Groundwater is a dependable freshwater resource in arid and semi-arid areas where its quality management is essential. However, untreated wastewater is a risk to safe water supply from aquifers. Wastewater treatment plants (WWTPs) can reduce pollutants, but their impact on groundwater quality versus their operating costs requires case studies. This research uses the two modules of the groundwater modeling system (GMS) to simulate the Varamin Plain, south-eastern Tehran, Iran. The MODFLOW and MT3D were used for groundwater quantity and quality modeling, respectively. Through these modules, the effectiveness of two WWTPs (Pakdasht and Varamin) in six waste load allocation (WLA) scenarios was compared based on nitrate reduction in 3-year and 10-year periods. The construction and operating costs of each WLA scenario were also calculated. The best WLA is a scenario with the lowest marginal cost. Therefore, constructing Varamin WWTP with 25% nitrogen removal was the selected option. Here, the average nitrate concentration in the aquifer is reduced from 28.4 mg/L (±4.1) to less than 25 mg/L (±2.4) with an annual marginal cost of 8 M$.L/mg. It implies that constructing more WWTPs or tertiary units for nitrate removal is not recommended as they do not add significant nitrate abatement in groundwater regarding the related costs.

  • Varamin aquifer is modeled by combined MODFLOW and MT3D modules.

  • Impacts of six WLA scenarios were compared in 3- and 10-year periods.

  • Optimal WLA is a scenario with the least annual marginal cost (8 M$.L/mg).

  • A costly tertiary unit is not necessarily a sustainable option for WLA.

  • The aquifer is gradually reactive to nitrate removal for more than a decade.

Groundwater management with competing users is a challenge in arid and semi-arid areas (Darbandsari et al. 2020). Its quality is also vulnerable to wastewater and leaching from domestic, industrial, and agricultural activities (Wada et al. 2021). In particular, nutrient puts groundwater resources at risk and has secondary impacts on health and the economy (Kariman et al. 2018; Golian et al. 2021). Recent research indicates increased global concerns about nitrate leaching into the groundwater. Water extraction and wastewater discharges can affect its concentration in an aquifer (Shahraki et al. 2020). Water with excessive nitrate concentration can cause serious health problems for livestock and humans (Lorenz et al. 2014; Najafi Alamdarlo et al. 2016). Methemoglobinemia in infants and cancer risk are some examples (Gardner et al. 2020; Liu et al. 2022). Nitrate concentration in soil and aquifer increases in areas with a high level of agricultural activity using fertilizers and manure (Imani et al. 2015, 2017). Nitrogenous fertilizers are heavily invested in the fields by farmers to maintain adequate production and increase yields (Jamshidi et al. 2020; Jamshidi & Naderi 2023). The excess nitrate leaches into groundwater and causes contamination problems (Martínez et al. 2020). In contrast to natural attenuation processes (Akbarzadeh et al. 2015), engineered systems, such as a wastewater treatment plant (WWTP), can significantly reduce nitrate pollution (Jamshidi & Niksokhan 2016). Thus, recent research efforts have focused on understanding the pathways of nitrate (NO3) generation and contamination in groundwater and developing eco-friendly approaches to remove NO3 from groundwater (Huno et al. 2018). Marshall et al. (2019) examined the spatiotemporal variability of wastewater parameters, including nitrate and their transport in groundwater. They could estimate the impacts of WWTP on groundwater pollution transport over time (Marshall et al. 2019).

