This paper aims to develop and validate an analytical equation to predict the concentration of residual chlorine exiting a typical pipe junction. In order to investigate the trend of the incoming flow rates before leaving the junction, experiments with inflow rates (North and West) ranging from 0.18 to 2.17 L/s, Reynolds numbers ranging from 14,324 to 110,780, and free chlorine concentrations ranging from 0.5 to 1.80 mg/L were performed. The results showed that flows tend to bifurcate rather than mix completely, and the bifurcation and mixing depend mainly on the relative flow rates entering the cross junction. Based on the experimental results, a dimensionless concentration (R) was estimated, allowing for predicting chlorine at the East outlet. Then, a solute mass balance was also performed within the cross junction to predict chlorine concentration at the South outlet. Finally, an adjustment of the R-value was performed by using 3D computational fluid dynamics (CFD), and the analytical equations were also validated with simulations. The standard k–ε turbulence model with enhanced wall treatment for modeling turbulence and near-wall effects, respectively, were used. More mixing models will improve water quality simulations to ensure proper control of chlorine and possible contaminants in water distribution systems.

  • Development of analytical equations to predict chlorine concentration of flow that exits cross junctions.

Graphical Abstract

Graphical Abstract
Graphical Abstract

Numerical modeling is a fundamental tool in managing water quality in the distribution network. One of its immediate advantages is that it can provide information on the behavior of water quality parameters in the whole network. Therefore, water utility operators can take safety measures to ensure better water management, and also make it possible to verify the extent to which water quality standards are maintained in the distribution network.

The transport and diffusion of water quality parameters within a network depend primarily on the hydraulic operation and the mixing phenomenon at cross junctions where different incoming flows and concentrations may exist. A detailed study of the intersection's flow pattern and geometric configuration is essential to understand this phenomenon better.

Many researchers have studied this phenomenon, which plays a vital role in water quality modeling. Their results show that at junctions that receive water from several pipes, the mixing can be considered instantaneous and perfect (Fowler & Jones 1991; Mays 2004). EPANET (Rossman 2000), a public domain, water distribution system modeling software package, assumes complete mixing of a solute such as free chlorine at a pipe junction.

Conversely, many researchers have conducted experiments that proved that the mixing at cross junctions is not perfect (Ho et al. 2007; Austin et al. 2008; Shao et al. 2014). As a result, the concentration of water quality parameters exiting the node in various directions could differ. Ho & O'Rear (2009) found that relative flows in and out of the junction can significantly affect the degree of mixing. Van Bloemen Waanders et al. (2005) emphasized that the flows in cross junctions tend to bifurcate and reflect off one another rather than mix completely.

Diverse other authors carried out experimental and numerical studies through computational fluid dynamics (CFD) using salt tracers (Song et al. 2009; Liu et al. 2011; Shao et al. 2014; Yu et al. 2014; Hernández-Cervantez et al. 2018), dyes (Ho & O'Rear 2009) and chlorine as soluble tracer (Mompremier et al. 2015) for concentration distribution analysis. It has been pointed out that the use of chlorine as solute turns out to be somewhat complicated; however, this is one of the most commonly used methods for water chlorine disinfection in real water distribution networks. Therefore, the result of interest is to address studies using chlorine directly as solute. Santos-Violante et al. (2020) conducted a CFD study in the turbulent regime of mixing phenomena in cross junctions by using chlorine as a solute tracer. They reported a good concordance with experimental measurements of chloride concentrations at the outlets reported by Mompremier et al. (2015).

One of the most critical aspects of the study of mixing at cross junctions is estimating the concentration of solute water that exits the junctions. To achieve this, the development of analytical equations that describe the behavior of flows is crucial. Unfortunately, much research conducted on this phenomenon has not resulted in analytical equations to estimate the chlorine concentration in the node's water.

Romero-Gomez et al. (2006) defined the dimensionless concentration (C*) to describe the degree of mixing using typical cross junctions in which the pipes were labeled as W (West inlet, tracer water with high concentration CW), S (South inlet, clean water with low concentration CS), E (East outlet, concentration CE), and N (North outlet, concentration CN). The analytical equations are described as follows:
(1)
(2)

and are the dimensionless concentrations of the east and North outlets.

Ho & O'Rear (2009) developed a solute mixing model in cross junctions with adjacent inlets and equal pipe sizes (see Figure 1).
Figure 1

Typical cross junction with two inlets and two outlets .

