This article presents the authors’ perspectives on modelling best practices for nature-based solutions (NBS). The authors led a workshop on NBS modelling as part of the 8th IWA Water Resource Recovery Modelling Seminar (WRRmod2022+) in January 2023, where the discussion centred around the design, use cases, and potential applications of NBS models. Four real-world case studies, encompassing an aerated lagoon, a biofilm-enhanced aerated lagoon, a stormwater basin, and a constructed wetland were reviewed to demonstrate practical applications and challenges in modelling NBS systems. The initial proposed modelling framework was derived from these case studies and encompassed eight sub-models used for these NBS types. The framework was subsequently extended to include eight additional NBS categories, requiring a total of 10 sub-models. In a subsequent step, with a different perspective, the framework was refined to focus on 13 primary use cases of NBS, identifying 10 sub-models needed or potentially required for these specific NBS applications. These frameworks help to identify the necessary sub-models for the NBS system at hand or the use case. This article also discusses the benefits and challenges of applying water resource recovery modelling best practices to NBS, along with recommendations for future research in this area.

  • Data scarcity is a primary challenge to NBS modelling, with limited data available for model calibration and validation.

  • The numerous use cases and categories of NBS technologies complicate the development of a broad and flexible modelling framework.

  • Inspired by four NBS case studies, the paper addresses diverse objectives and challenges in NBS modelling.

  • The proposed frameworks offer a structured approach to NBS modelling, considering various categories, use cases, and essential sub-models.

There is growing interest in nature-based solutions (NBS) as ‘green’ alternatives to conventional ‘grey’ approaches to wastewater treatment. ‘Grey’ refers to a reliance on concrete basins and mechanical equipment, whereas ‘green’ means infrastructure that is more natural in appearance (Cross et al. 2021), possibly utilizing existing natural features (Sowińska & García 2022) (natural ponds or wetlands) or else human-built structures that are engineered to mimic nature-like constructed ponds, wetlands (Haddis et al. 2020), swales, green roofs, and stormwater basins (Kuller et al. 2017). NBS are promoted for their sustainability and cost-effectiveness (Dorst et al. 2019) in providing a wide range of benefits, including pollutant removal (Pascual et al. 2021), flood prevention (Steis et al. 2020; Mubeen et al. 2021), water retention, and many co-benefits (Dagenais et al. 2017) such as heat dissipation, habitat creation for wildlife, and biodiversity enhancement (Cohen-Shacham et al. 2016; Sowińska & García 2022; Bousquet et al. 2023).

A useful classification system that distinguishes NBS as water-based or substrate-based systems as well as the types of influent wastewater that can be treated was presented by Cross et al. (2021). The classification system is applied to 21 distinct NBS types and achievable treatment efficiencies and co-benefits are identified. Whether NBS can meet expectations in practice, however, is not always evident. As stated in a recent publication from the UN, ‘there are also still too many cases where NBS are deployed based on uncertain science (Istenič et al. 2023) and then do not deliver on their stated impacts (Sowińska & García 2022)’ (WWAP 2018). Modelling tools could go a long way to bridging the knowledge gap or ‘uncertain science’ referred to in this statement. Mathematical models are how engineers typically codify knowledge and experience, but there is limited availability of NBS modelling tools in the literature. The authors propose the following reasons for the limited availability of modelling tools:

  • 1. Limitations in understanding of first principles and mechanisms of how a particular NBS operates. In this respect, NBS would be viewed by engineers somewhat as a black box. The NBS provides a benefit but the exact causes of this benefit (and therefore how to optimize it, or under what conditions the benefit may be lost) are unknown or poorly understood. For example, consider the benefit of pathogen removal by waste stabilization ponds (Nelson et al. 2004). A practitioner might be an expert in the behaviour of the NBS but may not understand the underlying mechanisms of pathogen removal.

  • 2. Underlying first principles and mechanisms are known but have not been consolidated into a comprehensive model that is broadly available to the community of NBS practitioners. There are a few mathematical models available, such as River Water Quality Model No. 1 (RWQM1) (Shanahan et al. 2001) for streams or SURFWET, a biokinetic model for surface-flow constructed wetlands (Aragones et al. 2020) but they are specific to only certain NBS categories. This is very common in engineering disciplines where specialized knowledge exists in a small group of specialists who have not seen the value in codifying and sharing a model.

  • 3. The mechanisms are known but of a complexity such that it is not practical to try to solve them mathematically in a computer model. Flow networks that require advanced computational fluid dynamics (CFD) to solve may fall into this category for most practical engineering applications (Rajabzadeh et al. 2015).

  • 4. The required inputs to the model are not quantifiable. For example, plant roots are known to provide surface area for bacterial nitrification in constructed wetlands and the nitrifying capacity of wetlands is directly proportional to this surface area (Morgan et al. 2008). Quantifying the surface area of all root structures (and how they change seasonally and under different loading conditions) may be seen as an impossible task.