NO3 is traceable and manageable through waste load allocation (WLA) policies (Menció et al. 2016; Alfarrah & Walraevens 2018). To predict NO3 contamination in groundwater, a nitrate-based transport model was recently used to estimate four WLA scenarios. In every scenario, NO3 concentration was influenced by discharged pollution loads. Its concentration decreased in all scenarios during the 20-year prediction period, while none of the scenarios could reduce it below the standard level (Karlović et al. 2022). Depending on the specific aquifer conditions, the types of contaminants, and related costs, each WLA scenario may control or reduce some pollution loads (Benjakul 2010; Matiatos et al. 2019). It is recommended to select the best-performing WLA systematically by evaluating its effectiveness or potential in water quality improvement (Samadi-Darafshani et al. 2021). Since pollution removal is set at a desired level in WLAs, the related cost of attaining that purity level increases as treatment improves (Jamshidi et al. 2014; Englande et al. 2015). Identifying appropriate strategies and financing for wastewater infrastructure under WLA is often challenging for decision-makers (van Afferden et al. 2015). Therefore, groundwater quality management by constructing WWTP requires a two-faceted economic-functional analysis. This should be implemented by an integrated simulation tool to estimate the fate and transport of pollutants and track the sensitivity of receiving aquifer to different emissions. For this purpose, numerical models are valuable tools in understanding groundwater systems and estimating their qualitative status under various WLA scenarios (Foster et al. 2021). Groundwater resources modeling poses challenges in understanding influential parameters and achieving proper model calibration, crucial for accurate results, and effective water resource management (Eini et al. 2020; Jafari et al. 2021). To solve WLA problems, it is necessary to understand the quality response of receiving water bodies to each scenario. Groundwater simulation is commonly carried out by two GMS software modules. The MODFLOW and MT3D modules are used for water quantity and quality modeling, respectively (Raetz 2022). For example, a new simulation-optimization method in a watershed has been devised to solve problems associated with multiple pollutants (Sadak et al. 2020). Multipollutant loads were allocated according to the locations of their sources using an optimization formula. However, groundwater systems may take a decade or more to respond to this strategy.

This study aims to compare the impacts of constructing two WWTPs (Pakdasht and Varamin) with different nitrate removal efficiencies on groundwater quality. This study uses aquifer flow simulation by MODFLOW, followed by contaminant fate and transport modeling by MT3D. These modules predict NO3 concentration in groundwater in different WLA scenarios during 3-year (T3) and 10-year (T10) periods. Here, WWTPs have different nitrate removal efficiencies with total abatement costs. Thus, on the basis of a numerical model, this research evaluates the effectiveness of WWTPs in remediating groundwater quality and considers related costs. By these means, the optimal WLA strategy is recommended in the study area. Accordingly, this study has two notable innovations in the field. Firstly, the research employs a combined qualitative and quantitative modeling for WLA in groundwater. This approach ensures a holistic understanding of the nitrogen reduction in aquifers by different wastewater treatments. Secondly, by incorporating multiple scenarios, the study provides a cost-effective analysis that enhances our understanding of potential management strategies. The question ‘is it necessary to upgrade both WWTPs with tertiary units?’ is answered by introducing the marginal cost (MC), as a decisive index, in the applied methodology.

Methodology

This study follows a three-step methodology (Figure 1). At first, the aquifer was simulated by focusing on nitrate concentration. Six WLA scenarios were then testified to compare WWTPs' impacts on groundwater quality improvement. These two steps can provide a framework for evaluating the most cost-effective WLA policy in the final step.
Figure 1

Methodology steps of this study.

Figure 1

Methodology steps of this study.

Close modal

Study area

This study examines the impacts of WWTPs on the Varamin Plain, located in the south-eastern part of Tehran province, Iran. This plain is between the latitudes of 35.39°N and 35.07°N and the longitudes of 51.26°E and 51.55°E and covers approximately 957 km2 area. Excessive water demands and unsustainable groundwater extraction in the Varamin aquifer have caused declining water levels, resulting in land subsidence and reduced groundwater table (Nayyeri et al. 2021). This plain supplies the agricultural and drinking water of two counties, Pakdasht and Varamin. Droughts in recent decades have made wastewater recharge an attractive option. It could partially compensate for water quantity for agriculture, whereas deteriorated water quality (Noghreyan et al. 2022). Here, untreated wastewater of Pakdasht and Varamin are the primary point sources (Ministry of power 2013; Nouri et al. 2020). It is planned to construct and operate two WWTPs for these two counties. WW1 locates in 35°24′0″N, 51°53′0″E (Varamin) and the WW2 blueprint is 35°28′0″N, 51°48′0″E (Pakdasht). WW1 and WW2 receive sewage from about 284,000 and 351,000 persons, respectively. Accordingly, this study seeks a cost-effective and environmentally sound WLA to answer the following question: which WWTP, WW1 or WW2, should be prioritized regarding groundwater quality variations and total costs?

Simulation and calibration

GMS software (version 10.1) was used to simulate the Varamin aquifer. MODFLOW and MT3DMs were the modules that simulated groundwater level and quality, respectively. Since the study area is quite large, it has been divided into six zones based on land use and available observation wells having water quality data. This zoning could provide an elaborate framework for demonstrating the sensitivity of groundwater to the WLA scenario in short term (3 years) and long term (10 years). For simulation, the study area was gridded by 250,000 m2 squares. The locations of observation wells, their temporal variations on water levels, and aquifer recharge were initially determined based on available data. Furthermore, qualitative information, such as NO3 concentrations and discharges from emission sources, were assigned to the nodes (Ministry of Energy 2013).

