Water quality has become a significant concern in many river basins in China due to both point and non-point source pollution. The SWAT model assessed pollution reduction scenarios and their effects on Donghe River basin water quality in southwest China. The calibrated model evaluated existing point and non-point emissions. Three schemes reduced point sources by 30, 60, and 90% and non-point sources by 25, 50, and 75%, respectively. Simulations analyzed annual and monthly total phosphorus (TP) concentrations under the scenarios. Results showed that the scenarios effectively improved water quality, meeting Class IV TP standards annually. However, TP exceeded standards in dry months (January–April, December) under all scenarios. A certain degree of negative correlation (R = −0.52, P = 0.11) between TP and rainfall suggests rainfall that influences TP. Comprehensive measures are needed to achieve standards year-round. In summary, the study found that reducing emissions improved Donghe water quality overall but more work is required to meet standards during dry periods. Rainfall correlates with and may affect TP. The work emphasizes implementing comprehensive approaches for year-round water quality improvements in the basin.

  • An appropriate SWAT model was established for the Donghe River Basin.

  • Non-point source pollution in the Donghe River Basin accounts for more than half of the total phosphorus emissions.

  • Rainfall is a critically important factor influencing the variation in total phosphorus concentration in the Donghe River Basin.

  • The months of January to April and December each year constitute the most critical period for total phosphorus pollution in the Donghe River Basin.

Water is not only a fundamental requirement for human life and health (Fath et al. 2017), but also a crucial resource for agriculture, industry, and energy production (Liu et al. 2015). Water quality prediction and management are key aspects of maintaining the health of water bodies and ensuring their sustainable utilization. Accurately predicting changes in water quality trends and identifying factors that influence water quality are essential for effective water resource management and environmental protection strategies (Vamvakeridou-Lyroudia & Karatzas 2017; Wang et al. 2020c). Numerous scholars and researchers worldwide have explored and applied various water quality models and prediction methods to assess and predict the pollution status of water bodies (Zhang et al. 2017b, 2019b; Li et al. 2020a). As a result, a variety of hydrological and water quality models such as water quality modeling network (WQMN) (Peng et al. 2018; Fu et al. 2019; Li et al. 2020a), corps of engineers water quality and eutrophication two-dimensional model (CE-QUAL-W2) (Reckendorfer et al. 2019; Safi et al. 2020), soil and water assessment tool (SWAT) (Zhang et al. 2016; Chen et al. 2020), hydrological simulation program-Fortran (HSPF) (Shoemaker & Brua 2018; Shrestha & Chen 2019), water quality analysis simulation program (QUAL2K) (Yin et al. 2017; Zhang et al. 2020), and aquatic toxicology model (AQUATOX) (Tsai et al. 2018; Wang et al. 2019a) have been successfully applied in various watershed contexts. The speed of updating optimization models using statistical analysis methods (Chen & Huang 2016; Zhang et al. 2018b), artificial intelligence methods (Wu et al. 2019b; Qu & Xia 2020), machine learning methods (Hadjisolomou et al. 2021; Kouadri et al. 2021; AlDahoul et al. 2022), and hybrid methods (Bai et al. 2018; Zeng et al. 2019) has been accelerated. The SWAT model is a widely used tool for watershed hydrological and water quality simulation and management strategy evaluation (Neitsch et al. 2011; Arnold et al. 2012). Initially developed with support from the United States Department of Agriculture-Agricultural Research Service (USDA-ARS), the SWAT model has a development history of over 30 years (Arnold et al. 1998). It is capable of integrating factors such as soil, hydrology, meteorology, and human activities to accurately simulate watershed hydrological and water quality processes, demonstrating high accuracy and reliability in simulating and predicting watershed hydrological processes (Neitsch et al. 2011; Fu et al. 2016). Particularly for mountainous watershed areas, characterized by significant terrain variations, unstable rainfall intensities, diverse land-use types, and complex water cycling processes, numerous studies have shown that the SWAT model performs well in simulating mountainous watershed areas (Gassman et al. 2007; Park et al. 2013; Wu et al. 2017).

As one of the most populous countries in the world, China has a tremendous demand for water resources (Huang & Wang 2019). However, with the accelerated population growth, economic development, and urbanization process, China is facing severe pressure and challenges in water pollution (Zhang et al. 2018a, 2018b, 2018c, Wang et al. 2019a, 2019b). In the Donghe River Basin of Baoshan City, Yunnan Province, water resources are generally insufficient. In recent years, due to rapid urbanization, rapid industrial development, increased agricultural activities, and inadequate matching of pollution control measures, domestic sewage and industrial and agricultural wastewater have been continuously discharged into the river, resulting in the exceeding of water environmental quality standards in the basin. The monitoring results in July 2021 showed that the main and tributary streams in the Donghe River Basin of Baoshan City, Yunnan Province, generally do not meet the Class IV surface water standards, and the main stem is even below Class V standards. The main pollutants in the basin are total phosphorus (TP), ammonia nitrogen (NH3-N), and chemical oxygen demand (COD), with TP being the major pollutant. Therefore, it is urgent to propose a comprehensive and integrated management plan for water environmental pollution in the Donghe River Basin. Preventing and controlling water environmental pollution in the Donghe River Basin is of great significance for local environmental improvement, promoting economic development, and improving people's well-being.

The main objectives of this study are: (1) to establish a highly applicable hydrological and water quality model based on the SWAT model in the Donghe River Basin, and to establish the response relationship between different pollutant emissions and TP concentration using SWAT model technology; (2) to construct three comprehensive pollution reduction scenarios with increasing emission reduction intensities based on the SWAT model, and to predict whether these scenarios can achieve the expected TP concentration standards in the Donghe River Basin; (3) to analyze the driving factors of TP concentration variations in the basin by combining the predictive results of the SWAT model with the actual situation of the basin. The results of this study will contribute to a better understanding of the current water resources status and water quality issues in the Donghe River Basin of Baoshan City, Yunnan Province, and provide references for the development of scientifically sound water resources management and protection strategies. Additionally, this study can provide valuable insights for water resources management and protection in similar basins. The application of the SWAT model will enhance the awareness of the importance of water resources management and support accurate and reliable decision-making for the protection and management of water resources.

Study area description

The Mengboluo River, the largest first-order tributary on the left bank of the lower Nu River, originates from the Monkey Stone Card in the northern part of the runoff area of the Beimiao Reservoir in Longyang District, Baoshan City. It has a total length of 207.6 km. Within Longyang District, the Mengboluo River is called the Donghe River (Zhang et al. 2018c; Wu et al. 2020). The Longyang District (24°46′ ∼ 25°38′N, 98°43′ ∼ 99°26′E) has a river length of 95.4 km and a basin area of 1,431 km2. The terrain is complex and diverse. The entire terrain slopes from northwest to southeast, with elevations ranging from 1,000 to 3,100 m. The central part of the basin is the mountain basin of the Baoshan Dam, which has a relatively gentle slope and covers an area of about 149.9 km2, accounting for 10.48% of the basin area. Other areas in the basin are mainly mountains and hills, with significant differences in slope. The basin has a subtropical monsoon climate, with an average annual precipitation of 967.1 mm and an average annual temperature of 15.5 °C. The climate is mild with abundant rainfall, distinct dry, and wet seasons. The main tributaries of the main stream include Dashan River, Xiaoshan River, Pumenqian River, Xiyi River, Bingma River, and Sancha River. There are four hydrological stations in the Longyang section of the basin: Beimiao Station, Baoshan Station, Xinjie Station, and Hanzhuang Station. The average annual flow rates at these stations are 1.94, 3.97, 7.393, and 0.801 m³/s, respectively. Due to the perennial water storage in the Beimiao Reservoir, the inflow is extremely small, so it is not included in the study area. The water system of the Donghe River Basin is shown in Figure 1.
Figure 1

Diagram of the water system of the Donghe River Basin. The inset (right) is a map of Yunnan Province in China, showing the location of the study area.

Figure 1

Diagram of the water system of the Donghe River Basin. The inset (right) is a map of Yunnan Province in China, showing the location of the study area.