The good news is that there is already rich literature on modelling wastewater to draw from. For example, hydrodynamics (Wicklein et al. 2016), sedimentation (Takács et al. 1991; Torfs et al. 2016), filtration, water chemistry (Fairlamb et al. 2003; Batstone & Flores-Alsina 2022), biokinetics (Henze et al. 2000), and biofilm processes (Wanner & Gujer 1986; Takács et al. 2007) have each been well studied and there exist good, published models to describe their behaviour. The challenge is packaging them together as ‘sub-models’ of a larger modelling framework that is appropriate to the context of NBS. For example, as illustrated in Figure 1, a wetland may include several sub-models to capture the relevant treatment behaviour.
Figure 1

Relationship between sub-models and an integrated model for a given NBS.

Figure 1

Relationship between sub-models and an integrated model for a given NBS.

Close modal

Certain sub-model details, however, may need to be rethought concerning parameterization and level of detail. For example, the settling properties of humic substances found in wetlands may be markedly different from what is assumed in a sedimentation model developed for (or borrowed from) clarifier technologies. Since humic substances in wetlands accelerate particle settling through bridging and sweep flocculation methods, they also significantly increase the hydraulic resistance of accumulated solids (Liu et al. 2019). Moreover, modelling flow through constructed wetland root structures using CFD may be computationally onerous and otherwise impossible given the lack of information on the nature and abundance of the roots themselves. These sorts of challenges are very common.

Fortunately, engineers are adept at making creative simplifications and approximations to manage complexity and still develop insightful design models with predictive power. Initially, simple rules of thumb and regression equations were used, along with the first-order k-C model – one of the earliest and most well-known models, which relate the rate of degradation of contaminants to their concentration in the water (Rousseau et al. 2004; Ho et al. 2017). However, after the 1990s, due to the rapid advancement of computer technology and a growing understanding of underlying NBS mechanisms, more dynamic and compartmental models were developed to better represent the behaviour of these systems (Rousseau et al. 2005; Houweling et al. 2008; Patry 2020). These models incorporate more detailed information about the physical, chemical, and biological processes that occur in NBS systems and are often used to predict their long-term performance (Meyer et al. 2015; Ho & Goethals 2020). Data-driven models, employing machine learning techniques to identify model structures for both linear and non-linear processes (Dunn 2020), CFD modelling and compartment-based modelling have also been applied to model NBS systems with greater accuracy (Wood et al. 1995; Alvarado et al. 2012).

The primary challenge to the application of NBS models remains data scarcity, i.e., the limited amount of data available for model calibration and validation (Ho et al. 2017). It is often assumed that a predictive NBS model must be calibrated and validated to be considered reliable and accurate. Using a calibrated and validated model to generate predictions may be considered the ‘gold standard’ of good modelling practice (Rieger et al. 2012). However, it may not always be practical, especially when working with new NBS models or when applying long-standing models to a new application. Still, an NBS model that is not fully calibrated or validated to its field of application can provide valuable information. Simulations can be run to identify parameter sensitivity (i.e., the sensitivity of model outputs to changes in input and model parameters) and define the limits of what is possible to achieve for a given NBS. In this way, even an NBS model that is not fully calibrated or validated can steer practitioners in their decision-making and help them avoid bad designs. As illustrated in Figure 2, this may be considered the ‘consolation prize’ of working with uncalibrated or unvalidated models.
Figure 2

Approaches for working with calibrated and uncalibrated NBS models.

Figure 2

Approaches for working with calibrated and uncalibrated NBS models.

Close modal

Parameter sensitivity analyses are standard procedures for applying NBS models in cases of ‘data scarcity’ where there is insufficient data to meet the ‘gold standard’ of model calibration and validation. Sensitivity analysis can then be combined with methods such as Monte Carlo Analysis to propagate parameter uncertainty into scenario simulation results (Sin et al. 2009; Ho et al. 2018; Borzooei et al. 2019). Sensitivity analysis also provides ancillary benefits to the NBS model user in revealing which parameters have the greatest influence and can be considered ‘governing parameters’, the latter being good candidates for further investigation through laboratory or field measurements. Identifying ‘which are the governing parameters’ is equivalent to identifying ‘which are the governing mechanisms’, an important insight that NBS models can provide.

The sheer number of use cases and categories of technologies are also challenges in developing a framework for modelling NBS. For instance, Cross et al. (2021) categorize NBS as either water-based (e.g., ponds and in-stream restoration) or substrate-based (e.g., soil infiltration, subsurface flow treatment wetlands), and there are numerous other possible categorizations and sub-categorizations, such as reactive vs. non-reactive and photosynthetic vs. mechanically aerated. Furthermore, difficulties arise in capturing transient phenomena that can impact system performance, such as storm events in wetlands, integrating and adapting the activated sludge model (ASM) kinetics for NBS systems with long solids retention time (SRT) (Friedrich et al. 2017).

A modelling framework for NBS should be both broad and flexible. To this end, this article adopts an approach inspired by a series of case studies with different objectives and challenges. These serve as the foundation for developing a multidimensional framework that accounts for the NBS type, use case, and required sub-models. It is then extended to cover a more inclusive list of NBS categories identified by Cross et al. (2021). It is the authors' hope that this framework may guide future development efforts, and in so doing, address the central question of this opinion article: ‘How can good modelling practices inspired by guidelines for activated sludge models be applied to bridge the knowledge gap in modelling NBS?’

