Fats, oil and grease (FOG) deposits in sewer systems are responsible for approximately 25% of all annual line blockages in the United States and lead to the release of 3–10 million gallons of untreated wastewater to the surrounding environment. Considerable effort has been made to maintain the conveyance of wastewater by cleaning pipes that have a significant FOG deposit accumulation. Changes in the urban landscape from the addition or deletion of food service establishments (FSEs), however, may pose challenges in determining the location of these high accumulation zones. This research focuses on the development of a sewer collection system model that predicts high FOG deposit accumulation zones. Two collection systems were simulated to test the prediction capabilities of the tool and to assess how changes in the urban landscape affect the location of these accumulation zones. The numerical tool incorporates a mechanistic-based FOG deposit formation kinetic model. Results showed that the model predicts about 65% of the reported high FOG deposit accumulating zones. Simulations also showed significant changes in the location of these high FOG deposit accumulating zones from changes in the number and locations of FSEs and from FSE discharge and background wastewater flow variations.
The detrimental effects of fats, oil and grease (FOG) deposits on sewer collection systems have been documented extensively. The EPA estimated that there are approximately 23,000 to 75,000 sanitary sewer overflows (SSOs) in the United States each year (US EPA 2004). Of these large numbers of SSOs, 47% of those that were caused by line blockages were associated with FOG accumulation in sewer lines (US EPA 2012). In a recent Australian study, one water utility company reported that 21% of all blockages were primarily due to FOG deposit accumulation (Mattsson et al. 2014).
FOG wastes are primarily composed of triglycerides, i.e., esters of glycerol and fatty acids, and are generated at food service establishments (FSEs) as by-products of food preparation activities (Williams et al. 2012). In addition to FSEs, a significant contribution to FOG production may come from residential sources, specifically in areas with high population densities (Ducoste et al. 2009).
Since a major source of FOG is FSEs, the presence of FSEs at different locations may increase the risk of FOG deposit accumulation and the subsequent SSO if no maintenance is performed. The extent of FOG deposit accumulation within the collection system can vary spatially and depends on many factors, including but not limited to pipe structural condition, pipe deformation, accumulation of debris or root intrusion (Marlow et al. 2010; Dominic et al. 2013), partial or inadequate flows (Marlow et al. 2010), location and density of FSEs, multifamily dwellings and high rise buildings (Gray 2002; Mattsson et al. 2014), and corresponding kitchen practices and poorly maintained grease interceptors (Williams et al. 2012). To prevent excessive FOG deposits' accumulation and subsequent SSOs, pretreatment managers perform routine maintenance by identifying locations with high rates of FOG deposit accumulation and using high pressure jets to clean the partially clogged pipe segments. While pretreatment managers may be aware of current maintenance requirements of an existing sewer system, the spatial distribution of FOG deposits may change due to the changing urban landscape (i.e., changes in the number and location of FSEs) caused by ongoing revitalization of many urban centers across the United States. Prediction of the new high FOG deposit accumulation zones would require a model that simulates the transport of wastewater and the reaction process that describes how FOG deposits are formed.
Research studies have shown that FOG wastes may undergo alkali-driven hydrolysis which results in the production of free fatty acids (FFA) (Iasmin et al. 2014, 2016). Fatty acids, which are a major constituent of edible oils and fats (Ma & Hanna 1999; Canakci 2007; Williams et al. 2012), may also be released as a result of cooking processes (Canakci 2007) or microbial activity (Brooksbank et al. 2007).
Hydrolysis is the precursor of a saponification reaction by which FOG deposits are formed (He et al. 2011, 2013; Iasmin et al. 2014). Iasmin et al. (2016) proposed a mechanistic model that included alkali-driven hydrolysis of triglyceride based on mass action principles and were able to predict changes in the rate of formation of saponified solids under different experimental conditions. They studied the kinetics of FOG deposits' formation for two types of fat and two types of calcium sources under three pH and two temperature conditions. In their work, an aqueous solution of calcium chloride/calcium sulfate was prepared and brought down to room temperature (22–25 °C). The liquid/melted-solid fat (canola or beef tallow) was then added to the aqueous calcium solution and mixed for 8 hours under different pH (7 ± 0.5, 10 ± 0.5, and ≈14) and temperature conditions (25 and 45 °C). Samples were collected at specific intervals and analyzed with Fourier transform infrared spectrometer for their spectral data. The experimental data were then compared to mechanistic and empirical models.
where kT = reaction rate constant for the hydrolysis of triglyceride (L3 mol−3 hr−1), ks = reaction rate constant for saponification of FFA and Ca2+ (L2 mol−2 hr−1), and kd= reaction rate constant for breakdown and/or dissolution (solid phase to liquid phase) of the saponified solids (hr−1).