Figure 1

Typical cross junction with two inlets and two outlets .

Close modal
Their results showed that the flow in the pipe with the most significant momentum is assumed to cross over the junction, deflecting the incoming flow from the adjacent inlet. As a result, the solute concentration at the adjacent outlet is equal to the solute concentration in the inlet of the greater flow rate and could be represented by:
(3)
The concentration in outlet pipe 3 is derived by performing a solute mass balance (by assuming constant liquid density) on the entire cross junction:
(4)
where represents the flow rate in the pipe with the most significant momentum, is the solute concentration in the inlet 1, are the flow rate and solute concentration in the inlet 2, respectively. Furthermore, denote flow rate and solute concentration in the outlet 3 (opposite inlet 1), and represent flow rate and solute concentration in the outlet 4. Using Equation (2) in Equation (3) results in the following equation for the solute concentration in outlet pipe 3:
(5)
In other study, a small-scale 3 × 3 pipe network was developed by Ho et al. (2007) to evaluate complete and incomplete mixing models in cross junctions of water-distribution pipe networks. Computational Fluid Dynamics simulations showed that incomplete mixing within cross junctions resulted from the bifurcation of incoming flows and depended mainly on the relative flow rates entering the cross junction. Hernández Cervantez et al. 2021 also proposed analytical equations to estimate chlorine concentration at the East and South outlets of cross junctions based on the following conservation equation:
(6)
in which C and Q denote the concentration and flow, respectively and according to their boundaries N, W, E, and S:
(7)
(8)
The OUT coefficient is the outlet concentrations ratio, i.e.,
(9)

in which, CE and CS are concentrations at the East and South outlets, respectively.

Finally, Mompremier et al. (2017) performed mixing scenarios using chlorine in different cross junction configurations. They investigated different combinations of flows, concentrations and, configurations to assess mixing phenomena at cross junctions. The study also sheds light on how the concentration of microorganism (total coliform and E. coli) can vary greatly in the same water network system due to the impact of the mixing of water with different physicochemical characteristics. The present research aims to determine a dimensionless concentration coefficient R based on experimental data and CFD simulations to develop an analytical equation to predict chlorine concentration in outlet cross junctions. In addition, the predictions of the analytical equation were compared with experimental results and CFD.

In order to formulate analytical equations that predict chlorine concentration in cross junction systems, a series of experiments was carried out in a laboratory network system. The experimental model consisted of a cross junction pipe system with two inlets: North and West, and two outlets: South and East. A schematic diagram of the experimental distribution network is shown in Figure 2. Polyvinylchloride (PVC) pipe material of diameter 32 mm was used. The system also included a water reservoir (4.0 m3 of capacity), two storage tanks (450 L capacity each) at an elevated position for gravity flow, and four flow meters (CZ300 s model Contazara S.A, Spain). The flow meters were located at each inlet and outlet of the cross junction to measure the instantaneous flow rate in the system. Two flow control valves (labeled 1 and 2) were used to change the system's operating conditions; two dosing pumps (BL3-12, HANNA instrument, Mexico) controlled the chlorine concentration released from the storage tank. Finally, a 4HME200 centrifugal pump was used to drive the water from the reservoir to the storage tanks.
Figure 2

Schematic diagram of the experimental distribution network.

Figure 2

Schematic diagram of the experimental distribution network.

Close modal

This study involved a scenario that simulated different inflow rates as water enters the cross junctions. The flows enter the cross junction at 90° (from North and West) and exit at South and East outlets. The principal goal of the experiments was to study the behavior of the incoming flows before leaving the cross junctions. Experiments with varying inflows (ranging from 0.36 to 2.70 L/s at North inlet and 0.18–1.68 L/s at West inlet) and varying chlorine concentrations were carried out. However, ten of them that were found to be more relevant in the context of this investigation are reported in this paper. During the experiments, clean water from the reservoir was pumped to the elevated storage tanks using a 4HME200 centrifugal pump. Sodium hypochlorite solution (at 13%) was added to the West and North storage tanks, which resulted in chlorine concentrations that ranged from 1.25 to 1.80 mg/L at the North inlet and 0.50–1.42 at the West inlet. The solutions in each tank were mixed using a manual mixer. Descriptions of the scenarios in terms of chlorine concentrations and flow rate at inlets are presented in Table 1.