Four case studies presented below are drawn from the academic research and consulting practice of the co-authors and participants of a workshop at the 8th IWA Water Resource Recovery Modelling Seminar (WRRmod2022 +) in January 2023. While they do not cover the full spectrum of existing NBS types and use cases, they do present sufficient variety in objectives and sub-models to form the foundation of the multidimensional framework proposed in this article. This article does not fully cover the modelling results of the case studies. Instead, it seeks to summarize the findings to demonstrate the accuracy of the models and highlight what is essential for supporting the proposed NBS modelling framework. The case studies include:

  • Municipal aerated lagoons (ALs) where the modelling objective is predicting BOD5 removal.

  • A biofilm-enhanced AL arrangement treating municipal effluent with the objective of modelling nitrification and the relationship between methane generation in the sediment layer and effluent TSS.

  • A stormwater basin with the objective of predicting pathogen removal.

  • A constructed wetland treating contaminated groundwater with the objective of validating use of supplemental oxygen supply to enhance nitrification capacity.

Case study 1: Aerated lagoon, Quebec, Canada

Le Gardeur ALs, located in Repentigny, Quebec, Canada, were constructed in 1988 to serve a municipal population of 25,000 (Luque et al. 2012). The system comprises a bar screen pre-treatment stage, followed by four ALs with a volume of 68,400 m3, a depth of 3.5 m, and an empty bed hydraulic retention time (HRT) of 6.2 days connected in series, as presented in the SUMO simulation software flowsheet in Figure 3 (Dynamita 2024).
Figure 3

Flowsheet of Le Gardeur ALs in SUMO simulation software (Dynamita, Sigale, France).

Figure 3

Flowsheet of Le Gardeur ALs in SUMO simulation software (Dynamita, Sigale, France).

Close modal

Each lagoon is equipped with subsurface aeration diffusers to meet the oxygen requirements at an aeration intensity equivalent to 2.18 m3 air/m3 treatment volume/d (or 1.94 W/m3) in the first lagoon. Information related to HRT, aeration intensity, and sediment accumulation is presented in Table 1.

Table 1

Sludge volume, aeration intensity, and net HRT of Le Gardeur aerated lagoon

LagoonVolume of sludge (%)Aeration intensity (W/m3)Net HRT (d)
9.1 1.94 5.6 
6.1 0.66 5.8 
4.7 0.31 5.9 
8.2 0.06 5.7 
LagoonVolume of sludge (%)Aeration intensity (W/m3)Net HRT (d)
9.1 1.94 5.6 
6.1 0.66 5.8 
4.7 0.31 5.9 
8.2 0.06 5.7 

ALs in Quebec are sized based on BOD5 removal objectives and the standard design model applied by the regulator is a first-order equation corrected for temperature. This model, the so-called Eckenfelder equation, is presented in Equation (1) (Eckenfelder & Ford 1970):
(1)
(2)
where Se is effluent BOD5C (mg/L); S0 is influent BOD5C (mg/L); t is the hydraulic retention time in the lagoon (d); Ke,T is BOD5C removal rate (d−1); Ke@20°C is BOD5C removal rate at 20 °C (d−1) (Ke@20°C = 0.37 d−1); T is the temperature (°C); CF is the correction factor; and θ is the temperature coefficient (θ = 1.07).

The correction factor ‘CF’ accounts for release of BOD5C from anaerobic decomposition in the lagoon sediment layer (CF = 1.05 in winter and 1.20 in summer). It is applied only to the first and second ponds for a series of three or more ponds. The removal coefficient at 20 °C (Ke@20°C) is 0.37 d−1 and the temperature coefficient (θ) is 1.07. The HRT in this model is varied based on the volume occupied by the accumulation of sludge at the bottom of the lagoons as well as for the formation of ice cover on the surface in winter (5%) for lagoons 2–4 (MELCC 2010).

The first-order model does not predict well the effluent of BOD5, as illustrated in Figure 4. The use of simple modelling equations based on first-order removal kinetics has the advantage of making the model easy to apply and calibrate to real-world data. However, in a first-order model, removal of substrate is ‘by definition’ linked only to HRT and not to the presence of biomass, which means that the impact of biomass washout or upgrade strategies with biofilm technologies and biomass augmentation cannot be simulated.
Figure 4

First-order modelled effluent BOD5 compared with measurements.

Figure 4

First-order modelled effluent BOD5 compared with measurements.

Close modal

The authors believe that many relevant mechanisms are improperly accounted for or simply out of scope. For example, the Eckenfelder model did not consider the interaction of water and sediment layer and temperature stratification in lagoons, especially during the fall. Additionally, it oversimplifies the decay kinetics assumption, failing to capture microbes' dormancy in cold weather, thus impacting BOD5 removal. It overlooks the influence of algae growth in the summer, potentially leading to increases in effluent TSS and BOD5. To enhance prediction accuracy in ALs, a more robust model was suggested to address these limitations. A model that includes two specific sub-models, one concerning biokinetics and another regarding the compartmentalization of the water column and sediment layer, is expected to improve the accuracy of the simulation. This model could also include a photosynthesis sub-model to capture the algal growth impact on AL performance, such as provided in the pond model included in the SUMO simulation software (Dynamita, Sigale, France).