Calibration was carried out on available data from September 2009–March 2012 (1,002 days). T0 corresponds to autumn 2011 when the model is calibrated, T3 represents the conditions 3 years after simulation (2011–2014), and T10 represents groundwater quality for each WLA scenario 10 years after the simulation ends (2011–2021). Figure 2 summarizes the average groundwater depth in 42 piezometric wells. R-square and the root mean square errors (RMSE) for the average simulated groundwater depth and observed data (2009–2011) are 0.81 and 0.46, respectively. The concentration of NO3 collected from observation wells with the collection time period (monthly) is expressed in Table 1.
Table 1

NO3 concentration in observation wells with time periods (Sep 2009-Mar. 2012)

TimeNO3 concentration in observation wells (mg/L)
G25G28G29G36G37G38G39G40
2009-09 24.5 29.9 31.2 25.6 24.8 63.9 23.6 26.1 
2009-12 24.8 28.7 31.4 25.6 24.9 66.1 21.6 26.1 
2010-03 25.1 24.2 31.3 25.5 25.0 63.2 19.6 26.0 
2010-06 25.4 19.7 30.9 25.5 25.1 57.4 17.7 25.9 
2010-09 25.6 19.3 30.4 25.5 25.2 53.6 17.2 25.8 
2010-12 25.9 20.0 30.0 25.4 25.5 52.4 17.5 25.8 
2011-03 26.1 18.0 29.6 25.3 25.8 49.6 17.0 25.7 
2011-06 26.4 15.6 29.0 25.2 26.1 45.5 15.8 25.6 
2011-09 26.7 16.2 28.4 25.2 26.6 42.8 15.6 25.6 
2011-12 27.0 17.8 28.0 25.1 27.2 42.4 16.2 25.5 
2012-03 27.3 16.5 27.6 25.0 27.7 41.3 15.7 25.4 
TimeNO3 concentration in observation wells (mg/L)
G25G28G29G36G37G38G39G40
2009-09 24.5 29.9 31.2 25.6 24.8 63.9 23.6 26.1 
2009-12 24.8 28.7 31.4 25.6 24.9 66.1 21.6 26.1 
2010-03 25.1 24.2 31.3 25.5 25.0 63.2 19.6 26.0 
2010-06 25.4 19.7 30.9 25.5 25.1 57.4 17.7 25.9 
2010-09 25.6 19.3 30.4 25.5 25.2 53.6 17.2 25.8 
2010-12 25.9 20.0 30.0 25.4 25.5 52.4 17.5 25.8 
2011-03 26.1 18.0 29.6 25.3 25.8 49.6 17.0 25.7 
2011-06 26.4 15.6 29.0 25.2 26.1 45.5 15.8 25.6 
2011-09 26.7 16.2 28.4 25.2 26.6 42.8 15.6 25.6 
2011-12 27.0 17.8 28.0 25.1 27.2 42.4 16.2 25.5 
2012-03 27.3 16.5 27.6 25.0 27.7 41.3 15.7 25.4 
Figure 2

Maximum, minimum and average observed and simulated groundwater depth (m).

Figure 2

Maximum, minimum and average observed and simulated groundwater depth (m).

Close modal

WLA scenarios

The effectiveness of six WLA scenarios on aquifer quality was investigated and compared through the calibrated model. Table 2 illustrates the specifications of these WLA scenarios. Differences in WLAs are basically in the locations of WWTPs (WW1 and WW2), the zoning of treated wastewater recharge, and their NO3 removal efficiency (25 and 50%). S0 depicts the basic status of the simulated aquifer in the study area without any projected WLA.

Table 2

Definition of WLA scenario in this study

ScenarioDescription
S0 Basic scenario 
S1 WW2 with 25% N removal and aquifer recharge 
S2 WW2 with 50% N removal and aquifer recharge 
S3 WW1 with 25% N removal and aquifer recharge 
S4 WW1 with 50% N removal and aquifer recharge 
S5 S1 + S3 
S6 S2 + S4 
ScenarioDescription
S0 Basic scenario 
S1 WW2 with 25% N removal and aquifer recharge 
S2 WW2 with 50% N removal and aquifer recharge 
S3 WW1 with 25% N removal and aquifer recharge 
S4 WW1 with 50% N removal and aquifer recharge 
S5 S1 + S3 
S6 S2 + S4 

In each WLA scenario (S1–S6), the abated nitrogen (N) was assigned to the target residential region as equivalent to reduced NO3 concentration (%). It is necessary as Pakdasht and Varamin counties have no WWTPs and the untreated wastewater is conventionally discharged to the aquifer. N mitigation in S1–S6 means that NO3 concentration in treated wastewater is decreased via constructing and operating WWTPs prior to any discharge or infiltration to the groundwater. The outcomes of all WLA scenarios were then analyzed and evaluated in both the objective area as well as the study area observation wells.

