) in granule |
XP,Be,granule | Particulate biodegradable organic P (from XBe) in granule |
XP,U,granule | Particulate unbiodegradable organic P in granule |
XINORG,granule | Inorganics in influent and biomass in granule |
The biological processes of Ordinary heterotrophic organisms (OHO), Carbon storing organisms (CASTO), Anoxic methanol utilizers (MEOLO), Aerobic ammonia oxidizers (AOB) and Nitrite oxidizers (NOB) have been duplicated from the flocs. The stoichiometric and kinetic parameters for these biological processes are identical in granules and flocs, except for the half-saturation parameters that are multiplied by a diffusion resistance factor. The default values of the diffusion resistance parameters vary between 1, for autotrophic biomasses which are located on the surface of the granule, and up to 4 for ordinary heterotrophic biomass. The variation of these values is representative of the results from Baeten et al. (2018), but the defaults values have been chosen lower than the one calibrated in Baeten et al. (2018). Indeed, their experimental results focused on AGS with an average diameter of 0.55mm, while densified sludge produces granules are mainly smaller, between 0.2 and 0.5mm (Roche et al, 2021).
Note that the model results are very sensitive to these parameters, as demonstrated in the chapter “Calibrating Diffusion Resistance (DR)” of the Quick Tutorial hereafter.
To handle the decay-regeneration of biomass inside the granule, specific biokinetic processes have been implemented:
Furthermore, to give the possibility to user to simulate attachment or detachment on granules processes, a biokinetic process for the “granules to floc net conversion” is added. By default, its kinetic rate “Granule to floc conversion rate” (qgranule,floc) is set to zero. This rate can be set at a positive (detachment) or negative (attachment) value.
The cyclone model for densified sludge selector must be chosen in the options of the cyclone.
This is a volumeless point separator process unit, that will only mass balance the state variable depending on few parameters:
J. Baeten, M.C.M. van Loosdrecht, E. Volcke (2018) “Modelling aerobic granular sludge reactors through apparent half-saturation coefficients.” 146. 134-145. Water Research.
Roche, C., Donnaz, S., Murthy, S., Wett, B., 2021. Biological process architecture in continuous‐flow activated sludge by gravimetry: Controlling densified biomass form and function in a hybrid granule–floc process at Dijon WRRF, France - Roche - 2022 - Water Environment Research - Wiley Online Library. Water Env. Res 2021;e1664.
An example with a cyclone configuration can be found under “Advanced” examples. Although, the following tutorial explains step by step how to build such configuration.
You can modify an existing Sumo model to work with the densification model. In this example, we will select the A2O plant from the list of Examples in the home screen.
To select the densification biokinetic model, go to the MODELS tab in the Sumo ribbon, select the “Advanced” option, and then the Sumo2_Granules option from the Focus models. This model is based on Sumo2, a 2-step nitrification model, with the modification that certain particulate state variables are divided between floccular and granular components.
To add a hydrocyclone to the flowsheet, select it from the “Separators” in the CONFIGURE tab of the Sumo ribbon. Make sure to select “Densified sludge separator” from the Options in the bottom left pane.
The hydrocyclone is added to the WAS stream together with a “Proportional side flow divider” to enable easy switching “On” and “Off” of the cyclone operations.
In the OUTPUTS tab, select the Cyclone element. Create a table and drag and drop the “Contributors to granular TSS” into the table for each of the Feed, Overflow and Underflow. You can drag and drop the input and output ports of the cyclone to create the different columns.
In the INPUTS tab of the Sumo ribbon, select the proportional side flow divider immediately upstream of the cyclone and check the “Scenario” box.
In the SIMULATE tab, this parameter will now appear as an option in the bottom left pane. Create and name two scenarios to represent Cyclone “On” and “Off” operations.
The model includes fractions to represent the amount of particulate inorganic (XINORG), particulate unbiodegradable (XU), particulate biodegradable (XB) and heterotrophs (XOHO) that are granular. The default values are 20%, 10%, 0% and 1%, respectively. The fractions are applied in the following manner: if the amount of influent XINORG is 75 mg/L then 15 mg/L (20%) will be assigned to XINORG,granule and the remaining 60 mg/L (80%) to regular “floccular” XINORG.
By including these in the scenarios we can use them to calibrate the amount unbiodegradable material that contributes to the densified fraction.
For example:
The diffusion resistance (DR) parameters are defined in the MODELS tab of the Sumo ribbon in the bottom left pane after selecting “Show all” under the heading “Granule diffusion resistance”. We can calibrate the impact of these parameters by selecting the “Scenario” boxes as shown below.
The following steps illustrate the sensitivity of the model results to the DR parameters:
The same steps for the “Cyclone” scenario and including the changes to the diffusion resistance parameters from 3 to 1.5, we see the change in Densified fraction “Fgranules” increase from 55.8% to 68.1%.
The model calculates a difference in ORP for fermentative organisms in the floc and the granules. The ORP for the flocs and granules can be viewed in a table by typing “Oxidation-reduction” into the dialog box in the bottom left pane of the OUTPUTS tab of the Sumo ribbon. As long as the “Variables” option is selected from the drop-down menu then the “Oxidation-reduction potential” for the flocs and granules should be displayed. As can be seen below, the ORP in the granules is lower than in the flocs.
The Cyclone operating parameters can be accessed in the INPUTS tab of the Sumo ribbon. The cyclone model is defined with only five parameters as previously described in Cyclone model specifics paragraph.
These parameters have to be calibrated based on the measurements around the cyclone and will impact the simulated Densified fraction.
The plant SRT calculation can be calculated as usual in the TOOLS ribbon, selecting the “Sludge Retention Time” feature and selecting the proper units with drag and drop method.
The calculation of granule SRT can be done on the basis of one of the granular TSS, as XTSS, granules. The “Ratio of variables” calculation has to be selected in the top left panel, and “custom” numerator and denominator variables should be set in the bottom left panel as “M_X_TSS_granules” and “F_X_TSS_granules” respectively. In the bottom right panel, the appropriate process units should be drag and drop at numerator and denominator.
In the following simulation with the cyclone activated, the process is intensified by increasing the WAS pumped flow from 300 m3/d to 900 m3/d. The SRT calculations results in 6.8d SRT for the plant and 15.5d SRT for granules.