Close modal

There are two sewage treatment plants operating at full capacity in the urban area. The first sewage treatment plant uses the Carrousel oxidation ditch process, and the effluent is discharged into the Donghe River after undergoing ultraviolet disinfection. The second sewage treatment plant uses the oxidation ditch activated sludge process. The effluent from both treatment plants complies with Grade B of the ‘Pollutant Discharge Standards for Urban Sewage Treatment Plants’ (GB18918-2002). However, the current centralized treatment capacity of the domestic sewage treatment plants is small, and the design standards for effluent are relatively low, making it difficult to ensure the complete treatment of sewage in the urban area.

Current status of watershed water pollution

In July 2021, a watershed water quality survey was conducted in the Donghe River Basin with 51 monitoring points established (the locations of monitoring points are detailed in Table 1, and the pollutant detection methods used in this study are described in Table 2). The results indicated that the main pollutants in the watershed were TP, NH3-N, and COD, with TP being the most severe (the TP detection method used in this study is shown in Figure 2). Based on the evaluation criteria of GB3838-2002 ‘Surface Water Environmental Quality Standards,’ TP was used as the assessment indicator to evaluate the water quality of various river sections in the watershed. The evaluation results are presented in Figure 3. From Figure 3, it can be observed that the water quality in the upstream of the Donghe River main channel is relatively good and can meet the standards of surface water Class II. However, as the Donghe River main channel flows southward through the Baoshan Dam area, the water quality deteriorates rapidly and reaches Class V. With the inflow of tributaries such as Taizi River, the water quality further degrades to Class Inferior V due to limited self-purification capacity. Most of the first-order tributaries, including Da Sha River, Xiao Sha River, Xi Yi River, and Bing Ma River, also have water quality classified as Class V or Inferior V. The exceedance rate of TP among the 51 monitoring sections reached 60.8%.
Table 1

Table of monitoring site setup information in the Donghe River Basin

Monitoring point numberLongitudeLatitudeMonitoring point numberLongitudeLatitude
99.2131 25.2354 27 99.2001 25.1070 
99.2203 25.2104 28 99.1997 25.1015 
99.2200 25.2111 29 99.1993 25.0955 
99.2215 25.2057 30 99.1997 25.0940 
99.2210 25.1932 31 99.2009 25.0805 
99.2206 25.1850 32 99.2018 25.0701 
99.2201 25.1782 33 99.2008 25.0776 
99.2192 25.1630 34 99.2009 25.0652 
99.2184 25.1508 35 99.2021 25.0652 
10 99.2184 25.2157 36 99.0202 25.0702 
11 99.2205 25.1848 37 99.2030 25.0578 
12 99.2203 25.1827 38 99.2030 25.0546 
13 99.2201 25.1774 39 99.2037 25.0458 
14 99.2191 25.1675 40 99.2101 25.0346 
15 99.2174 25.1420 41 99.2128 25.0346 
16 99.2173 25.1418 42 99.2005 25.0383 
17 99.2150 25.1364 43 99.2142 25.0296 
18 99.2131 25.1325 44 99.2621 24.9791 
19 99.2096 25.1257 45 99.2337 25.0228 
20 99.2090 25.1227 46 99.2594 24.9839 
21 99.2025 25.1130 47 99.2784 24.9610 
22 99.2086 25.1260 48 99.2968 24.9486 
23 99.2020 25.1122 49 99.3261 24.9793 
24 99.2006 25.1025 50 99.3703 24.9687 
25 99.2091 25.1268 51 99.4454 24.9789 
26 99.2020 25.1122    
Monitoring point numberLongitudeLatitudeMonitoring point numberLongitudeLatitude
99.2131 25.2354 27 99.2001 25.1070 
99.2203 25.2104 28 99.1997 25.1015 
99.2200 25.2111 29 99.1993 25.0955 
99.2215 25.2057 30 99.1997 25.0940 
99.2210 25.1932 31 99.2009 25.0805 
99.2206 25.1850 32 99.2018 25.0701 
99.2201 25.1782 33 99.2008 25.0776 
99.2192 25.1630 34 99.2009 25.0652 
99.2184 25.1508 35 99.2021 25.0652 
10 99.2184 25.2157 36 99.0202 25.0702 
11 99.2205 25.1848 37 99.2030 25.0578 
12 99.2203 25.1827 38 99.2030 25.0546 
13 99.2201 25.1774 39 99.2037 25.0458 
14 99.2191 25.1675 40 99.2101 25.0346 
15 99.2174 25.1420 41 99.2128 25.0346 
16 99.2173 25.1418 42 99.2005 25.0383 
17 99.2150 25.1364 43 99.2142 25.0296 
18 99.2131 25.1325 44 99.2621 24.9791 
19 99.2096 25.1257 45 99.2337 25.0228 
20 99.2090 25.1227 46 99.2594 24.9839 
21 99.2025 25.1130 47 99.2784 24.9610 
22 99.2086 25.1260 48 99.2968 24.9486 
23 99.2020 25.1122 49 99.3261 24.9793 
24 99.2006 25.1025 50 99.3703 24.9687 
25 99.2091 25.1268 51 99.4454 24.9789 
26 99.2020 25.1122    
Table 2

Table of monitoring parameters, methods, and analytical equipment for monitoring sites in the Donghe River Basin

Testing itemTesting methodAnalytical equipment
Permanganate index Chemical titration method 25 ml brown burette 
Five-day biochemical oxygen demand (BOD5Serial dilution and inoculation method 50 ml brown burette 
COD Dichromate method 50 ml brown burette 
TP Ammonium molybdate spectrophotometric method 722S visible spectrophotometer 
Total nitrogen (TN) Alkaline potassium persulfate digestion-UV spectrophotometric method L5S UV-visible spectrophotometer 
Ammonia nitrogen (NH3-N) Nessler's reagent spectrophotometric method 722S visible spectrophotometer 
Anionic surfactant (AS) Methylene blue spectrophotometer 722S visible spectrophotometer 
Fecal coliform bacteria Multiple tube fermentation method SW-CJ-ID single-person purification workstation 
Testing itemTesting methodAnalytical equipment
Permanganate index Chemical titration method 25 ml brown burette 
Five-day biochemical oxygen demand (BOD5Serial dilution and inoculation method 50 ml brown burette 
COD Dichromate method 50 ml brown burette 
TP Ammonium molybdate spectrophotometric method 722S visible spectrophotometer 
Total nitrogen (TN) Alkaline potassium persulfate digestion-UV spectrophotometric method L5S UV-visible spectrophotometer 
Ammonia nitrogen (NH3-N) Nessler's reagent spectrophotometric method 722S visible spectrophotometer 
Anionic surfactant (AS) Methylene blue spectrophotometer 722S visible spectrophotometer 
Fecal coliform bacteria Multiple tube fermentation method SW-CJ-ID single-person purification workstation 
Figure 2

Total phosphorus detection method in the Dong River Basin.

Figure 2

Total phosphorus detection method in the Dong River Basin.

Close modal
Figure 3

The current situation of water environment quality in the Donghe River Basin.

Figure 3

The current situation of water environment quality in the Donghe River Basin.

Close modal

Among various pollutant indicators such as TP, COD, and NH3-N, we selected TP as the focus of our study based on several considerations: (1) Our previous sampling and testing of the water and sediments in various river sections of the study area revealed that TP was the most severe pollutant, significantly impacting water quality deterioration. (2) TP is widely recognized as an important indicator of eutrophication and water quality pollution and is extensively used in water environmental research and management. Exploring its concentration variation can provide further insights into the extent of agricultural, industrial, domestic, and livestock and poultry emissions' impact on water quality (Zhang et al. 2019a; Liu et al. 2020a). (3) TP is closely related to the stability and health of aquatic ecosystems, making its study crucial for understanding water health conditions and environmental management (Huang et al. 2021).