It should be added that WLA scenarios were individually defined in the calibrated model and NO3 concentration at eight observation wells was obtained by GMS outputs. The impact of each scenario on pollution abatement is estimated using the average T3 and T10 concentrations from all observation wells. Following that WLA scenarios were qualitatively ordered based on their effectiveness on groundwater quality. In this case, the most environmentally favorable WLA is the one with the lowest average NO3 concentration in the entire plain based on NO3 concentration at both T3 and T10. Nevertheless, a viable WLA scenario needs economic analysis as well.

Economic analysis

Total cost (TC) is required for conducting economic analysis for WLAs. For WWTPs, TC attributes to their construction and operation costs in their lifetime. In WLA scenarios, it can be defined according to the required biochemical oxidation demand (BOD) and N removal efficiencies in WWTPs as Equation (1) (Jamshidi & Niksokhan 2016)
(1)
where CW is the annual capital and operation costs (million$/yr), Q is the annual average wastewater inflow (m3/s), and T is the annual capital and operating cost of WWTPs per unit volume (million$/m3) which is calculated by Equation (2)
(2)
Here, TBOD and TNO3 are the costs of reducing BOD and NO3 pollutants, respectively (M$/m3). They depend on the required efficiency as calculated by Equations (3) and (4), respectively.
(3)
X denotes BOD concentration abatement in WWTP that ranges between 0 and 1. In this study, BOD concentration reduction for all WWTPs is assumed as 0.9, meaning that WWTPs should at least remove 90% of the BOD concentration of wastewater in any scenario. However, it is noteworthy that BOD is only used for cost evaluations and is not included in water quality assessment in simulation and WLA.
(4)
where Z represents the NO3 removal efficiency of WWTPs and it ranges between 0 and 1. For example, in S1 with 25% N removal, Z equals 0.25.
The average MC of WLAs is an economic index that can be calculated using Equation (5).
(5)
where MCW is the annual average marginal cost of each WLA scenario (M$.L/mg), R is the abated nitrate concentration of the aquifer of each WLA in comparison with S0 (mg/L), and CW is defined earlier.

Simulation results

Simulation results show that the average groundwater level at T0 is 852 m and the average nitrate concentration in the aquifer is 28.4 mg/L. The latter varies between 17.7 mg/L and 57.4 mg/L in the whole plain (Figure 3). It is clear that the distribution of contaminants is not uniform across the plain, with relatively high NO3 concentrations in the northern and central-south parts of the plain.
Figure 3

Groundwater level (Left) and simulated NO3 concentration (Right) at T0.

Figure 3

Groundwater level (Left) and simulated NO3 concentration (Right) at T0.

Close modal
Figure 4 illustrates the average, minimum, and maximum of NO3 concentration in observation wells during T3 and T10 for all WLA scenarios. Comparatively, S6 has the lowest nitrate concentration in both periods. Nonetheless, the optimal WLA policy is a strategy that fulfills the lowest pollutant concentration with the least cost. In S0, NO3 concentration decreases during T10 as a matter of aquifer recharge with treated wastewater without nitrate removal in WWTPs. The difference between S6 and S0 in T3 and T10 indicates how much nitrate reduction in WWTPs is effective on groundwater in the mid term and long term.
Figure 4

The average with minimum and maximum concentrations of NO3 (mg/L) in aquifer at T3 (a) and T10 (b) for all WLA scenarios (S0-S6).

Figure 4

The average with minimum and maximum concentrations of NO3 (mg/L) in aquifer at T3 (a) and T10 (b) for all WLA scenarios (S0-S6).