Case study 2: Biofilm-enhanced aerated lagoon, Quebec, Canada

The Grandes-Piles ALs, situated in Quebec, Canada, serve a population of 415 inhabitants. The lagoon is divided into two equal parts (Figure 5), and in one half, a biofilm-enhanced system was introduced to improve the nitrification process, increase the concentration of biomass, decrease the effluent TSS, and enhance the lagoon's capacity. This system was developed by the BIONEST company (Shawinigan, QC, Canada) and is implemented as the KAMAK™ technology. KAMAK™ implements a division of the AL volume into five zones, comprising three clarifications (Cl1, Cl2, and Cl3) and two biofilm reactor zones (RX1 and RX2). The biofilm zones are equipped with BIONEST bacterial support, featuring a large specific surface area (210 m2/m3 of support) (Patry et al. 2021). A detailed characteristic of each zone is presented in Table 2.
Table 2

Dimensions and average HRT of the original lagoon and KAMAK™ system (Patry 2020)

LagoonVolume (m3)HRT (d)Available area (m2)
Original lagoon 1,475 17,5  
Kamak system 520 6,2 2,127 
Cl1 149 1.8  
RX1 (10 columns) 34 0.4 1,418 
Cl2 149 1.8  
RX2 (5 columns) 37 0.4 709 
Cl3 149 1.8  
LagoonVolume (m3)HRT (d)Available area (m2)
Original lagoon 1,475 17,5  
Kamak system 520 6,2 2,127 
Cl1 149 1.8  
RX1 (10 columns) 34 0.4 1,418 
Cl2 149 1.8  
RX2 (5 columns) 37 0.4 709 
Cl3 149 1.8  
Figure 5

General view of the KAMAK™ system of Grandes-Piles (Patry 2020).

Figure 5

General view of the KAMAK™ system of Grandes-Piles (Patry 2020).

Close modal
The model was built in the WEST simulation software (DHI, Hørsholm, Denmark) (Vanhooren et al. 2003) and the flowsheet, as presented in Figure 6, includes seven unit processes. These unit processes include biofilm reactors, variable volume sediment digesters, settlers, non-reactive continuous stirred-tank reactors (CSTRs), controllers, flow splitters, and flow combiners. Sub-models include the standard biokinetic model from the WEST library, one-dimensional biofilm models, a gas–liquid transfer model for the digester unit sub-model and a control sub-model to relate the gas production in the digester to solids resuspension into the non-reactive CSTRs.
Figure 6

Complete KAMAK™ system model layout in the WEST simulation software (DHI, Hørsholm, Denmark) (Patry 2020).

Figure 6

Complete KAMAK™ system model layout in the WEST simulation software (DHI, Hørsholm, Denmark) (Patry 2020).

Close modal

All biochemical reactions were assumed to occur in the biofilm reactors and digesters, hence the use of the ‘non-reactive CSTR’ to represent the lagoon water column. This simplification of the model combines the activity of the biofilm with the potentially present activity of the suspended biomass in the real system. The connection from the settler model to the digester model, representing the sedimentation flux, has a minimal liquid flow through the digester block (0.001 m3/d), and it was confirmed that this flow has no discernible impact on the overall lagoon hydraulics. Additionally, there is a return link from the digester to the non-reactive CSTR describing the bulk liquid volume above the sediment layer, enabling the modelling of biogas-induced sediment resuspension (ebullition) and the release of soluble compounds from the sediments.

The modelling result for nitrification, which only occurs seasonally in the system, is shown in Figure 7. Accurately calibrating NH4-N dynamics in spring and autumn (the starting and ending seasons of nitrification in AL) proved challenging. The proposed solution was to modify the biokinetic sub-model by dividing the autotrophic biomass into two groups of bacteria (Young et al. 2017). A slow-growing group (XBA,1) to represent the slow nitrification starting early in May and a fast-growing group (XBA,2) to take over at the end of summer. Using only one group of nitrifiers did not allow for a satisfactory description of the year-long performance.
Figure 7

Modelled effluent NH4-N considering the two groups of autotrophic bacteria compared to measurements (Patry 2020).

Figure 7

Modelled effluent NH4-N considering the two groups of autotrophic bacteria compared to measurements (Patry 2020).

Close modal
The unexpected summer nitrification loss occurring at an ideal temperature is correlated with an increase in TSS in the system's effluent, as illustrated in Figure 8. The proposed explanation, given by Patry et al. (2021), links gas production in sedimentation zones to biofilm reactor performance. This suggests that anaerobic digestion and associated gas production lead to sediment resuspension, influencing biofilm composition (attachment of resuspended solids) and subsequently affecting nitrification performance.
Figure 8

Modelled effluent TSS compared to measurements (Patry 2020).

Figure 8

Modelled effluent TSS compared to measurements (Patry 2020).

Close modal

The results of this case study suggest that the selected sub-models and the strategy of dividing autotrophic bacteria into two groups have the potential to improve the modelling of enhanced-biofilm AL.

Case study 3: Stormwater basin, Quebec, Canada

The Chauveau stormwater basin is situated in Faubourg Le Raphaël, Quebec City, QC, Canada. The basin was constructed in 2005 to collect rainwater from a residential area of 15.1 ha. The basin has a maximum water height before overflow of 1.7 m and a volume of 4,300 m3 as shown in Figure 9. The stormwater basin has a minor entrance with a 900 mm diameter pipeline and a major entrance with a stone overflow. The inlet pipe has a diameter of 900 mm and the outlet has a diameter of 450 mm with a bottom drain with a diameter of 300 mm. These two inlets converge at the outlet, where a flow restrictor limits the discharge to 350 L/s (Vallet et al. 2016).
Figure 9

Chauveau watershed (red) and stormwater basin (yellow) and location of the inlet, outlet, and bottom drain (Vallet 2011).