Table 1

Description of scenarios in terms of flow rate and chlorine concentration at the inlets

Q North [L/s]Q West [L/s][mg/L][mg/L]
Experiment 1 0.360 0.180 1.75 0.70 
Experiment 2 0.582 0.360 1.65 0.70 
Experiment 3 0.840 0.420 1.75 0.75 
Experiment 4 0.500 0.320 1.25 0.87 
Experiment 5 1.050 0.540 1.80 1.42 
Experiment 6 1.440 0.720 1.65 0.80 
Experiment 7 2.400 1.440 1.25 0.85 
Experiment 8 2.150 1.050 1.75 0.75 
Experiment 9 2.340 1.680 1.55 0.80 
Experiment 10 2.700 1.320 1.39 0.50 
Q North [L/s]Q West [L/s][mg/L][mg/L]
Experiment 1 0.360 0.180 1.75 0.70 
Experiment 2 0.582 0.360 1.65 0.70 
Experiment 3 0.840 0.420 1.75 0.75 
Experiment 4 0.500 0.320 1.25 0.87 
Experiment 5 1.050 0.540 1.80 1.42 
Experiment 6 1.440 0.720 1.65 0.80 
Experiment 7 2.400 1.440 1.25 0.85 
Experiment 8 2.150 1.050 1.75 0.75 
Experiment 9 2.340 1.680 1.55 0.80 
Experiment 10 2.700 1.320 1.39 0.50 

In all the experiments, incoming flow rates and chlorine concentration at the North inlet were higher than in the West pipe. The flow meters measured instantaneous flow rates at each inlet and outlet of the cross junctions. Free chlorine concentrations were also measured at each inlet and outlet. An advanced system (CL763, B&C electronics, Italy) that detects chlorine concentration in the range of 0.1–20 mg/L was installed in the cross junction (at inlets and outlets), designed for continuous inflow measurement of residual chlorine in solution. The collected signals were transferred to a data logger (El-USB-4, Lascar Electronics, USA) connected to each controller and a PC for analysis. Every experiment was repeated twice to obtain the average results.

Estimating dimensionless concentration R and analytical equations

As flows in cross junctions tend to bifurcate and reflect off one another rather than mix completely, in this study where (), a dimensionless R-concentration to predict East-exit chlorine concentration as a function of concentration in the North inlet was calculated:
(10)
in which, and are chlorine concentrations at the East outlet and North inlet, respectively. It is important to note that the R-value is calculated for each experiment, followed by an average of the data to obtain the final value. And the Equation (10) becomes:
(11)
Then, a solute mass balance is performed within the cross junction to obtain the concentration at the South outlet, as follows:
(12)

In which,

The terms on the left-hand side of Equation (12) represent the total mass at inlets ( and Equation (13) becomes:
(13)
where is the total mass of chlorine at North and West inlets.
Finally, the concentration at the South outlet can be expressed as a function of the flow rates of the East and South outlets and the North inlet chlorine concentration.
(14)
For the numerical implementation, first, selecting the solution domain and its discretization is necessary. The geometry and computational mesh of the physical model were generated in the Ansys© 17.1 DesignModeler and Meshing modules, respectively. The origin of the Cartesian coordinates was set at the pipe cross center. The solution domain was chosen to extend from the cross center junction to 4.5 diameters upstream of both inlets (North and West) and 61.125 diameters downstream of the outlets (South and East). This reduced solution domain reduced the computational cost by approximately 46%. The 3D view of the geometry and computational mesh is shown in Figure 3.
Figure 3

3D-view of the geometry and computational mesh near to the cross junction.

Figure 3

3D-view of the geometry and computational mesh near to the cross junction.

Close modal

In simulations, the mesh quality is an important aspect to consider since it determines the accuracy and convergence of the numerical computation. The discretization of the cross-junction volume was done using a mesh with only hexahedral cells, and all employed meshes had a maximum cell skewness of 0.8. Extra refinement was implemented in the near-wall region using the inflation tool incorporated in Ansys©-Meshing to capture detailed current velocity gradients in the wall proximities, as can be seen in Figure 3. The boundary between the different computational regions was conformal, i.e., the grid node location was identical at the boundary. A mesh independence analysis was performed to verify that the numerical results are independent of the mesh density at the highest Reynolds number examined in this study (Re = 110780), resulting in a mesh containing approximately 1,500,000 elements, which can be considered independent. For each computational mesh, the first layer thickness adjacent to the wall along the axial locations was displaced by a value below 1 of the wall function, i.e., Y + <1, for the range of exanimated Reynolds numbers (7380 ≤ Re ≤ 110780).