Close modal
Figure 5 illustrates NO3 removal efficiency (%) of different WLAs in the aquifer for both T3 and T10. It shows that S6 has the highest NO3 reduction in groundwater in both periods. The average abated NO3 of S6 in T3 and for T10 are 4.3% (±2.1) and 11.7% (±2.9), respectively. On the contrary, the least effective WLAs on NO3 removal in T3 and T10 are S1 and S3 with 0.3% (±0.4) and 3.3% (±1.7), respectively. It means that constructing WW1 and WW2 with 50%N removal is more effective than constructing just one WWTP. However, economic evaluation analysis is also required to compare the cost-effectiveness of these WLAs.
Figure 5

Pollution reduction of WLAs (%) in the aquifer in T3 and T10.

Figure 5

Pollution reduction of WLAs (%) in the aquifer in T3 and T10.

Close modal

Economic evaluation

Figure 6 illustrates MC and TC required for switching from S0 to each WLA in the logarithmic scale. The MC for T10 is determined by the average impact of each scenario on groundwater quality. The least cost option is S3 (38.3 M$/yr), whereas the most costly strategy is S6 (99.6 M$/yr). Due to the accumulated cost of building WWTPs, it is obvious that WLAs with two WWTPs (S5 and S6) have relatively higher costs than other scenarios (S1–S4). As shown in Figure 6, annual NO3 removal MC ranges between 8 (S3) and 14.6 M$.L/mg (S6). It means that annually 8 million US$ is required in S3 for 1 mg/L nitrate abatement from the Varamin aquifer for 10 years. Hence, S3 is the best cost-effective scenario because it has the highest economic return for stakeholders and has the least MC and TC.
Figure 6

Required total cost (M$/yr) and the annual marginal cost (M$.L/mg) for one unit pollutant reduction in each WLA scenario in logarithmic scale.

Figure 6

Required total cost (M$/yr) and the annual marginal cost (M$.L/mg) for one unit pollutant reduction in each WLA scenario in logarithmic scale.

Close modal

In this research, we conducted a comprehensive assessment of various WLA scenarios and their implications for long-term groundwater quality and economic considerations. Our study was based on the NO3 parameter recommended by Nzama et al. (2021), as it is considered a critical groundwater pollutant that can be managed through land-use changes and WWTPs (Nzama et al. 2021). The effectiveness of these practices was verified through simulations using MODFLOW and MT3DMs, recognized as efficient groundwater modeling techniques (Raetz 2022).

Our investigation on the Varamin Plain showed that the simultaneous implementation of two WWTPs presents relatively higher pollution abatement compared to WLA policies involving a single WWTP. However, their pollution abatement is not significant in groundwater in the short term, and therefore, implementing both WWTPs is not recommended considering the related costs. Interestingly, this finding aligns with the results of Wada et al. (2021), where a single WWTP had a more significant impact on groundwater quality. Our results also contradict the findings of Adebowale et al. (2019), with the notion that constructing multiple WWTPs yields greater efficiency, particularly in the areas surrounding the WWTPs, within a shorter time period (Adebowale et al. 2019).

In a recent study by Saadatpour et al. (2019), it was concluded that WWTPs can improve the water quality index, and increasing the investment cost leads to greater quality improvements. However, there is a specific limit beyond which the water quality index cannot be further improved, regardless of the cost incurred or equity sacrificed (Saadatpour et al. 2019). In our current study, we also found that increasing the cost of WWTPs results in greater quality improvements. However, once specific limits are reached, more investment would be futile.

It has also become evident that pollution concentration limits set by regulatory bodies must consider a combination of pollution objectives and stakeholder demands to ensure the development of user-friendly applications. By doing so, water quality violations can be minimized for up to 20 years (Dinar & Quinn 2022). Moreover, previous studies have highlighted the practicality of pollution removal in WWTPs (Jamshidi & Niksokhan 2016) within the context of WLA. These factors, coupled with our latest research findings, underscore the importance of integrating economic objectives and practical considerations to establish sustainable groundwater quality management strategies.

This study used GMS modules to simulate the impacts of 6 WLA scenarios on NO3 reduction in two time periods (T3 and T10). Results showed that GMS is a reliable and practical tool for groundwater simulation prior to WLA analysis. The MODFLOW and MT3D modules can be used for quantity and quality modeling, respectively. According to the results, WWTPs in the study area would not be considerably effective on NO3 abatement in less than 10 years. Here, constructing two WWTPs (WW1 and WW2) is the most leading WLA for groundwater quality enhancement. However, it requires considerable costs. In addition, improving aquifer quality is not linear to the number of constructed WWTPs. Thus, this study recommended calculating the marginal costs, as an efficiency index, for referring to the optimal WLA. By this approach, S3 (WW1 with 25%N removal), S1 (WW2 with 25%N removal), and S4 (WW1 with 50%N removal) are prioritized as cost-effective WLAs.