Figure 9

Chauveau watershed (red) and stormwater basin (yellow) and location of the inlet, outlet, and bottom drain (Vallet 2011).

Close modal

The model of this stormwater basin was built in the WEST modelling software (DHI, Hørsholm, Denmark) (Vanhooren et al. 2003). The model discussed in the case study extends the stormwater sedimentation model of Vallet et al. (2016) and focuses on Escherichia coli removal mechanisms, primarily through sedimentation of particles to which E. coli is attached. This model utilizes a layered approach and a mass balance to describe spatial heterogeneity, simulating particle concentration gradients and pollutant behaviour.

The model defines a population of particle classes with different sedimentation velocities and associated suspended solids masses. The ViCAs protocol (Chebbo & Grommaire 2009) is employed for experimental determination of particle class fractions. The population balance model, incorporating sorption/desorption processes, simulates pathogen dynamics in stormwater basins. Inactivation of E. coli is described through natural decay, predation, and solar disinfection, with these processes applied to both particulate and free E. coli populations. The overall sorption/desorption process rate, base decay, and solar disinfection are detailed in the model, offering a comprehensive understanding of E. coli dynamics in stormwater systems (Vergeynst et al. 2012).

The proposed stormwater basin model consists of three sub-models, including a one-dimensional, vertical flux hydraulic model, an influent fractionation model to distinguish between soluble and particulate components and to classify particulate components according to their sedimentation velocities and a sedimentation model.

Simulation results for a model with a single class of particles with a settling velocity of 1.0 m/d are illustrated in Figure 10. The graphs illustrate light intensity and free E. coli concentration in different layers: surface (L1), middle (L5), bottom (L9), and sediment layers (L10). Light intensity follows a sinusoidal pattern, reaching its maximum at the surface. Over the simulation period, light penetration increases in deeper layers as suspended solids settle, with a slower increase in deeper layers due to the larger distance for particles to settle over. The scenarios highlight that light intensity evolution depends on particle settling velocity. The simulations assume a single particle class, but in real stormwater, with uncertain and varied settling velocities, light penetration would likely reach deeper layers faster (Vallet et al. 2016).
Figure 10

Simulation results for light intensity (a) and free (b) E. coli concentrations in layers 1, 5, 9, and 10 for a single particle class with a settling velocity of 1.0 m/d (Vergeynst et al. 2012).

Figure 10

Simulation results for light intensity (a) and free (b) E. coli concentrations in layers 1, 5, 9, and 10 for a single particle class with a settling velocity of 1.0 m/d (Vergeynst et al. 2012).

Close modal

The removal of free E. coli (Figure 10(b)) increases as particulate concentration decreases, leading to enhanced disinfection. In the absence of radiation at night, the removal of free pathogens is solely due to base decay. The rise in solar disinfection takes longer in deeper layers and for slower-settling particles, resulting in lower light intensities and noticeable wave-shaped concentration profiles. Solar disinfection's importance is evident in the decrease of free bacteria in deeper layers (Figure 10), particularly when higher light intensity reaches subsurface layers during the second day. The model successfully replicates various stormwater basin phenomena, including decay, adsorption/desorption to particles, settling, and solar disinfection (Vergeynst et al. 2012).

The robustness of this model still requires validation through longer datasets or by including other NBS categories. Nevertheless, this case study illustrates how these three sub-models were developed for a specific use case, pathogen removal.

Case study 4: Constructed wetland, Michigan, USA

In 2015, a surface flow wetland with a 23 ha wetted area was designed and built in Michigan (USA) to treat up to 1,500 m3/d of groundwater contaminated with up to 50 mg/L of ammonia and to reduce it to less than 1 mg/L. The hydraulic design of the wetland is based on Lightbody et al. (2009) and includes two distinct zones: a deep zone with oversaturated water inflow and a shallow zone with planted native emergent vegetation. Figure 11 on the left side presents a schematic top view of the surface flow wetland and the right side presents a schematic cross-sectional view.
Figure 11

Overview of the surface flow wetland design in Michigan. Schematic top (left) and cross-sectional view (right) (Austin et al. 2018).

Figure 11

Overview of the surface flow wetland design in Michigan. Schematic top (left) and cross-sectional view (right) (Austin et al. 2018).

Close modal

The first objective of the study was to determine the adequacy of existing modelling tools for simulating a surface flow wetland. The second objective was to use the model to fill in data gaps, notably concerning the relative contributions of the deep and shallow zones to overall treatment performance, and based on this, evaluate the validity of the original design assumptions. The two distinct zones and the mass balance on nitrogen were modelled using two existing unit processes from the SUMO™ (Dynamita, Sigale, France) model library: a moving-bed biofilm reactor (MBBR) unit to simulate the root (shallow) zone and a Pond unit to simulate the open water (deep zone). Each unit process included several sub-models such as a gas–liquid transfer model for relevant gases including oxygen (MBBR and pond unit), an influent wastewater fractionation model to distinguish between soluble and particulate biodegradable and non-biodegradable components (MBBR and pond unit), a biokinetic model (MBBR and pond unit), a one-dimensional biofilm model (MBBR unit), a two-compartment water column/sediment layer model (pond model), and a sedimentation model (pond model).