Although the model described by Iasmin et al. (2016) was based on reactions between pure fats and calcium in the background wastewater (BGWW), it does provide an initial framework that could be used in a system-wide description of the sewer collection system. What is still missing, however, is a description of accumulating solids in any particular sewer pipe section.
In rheological experiments performed by Iasmin et al. (2014) on FOG deposits and calcium-based fatty acid salts, results showed that both calcium-based fatty acid salts and FOG deposits displayed rigid stability indicating their limited flow properties when adhered to the sewer wall. Keener et al. (2008) and He et al. (2011) showed that FOG deposits also demonstrated adhesive characteristics and can become securely bound to the interior pipe wall. The results of Keener et al. (2008), He et al. (2013), and Iasmin et al. (2014), clearly showed that FOG deposits, whether formed in the wastewater bulk solution or directly on the pipe wall, can accumulate along the pipe surface due to their rheological properties. Consequently, a mechanism must be developed that describes the FOG deposit adhesion process.
This research presents a model that describes the fate and transport of FOG deposits and their intermediates through the sewer collection system. To the authors' knowledge, no previous research on modeling FOG deposit accumulation in a system-wide sewer collection model has been performed. The model uses CITY DRAIN 2.0.3 (Achleitner et al. 2007; Achleitner 2008), which is an open-source software integrated within MATLAB/Simulink, that monitors the locations with the highest rate of FOG deposits' accumulation at the pipe wall. These locations are addressed as ‘hotspots’ throughout this study and represent the highest risk of an SSO occurrence due to FOG deposit accumulation. The purpose of this model is to investigate the potential impact of changes in the number and location of FSEs on the predicted locations of hotpots. The goal of this research and model is to develop a predictive tool that pretreatment managers could use to assess future sewer maintenance requirements with respect to high FOG deposit accumulating pipe segments.
CITYDRAIN 2.0.3 was used to model the sanitary sewer collection system. The graphical interface of CITYDRAIN includes various blocks representing straight pipes, mixers, and separators that make the user able to construct a model of an urban drainage system block by block.
Muskingum's method of flood routing
Transport and kinetics of FOG deposit formation
It was assumed that the solids, Sw, will occupy the interior pipe volume associated with the pipe segment. Therefore, the final wall solids accumulated in any pipe segment was computed by multiplying Sw by the ratio of storage volume, V, divided by the pipe segment volume.
Sewer collection system case studies
The formation of FOG deposits was simulated for two sewer collection systems: one in the North East USA and designated as NE, the other in the South West USA and designated as SW. The NE municipality provided information on locations of local restaurants in 2009, average monthly flow rate of wastewater for the duration of two years, geographical information system (GIS) data of the sewer collection system, and a map of reported high FOG deposit accumulation zones that were determined from visual observations. Since FSEs may open and/or go out of business frequently, the geographical data of all FSEs that have been in operation in 2009 were updated. Google map data were used to verify that the FSEs were still in operation. If the FSE was no longer in operation, it was deleted from the list. On the other hand, Google and Google map data were used to add additional FSEs that started operating after 2009 to 2012 (the year this research was performed) to the list. The list of FSE reported in 2009 was called ‘current FSEs’ since the simulation was performed with the data corresponding to year 2009. The map of additional FSEs added after 2009 to the year this research was done (year: 2012) was called ‘new FSEs’. For both current FSE and new FSE scenarios, geographical latitude and longitude of every FSE location were extracted and incorporated into GIS maps.
For the SW model, a map of the urban drainage system containing wastewater flow pattern, locations of FSEs as of 2009, and information on how frequent different pipe segments were cleaned were provided by the SW municipality. Since the information on when FSEs were in operation in different years was not available for the SW collection system nor was there information about where to add commercial establishments in regions of the collection system that may be zoned for those additions, the new FSEs scenario for SW was defined by randomly reducing the number of current FSEs to half of its original number. A real-world example for this case may be when FSEs have gone out of business and therefore do not discharge FOG waste.