SWAT model

Building SWAT model

The operation of the SWAT model requires a substantial amount of input data, which can be broadly categorized as spatial data and attribute data. Spatial data include digital elevation models, land-use types, soil types (Figure 4), and so on. (For more detailed information on land use, please refer to Table 3. For more detailed information on soil, please refer to Table 4), (Yang et al. 2019), while attribute data include meteorological databases, land-use status, soil physical and chemical properties, hydrological and water quality data, as well as pollutant source data (Li et al. 2020b; Zhang et al. 2021b). The data sources and descriptions for various data types in the model are presented in Table 5. In this study, the ArcGIS 10.2 platform was utilized for data preprocessing of the input data for the SWAT model. This involved masking extraction of the DEM data within the study area range, projection transformation of geospatial raster data, such as DEM, land-use type map, and soil type map to the Albers equal area conic projection, and establishing connections between geospatial and non-spatial data. The meteorological data used in the model consisted of daily maximum temperature, minimum temperature, precipitation, wind speed, and humidity data from the Baoshan meteorological station for the period of 2017–2020. Solar radiation data were simulated using a weather generator.
Table 3

Land-use types and area statistics table of the Donghe River Basin

NumberLand-use classificationLand-use classification codesArea (km2)Proportion (%)
Construction land URHD 67.83 4.98 
Forest land FRST 781.40 57.41 
Water area WATR 6.21 0.46 
Wetland WETL 0.23 0.02 
Cultivated land ARGL 354.50 26.04 
Grassland PAST 133.68 9.82 
Bare land BARR 17.30 1.27 
NumberLand-use classificationLand-use classification codesArea (km2)Proportion (%)
Construction land URHD 67.83 4.98 
Forest land FRST 781.40 57.41 
Water area WATR 6.21 0.46 
Wetland WETL 0.23 0.02 
Cultivated land ARGL 354.50 26.04 
Grassland PAST 133.68 9.82 
Bare land BARR 17.30 1.27 
Table 4

Soil types and area statistics table of the Donghe River Basin

NumberSoil seriesSoil classSoil taxonomy codesArea (km2)Proportion (%)
Hcmp ash-soaked soil Yellow-brown soil MHPN 7.77 0.59 
Black foam soil Limestone soil HPT 44.62 3.39 
Chicken manure soil Paddy soil JFTT 234.27 17.8 
Dark red soil Rice soil AHNT 8.42 0.64 
Lancang red soil Red soil LCCHN 127.14 9.66 
Mojiang red soil Ferric soil MJCNT 573.18 43.55 
Huangda soil Yellow soil HDT 320.87 24.38 
NumberSoil seriesSoil classSoil taxonomy codesArea (km2)Proportion (%)
Hcmp ash-soaked soil Yellow-brown soil MHPN 7.77 0.59 
Black foam soil Limestone soil HPT 44.62 3.39 
Chicken manure soil Paddy soil JFTT 234.27 17.8 
Dark red soil Rice soil AHNT 8.42 0.64 
Lancang red soil Red soil LCCHN 127.14 9.66 
Mojiang red soil Ferric soil MJCNT 573.18 43.55 
Huangda soil Yellow soil HDT 320.87 24.38 
Table 5

SWAT model data type and description

Data typeData nameData sourceData description
Spatial data DEM data Geo-cloud spatial data center 30 × 30 m, elevation, slope, etc. 
Land-use data CLCD Data set 30 × 30 m, land-use type and spatial distribution 
Soil type and attribute data HWSD China soil database 1: 1 million, soil species, and spatial distribution 
Attribute data Meteorological data Baoshan Meteorological Bureau Daily temperature, precipitation, wind speed, and humidity from 2017 to 2020 
Hydrological data of the hydrological station Baoshan Hydrology Bureau Daily runoff of Baoshan, Hanzhuang, and Xinjie hydrological stations in 2017 and 2020 
Water quality data of monitoring section Baoshan Municipal Bureau of Ecological Environment Average monthly NH3-N and TP concentrations in water quality monitoring sections of Shaba, Shilongping, and Dieshui River Bridge from 2017 to 2020 
Pollution source data Baoshan Municipal Bureau of Ecological Environment Emission modes and emissions of various pollution sources from 2020 to 2021 
Data typeData nameData sourceData description
Spatial data DEM data Geo-cloud spatial data center 30 × 30 m, elevation, slope, etc. 
Land-use data CLCD Data set 30 × 30 m, land-use type and spatial distribution 
Soil type and attribute data HWSD China soil database 1: 1 million, soil species, and spatial distribution 
Attribute data Meteorological data Baoshan Meteorological Bureau Daily temperature, precipitation, wind speed, and humidity from 2017 to 2020 
Hydrological data of the hydrological station Baoshan Hydrology Bureau Daily runoff of Baoshan, Hanzhuang, and Xinjie hydrological stations in 2017 and 2020 
Water quality data of monitoring section Baoshan Municipal Bureau of Ecological Environment Average monthly NH3-N and TP concentrations in water quality monitoring sections of Shaba, Shilongping, and Dieshui River Bridge from 2017 to 2020 
Pollution source data Baoshan Municipal Bureau of Ecological Environment Emission modes and emissions of various pollution sources from 2020 to 2021 

Note: CLCD stands for ‘Current Land Cover Database’ and HWSD stands for ‘Harmonized World Soil Database’.

Figure 4

Spatial data presentation. (a) Elevation map of Donghe River Basin. (b) Land-use map of the Donghe River Basin. (c) Soil type map of Donghe River Basin.

Figure 4

Spatial data presentation. (a) Elevation map of Donghe River Basin. (b) Land-use map of the Donghe River Basin. (c) Soil type map of Donghe River Basin.

Close modal
The subdivision of sub-basins and hydrological response units (HRUs) was achieved through the application of the ‘burn-in’ algorithm to the digital river network layer (Neitsch et al. 2005). This algorithm is based on the concepts of network dilation and erosion and selectively removes non-main tributaries while preserving the main flow paths and basin structure. It offers advantages over other algorithms in terms of improving model accuracy and interpretability. Subsequently, flow accumulation calculations were performed to obtain the basin boundaries and corresponding river network. Furthermore, the sub-basins were further divided into smaller HRUs by setting thresholds for land-use types, soil types, and slopes (Gassman et al. 2007; Chen et al. 2021b). Each HRU was assigned the same land-use conditions, soil characteristics, and slope. As a result, a total of 94 sub-basins (Figure 5) and 752 HRUs were delineated.
Figure 5

Sub-basin division of the Donghe River Basin.

Figure 5

Sub-basin division of the Donghe River Basin.

Close modal

Based on the reference year of 2020, the point source and non-point source pollution emissions of TP in the Donghe River Basin were calculated (refer to the information on TP pollution source analysis in Table 6). Point source pollution mainly includes industrial point sources, urban sewage treatment plants, and livestock and poultry farming. A point source database was compiled based on the emission characteristics and TP discharge of point sources, and it was incorporated into the SWAT model. Non-point sources were calculated at the sub-basin level and then coupled with HRUs in the model. Non-point source loads of HRUs were obtained through weight allocation (Zhang et al. 2021a). However, from Table 6, we can observe that the largest contributor to TP emissions is non-point source pollution from domestic sources, accounting for 50.6% of the TP emissions. Agricultural non-point source pollution is the next important contributor, accounting for 27.7%.

Table 6

Summary of emissions from TP pollution sources in the study area

All kinds of pollution sourcesTP emission (t·a−1)Proportion (%)
Point source Sewage treatment plant 10.8 
Industrial sewage outlet 2.4 
 Livestock and poultry breeding pollution 8.4 
Non-point source Domestic non-point source pollution 42 50.6 
Farmland non-point source pollution 23 27.7 
Total 83 100 
All kinds of pollution sourcesTP emission (t·a−1)Proportion (%)
Point source Sewage treatment plant 10.8 
Industrial sewage outlet 2.4 
 Livestock and poultry breeding pollution 8.4 
Non-point source Domestic non-point source pollution 42 50.6 
Farmland non-point source pollution 23 27.7 
Total 83 100 

Calibration and validation of SWAT model

SWAT-CUP is a tool specifically designed for calibration and validation of the SWAT model (Abbaspour et al. 2007a, 2015). It provides a comprehensive set of statistical methods and algorithms to help researchers optimize model parameters and improve model performance and accuracy. We used the SWAT-CUP software to calibrate and validate the constructed SWAT model. The SUFI-2 algorithm (Arnold et al. 2012) has the advantage of a global search for the optimal solution, the CE-UA algorithm (Duan et al. 1994) has the advantages of global search and adaptive adjustment, and the trial-and-error method has the advantage of flexible adjustment based on specific problems and actual conditions. We comprehensively used the SUFI-2 algorithm (a global optimization algorithm for uncertainty analysis of model parameters), the SCE-UA algorithm, and the trial-and-error method, following the principle of adjusting runoff parameters before adjusting nutrient parameters (Moriasi et al. 2007), to select sensitive parameters for runoff and TP(The specific calibrated hydrological parameters and water quality parameters can be found in Tables 7 and 8, respectively). The period from 2017 to 2018 was selected as the warm-up period for parameter calibration, and the period from 2019 to 2020 was used for validation. The calibration and validation of runoff and TP simulation results were conducted at a monthly time scale. The specific calibration and validation process is as follows: firstly, the runoff parameters were calibrated and validated using the hydrological stations in Baoshan, Hanzhuang, and Xinjie. Then, the monthly average TP concentration data from the Sandaba and Shilongping national control sections were multiplied by the simulated water quantity data to obtain TP loads as the observed values for calibration and validation of nutrient parameters in the watershed.