Biological conversion of carbon and nitrogen was modelled using a biokinetic model that includes ASM processes with additional kinetic equations for algae. The wetland flowsheet presented in Figure 12 includes a series of 8-unit processes: four MBBR units and four Pond units.
Figure 12

Model structure of the surface flow wetland: (top) schematic cross-sectional view (Austin et al. 2018) and (bottom) SUMO model layout.

Figure 12

Model structure of the surface flow wetland: (top) schematic cross-sectional view (Austin et al. 2018) and (bottom) SUMO model layout.

Close modal

The MBBR units represent shallow zones where flow through root structure biofilms is the dominant process. The pond units represent flow through deep zones where water supersaturated in oxygen is injected. The three first ponds have two inflows: recirculated aerated water and water from the previous zone.

It is assumed in the calibration protocol that most of the biological treatment occurs in the shallow zone, except for algae growth. Because the shallow zone is mostly composed of plants, which means that direct sunlight does not reach the water, algae growth should occur in the deep zone, which is modelled as a pond. Existing pond models were used to model the deep zone, and algae concentrations were simply fitted by slightly increasing the sun radiation data within their range of uncertainty. The shallow zone is modelled as an MBBR model, and the parameters in the MBBR model were calibrated to fit carbon and nitrogen water quality data. The soluble effluent pollutant concentrations were fitted by calibrating the biomass surface in the MBBR model through a reduction in media fill (from 50 to 20%) and specific surface (from 500 to 250 m2/m3). Arrhenius constants were also reduced (to 1.12 and 1.06) because the model simulated too much nitrification during the winter (below 5 °C).

Finally, surface oxygenation via Henry's law was calibrated by reviewing results for the lead plant zone (MBBR), which did not have an oxygen source. The available surface area for atmospheric transfer, which would be affected by plantings, was reduced significantly to provide for a reasonable aerobic environment (DO of 1–1.5 mg/L). The results of the simulation are provided in Figure 13.
Figure 13

Simulated ammonia versus measurements at the influent and effluent of the surface flows wetland. Measurement data provided by Austin et al. (2018).

Figure 13

Simulated ammonia versus measurements at the influent and effluent of the surface flows wetland. Measurement data provided by Austin et al. (2018).

Close modal

Figure 13 demonstrates that the SUMO model can simulate the breakthrough in effluent ammonia concentrations from the surface flow wetland during cold months (below 5 °C). The first objective (modelling the surface flow wetland) can therefore be met, despite the lack of a dedicated constructed wetland unit process, through a combination of MBBR and pond modelling units.

The model developed has not yet been validated on independent datasets and it is unknown at this point if the model is ready to access the design assumptions (second modelling objective) of the surface flow wetland design. Nevertheless, this case study provided a valuable example of how NBS models can be developed in practice: (1) identify the modelling purpose, (2) identify the mass balances of interest, (3) identify the relevant sub-models required, and (4) combine unit processes that include the required sub-models.

The four case studies presented a modelling approach for different NBS systems, each with different objectives. In the authors' opinion, this approach could be extrapolated into a reference framework to assist in creating useful models for various NBS systems. In case study 4, for example, this concept is effectively demonstrated. By identifying the necessary sub-models and combining two process units – a pond and a media biofilm (MBBR) – the authors developed a model for a constructed wetland with the objective of modelling nitrification. Table 3 presents the initial proposed framework for modelling NBS according to their ‘category’ and the required ‘sub-models’. Here, the ‘category’ in this table refers to the case studies discussed.

Table 3

Sub-models utilized in the four case studies

Sub-modelInfluent modelHydraulic balanceSegregating water column and sediment layerLayered sedimentation (1D Flux)Biofilm modelBiokinetic modelPhotosynthesis and/or light availabilityAeration, gas transfer
Case study 1a: Aerated lagoon      ●   
Case study 1b: Aerated lagoons ● ● ●   ● ● ● 
Case study 2: Biofilm-enhanced aerated lagoon ● ● ●  ● ●  ● 
Case study 3: Stormwater basin ● ● ● ●  ● ●  
Case study 4: Constructed wetland ● ●   ● ● ● ● 
Sub-modelInfluent modelHydraulic balanceSegregating water column and sediment layerLayered sedimentation (1D Flux)Biofilm modelBiokinetic modelPhotosynthesis and/or light availabilityAeration, gas transfer
Case study 1a: Aerated lagoon      ●   
Case study 1b: Aerated lagoons ● ● ●   ● ● ● 
Case study 2: Biofilm-enhanced aerated lagoon ● ● ●  ● ●  ● 
Case study 3: Stormwater basin ● ● ● ●  ● ●  
Case study 4: Constructed wetland ● ●   ● ● ● ● 

aEckenfelder equation prescribed for design by the environmental regulator.

bSUMO™ model.