A fully developed turbulent velocity profile was imposed in both inlets as a boundary condition by programming a C++ User-Defined Function (UDF). This strategy ensured that both inlet flows would achieve a fully developed state before entering the cross junction. Instead of using the known values of the tracer concentrations in the inlets (showed in Table 1), a tracer mass fraction of one (1) was imposed as a boundary condition in the North inlet, while in the West inlet, a tracer mass fraction of zero was imposed.

The concentrations of free chloride in the East () and South () outlets were obtained from simulations as follows (Bird et al. 1960):
(15)
(16)

In which, and are, respectively, the area-weighted average tracer mass fraction in each outlet boundary surface (East and South) extracted from simulations. Pressure outlet boundary conditions were imposed at the pipe outflows (South and East) with a gauge pressure equal to zero. In addition, non-slip boundary conditions were set on all wall surfaces.

The standard k-epsilon turbulence model with enhanced wall treatment for the near-wall treatment was used for modeling the three-dimensional turbulent flow. It has been reported that this model produces similar results for mixing in cross-pipe junction and T-junction compared with the shear-stress transport (SST) turbulence model with less computational expense (Walker et al. 2010; Santos-Violante et al. 2020). The species transport model incorporated in Ansys©-Fluent was used to predict the solute concentrations at the outlets. The binary diffusion coefficient of the tracer species in the fluid was D = 1.26 × 10 − 9 m2/s, which corresponds to the diffusion coefficient of chlorine in water at 25 °C. It was assumed that the tracer fluid (free chlorine in water) had the same viscosity (μ) and density (ρ) as the main water flow, i.e., μ = 0.001 Pa·s and ρ = 998.3 kg/m3. Standard model constants predetermined in Fluent were used in all simulations.

Finally, Ansys©-Fluent 17.1 software was used in all numerical simulations with steady-state conditions. The standard pressure–velocity together with the coupled scheme was employed for the pressure–velocity coupling. A high-order spatial discretization was used for the pressure and equations of momentum, turbulent kinetic energy, turbulent dissipation rate, and species transport. The solutions were considered converged when the residual of the equations reached a value below 10−5.

Experimental results

The principal goals of the experiments were to study the hydraulic behavior of the inflows (North and West) before leaving the junctions and, on the other hand, to formulate analytical equations to predict the chlorine concentration at the outflows (South and East). Many studies have reported that mixing at cross junctions is not always perfect. In many cases, flows tend to bifurcate rather than mix completely (Mompremier et al. 2012; Mompremier et al. 2017). In this study, experiments were conducted with varying incoming flows and varying initial concentrations. The instantaneous flow rates and free chlorine concentration were measured at each inflow and outflow of the cross junction. Every experiment was repeated twice to obtain the average results. In all the experiments, it was observed that chlorine concentration varied from one outlet to another (Mompremier et al. 2015) and may be explained by the fact that the flow at the West inlet was partially blocked by the incoming flow from the North, which had greater flow rate. As a result, the flow (from the West inlet) was pushed across the junction and exited through the South outlet. The chlorine concentration at outlets ranges from 0.88 to 1.65 mg/L at the South outlets and from 1.16 to 1.75 mg/L at the East outlet. The findings are presented in Figure 4.
Figure 4

Boundary conditions: Left: Flow rates at inlets and outlets Right: Average chlorine concentration at inflows and outflows.

Figure 4

Boundary conditions: Left: Flow rates at inlets and outlets Right: Average chlorine concentration at inflows and outflows.

Close modal

Influence of the initial chlorine concentration

The initial chlorine concentration of the water entering the junctions could be considered a determining factor of the outflow's chlorine concentration. For example, in experiment 5, chlorine concentrations at the North and West inlets were 1.80 mg/L and 1.60 mg/L, respectively, while in experiment 6, 1.42 mg/L at the North inlet and 0.80 mg/L at the West inlet. On the other hand, the inflow rates in the North inlet were approximately two times greater than in the West (in both experiments). Therefore, the effluent leaving the East outflow contained a higher chlorine concentration as it mainly contained water from the North inflow. Consequently, in these experiments where the value of chlorine at the East outlet depends on the value of the North entrance. As a result, the higher the chlorine concentration is in the North inflow stream, the higher it will be in the East outflow. The same trend was observed in the other experiments.