FOG deposit formation happens over a three-month to two-year period (Keener et al. 2008). However, a 7-day period with 300 seconds interval was chosen to reduce the overall model simulation time.
The wastewater was divided into two major streams for both NE and SW models: BGWW, which represents typical domestic wastewater and contains insignificant FOG concentration, and FSE wastewater (FSE WW) representing the effluent of the grease interceptor from an FSE facility with 200 ppm triglyceride. The calcium concentration was assumed to be identical for both BGWW and FSE wastewater streams and was chosen to be 50 ppm.
For both NE and SW models, the FSE WW flow rate is 6.31 × 10−4 m3/s (10 gal/min), which was taken from a cumulative distribution function for FSE flows at 95% less than the value in Aziz et al. (2012).
The NE BGWW flow rate (0.1503 m3/s) was adjusted such that the sum of the BGWW and FSE wastewater flow rate would be equal to the annual average flow provided by the municipality. Assuming a pipe diameter of 0.381 m (equals 15 inches, a frequently used diameter for sewer pipes), the scour velocity for NE sewer collection pipes would be more than 0.762 m/s (2.5 ft/s). This 0.762 m/s (2.5 ft/s) value is the recommended minimum scour velocity used by the wastewater industry to avoid debris deposition in sewer pipes. The SW BGWW flow rate, 0.026 m3/s, was calculated using Manning's equation, a pipe scour velocity greater than 0.762 m/s and a sewer pipe diameter of 0.381 m.
Both NE and SW are local city municipalities with separated sewers. NE has an approximate per capita flow of 4 × 10−6 m3/s (about 90 gallon per day per capita) while SW has about 3 × 10−6 m3/s (approximately 70 gallon per day per capita). This flow corresponds to the section of the collection system that was modeled.
Determining hotspots and model calibration
Hotspots were defined as locations in the urban drainage system where there is a high rate of FOG deposits' accumulation, and consequently, a potential for an SSO occurrence. The rate of FOG deposits' accumulation was computed based on the time rate of change in the FOG deposit concentration at the wall.
Model calibration was performed by adjusting the saponification reaction rate constants (kTri, kSAP, and kAGG) such that the model's rate of saponified solids' formation at the wall coincides with sewer system pipe locations where there are high FOG deposit accumulation zones from visual observation or where a high frequency of maintenance was reported by the municipality. A Monte Carlo sampling approach consisting of drawing a random value from a defined probability distribution for all model inputs was performed in this study. A range of values was provided for each rate constant in the saponification model assuming a log normal distribution with an assigned mean value and variance. Initial ranges used for these rate constants were 2.86 × 10−4 ± 3.54 × 10−4 for KTri, 3.82 × 10−4 ± 6.31 × 10−4 for KSAP, and 2.99 × 10−4 ± 5.31 × 10−4 for KAGG. Wider ranges (50% increase) were also examined and no significant improvement (i.e., less than 5%) in the fitted constants was noted. The equations used to generate the random samples for each distribution are defined in Morgan & Henrion (1990) and are based on the method of inverting the cumulative distribution function (Papoulis 1991). For a 95% confidence interval with a 10% maximum error on the mean value estimate, more than 96 runs should be conducted (Hogg & Tanis 1993). Ninety-eight sets of rate constants, one for each input (kTri, kSAP, and kAGG), were randomly generated. The three models were simulated with these 98 rate constant scenarios and the rate of change of FOG deposit accumulation at the wall was calculated for each monitoring point in the sewer collection system. The points with the highest rate of FOG accumulation, which consisted of the top 20% of all monitoring, were compared to pipe segments that were reported to have high FOG deposit accumulation from visual inspection or that required a high frequency of cleaning to remove FOG deposit accumulation.
Twenty percent provided enough locations to compare with the data provided by each of the two sewer collection systems. Higher percentages did not change the performance of the model since 20% covered all the problem areas reported by the two municipalities in the section of the collection system simulated.
A sensitivity analysis was performed using the data generated from the Monte Carlo statistical method presented in the previous section to investigate the sensitivity of hotspot locations on the selection of kTri, kSAP, and kAGG. The results of each scenario were then analyzed using Spearman rank correlation to determine the sensitivity of the hotspots to these three rate constants.