Most of the sub-models listed in Table 3 are available, in some form, within commercial simulation software packages similar to those used in case studies 1–4. Descriptions of most of these sub-models can be found in the literature, such as influent sub-model (Rieger et al. 2012), layered sedimentation sub-model model (Takács et al. 1991; Torfs et al. 2016), sub-model to segregate water column and sediment (Houweling et al. 2008; Hoque et al. 2014; Ho et al. 2018), biofilm sub-model (Wanner & Gujer 1986; Takács et al. 2007), biokinetic sub-model (Henze et al. 2000), algal growth sub-model (Wágner et al. 2016; Casagli et al. 2021), pH sub-model (Fairlamb et al. 2003; Batstone & Flores-Alsina 2022), and aeration sub-models (Bencsik et al. 2022).

The NBS categories and sub-models are not limited to those listed in Table 3; therefore, the proposed framework should be extended in both NBS categories and sub-models. The extended framework detailed in Table 4 provides information on which sub-models should be included based on NBS categories. Except for the non-ideal hydraulic flow and the water chemistry sub-models, all sub-models included in Tables 4 and 5 were used in the four case studies. Other sub-models, such as a heat balance or a chemical precipitation sub-model, should eventually be included. These sub-models were not yet included because the main objective is to present how the framework can be generalized from case studies. The authors' opinion is that the framework could be further extended in future studies as new case studies are included.

Table 4

Sub-model requirements according to NBS categories

Sub-modelInfluent modelHydraulic balanceSegregating water column and sediment layerLayered sedimentation (1D flux)Biofilm modelBiokinetic modelPhotosynthesis and/or light availabilityGas transfer, aerationNon-ideal hydraulic flow model (e.g., Compartmentalization, CFD)Water chemistry/pH
Surface flow wetlands* ● ● ○ ○ ○ ● ○ ○ ○ ○ 
Subsurface flow wetlands ○ ● ○  ○ ●   ○ ○ 
Lagoon/ponds* ● ● ● ○ ○ ● ○ ○ ○ ○ 
Streams ○ ● ○ ○  ○ ○ ○ ● ○ 
Hydroponics and aquaponics ○ ●   ○ ○ ● ●  ○ 
Infiltration systems ○ ●    ○   ○  
Building-based systems (living walls etc.)  ●   ○      
Zero-discharge willow systems (Water evaporates or is used in plant growth)  ●      ○   
Sub-modelInfluent modelHydraulic balanceSegregating water column and sediment layerLayered sedimentation (1D flux)Biofilm modelBiokinetic modelPhotosynthesis and/or light availabilityGas transfer, aerationNon-ideal hydraulic flow model (e.g., Compartmentalization, CFD)Water chemistry/pH
Surface flow wetlands* ● ● ○ ○ ○ ● ○ ○ ○ ○ 
Subsurface flow wetlands ○ ● ○  ○ ●   ○ ○ 
Lagoon/ponds* ● ● ● ○ ○ ● ○ ○ ○ ○ 
Streams ○ ● ○ ○  ○ ○ ○ ● ○ 
Hydroponics and aquaponics ○ ●   ○ ○ ● ●  ○ 
Infiltration systems ○ ●    ○   ○  
Building-based systems (living walls etc.)  ●   ○      
Zero-discharge willow systems (Water evaporates or is used in plant growth)  ●      ○   

● denotes required; ○ denotes it may be required; empty box denotes not required or atypical cases.

*Use case from Table 3.

Table 5

Sub-model requirements according to NBS use cases

Sub-modelInfluent modelHydraulic balanceSegregating water column and sediment layerLayered sedimentation (1D flux)Biofilm modelBiokinetic modelPhotosynthesis and/or light availabilityGas transfer, zerationNon-ideal hydraulic flow model (e.g., Compartmentalization, CFD)Water chemistry/pH
BOD and TSS* ● ● ● ○ ○ ●  ●   
Nitrification ● ● ●  ○ ●  ●   
Nutrient removal ● ● ●  ○ ●  ●   
Resource recovery ● ● ○ ○ ○ ○ ○ ○  ● 
Surface water rehabilitation* ● ● ○ ○ ○ ● ● ○  ○ 
Pathogen removal*  ● ○ ○  ● ○    
Micropollutant removal ● ● ○ ○ ○ ○ ○ ○  ○ 
Sludge handling ○ ● ● ○  ○  ○  ○ 
Odour control ● ● ○ ○ ○ ●  ● ○ ● 
Irrigation ○ ●         
Water harvesting  ●         
Flow equalization  ●         
Groundwater recharge ○ ●        ○ 
Sub-modelInfluent modelHydraulic balanceSegregating water column and sediment layerLayered sedimentation (1D flux)Biofilm modelBiokinetic modelPhotosynthesis and/or light availabilityGas transfer, zerationNon-ideal hydraulic flow model (e.g., Compartmentalization, CFD)Water chemistry/pH
BOD and TSS* ● ● ● ○ ○ ●  ●   
Nitrification ● ● ●  ○ ●  ●   
Nutrient removal ● ● ●  ○ ●  ●   
Resource recovery ● ● ○ ○ ○ ○ ○ ○  ● 
Surface water rehabilitation* ● ● ○ ○ ○ ● ● ○  ○ 
Pathogen removal*  ● ○ ○  ● ○    
Micropollutant removal ● ● ○ ○ ○ ○ ○ ○  ○ 
Sludge handling ○ ● ● ○  ○  ○  ○ 
Odour control ● ● ○ ○ ○ ●  ● ○ ● 
Irrigation ○ ●         
Water harvesting  ●         
Flow equalization  ●         
Groundwater recharge ○ ●        ○ 

● denotes required; ○ denotes it may be required; empty box denotes not required or atypical cases.