Table 7

Calibration of runoff process parameters in the Donghe River basin

Hydrological parameters
ParametersSimulation processDescriptionParameter rangeFinal value
CN_AGRL Surface runoff Number of runoff curves of agricultural land 40~80 79 
CN_FRST Surface runoff Number of forestland runoff curve 40~80 41 
CN_PAST Surface runoff Number of grassland runoff curve 40~80 65 
ESCO Evapotranspiration Soil evaporation compensation coefficient 0~1 0.49 
CANMX Evapotranspiration Canopy interception of vegetation 0~100 3.95 
GW_REVAP Groundwater Groundwater evaporation coefficient 0~0.2 0.079 
GWQMN Groundwater Critical value of regression flow in shallow groundwater 0~2 1.13 
ALPHA_BF Groundwater α coefficient of basic flow 0~1 0.73 
REVAPMN Groundwater Critical value of shallow groundwater evaporation 0~10 1.59 
CH_N2 River channel flow Manning coefficient of main channel 0~0.3 0.238 
CN_K2 River channel flow Effective hydraulic conductivity of main river 5~50 9.57 
SOL_AWC Soil Surface soil moisture bulk density 0–1 0.02 
SOL_K Soil Saturated hydraulic conductivity −0.8 to 0.8 −0.56 
SOL_ALB Soil Wet soil reflectance 0–0.25 0.183 
SFTMP Soil Snowfall temperature −5 to 5 4.81 
BIOMIX Surface runoff Biological mixing efficiency coefficient 0–1 0.19 
Hydrological parameters
ParametersSimulation processDescriptionParameter rangeFinal value
CN_AGRL Surface runoff Number of runoff curves of agricultural land 40~80 79 
CN_FRST Surface runoff Number of forestland runoff curve 40~80 41 
CN_PAST Surface runoff Number of grassland runoff curve 40~80 65 
ESCO Evapotranspiration Soil evaporation compensation coefficient 0~1 0.49 
CANMX Evapotranspiration Canopy interception of vegetation 0~100 3.95 
GW_REVAP Groundwater Groundwater evaporation coefficient 0~0.2 0.079 
GWQMN Groundwater Critical value of regression flow in shallow groundwater 0~2 1.13 
ALPHA_BF Groundwater α coefficient of basic flow 0~1 0.73 
REVAPMN Groundwater Critical value of shallow groundwater evaporation 0~10 1.59 
CH_N2 River channel flow Manning coefficient of main channel 0~0.3 0.238 
CN_K2 River channel flow Effective hydraulic conductivity of main river 5~50 9.57 
SOL_AWC Soil Surface soil moisture bulk density 0–1 0.02 
SOL_K Soil Saturated hydraulic conductivity −0.8 to 0.8 −0.56 
SOL_ALB Soil Wet soil reflectance 0–0.25 0.183 
SFTMP Soil Snowfall temperature −5 to 5 4.81 
BIOMIX Surface runoff Biological mixing efficiency coefficient 0–1 0.19 
Table 8

Calibration of nitrogen and phosphorus parameters in the Donghe River basin

Water quality parameters
ParametersDescriptionParameter rangeFinal value
SPCON Sediment transport linear coefficient 0.001–0.1 0.04 
SPEXP Sediment transport exponent coefficient 1–1.5 1.21 
RSDCO Crop residue mineralization rate 0.02–0.1 0.01 
N_UPDIS Nitrogen uptake distribution parameter 20–100 46.09 
SDNCO Soil moisture threshold for denitrification 0–1 0.76 
PPERCO Phosphorus infiltration coefficient 10–18 16.88 
PHOSKD Soil phosphorus distribution coefficient 100–200 90.21 
PSP Phosphorus effectiveness index 0.01–0.7 0.25 
USLE_P Universal soil loss equation (USLE) conservation practice factor 0–1 0.69 
SLSUBBSN Mean slope length 0–100 30.02 
USLE_K Soil erosion factor 0–0.65 0.10 
SOL_ORGN Initial concentration of soil organic nitrogen 20–100 80.29 
BC1 Ammonium nitrogen biological oxidation rate 0.1–1 0.32 
ERORGN Nitrogen infiltration coefficient 0–5 2.14 
ERORGP Phosphorus infiltration coefficient 0–5 0.06 
SOL_ORGP Initial concentration of soil organic phosphorus 0–100 66.47 
Water quality parameters
ParametersDescriptionParameter rangeFinal value
SPCON Sediment transport linear coefficient 0.001–0.1 0.04 
SPEXP Sediment transport exponent coefficient 1–1.5 1.21 
RSDCO Crop residue mineralization rate 0.02–0.1 0.01 
N_UPDIS Nitrogen uptake distribution parameter 20–100 46.09 
SDNCO Soil moisture threshold for denitrification 0–1 0.76 
PPERCO Phosphorus infiltration coefficient 10–18 16.88 
PHOSKD Soil phosphorus distribution coefficient 100–200 90.21 
PSP Phosphorus effectiveness index 0.01–0.7 0.25 
USLE_P Universal soil loss equation (USLE) conservation practice factor 0–1 0.69 
SLSUBBSN Mean slope length 0–100 30.02 
USLE_K Soil erosion factor 0–0.65 0.10 
SOL_ORGN Initial concentration of soil organic nitrogen 20–100 80.29 
BC1 Ammonium nitrogen biological oxidation rate 0.1–1 0.32 
ERORGN Nitrogen infiltration coefficient 0–5 2.14 
ERORGP Phosphorus infiltration coefficient 0–5 0.06 
SOL_ORGP Initial concentration of soil organic phosphorus 0–100 66.47 

Deterministic coefficient (R2) is a commonly used evaluation metric that measures the extent to which the model explains the variance of the observed data. A higher R2 value indicates a better agreement between the simulated values in the SWAT model and the observed values. Nash coefficient (NSE) is a comprehensive evaluation criterion that combines the Nash–Sutcliffe Efficiency (NSE) and the root mean square error (RMSE). It considers both the accuracy and variability of the model, providing a more comprehensive assessment of the simulation performance. By calculating NSE, we can consider the model's ability to simulate the hydrological processes in the watershed (Sun et al. 2020a; Xu et al. 2020), including the agreement between the mean, variance, and temporal aspects of the simulated and observed values. The closer the values of R2 and NSE are to 1, the better the model's simulation performance. The formulas for calculating R2 and NSE are as follows:
(1)
(2)

In Equations (1) and (2), represents the observed values, represents the simulated values, represents the multi-year average observed values, n represents the number of samples.

We select the deterministic coefficient (R2) and Nash coefficient (NSE) to evaluate the simulation effect of the model (Sun et al. 2020a; Xu et al. 2020), the calibration and validation results can be found in Figures 69, and the evaluation results are shown in Table 9. As can be seen from Table 9, the deterministic coefficient (R2) and Nash coefficient (NSE) of runoff simulation at Baoshan Station, Hanzhuang Station, and Xinjie Station are all greater than 0.8, the deterministic coefficient (R2) of TP load simulation at Shaba and Shilongping section are all greater than 0.8, and the Nash coefficient (NSE) is more significant than 0.7. This illustrates that the simulated runoff and TP agree with the measured values, indicating that the calibrated SWAT model can effectively simulate the runoff characteristics and TP migration process in the Donghe River Basin. Additionally, the data input sequence and operational logic of the model in this study are described in detail in Figure 10.
Table 9

Calibration parameters of runoff and TP simulation process

ParametersSite/sectionRate period
Validation period
R2ENSR2ENS
Runoff Baoshan Station 0.82 0.81 0.81 0.78 
Hanzhuang Station 0.88 0.87 0.85 0.86 
Xinjie Station 0.87 0.80 0.84 0.76 
TP Shaba 0.85 0.73 0.82 0.72 
Shilongping 0.90 0.76 0.88 0.73 
ParametersSite/sectionRate period
Validation period
R2ENSR2ENS
Runoff Baoshan Station 0.82 0.81 0.81 0.78 
Hanzhuang Station 0.88 0.87 0.85 0.86 
Xinjie Station 0.87 0.80 0.84 0.76 
TP Shaba 0.85 0.73 0.82 0.72 
Shilongping 0.90 0.76 0.88 0.73 
Figure 6

The figure illustrates the monthly streamflow of three hydrological stations in the lower Donghe River basin, including observed and simulated data. The vertical dashed line divides the study period into a calibration period (January 2017–June 2019) and a validation period (July 2019–December 2020). The calibration and validation periods' values of the coefficient of determination (R2) and NSE are provided below each hydrological station graph. (a) Baoshan Station, (b) Hanzhuang Station, (c) Xinjie Station.