Since microbially induced concrete corrosion (MICC) has been recently identified as a potential pathway to FOG deposit formation (He et al. 2013) by releasing significant amounts of calcium, a sensitivity analysis was also performed using 98 randomized values for calcium concentration in FSE wastewater. The values ranged from 50 to 100 ppm. This analysis may show how different rates of MICC at different locations throughout the collection system could impact FOG deposit formation.
Effect of flow variation
For the FSE flow, a peak factor of 6.2 was calculated according to Aziz et al. (2012). The minimum flow was assumed to be zero (Aziz et al. 2012) since there is no FOG waste produced during the times that FSEs are closed (1:00 a.m. to 9:15 a.m.). There are three peak times during the activity of the FSEs: (i) around lunch time (11:30 a.m. to 12:30 p.m.), (ii) around dinner time (8:30 p.m. to 9:30 p.m.), and (iii) when cleaning activities are being performed before closing time (12:00 a.m. to 1:00 a.m.) (Aziz et al. 2012). The FSE flow at all other times was adjusted such that the average flow would match the average value of 6.31 × 10−4 m3/s (10 gal/min).
For NE BGWW, the peak and minimum flow factors were calculated to be 3.5 and 0.3, respectively, based on city population (Qasim 1998). Similarly for the SW BGWW, the peak and minimum flow factors were 2.5 and 0.4, respectively (Qasim 1998). Generally, low municipal wastewater flows occur at night with peak flows during morning and evening periods (Butler & Davies 2004).
RESULTS AND DISCUSSION
The model also predicted hotspot locations that were not reported by the municipality (circles with triangle in Figures 1 and 2), as well as not predicted zones of FOG deposit accumulation that were reported by the municipality (black circles in Figures 1 and 2). The inability of models to predict hotspots reported by the municipality can be due to a number of factors. Pipe deformations such as pipe sags have been shown to preferentially accumulate FOG deposits due to the low flow conditions in the deformed pipe segment (Dominic et al. 2013). Low flow conditions will reduce the ability to wash out any accumulated FOG and transport it further downstream beyond the sag location, thus increasing the possibility of a saponification reaction or attachment to the pipe wall at the pipe sag location (Dominic et al. 2013). Another possible location for FOG deposits' accumulation is where roots intrude into the pipe and obstruct the cross-sectional area (Dominic et al. 2013). The tendency of FOG deposits to accumulate on roots is due to the higher surface area provided by the roots (Dominic et al. 2013) or the occurrence of preferential accumulation of FOG by the roots (Ducoste et al. 2009). Other locations where FOG and FOG deposits may accumulate include wet wells and pump stations (Cox & Cox 2009).
In this research, only non-residential FOG producers were considered. Residential dwellings, specifically in densely populated areas, may have a substantial contribution to producing FOG considering the cooking processes in household kitchens (Ducoste et al. 2009). FOG produced and released to the sewer system by residential contributors can significantly modify wastewater quality and thus change the location of hotspots. The model also assumes that FOG waste released by all FSEs has the same characteristics. Iasmin et al. (2014) have shown that different oil types will result in different FOG deposit formation rates. They also showed that pH and temperature have a significant influence on the kinetics of FOG deposit formation. In addition, commercial detergents used by FSEs as well as household detergents used by residential communities have been shown to increase the FOG deposit formation rate and quantity due to pH effects as well as surfactants found in these detergents (Iasmin 2014). As discussed in He et al. (2013) and Iasmin et al. (2014), the extent of concrete corrosion can impact the amount of calcium leaching, which will also have a considerable effect on the saponification rate, especially in older sewer collection systems where corrosion and calcium leaching is of higher concern. Thus, identifying the locations with higher rates of concrete corrosion may improve the accuracy of the model.
Impact of changes in simulation and Muskingum parameters
As mentioned in the Methods section, the corresponding values for , X, and in the Muskingum method were 300 seconds, 0.1, and 300 seconds, respectively. Simulations were performed with an increased number of subreaches (i.e., n = 4, 5, and 6) and reduction in , X, and values (i.e., 10 and 20% reduction).
For FOG deposit formation period and time steps, simulations of longer than a 7-day period and/or different time steps than 300 seconds displayed no change in the predicted pipe segments with high FOG deposit accumulation rates. Longer simulation periods only changed the amount of FOG deposit accumulation at these high accumulated pipe segments.