Influence of Reynolds number on the level of mixing

Reynolds number (Re) ranged from approximately 14324 to 110780 (North inlets) and from approximately 7380 to 68934 at West inlet, indicating turbulent flow through all pipes. The results show that Re number (especially, in turbulent flow) does not govern the cross junction mixing level. For example, in experiment 3, the North and West chlorine concentrations were 1.75 and 0.75 mg/L, and Re numbers were 33400 and 17200, respectively; the mixing was incomplete. The East and South outlets had chlorine concentrations of 1.27 and 1.63 mg/l, respectively. Therefore, it is logical to expect that the increased turbulence intensity enhances mixing with the increase of the Re numbers. Results of experiment 8, however, are not corroborated with this approach. While chlorine concentrations at North and West inlets were similar to those measured in experiments 3 (1.75 and 0.75), the increase of Re at inlets (85500 and 41800) would be expected to increase chlorine concentration at the South outlet. The results, however, indicate that chlorine concentration at the South outlet was similar to that obtained in experiment 3 (with only a minimal difference of 0.02 mg/L). The results of this study with those obtained by Shao et al. (2019). In their experimental study on mixing phenomenon at cross junction. They observed that under Re < 1,500 or laminar flow regime, the mixing is reduced as the Reynolds number increases. In transient flow (500 < Re < 3,000), mixing increases with increasing Reynolds numbers; and finally, in the turbulent flow of Re the >3,000, the degree of mixing is constant or invariant of flow variations.

Analytical equation of this study versus computational fluid dynamic findings

Simulations describing the mixing phenomenon at cross junctions and predicting chlorine concentration at outlets were performed through CFD to validate the analytical equations developed in this study. Therefore, the CFD results are compared with those obtained with these equations. For this purpose, a percentage of relative error (% Error) has been calculated and it is defined in Equation (17):
(17)
It is essential to point out that full-featured and accurate hydraulic modeling is a prerequisite for effective water quality modeling. The behavior of the incoming and outgoing flow was reproduced first in CFD. The results of the simulations show errors ranging from 0.26% to 12% when compared to experimental measurements. The distribution of water flow lines and tracer contour concentrations in the cross junction is shown in Figure 5. As can be seen, in the East outlet, the chlorine concentration is 1.65 mg/L, which is the same as that in the North inlet (red contour). In comparison, in the West inlet, the chlorine concentration is 0.80 mg/L (blue contour), and a partial mixing of the inlets (a mixture of contours between blue and red color) can be observed in the South outlet. All experiments showed the same pattern.
Figure 5

The distribution of water flow lines and tracer scalar concentration in cross junctions for Experiment 6 (.

Figure 5

The distribution of water flow lines and tracer scalar concentration in cross junctions for Experiment 6 (.

Close modal
Chlorine concentrations in the outlet pipes of the cross junctions were determined from Equations (15) and (16). The results of these simulations indicate incomplete mixing and bifurcation at cross junctions, which were experimentally reported using colored tracers in the inlets (Ho & O'Rear 2009). Figure 6 provides a comparison between our experimental results and CFD simulation results.
Figure 6

Comparison between experimental and numerical studies (CFD).

Figure 6

Comparison between experimental and numerical studies (CFD).

Close modal

The numerical simulation results show that the incoming flow rate is the principal parameter influencing the mixing. As illustrated in Figures 5 and 6, the trend maintains reasonable proximity to the tracer distribution in all experiments. In addition, the results show errors lower than 8% at East outlets and lower than 12% at South outlets with respect to the experimental measurements.

Adjustment of the R-value

Based on the CFD simulation results, an adjustment of the R-value is performed. Since chlorine concentration in the North inlet and East outlet is almost similar in all the experiments (with a minimum difference of 0.01), R-value is equal to 0.99. The difference in the dimensionless R-concentration values between experiments (R = 0.93) and that obtained in the numerical simulations (R = 0.99) is less than 6.5%. This slight discrepancy could be attributed to the fact that in experiments, it is complicated to keep the inlets and outlet pipe sections without deflection. At the same time, in the simulations, it is considered that these sections are straight pipes without the effects of the gravitational forces. Figure 7 compares the results obtained using the analytical equations of the current study with those obtained with CFD.
Figure 7

Comparison between numerical results (CFD versus the analytical equations of this study).