*Use case from Table 3.

During the brainstorming session, workshop participants found it more instructive to consider sub-model requirements through the perspective of use cases. For instance, when modelling a waste stabilization pond, the relevant sub-models may vary significantly based on the use case being considered, such as (a) reusing the effluent for irrigation or (b) estimating capacity and planning desludging events. In scenario (a), specific hydraulic sub-models may be necessary to address storage volumes, effluent pumping, and minimum drawdowns. In contrast, for scenario (b), the focus may shift more towards influent loading and fractionation. Table 5 developed an alternative perspective on the framework by using use cases instead of NBS categories.

The cells in Table 4 corresponding to NBS categories (such as surface flow wetland and lagoon) were typically populated based on a logical idea. A black dot (●) in a cell indicates that most of the study cases utilize the sub-model; a blank dot (○) indicates that at least one of the study cases uses the sub-model; and empty boxes signify that none of the study cases employ a particular sub-model. The same logic was applied to Table 5.

The methodology proposed for developing the framework mirrors the scientific method in modelling: project definition and data collection, setting up a plant model, and then calibrating and validating the model, as represented in Figure 14. It is suggested that the sub-model structure be set up first based on NBS categories (Tables 3 and 4), and then modifications be made based on the required sub-models for specific use cases (Table 5). Based on this proposed methodology, for example, sub-models for segregating water column and sediment layer should be considered usually required (●) in a lagoon and pond model (Table 4). However, in use cases where there is a focus on pathogen removal, such sub-models may not be required (○). Similarly, in modelling a lagoon or pond, sub-models for water chemistry/pH may not be necessary (○). Yet, in a use case focusing on odour control, such sub-models should be considered usually required (●) (Table 5).
Figure 14

Methodology for framework development by identifying NBS modelling requirements.

Figure 14

Methodology for framework development by identifying NBS modelling requirements.

Close modal

Each sub-model that is usually required (●) or that may be required (○) to model a specific NBS category or use case was deduced based on the authors' opinion. The authors hope that this framework may serve as a guide for NBS practitioners and software developers in the future. These frameworks overall provide a lookup tool to enable practitioners and researchers to get started pre-selecting sub-models according to the system or use case.

The recommended approach for modelling NBS systems emphasizes the importance of seeking the simplest model that adequately addresses the specific problem at hand. The decision-making process for modelling NBS systems involves several steps, each dedicated to determining specific aspects of the model.

The initial step entails establishing the project definition and collecting data for representation in NBS modelling within a specific time frame. For example, when modelling sludge accumulation in ALs, the process unfolds over many years in response to the accumulation of organic and inorganic materials. This longer-term perspective may overlook short-duration phenomena, highlighting the need for long-term data collection and representation. Conversely, phenomena like the resuspension of sediments can impact nitrification performance (as seen in case study 2) and affect water quality within hours or days. This necessitates detailed modelling and more accurate short-term data collection.

The next step is a pivotal aspect of the decision-making process, involving the identification of components and processes to include in the model and those to exclude. Through a series of case studies, this article developed a framework for identifying the sub-models required to simulate a broad range of NBS technologies. A set of tables is presented to identify necessary sub-models based on NBS categories or use cases. Most sub-models are available in simulation software process unit libraries and can be referenced in scientific literature. The demonstration illustrated how combining readily available process units in software can lead to an adequate simulation of NBS technologies that are not explicitly modelled. This is important due to the tremendous variety of NBS technologies and use cases, coupled with the relative scarcity of process models dedicated to them. An example of the utility of this article is demonstrated when setting up the sub-models' structure for a specific NBS so that it aligns with a given column in Table 4 or 5. This exemplifies the practical utility of the framework in aligning specific NBS instances with appropriate modelling components. After establishing the model variables and reactions, the final decision can be made, with a focus on determining the boundary conditions for the model.

In moving forward, it is crucial to rephrase challenges as opportunities. Models, while not necessarily filling gaps in missing data, exhibit the capacity to identify reasonable ranges and sensitivities. Rather than viewing the absence of inputs as a challenge, the focus shifts to the potential for model sensitivity analysis to reveal which input is significant. These insights present opportunities for revisiting and refining conclusions, fostering a continuous improvement cycle in NBS modelling.

The work of A.R.D.T., Y.C., and P.A.V. was supported by the FRQNT projet d’équipe ‘Étangs aérés facultatifs: modélisation de la matière organique (DBO5, boues, algues) et de l'azote pour prédire et assurer leur performance toute l'année, et réviser le guide de conception’. The work of P.A.V. and J.-M.P. was further supported by the NSERC Discovery Grant RGPIN-2021-04347 ‘Towards digital twin-based control of water resource recovery facilities – Methods supporting the use of adaptive hybrid digital twins’.

All relevant data are included in the paper or its Supplementary Information.

The authors declare there is no conflict.

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