Impact of changes in urban landscape
Effect of flow variation
The initial simulations were performed under steady flow conditions. Wastewater discharge may vary depending on the time period of the day. Wastewater from FSEs is also subject to wide fluctuations over time (Aziz et al. 2012). To investigate the influence of transient flow variation, both NE and SW models were simulated with varying FSEWW discharge and BGWW flow patterns (as described in the Methods section) using the calibrated rate constants. Table 1 displays the results in terms of the number of hotspot locations that changed from introducing flow variation.
|.||Current FSES .||New (increased) FSEs .||Current FSES (30 FSEs) .||Eliminated FSEs (15 FSEs) .|
|Variable BGWW flow||0||0||6||5|
|Variable FSE WW||1||3||6||6|
|Variable BG and FSE WW||1||2||6||5|
|.||Current FSES .||New (increased) FSEs .||Current FSES (30 FSEs) .||Eliminated FSEs (15 FSEs) .|
|Variable BGWW flow||0||0||6||5|
|Variable FSE WW||1||3||6||6|
|Variable BG and FSE WW||1||2||6||5|
The modifications in the number of hotspots suggest that the sewer collection system model should include flow variability to completely predict the spatial distribution of locations where there are high risks of FOG deposit accumulation. The effect of these variations may be more significant if seasonal changes are included due to higher peaks and lower minimums.
The impact of flow variation was more significant on the SW collection system compared to the NE collection system. The increased sensitivity to flow variation was due to the difference in the relative distance between the FSEs and the high FOG deposit accumulation zones in SW compared to NE collection systems. For both current and new FSEs in the NE collection system, the majority of the high FOG deposit accumulation zones occur in an area with several FSEs. Many of the new FSEs were also located in this same region and therefore their additional FOG discharge did not change the FOG deposit accumulation location but did change the rate of formation. In the SW collection system, the FSEs and the resulting hotspots are more widely spread out and hence, the result of variable flow was more significant. However, for both current and eliminated FSEs scenarios in the SW collection system, all six locations of hotspots for each variable flow condition are the same. These SW collection system results suggest that SW may also have an apparent bottleneck location that funnels much of the FOG deposit formation precursors into a specific location.
Sensitivity analysis of FOG deposit formation rate constants and calcium concentration
The results of each scenario from the Monte Carlo approach for NE and SW sewer systems were analyzed using Spearman's rank correlation. Figures S1 to S23 and Tables S1 to S23 in the Supplementary material (available with the online version of this paper) display the distribution and statistical analysis of the variation in the NE collection system, respectively. For both collection systems, the analysis showed that the rate of change of saponified solid accumulation is sensitive to all three rate constants; kTri, kSAP, and kAGG, with the greatest sensitivity to kTri, the rate of FOG hydrolysis, followed by kSAP and kAGG. For the NE collection system with the 2009 FSEs (current FSEs), the correlation coefficients were in the following ranges: 0.1663 to 0.9531 for kTri, 0.04806 to 0.8662 for kSAP, and −0.0719 to 0.3168 for kAGG. For the SW collection system, kTri, kSAP, and kAGG were in the range of 0.3414 to 0.8307. The results in Tables S1 to S23 show that all monitored locations are sensitive to the rate constant values with coefficient of variations all higher than 0.4. The distributions of these wall FOG deposit accumulation rates shown in Figures S1 to S23 are primarily skewed to the right, which is similar to the shape of the rate constant distributions. Locations in the sewer collection system with the greatest impact coincided with regions near one of the pump stations in the collection system that pumps the sewer to the treatment plant. One possible reason for the greatest sensitivity to these rate constants in those regions is higher available concentrations of FOG since different pipes connect to a larger inflow pipe to the pump station. This region is also downstream of several FSEs where FOG has had sufficient time to hydrolyze and react with calcium to form deposits.
These results suggest that limiting FOG hydrolysis and the conditions that promote the saponification reaction will have a significant impact on FOG deposit accumulation in the sewer collection system. From a practical standpoint, the mitigation of FOG hydrolysis may be challenging since there may be several pathways that lead to the breakdown of FOG. However, limiting the saponification reaction could be achieved with effective removal of long chain FFA or directing these long chain FFA to undergo alternative chemical reactions so that they are unavailable to react with Ca. Future research should be performed to investigate alternative reactions with long chain FFA or for improving the separation performance of grease interceptors for the removal of FOG and long chain FFA.