Figure 6

The figure illustrates the monthly streamflow of three hydrological stations in the lower Donghe River basin, including observed and simulated data. The vertical dashed line divides the study period into a calibration period (January 2017–June 2019) and a validation period (July 2019–December 2020). The calibration and validation periods' values of the coefficient of determination (R2) and NSE are provided below each hydrological station graph. (a) Baoshan Station, (b) Hanzhuang Station, (c) Xinjie Station.

Close modal
Figure 7

The figure shows the fit between observed and simulated monthly streamflow data from three hydrological stations in the Donghe River basin using the SWAT model. (a) Baoshan Station, (b) Hanzhuang Station, (c) Xinjie Station.

Figure 7

The figure shows the fit between observed and simulated monthly streamflow data from three hydrological stations in the Donghe River basin using the SWAT model. (a) Baoshan Station, (b) Hanzhuang Station, (c) Xinjie Station.

Close modal
Figure 8

The figure presents the observed and simulated data of total phosphorus for two monitoring stations in the lower Donghe River basin. The vertical dashed line divides the study period into a calibration period (January 2017–December 2018) and a validation period (January 2019–April 2020). The coefficient of determination (R2) and NSE values for the calibration and validation periods are provided below each monitoring station graph. (a) Shaba Monitoring station, (b) Shilongping Monitoring station.

Figure 8

The figure presents the observed and simulated data of total phosphorus for two monitoring stations in the lower Donghe River basin. The vertical dashed line divides the study period into a calibration period (January 2017–December 2018) and a validation period (January 2019–April 2020). The coefficient of determination (R2) and NSE values for the calibration and validation periods are provided below each monitoring station graph. (a) Shaba Monitoring station, (b) Shilongping Monitoring station.

Close modal
Figure 9

The figure represents the fitting of observed and simulated monthly total phosphorus loads in two monitoring stations in the lower Donghe River basin using the SWAT model. (a) Shaba Monitoring station, (b) Shilongping Monitoring station.

Figure 9

The figure represents the fitting of observed and simulated monthly total phosphorus loads in two monitoring stations in the lower Donghe River basin using the SWAT model. (a) Shaba Monitoring station, (b) Shilongping Monitoring station.

Close modal
Figure 10

The data input sequence and operational logic of the SWAT model in the Donghe Basin are described in detail.

Figure 10

The data input sequence and operational logic of the SWAT model in the Donghe Basin are described in detail.

Close modal

Setting scenarios

The objectives that need to be met in setting up the scenarios for this study are as follows: (1) the implemented emission reduction scenarios should achieve a significant reduction in emissions. (2) The selected emission reduction scenarios should have low-cost investment and high operational feasibility (Liu et al. 2020c). (3) The selected emission reduction scenarios should comply with local policies for the ecological environment and water resource protection (Jin et al. 2019).

According to the investigation results of TP pollution sources in the Donghe River Basin presented in Table 6, the top three sources of TP emissions are domestic non-point sources, agricultural non-point sources, and sewage treatment plant point sources, accounting for 50.6, 27.7, and 10.8% of the TP emissions, respectively. Therefore, based on this scenario concept, we propose the construction of three new sewage treatment plants around the urban area and the upgrading of all sewage treatment plants in terms of operational scale and pollutant discharge standards to increase the collection rate of urban domestic wastewater and reduce pollution from domestic non-point sources near the urban area. Additionally, in sub-basins 26 and 28, a water diversion project will be implemented to dilute the TP concentration in the urban river section and prevent excessive pollution load. Furthermore, measures will be taken to address rural domestic wastewater, industrial pollution sources, and livestock and poultry farming sources located away from the urban area, aiming to continuously improve the TP concentration in the entire basin (the actual layout of the new sewage treatment plants and their drainage areas can be found in Figure 11(a), while the information about the water replenishment locations in the basin is shown in Figure 11(b)).
Figure 11

Schematic diagram of urban sewage treatment and water refill points in basin. (a) The map of urban pollution control, (b) the map of Basin water refill.

Figure 11

Schematic diagram of urban sewage treatment and water refill points in basin. (a) The map of urban pollution control, (b) the map of Basin water refill.

Close modal

To achieve this, a baseline scenario was established as a reference along with three gradually increasing reduction scenarios. In the three scenarios, pollution from domestic non-point sources will be reduced by 25, 50, and 75%, respectively, while point source pollution will be reduced by 30, 60, and 90%, respectively. In scenarios 2 and 3, water diversion will be implemented in the urban river section. (See Tables 10 and 11 for the scenario settings in the Donghe River Basin).

Table 10

Reduction status of pollution sources

Scenario schemeReduction situation
Non-point sourcePoint source
Benchmark scheme Reduction of 0% Reduction of 0% 
Scenario 1 Reduction of 25% Reduction of 30% 
Scenario 2 Reduction of 50% Reduction of 60% 
Scenario 3 Reduction of 75% Reduction of 90% 
Scenario schemeReduction situation
Non-point sourcePoint source
Benchmark scheme Reduction of 0% Reduction of 0% 
Scenario 1 Reduction of 25% Reduction of 30% 
Scenario 2 Reduction of 50% Reduction of 60% 
Scenario 3 Reduction of 75% Reduction of 90% 
Table 11

Actual implementation of reduction measures for each pollution source

Scenario contentScenario scheme
Benchmark schemeReduction scenarios
Scenario 1Scenario 2Scenario 3
Urban sewage treatment plant and pipe network project Sewage treatment plant 1 30,000 m3/day, Class IV standards. 30,000 m3/day, first-class B standard. 30,000 m3/day first-class A standard. 30,000 m3/day first-class A standard. 
Sewage treatment plant 2 20,000 m3/day, Class IV standards. 20,000 m3/day, first-class B standard. 20,000 m3/day first-class A standard. 25,000 m3/day first-class A standard. 
Sewage treatment plant 3 Not running 20,000 m3/day, first-class B standard. 25,000 m3/day, first-class A standard. 30,000 m3/day, the first-class A standard. 
Industrial and trade park sewage treatment plant Not running Not running 15,000 m3/day, first-class B standard. 40,000 m3/day, first-class A standard. 
Byatang sewage Station Not running Not running 3,400 m3/day, first-class A standard.  
Water diversion and replenishment project of river basin None None Water diversion 50,000 m3/day Water diversion 100,000 m³/day 
Rural domestic sewage The effluent implements the secondary standard of DB53/T953-2019. 
Industrial pollution source Basically maintained the status quo 
Livestock and poultry breeding source     
Agricultural non-point source     
Scenario contentScenario scheme
Benchmark schemeReduction scenarios
Scenario 1Scenario 2Scenario 3
Urban sewage treatment plant and pipe network project Sewage treatment plant 1 30,000 m3/day, Class IV standards. 30,000 m3/day, first-class B standard. 30,000 m3/day first-class A standard. 30,000 m3/day first-class A standard. 
Sewage treatment plant 2 20,000 m3/day, Class IV standards. 20,000 m3/day, first-class B standard. 20,000 m3/day first-class A standard. 25,000 m3/day first-class A standard. 
Sewage treatment plant 3 Not running 20,000 m3/day, first-class B standard. 25,000 m3/day, first-class A standard. 30,000 m3/day, the first-class A standard. 
Industrial and trade park sewage treatment plant Not running Not running 15,000 m3/day, first-class B standard. 40,000 m3/day, first-class A standard. 
Byatang sewage Station Not running Not running 3,400 m3/day, first-class A standard.  
Water diversion and replenishment project of river basin None None Water diversion 50,000 m3/day Water diversion 100,000 m³/day 
Rural domestic sewage The effluent implements the secondary standard of DB53/T953-2019. 
Industrial pollution source Basically maintained the status quo 
Livestock and poultry breeding source     
Agricultural non-point source     

Note:30,000 m3 /day represents the operation scale;Class IV of surface water standards represents the Class IV effluent water quality standard for surface water discharge, with total phosphorus ≤ 1 mg/L; First-class B standard represents the first-class B effluent quality standard, with total phosphorus ≤ 1 mg/L; First-class A standard represents the first-class A effluent quality standard, with total phosphorus ≤ 0.5 mg/L; Secondary standard of DB53/T953-2019 represents the secondary effluent standard stipulated in DB53/T953-2019, with total phosphorus ≤ 1.5 mg/L.