M.A.S. led the investigation, prepared the methodology, did software analysis, validated, analyzed, did data curation, visualized, and wrote the original draft. S.J. conceptualized the study, prepared the methodology, did analysis, supervised, did project administration, and wrote (reviewed and edited) the article. H.K.M. collected resources, did software analysis, validated, and visualized the study.

Iran Water Resource Management Co. under contract No. S.07.1401 with the University of Isfahan partially contributed to the funding of this research.

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

The authors declare there is no conflict.

Adebowale
T.
,
Surapaneni
A.
,
Faulkner
D.
,
McCance
W.
,
Wang
S.
&
Currell
M.
2019
Delineation of contaminant sources and denitrification using isotopes of nitrate near a wastewater treatment plant in peri-urban settings
.
Science of The Total Environment
651
,
2701
2711
.
https://doi.org/10.1016/j.scitotenv.2018.10.146
.
Akbarzadeh
A.
,
Jamshidi
S.
&
Vakhshouri
M.
2015
Nutrient uptake rate and removal efficiency of vetiveria zizanioides in contaminated waters
.
Pollution
1
(
1
),
1
8
.
Alfarrah
N.
&
Walraevens
K.
2018
Groundwater overexploitation and seawater intrusion in coastal areas of arid and semi-arid regions
.
Water
10
(
2
),
143
.
https://doi.org/10.3390/w10020143
.
Benjakul
R.
2010
Simulating Dioxane Transport in A Heterogeneous Glacial Aquifer System (Washtenaw County, Michigan) Using Publicly Available Models and Data
.
Michigan Technological University
.
https://doi.org/10.37099/mtu.dc.etds/313
.
Darbandsari
P.
,
Kerachian
R.
,
Malakpour-Estalaki
S.
&
Khorasani
H.
2020
An agent-based conflict resolution model for urban water resources management
.
Sustainable Cities and Society
57
,
102112
.
https://doi.org/10.1016/j.scs.2020.102112
.
Eini
M. R.
,
Javadi
S.
,
Delavar
M.
,
Gassman
P. W.
&
Jarihani
B.
2020
Development of alternative SWAT-based models for simulating water budget components and streamflow for a karstic-influenced watershed
.
CATENA
195
,
104801
.
https://doi.org/10.1016/j.catena.2020.104801
.
Englande
A. J.
,
Krenkel
P.
&
Shamas
J.
2015
Wastewater treatment & water reclamation
.
Reference Module in Earth Systems and Environmental Sciences
.
Elsevier. https://doi.org/10.1016/B978-0-12-409548-9.09508-7
.
Foster
L. K.
,
White
J. T.
,
Leaf
A. T.
,
Houston
N. A.
&
Teague
A.
2021
Risk-based decision-support groundwater modeling for the lower San Antonio River Basin
.
Groundwater
.
59
(
4
),
581
596
. Texas, USA.
Gardner
S. G.
,
Levison
J.
,
Parker
B. L.
&
Martin
R. C.
2020
Groundwater nitrate in three distinct hydrogeologic and land-use settings in southwestern Ontario, Canada
.
Hydrogeology Journal
28
(
5
),
1891
1908
.
https://doi.org/10.1007/s10040-020-02156-4
.
Golian
M.
,
Saffarzadeh
A.
,
Katibeh
H.
,
Mahdad
M.
,
Saadat
H.
,
Khazaei
M.
,
Sametzadeh
E.
,
Ahmadi
A.
,
Sharifi Teshnizi
E.
,
Samadi Darafshani
M.
&
Dashti Barmaki
M.
2021
Consequences of groundwater overexploitation on land subsidence in Fars Province of Iran and its mitigation management programme
.
Water and Environment Journal
35
(
3
),
975
985
.
https://doi.org/10.1111/wej.12688
.
Huno
S. K. M.
,
Rene
E. R.
,
van Hullebusch
E. D.
&
Annachhatre
A. P.
2018
Nitrate removal from groundwater: a review of natural and engineered processes
.
Journal of Water Supply: Research and Technology-Aqua
67
(
8
),
885
902
.
https://doi.org/10.2166/aqua.2018.194
.
Imani
S.
,
Delavar
M.
&
Niksokhan
M. H.
2016