Figure 7

Comparison between numerical results (CFD versus the analytical equations of this study).

Close modal

As illustrated in Figure 7, the trend seen with both models is similar, indicating that the proposed analytical equations describe the mixing phenomenon observed in the cross junctions. Furthermore, the relative error between experimental and numerical findings (analytical equations of this study) is below 1% at East outlets and less than 8% at South outlets, proving the proposed model's goodness. The results agree with those obtained by Santos-Violante et al. (2020), who conducted a 3D CFD study of mixing in cross junctions with two adjacent inlets and proposed the implementation of an internal device inside the cross junction to improve the mixing in the two outlet flows.

Finally, the analytical equations developed as part of this study were used to predict exit concentrations of an experimental study reported by Ho & O'Rear (2009). Their study explored the effect of alternative configurations on solute mixing in junction adjacent inlets with equal pipe sizes. The boundary conditions were as follows:

; the normalized concentration of the tracer was 1 mg/L, and the normalized concentration of the clean water was 0. .

As a result, the normalized concentration was 1 mg/L for effluent adjacent to the Q tracer and 0.55 mg/L for effluent opposite the Q tracer. Furthermore, Equations (11) and (14) predicted the normalized effluent concentrations. The predicted values were 0.99 and 0.543 mg/L in both outlets respectively. A relative error of less than 2% at both outlets was observed. Obtained results suggest that the analytical equations can be used as a good representation of experimental data.

The obtained results validated the analytical equations developed in this study that predict solute concentrations in the outlets. Experiments were carried out with varying flow and chlorine concentrations at the inlet pipes in which solute mixing is incomplete due to the bifurcation of the incoming adjacent flows. A dimensionless concentration R was calculated for each scenario in order to provide a means to determine the outlet concentrations based on the inlet concentrations. For example, chlorine concentration at the East outlet was calculated by multiplying R by the chlorine concentration of the North inlet. In addition, a solute mass balance was performed within the cross junction to predict the concentration at the South outlet. Finally, the k–e turbulence model with enhanced wall treatment, solved by the Ansys© 17.1 -Fluent software, was employed to validate the analytical equations proposed in this study to predict the chlorine concentrations leaving the junction. Experimental and CFD simulation results assessed the effectiveness of the analytical equation formulated in this study. One of the limitations of these equations is that they (analytical equations) can only be used when the higher incoming flow rates have a higher chlorine concentration. In future studies, it is suggested to conduct experiments with higher incoming flow rates containing lower chlorine concentration. It is also suggested to perform more experiments with a greater flow range, unequal pipe diameters, and higher chlorine doses. Decisions on protecting public health against drinking water contamination threats have become necessary. The results of this study can help to prepare water utility operators for making these critical decisions during an intense course of emergency. Finally, it has been shown that the CFD method can readily and reliably evaluate the mixing phenomenon in cross junctions as a complement to experimental measurements.

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

The authors declare there is no conflict.