To better reflect the interannual variation of TP concentration in the Donghe River Basin, the cumulative departure percentage of annual flow was calculated based on the natural flow data from the Baoshan hydrological station for the years 2007–2020. The year 2018 was determined as a wet year, while 2019 was identified as a dry year (Zhang et al. 2009; Yang et al. 2013; Sun et al. 2020b). Using the meteorological and runoff conditions of 2018 and 2019, the TP load under the baseline scenario and the three reduction scenarios were simulated, and the resulting concentration changes were inferred.

Result analysis

To clearly illustrate the improvement in TP concentration resulting from the three reduction scenarios in the Donghe River Basin, we selected the Shuangqiao (Dashahe), Shuangqiao (Donghe), Shilongping, and Dieshuiheqiao monitoring sections to analyze the changes in TP concentration. These sections represent the Dashariver tributary entering the Donghe River, the midstream near the urban area of the Donghe River, and the downstream entering the Nu River, respectively (Guo et al. 2018; Li et al. 2019a; Wu et al. 2019a). The TP concentration of the baseline scenario and the reduction scenarios in each section were analyzed using GB3838-2002 ‘Environmental Quality Standards for Surface Water’ as the evaluation criteria. The annual average TP concentration and monthly average TP concentration changes in the four monitoring sections during wet and dry years are shown in Figures 12 and 13, respectively. The monthly average rainfall in 2018 and 2019 is shown in Figure 14.
Figure 12

Annual mean concentration of TP in four monitoring sections during wet and dry years. (a) The annual mean TP concentration of four monitoring sections in wet year. (b) The annual mean TP concentration of four monitoring sections in dry year.

Figure 12

Annual mean concentration of TP in four monitoring sections during wet and dry years. (a) The annual mean TP concentration of four monitoring sections in wet year. (b) The annual mean TP concentration of four monitoring sections in dry year.

Close modal
Figure 13

The variation of monthly mean TP concentration in wet and dry years in four monitoring sections. (a) The variation of monthly mean TP concentration in four monitoring sections in wet years. (b) The variation of monthly mean TP concentration in four monitoring sections in dry years.

Figure 13

The variation of monthly mean TP concentration in wet and dry years in four monitoring sections. (a) The variation of monthly mean TP concentration in four monitoring sections in wet years. (b) The variation of monthly mean TP concentration in four monitoring sections in dry years.

Close modal
Figure 14

Monthly average rainfall in wet and dry years.

Figure 14

Monthly average rainfall in wet and dry years.

Close modal

Analysis of annual mean concentration change

The changes in TP annual average concentration in the four monitoring sections during wet and dry years are shown in Figure 12. According to Figure 12, the Shuangqiao (Dashahe) section has a TP annual average concentration that falls within Class V in the baseline scenario. In the three reduction scenarios, the TP annual average concentration in this section meets Class II standards, and it is observed that there is minimal variation in TP concentration across the three scenarios. The Shuangqiao (Donghe), Shilongping, and Dieshuiheqiao sections have TP annual average concentrations in the baseline scenario that are classified as Class V. In the three reduction scenarios, the TP annual average concentrations in these sections meet Class IV to Class III standards. Among them, for the section of the Donghe River, the Shuangqiao (Donghe) section has higher TP concentrations compared to the Shilongping and Dieshuiheqiao sections in the baseline scenario, indicating higher phosphorus loading and more severe TP pollution in the urban river section.

The Shuangqiao (Donghe) section shows a greater reduction in TP concentration compared to the Shilongping and Dieshuiheqiao sections, indicating that the primary measures of reducing pollution from non-point sources and dilution through water diversion in the urban river section have a more significant impact on improving TP concentration in the middle reaches of the Donghe River. This demonstrates the effectiveness of scaling up sewage treatment plants and improving discharge standards in improving water quality. Under Scenario 1 and Scenario 2 conditions, there is little change in TP concentration in the Shilongping and Dieshuiheqiao sections. Only when the sewage collection rate and water quality are significantly improved at the industrial and commercial park sewage treatment plant in Scenario 3, do these sections show some improvement in TP concentration. This indicates that TP concentration in these two monitoring sections is significantly influenced by centralized sewage treatment in the industrial and commercial parks.

In terms of interannual variations, during dry years, the flow rate in the Donghe River basin is lower, resulting in slower water velocity and reduced exchange with the surroundings. This limited exchange makes TP less likely to diffuse, leading to higher TP concentrations in the basin during dry years. Compared to wet years, it is more challenging to meet the TP concentration standards during dry years.

From a spatial distribution perspective, the order of TP concentrations in the monitored sections, including Shuangqiao (Dashahe), Shuangqiao (Donghe), Shilongping, and Dieshuiheqiao, under the emission reduction scenarios can be roughly summarized as follows: Dieshuiheqiao > Shilongping > Shuangqiao (Donghe) > Shuangqiao (Dashahe). Along the mainstream of the Donghe River, these sections are sequentially distributed from the middle to the lower reaches. The following reasons contribute to this pattern: (1) As the river flows from the upper to middle reaches, the water volume gradually increases, while the lower reaches may experience reduced flow velocity, decreased water volume, and insufficient hydraulic energy. This can result in slow water flow and lower velocity in the downstream section, weakening the transport and dilution capacity of TP, and increasing the risk of TP accumulation in the water. (2) The downstream section of the river is more susceptible to other pollution sources, such as non-point source pollution from agricultural fields, livestock farming, industrial sources, and rural domestic sewage. (3) In the scenario plan, the reduction in TP emissions from non-point source pollution is not uniformly distributed across the entire basin but rather varies based on the establishment of wastewater treatment plants in specific areas and the improvement of discharge standards. Since the coverage of wastewater treatment plants is limited to certain regions, the establishment of a treatment plant in a specific area may contribute significantly to reducing TP concentrations in nearby river sections, while the improvement in TP conditions in the entire basin may not be as pronounced. Therefore, the order in which wastewater treatment plants are established may also have some influence on the results.

In general, the annual average TP concentrations in the four monitored sections show an overall decreasing trend in both wet and dry years under the three emission reduction scenarios. Furthermore, the TP concentrations under the emission reduction scenarios are significantly lower than those under the baseline scenario. All three emission reduction scenarios can ensure that the annual average TP concentrations in the tributaries of the Dashariver and the main stream of the Donghe River, which flows into the Nu River, meet the water quality standards. This indicates that by implementing different emission reduction scenarios, it is possible to effectively reduce TP concentrations and improve water quality in the Donghe River Basin. Moreover, these improvements in TP concentrations are stable and consistent under different annual conditions.

Analysis of monthly mean concentration change

The monthly average TP concentration variations in the four monitored sections during wet and dry years are shown in Figure 13. According to Figure 13, under the baseline scenario, the tributary section of Shuangqiao (Dashariver) meets the Class III standard for only 4 months throughout the year, while in the emission reduction scenarios, it fails to meet the Class III standard in May during wet years and in April during dry years. Shuangqiao (Donghe), Shilongping, and Dieshuihe Bridge sections under the baseline scenario only meet the Class IV standard in July or August and fail to meet the standard in the remaining months. Under scenario 1, TP concentrations do not meet the standard from January to April, and under scenario 2, TP concentrations do not meet the standard in January, March, and April. In scenario 3, TP concentrations in April during dry years do not meet the standard. It can be observed that the number of non-compliant months decreases significantly under the emission reduction scenarios. The non-compliant months in the four monitoring sections are mostly concentrated in January to April, and among these months, TP concentrations in dry years are generally higher compared to wet years.