The NE collection system model was simulated with 98 different calcium concentrations of FSE wastewater ranging from 50 to 100 ppm, and using the calibrated rate constants. The results were then compared with prior NE collection system simulations with FSE wastewater containing 50 ppm of calcium. Tables S24 to S44 in the Supplementary material (available with the online version of this paper) display the statistical analysis of the locations in the sewer collection system. The results of this sensitivity analysis showed that the locations of hotspots did not significantly change with the different amounts of calcium in FSE wastewater. As noted by the low coefficient of variation in Tables S24 to S44, the FOG deposit accumulation rates at the wall did not change significantly over the range of calcium concentration simulated. The results of this sensitivity analysis showed that the locations of hotspots did not significantly change with the different amounts of calcium in FSE wastewater. The present model, however, does not capture some of the mechanisms leading to the accumulation of calcium in FOG deposits, i.e., the potential accumulation of calcium in the deposits due to Derjaguin-Landau-Verwey-Overbeek (DLVO) interaction. During saponification, unreacted FFA may be attracted to the saponified solids and be incorporated in the solid matrix. These unreacted FFA likely draw calcium and other cations toward the solid core matrix based on the effects of van der Waals attraction and electrostatic repulsion (i.e., DLVO theory) (He et al. 2011, 2013). Another group of researchers suggested that biocalcification may be an alternative mechanism that leads to high calcium levels in FOG deposit samples (Williams et al. 2012.) Overall, more measurements and research are needed to prove these different hypotheses.
The wastewater collection systems of two cities in the USA (NE and SW) were modeled and simulated using CITYDRAIN 2.0.3, a MATLAB Simulink model to help assess changes in the wastewater quality in the sewer system due to changes in the urban landscape. Simulations focused on the changes in the quality of wastewater made by the discharge of FOG into the sewers from FSEs. Results of these simulations suggested that a sewer collection system model that incorporates the kinetics and transport FOG chemicals and saponification reactions has the potential to predict many of the FOG deposit accumulating hotspots for a given sewer collection system. While the models were able to demonstrate the impact of spatial changes in the discharge from FSEs on pipe segments with high FOG deposit accumulation, the models did not include important engineering aspects that could influence the outcome of the model predictions. As previously mentioned, pipe deformations such as pipe sags can exacerbate the accumulation of debris including the accumulation of FOG deposits (Dominic et al. 2013). The occurrence of pipe sags may be more prevalent in older sewer collection systems. These Simulink simulations could be enhanced if the hydraulics of these pipe sags were included, where known, in sewer systems. The NE sewer collection system is an older sewer pipe network that contains a significant number of pipe sags where FOG deposit accumulation has been observed. It is possible that unique hydraulic characteristics of these pipe sags could be contributing to the accumulation of FOG deposits and may help explain some of the deviations between the model predictions and the visual observations of FOG deposits' accumulation zones.
In addition, it is likely that different FSEs (i.e., type of restaurant, coffee shop, bakery, etc.) release their wastewater with different FOG and FFA concentrations into the sewer collection system. This concentration variation may occur over hours to days. The current model simulation did not include the impact of spatial concentration discharge variation among the different FSEs in the collection system. Further, the model also did not account for the FSEs to discharge an initial concentration of long chain FFAs. All FFAs produced in the sewer collection system resulted from FOG hydrolysis after FOG discharge from the FSE. To improve the model performance, knowledge of these dynamic changes in FSE wastewater concentration will be important.
Finally, the contribution of non-restaurant and non-fast food FSEs was not considered in the present model. Bakeries, creameries, bars, and coffee shops are just a few other FSEs producing FOG daily. Residential areas are another potential FOG producer and unlike FSEs, are not regulated for discharging waste water containing FOG. By incorporating the above-mentioned missing items into future model development, the results would assist pretreatment managers to plan their future routine maintenances more efficiently, with greater reliability in the model accounting for more existing conditions.
As the urban landscape continues to change with the revitalization of major metropolitan cities, this analysis could be helpful to assess changes in wastewater quality in the sewer system. These hotspot predictions can be performed for any sewer collection system if the necessary GIS data are provided. Predictions from a sewer collection system model that includes FOG deposit formation kinetics will help assist pretreatment coordinators to plan periodic maintenance schedules and avert detrimental FOG deposit-related SSOs.
We would like to thank the United States Environmental Protection Agency (EPA STAR grant: 83426401) for funding this research.