Austin
R. G.
,
van Bloemen Waanders
B.
,
McKenna
S. A.
&
Choi
C. Y.
2008
Mixing at cross junctions in water distribution systems. II: Experimental study
.
Journal of Water Resources Planning and Management
134
,
295
302
.
Bird
R. B.
,
Stewart
W.
&
Lightfoot
E.
1960
Transport Phenomena
.
John Wiley & Sons
,
New York
.
Fowler
A. G.
&
Jones
P.
1991
Simulation of water quality in water distribution systems
. In:
Proceeding of the Water Quality Modeling in Distribution Systems
.
AWWARF/EPA
,
Cincinnati, Ohio
.
Hernández-Cervantes
D.
,
Delgado-Galván
X.
,
Nava
J. L.
,
López-Jiménez
P. A.
,
Rosales
M.
&
Mora Rodríguez
J.
2018
Validation of a computational fluid dynamics model for a novel residence time distribution analysis in mixing at cross-junctions
.
Water
10
(
6
),
733
.
Hernández Cervantes
D.
,
López-Jiménez
P. A.
,
Arciniega Nevárez
J. A.
,
Delgado Galván
X.
,
Jiménez Magaña
M. R.
,
Pérez-Sánchez
M.
&
Mora Rodríguez
J.
2021
Incomplete mixing model at cross-junctions in Epanet by polynomial equations
.
Water
13
(
4
),
453
.
Ho
C. K.
&
O'Rear
L.
Jr.
2009
Evaluation of solute mixing in water distribution pipe junctions
.
Journal of the American Water Works Association
101
,
116
.
Ho
C. K.
,
Choi
C. Y.
&
McKenna
S. A.
2007
Evaluation of complete and incomplete mixing models in water distribution pipe network simulations
. In:
Proceedings of the 2007 World Environmental and Water Resources Congress
,
May 15–19, 2007
,
Tampa, FL
.
(SAND2007-0492C)
.
Liu
H.
,
Yuan
Y.
,
Zhao
M.
,
Zheng
X.
,
Lu
J.
&
Zhao
H.
2011
Study of mixing at cross-junction in water distribution systems based on computational fluid dynamics
. In:
Proceedings of the International Conference on Pipelines and Trenchless Technology
,
26–29 October 2011
,
Beijing, China
, pp.
552
561
.
Mays
L. W.
2004
Water Supply Systems Security
.
McGraw-Hill Professional
,
New York
.
Mompremier
R.
,
Fuentes Mariles
O. A.
&
De Luna Cruz
F.
2012
Resultados de pruebas de laboratorio para analizar la difusión del cloro en cruces de tuberías
. In:
XXII Congreso Nacional de Hidráulica
,
Noviembre 2012
,
Acapulco, Guerrero, México
.
AMH
.
Mompremier
R.
,
Pelletier
G.
,
Fuentes
M. O. A.
&
Ghebremichael
K.
2015
Impact of incomplete mixing in the prediction of chlorine residuals in municipal water distribution systems
.
Journal of Water Supply: Research and Technology – AQUA
64
(
8
),
904
914
.
Mompremier
R.
,
Fuentes Mariles
O. A.
,
Silva Martínez
A. E.
,
Becerril Bravo
J. E.
&
Ghebremichael
K.
2017
Impact of mixing phenomenon at cross junctions on the variation of total coliform and E. coli in water distribution systems: experimental study
.
Journal of Water Supply: Research and Technology-Aqua
66
(
5
),
308
318
.
Romero-Gomez
P.
,
Ho
C. K.
&
Choi
C. Y.
2006
Mixing at cross junctions in water distribution systems. I: numerical study
.
Journal of Water Resources Planning and Management
134
,
285
294
.
(SAND2007-0774 J)
.
Rossman
L. A.
2000
EPANET User's Manual
.
US Environmental Protection Agency
,
Cincinnati, Ohio
.
Santos-Violante
H. A.
,
Ramirez-Muñoz
J.
,
Mompremier
R.
,
Márquez-Baños
V. E.
,
Guadarrama-Pérez
R.
&
Gómez-Núñez
J.
2020
CFD study of the effect of an internal device within a cross junction on mixing phenomenon
. In;
2020 Virtual AICHE Annual Meeting Proceedings
.
ISBN: 978-0-8169-1114-1
.
Shao
Yu.
,
Zhao
L.
,
Yang
Y. J.
,
Zhang
T.
&
Ye
M.
2019
Experimentally determined solute mixing under laminar and transitional flows at junctions in water distribution systems
.
Advances in Civil Engineering
2019
,
3686510
.
Song
I.
,
Romero-Gomez
P.
&
Choi
C. Y.
2009
Experimental verification of incomplete solute mixing in a pressurized pipe network with multiple cross-junctions
.
Journal of Hydraulic Engineering
135
,
1005
1011
.
Van Bloemen Waanders
B.
,
Hammond
G.
,
Shadid
J.
,
Collis
S.
&
Murray
R.
2005
A comparison of Navier-Stokes and network models to predict chemical transport in municipal water distribution systems
. In:
Proceedings of the World Water and Environmental Resources Congress
,
Anchorage, AK
,
USA
,
15–19 May 2005
; pp.
1
10
.
Walker
C.
,
Manera
A.
,
Niceno
B.
,
Simiano
M.
&
Prasser
H. M.
2010
Steady-state RANS-simulations of the mixing in a T-junction
.
Nuclear Engineering and Design
240
(
9
),
2107
2115
.
Yu
T. C.
,
Shao
Y.
&
Shen
C.
2014
Mixing at cross joints with different pipe sizes in water distribution systems
.
Journal of Water Resources Planning and Management
140
,
658
665
.
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