In terms of seasonal variations, the TP concentrations in the four monitoring sections of the Donghe River Basin generally exhibit an increase during winter and spring, followed by a decrease during summer and autumn. They rise from January to April, reaching the peak TP concentration during March and April, and gradually decrease in a fluctuating pattern from May to October. There is a slow increase again in TP concentrations from November to December. Based on Table 12, it can be observed that there is a certain degree of negative correlation between changes in TP concentration and rainfall in the watershed. The Donghe River Basin experiences distinct wet and dry seasons, with a long and abundant rainy season during summer and autumn. During this period, TP concentrations in the river are reduced due to dilution from rainfall. However, during the dry season of winter and spring, with less rainfall and reduced groundwater replenishment, decreased flow and insufficient hydraulic energy, TP accumulates in the water, leading to an increase in TP concentrations. From a seasonal perspective, the dry season extends from early November to late April of the following year, indicating that TP concentrations in the Donghe River Basin reach a peak in March and April each year. During the TP concentration peak, the order of TP concentrations from high to low in the monitoring sections is roughly as follows: Dieshuihe Bridge > Shilongping > Shuangqiao (Donghe) > Shuangqiao (Dashahe).

Table 12

The correlation and significance test for the relationship between the monthly average TP concentrations and monthly rainfall of each monitoring section under the three emission reduction scenarios

Monitoring sectionsPearson correlation coefficient
Wet year
Dry year
rP-valuerP-value
Shuangqiao (Dashahe) Scenario 1 −0.63 0.0293 −0.63 0.0296 
Scenario 2 −0.54 0.0727 −0.60 0.0399 
Scenario 3 −0.51 0.0899 −0.59 0.0456 
Shuangqiao (Donghe) Scenario 1 −0.57 0.0507 −0.60 0.0405 
Scenario 2 −0.67 0.2421 −0.48 0.1180 
Scenario 3 −0.48 0.0842 −0.41 0.1845 
Shilongping Scenario 1 −0.54 0.0706 −0.56 0.0596 
Scenario 2 −0.44 0.2818 −0.46 0.1330 
Scenario 3 −0.54 0.1472 −0.40 0.0013 
Dieshuiheqiao Scenario 1 −0.55 0.1949 −0.44 0.1542 
Scenario 2 −0.49 0.2923 −0.34 0.1764 
Scenario 3 −0.54 0.0559 −0.49 0.1073 
   −0.52  0.1126 
Monitoring sectionsPearson correlation coefficient
Wet year
Dry year
rP-valuerP-value
Shuangqiao (Dashahe) Scenario 1 −0.63 0.0293 −0.63 0.0296 
Scenario 2 −0.54 0.0727 −0.60 0.0399 
Scenario 3 −0.51 0.0899 −0.59 0.0456 
Shuangqiao (Donghe) Scenario 1 −0.57 0.0507 −0.60 0.0405 
Scenario 2 −0.67 0.2421 −0.48 0.1180 
Scenario 3 −0.48 0.0842 −0.41 0.1845 
Shilongping Scenario 1 −0.54 0.0706 −0.56 0.0596 
Scenario 2 −0.44 0.2818 −0.46 0.1330 
Scenario 3 −0.54 0.1472 −0.40 0.0013 
Dieshuiheqiao Scenario 1 −0.55 0.1949 −0.44 0.1542 
Scenario 2 −0.49 0.2923 −0.34 0.1764 
Scenario 3 −0.54 0.0559 −0.49 0.1073 
   −0.52  0.1126 

Note: , Comprehensive correlation coefficient; , Comprehensive p-value.

From the monthly average concentration variations in wet and dry years, it can be observed that the TP concentrations in all sections show a fluctuating decreasing trend under the three reduction scenarios. None of the three reduction scenarios were able to achieve full-year compliance with TP concentration standards in the Dashariver section of the Donghe River. Only Scenario 3 during wet years was able to achieve full-year compliance with TP concentrations in the main stream of the Donghe River entering the Nujiang River, while the rest of the scenarios did not meet the standards. The months of non-compliance are mostly concentrated in the dry season, from January to April and in December. Compared to wet years, there is an increase in non-compliance months during dry years.

Discussion

This study investigated the variations in TP concentrations at four monitoring sections, namely Dashariver (Shuangqiao), Donghe (Shuangqiao), Shilongping, and Dieshuiheqiao, in the Donghe River basin under three integrated reduction scenarios. Based on the simulation results using the SWAT model, it can be observed that the reduction scenarios, involving the reduction of pollution from domestic sources, dilution through water diversion in urban river sections, and other measures, have shown positive effects on reducing TP concentrations and achieving water quality compliance in the Dashahe tributary and the main stream of the Donghe River. However, during the dry season months of January to April and December, when rainfall is reduced, the decreased river flow and limited dilution and exchange processes result in restricted TP diffusion and increased accumulation (Zhu et al. 2017; Xie et al. 2019; Xu et al. 2021). This indicates that there is still a possibility of TP concentration exceeding the standards in the Donghe River basin despite the improvement achieved by the reduction scenarios. It emphasizes the need for further exploration and refinement of the reduction strategies.

According to the simulation results of the SWAT model in the Donghe River basin, further optimization of the reduction strategies is required to achieve TP concentration compliance throughout the entire basin. The following aspects should be considered: (1) wastewater treatment plants play a crucial role in reducing domestic pollution and improving water quality. It is necessary to continue expanding the operational scale and pollution reduction capacity of urban wastewater treatment plants. (2) Water replenishment is an important direction. Emphasis should be placed on supplying water from December to April of the following year to increase river flow and hydraulic energy, promoting self-purification and dilution effects. Furthermore, considering the specific conditions of the Donghe River basin, the following issues should be addressed in future research: (1) Rural domestic pollution, agricultural non-point source pollution, industrial sources, and livestock and poultry farming continue to be significant sources of TP in the Donghe River basin. Macroscopic and microscopic improvements and enhancements should be gradually implemented. Macroscopically, this involves considering the planning and optimal siting of pollution sources, as well as methods and mechanisms for coordinated pollution control. Microscopically, effective and rational reduction and control measures should be implemented for each pollution source (Chen et al. 2018b, 2019; Xiong et al. 2020), such as improving agricultural management practices (Chinnasamy et al. 2015), implementing appropriate fertilization techniques, and constructing wetlands and retention facilities (Wang et al. 2020b; Chen et al. 2021a). (2) Pollutants such as BOD5, COD, NH3-N, TN, and SS remain significant concerns for water pollution in the basin. It is essential to establish a comprehensive monitoring system for the entire basin and conduct regular monitoring and water environmental safety assessments (Tan et al. 2017; Liu et al. 2020d).

According to the analysis of the results, it is found that there is a certain negative correlation between TP concentration in the tributaries of the Da Sha River and the main stem of the East River and rainfall. It is concluded that seasonal rainfall may be a driving factor for TP concentration variations in the East River basin. Further investigation should be conducted to explore the relationship between characteristics of rainfall such as spatial and temporal distribution, event size, and frequency (Zhang et al. 2017a), and TP concentration. Combining rainfall characteristics (Li et al. 2018; Sun et al. 2019) with water quality management measures, more detailed management strategies can be developed to reduce TP input. In addition to rainfall, the TP concentration dynamics in the Donghe River basin may involve various hydrological, physical, and biological processes. Hydrological processes (Wang et al. 2020a), such as evapotranspiration, streamflow velocity (Alizadeh et al. 2018), water level, hydraulic energy, and groundwater recharge, play a role. Physical processes include the transport and deposition of pollutants in rivers and the interception and removal of sediments by lakes and reservoirs (Deng et al. 2019). Biological processes, such as the degradation of pollutants by phytoplankton and algae (Chen et al. 2018a; Shamshirband et al. 2019), are also relevant. Furthermore, climate change can have a significant impact on rainfall patterns and hydrological processes (Liu et al. 2020b). Investigating the relationships between other factors and pollutant concentrations can provide a more comprehensive and in-depth understanding of the underlying mechanisms driving the concentration, transport, transformation, and cycling of pollutants in the Donghe River basin.