Periodical effects of land uses on water quality of Zrebar Lake, Iranian. Journal of Geology
9
(
36
),
1
10
.
Imani
S.
,
Delavar
M.
&
Niksokhan
M. H.
2017
Simulation and assessment of management practices for reduction of nutrients discharge to the zrebar lake using swat model
.
Iran-Water Resources Research
13
(
1
),
69
87
.
Jafari
T.
,
Kiem
A. S.
,
Javadi
S.
,
Nakamura
T.
&
Nishida
K.
2021
Fully integrated numerical simulation of surface water-groundwater interactions using SWAT-MODFLOW with an improved calibration tool
.
Journal of Hydrology: Regional Studies
35
,
100822
.
https://doi.org/10.1016/j.ejrh.2021.100822
.
Jamshidi
S.
&
Niksokhan
M. H.
2016
Multiple pollutant discharge permit markets, a challenge for wastewater treatment plants
.
Journal of Environmental Planning and Management
59
(
8
),
1438
1455
.
https://doi.org/10.1080/09640568.2015.1077106
.
Jamshidi
S.
,
Niksokhan
M. H.
&
Ardestani
M.
2014
Surface water quality management using an integrated discharge permit and the reclaimed water market
.
Water Science and Technology
70
(
5
),
917
924
.
https://doi.org/10.2166/wst.2014.314
.
Jamshidi
S.
,
Imani
S.
&
Delavar
M.
2020
Impact assessment of best management practices (BMPs) on the water footprint of agricultural productions
.
International Journal of Environmental Research
14
(
6
),
641
652
.
https://doi.org/10.1007/s41742-020-00285-y
.
Kariman
A. S.
,
Salimi
L.
&
Jamshidi
S.
2018
Determining the economic value of surface water quality improvements to trout farmers
.
Journal of Water Supply: Research and Technology – Aqua
67
(
2
),
192
201
.
https://doi.org/10.2166/aqua.2017.229
.
Karlović
I.
,
Posavec
K.
,
Larva
O.
&
Marković
T.
2022
Numerical groundwater flow and nitrate transport assessment in alluvial aquifer of Varaždin region, NW Croatia
.
Journal of Hydrology: Regional Studies
41
,
101084
.
https://doi.org/10.1016/j.ejrh.2022.101084
.
Liu
R.
,
Xia
L.
,
Liu
M.
,
Gao
Z.
,
Feng
J.
,
You
H.
,
Qu
W.
,
Xing
T.
,
Wang
J.
&
Zhao
Y.
2022
Influence of the carbon source concentration on the nitrate removal rate in groundwater
.
Environmental Technology
43
(
22
),
3355
3365
.
https://doi.org/10.1080/09593330.2021.1921053
.
Lorenz
K.
,
Iwanyshyn
M.
,
Olson
B.
,
Kalischk
A.
&
Pentland
J.
2014
Livestock Manure Impacts on Groundwater Quality in Alberta
.
Marshall
R. E.
,
Levison
J.
,
McBean
E. A.
&
Parker
B.
2019
Wastewater impacts on groundwater at a fractured sedimentary bedrock site in Ontario, Canada: implications for First Nations’ source-water protection
.
Hydrogeology Journal
27
(
8
),
2739
2753
.
https://doi.org/10.1007/s10040-019-02019-7
.
Martínez
R.
,
Vela
N.
,
el Aatik
A.
,
Murray
E.
,
Roche
P.
&
Navarro
J. M.
2020
On the use of an IoT integrated system for water quality monitoring and management in wastewater treatment plants
.
Water
12
(
4
),
1096
.
https://doi.org/10.3390/w12041096
.
Matiatos
I.
,
Varouchakis
E. A.
&
Papadopoulou
M. P.
2019
Performance evaluation of multiple groundwater flow and nitrate mass transport numerical models
.
Environmental Modeling & Assessment
24
(
6
),
659
675
.
https://doi.org/10.1007/s10666-019-9653-7
.
Menció
A.
,
Mas-Pla
J.
,
Otero
N.
,
Regàs
O.
,
Boy-Roura
M.
,
Puig
R.
,
Bach
J.
,
Domènech
C.
,
Zamorano
M.
,
Brusi
D.
&
Folch
A.
2016
Nitrate pollution of groundwater; all right…, but nothing else?
Science of The Total Environment
539
,
241
251
.
https://doi.org/10.1016/J.SCITOTENV.2015.08.151
.
Ministry of power
.
2013
Report on the Flow of Water Sources in the Study Area of Varamin
.
Najafi Alamdarlo
H.
,
Ahmadian
M.
&
Khalilian
S.
2016
Groundwater management at varamin plain: the consideration of stochastic and environmental fffects
.
International Journal of Environmental Research
10
(
1
),
21
30
.
https://doi.org/10.22059/ijer.2016.56884
.
Nayyeri
M.
,
Hosseini
S. A.
,
Javadi
S.
&
Sharafati
A.
2021
Spatial differentiation characteristics of groundwater stress index and its relation to land use and subsidence in the Varamin Plain, Iran
.
Natural Resources Research
30
(
1
),
339
357
.
https://doi.org/10.1007/s11053-020-09758-5
.
Noghreyan
A.
,
Samani
J. M.
&
Mazaheri
M.
2022
Comparison of the SINTACS aquifer vulnerability model to nitrate with three-dimensional numerical model (case study of varamin plain aquifer)
.
Iranian Journal of Soil and Water Research
53
(
1
),
15
31
.
https://doi.org/10.22059/ijswr.2022.323930.668975
.
Nouri
B.
,
Nouri
H.
,
Zehtabian
G.
,
Ehsani
A.
,
Khosravi
H.
&
Azarninvand
H.
2020
Estimation of virtual water and water requirement of desert margin vegetation using satellite images (a case study: varamin plain)
.
Journal of Water and Soil Science
23
(
04
),
113
127
.
https://doi.org/10.47176/jwss.23.4.24304
.
Nzama
S. M.
,
Kanyerere
T. O. B.
&
Mapoma
H. W. T.
2021
Using groundwater quality index and concentration duration curves for classification and protection of groundwater resources: relevance of groundwater quality of reserve determination, South Africa
.
Sustainable Water Resources Management
7
(
3
),
31
.
https://doi.org/10.1007/s40899-021-00503-1
.
Raetz
A.
2022
Simulating Groundwater Pollutant Transport for Remediation Design, Antrim County, Michigan
.
Michigan Technological University
.
https://doi.org/10.37099/mtu.dc.etdr/1384
.
Saadatpour
M.
,
Afshar
A.
&
Khoshkam
H.
2019
Multi-objective multi-pollutant waste load allocation model for rivers using coupled archived simulated annealing algorithm with QUAL2Kw
.
Journal of Hydroinformatics
21
(
3
),
397
410
.
https://doi.org/10.2166/hydro.2019.056
.
Sadak
D.
,
Ayvaz
M. T.
&
Elçi
A.
2020
Allocation of unequally-weighted wastewater discharge loads using a simulation-optimization approach
.
Journal of Hydrology
589
,
125158
.
https://doi.org/10.1016/j.jhydrol.2020.125158
.
Samadi-Darafshani
M.
,
Safavi
H. R.
,
Golmohammadi
M. H.
&
Rezaei
F.
2021
Assessment of the management scenarios for groundwater quality remediation of a nitrate-contaminated aquifer
.
Environmental Monitoring and Assessment
193
(
4
).
https://doi.org/10.1007/s10661-021-08978-3
.
Shahraki
Z. M.
,
Mao
X.
,
Waugh
S.
,
Lotfikatouli
S.
,
Walker
H. W.
,
Gobler
C.
&
Wanlass
J.
2020
Potential release of legacy nitrogen from soil surrounding onsite wastewater leaching pools
.
Water Research
169
,
115241
.
https://doi.org/10.1016/j.watres.2019.115241
.
van Afferden
M.
,
Cardona
J. A.
,
Lee
M.-Y.
,
Subah
A.
&
Müller
R. A.
2015
A new approach to implementing decentralized wastewater treatment concepts
.
Water Science and Technology
72
(
11
),
1923
1930
.
https://doi.org/10.2166/wst.2015.393
.
Wada
C. A.
,
Burnett Id
K. M.
,
Okuhata
B. K.
,
Delevaux
J. M. S.
,
Dulai
H.
,
El-Kadi
A. I.
,
Gibson
V.
,
Smith
C.
&
Bremer
L. L.
2021
Identifying wastewater management tradeoffs: costs, nearshore water quality, and implications for marine coastal ecosystems in Kona, Hawai'i
.
https://doi.org/10.1371/journal.pone.0257125
.
This is an Open Access article distributed under the terms of the Creative Commons Attribution Licence (CC BY 4.0), which permits copying, adaptation and redistribution, provided the original work is properly cited (http://creativecommons.org/licenses/by/4.0/).