During the modeling process of the SWAT model, we identified the limitations and shortcomings of the model and proposed directions for improvement. Firstly, reducing the uncertainty of SWAT model parameters is crucial. Improvement lies in enhancing parameter sensitivity analysis and optimizing parameter fitting (Abbaspour et al. 2007b). For parameter sensitivity analysis, multiple sensitivity indices, such as impact coefficient, variance analysis, total effect indices, and local sensitivity indices can be utilized to obtain more comprehensive and accurate information about parameter sensitivity. Non-parametric sensitivity analysis methods, such as machine learning algorithms and neural networks, can also be employed to uncover complex parameter relationships and nonlinear responses. Additionally, sensitivity analysis can be conducted at both global and local levels. Global sensitivity analysis reveals the model's overall response to parameter variations, while local sensitivity analysis delves into specific parameter impacts. For parameter optimization, a combination of different optimization algorithms such as genetic algorithms, particle swarm optimization algorithms, and simulated annealing algorithms can be considered (Bekele & Nicklow 2005) to form hybrid optimization algorithms. This approach leverages the strengths of various algorithms to improve parameter optimization outcomes. Constraints can also be introduced during the optimization process, such as physical constraints, statistical constraints, or constraints based on observational data. Expert knowledge (Panday & Huyck 2004) can be utilized to limit parameter ranges or provide initial parameter values, narrowing down the parameter search space and accelerating the optimization process. This ensures that the parameter estimation results align with reality and feasibility. Secondly, accounting for the basin characteristics and spatial heterogeneity of the actual watershed is essential. No model can perfectly replicate the mechanisms operating in an actual watershed. To improve the model's performance in capturing basin characteristics and spatial heterogeneity, algorithmic improvements (Li et al. 2019a, 2019b), the introduction of new parameter estimation methods from a watershed perspective (Abbaspour & Rouholahnejad 2015), the inclusion of new hydrological process modules (Du et al. 2018), or multi-model fusion can be considered.

This study investigated the effectiveness of three emission reduction scenarios in reducing the concentration of TP, the primary pollutant, in the Dong River Basin in Longyang District, Yunnan Province, China, using the SWAT model. The findings are as follows:

  • (1)

    The SWAT model, calibrated and validated at Bao Shan, Han Zhuang, and Xin Jie stations located in sub-basins of the study area, demonstrated good applicability in simulating both runoff and TP concentration, with determination coefficients (R2) and Nash–Sutcliffe efficiency (NSE) values exceeding 0.75 for runoff and R2 and NSE values exceeding 0.70 for TP concentration at Sha Ba and Shi Long Ping monitoring sections. However, limitations still exist when applying the model to the actual basin, suggesting the need for employing multiple analytical methods for parameter sensitivity analysis and optimization to enhance simulation accuracy.

  • (2)

    The simulation results of the three TP reduction scenarios using the SWAT model revealed notable improvements in TP concentrations in the target river sections, where the tributaries of Da Sha River join the Dong River and where the Dong River flows into the Nu River. These findings demonstrate the effectiveness of emission reduction scenarios in mitigating TP pollution in the Dong River Basin. Nevertheless, during the dry season months of January to April and December, particularly the peak TP concentration in April, the reduced dilution effect of rainfall leads to TP accumulation. As a result, there is still a risk of TP concentrations exceeding the standards in the Dong River Basin during this period, emphasizing the importance of implementing preventive measures to ensure year-round water quality compliance.

  • (3)

    The pollution control and management of the Dong River Basin exhibit complex and comprehensive characteristics, requiring long-term, multifaceted prevention, treatment, and adjustment strategies. In addition to pollution sources from urban areas and wastewater treatment plants, rural domestic sources, agricultural sources, industrial sources, and livestock and poultry farming sources are also significant contributors to TP in the Dong River Basin. Furthermore, the basin faces challenges related to other pollutants such as biochemical oxygen demand (BOD5), chemical oxygen demand (COD), ammonia nitrogen (NH3-N), total nitrogen (TN), and suspended solids (SS). Therefore, future research should focus on continuous improvement and refinement of pollution control strategies to address these issues effectively.

This work was supported by the National Key R&D Program of China (2016YFC0401701), the Belt and Road Special Foundation of the State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering (2019490911), the Belt and Road Special Foundation of the State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering (2020491111) and the Natural Science Foundation of Hebei Province of China (Grant No. E2020402057).

C.Z. conceptualized the whole article, developed the methodology, brought the resources, validated and wrote the review and edited the article. Y. W. conducted formal analysis, visualized the article, validated and wrote the original draft. C. H. investigated the process and arranged the resources. W. H. validated the article.

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

The authors declare there is no conflict.

Abbaspour
K. C.
,
Rouholahnejad
E.
,
2015
A review of the SWAT-CUP program for uncertainty analysis
. In:
SWAT: Soil and Water Assessment Tool: Theory and Practice
(
Baltas
E. A.
,
Kovar
K.
&
Rousseau
K.
, eds).
Springer
, pp.
521
536
.
Abbaspour
K. C.
,
Vejdani
M.
&
Haghighat
S.
2007a
SWAT-CUP2: SWAT Calibration and Uncertainty Programs – A User Manual
.
Swiss Federal Institute of Aquatic Science and Technology (EAWAG)
.
Abbaspour
K. C.
,
Yang
J.
,
Maximov
I.
,
Siber
R.
&
Bogner
K.
2007b
Modelling hydrology and water quality in the pre-alpine/alpine Thur watershed using SWAT
.
Journal of Hydrology
333
(
2–4
),
413
430
.
Abbaspour
K. C.
,
Vejdani
M.
&
Haghighat
S.
2015
SWAT-CUP calibration and uncertainty programs for SWAT
.
The Science of the Total Environment
538
,
844
857
.
AlDahoul
N.
,
Ouarda
T. B. M. J.
&
Nistor
I.
2022
A comparison of machine learning models for suspended sediment load classification
.
Engineering Applications of Computational Fluid Mechanics
16
(
1
),
1211
1232
.
Alizadeh
M. J.
,
Jafari
N.
&
Sadrpour
S.
2018
Effect of river flow on the quality of estuarine and coastal waters using machine learning models
.
Engineering Applications of Computational Fluid Mechanics
12
(
1
),
810
823
.
Arnold
J. G.
,
Srinivasan
R.
,
Muttiah
R. S.
&
Williams
J. R.
1998
Large area hydrologic modeling and assessment: part I. Model development
.
Journal of the American Water Resources Association
34
(
1
),
73
89
.
Arnold
J. G.
,
Moriasi
D. N.
,
Gassman
P. W.
,
Abbaspour
K. C.
,
White
M. J.
,
Srinivasan
R.
,
Santhi
C.
,
Harmel
R. D.
,
Van Griensven
A.
,
Van Liew
M. W.
,
Kannan
N.
&
Jha
M. K.
2012
SWAT: Model use, calibration, and validation
.
Transactions of the ASABE
55
(
4
),
1491
1508
.
Bai
Y.
,
Zhang
Y.
&
Liu
Y.
2018
Hybrid optimization algorithm for improving the performance of water quality models
.
Water Resources Management
32
(
10
),
3373
3389
.
Bekele
E. G.
&
Nicklow
J. W.
2005
Multi-objective auto-calibration of SWAT using NSGA-II
.
Journal of Hydrology
306
(
1–4
),
1
23
.
Chen
S.
&
Huang
G.
2016
Optimal model construction for the prediction of water quality parameters using statistical analysis
.
Environmental Science and Pollution Research
23
(
4
),
3051
3062
.
Chen
X.
,
Zhang
Y.
,
Xu
D.
,
Liu
Z.
&
Li
Y.
2018a
Phytoplankton community structure and its response to environmental factors in the Donghe Reservoir
.
Environmental Science and Pollution Research
25
(
17
),
17025
17038
.
Chen
M.
,
Shang
S.
,
Wang
Y.
,
Chen
W.
&
Lin
Y.
2021a
Integrated assessment of nonpoint source pollution control strategies in an agricultural catchment of the Three Gorges Reservoir Region, China
.
Science of the Total Environment
753
,
141925
.
Chen
Y.
,
Zhang
Y.
,
Zhang
L.
&
Fu
G.
2021b
An efficient approach for automated delineation of subbasins and hydrologic response units in SWAT models
.
Science of the Total Environment
783
,
147072
.
Chinnasamy
P.
,
Srinivasan
R.
,
Chaubey
I.
&
Zimba
P. V.
2015
Application of SWAT model for water quality simulation and management in the Thachin River Basin, Thailand
.
Environmental Earth Sciences
74
(
4
),
3389
3405
.
Deng
X.
,
Zhou
Y.
,
Wang
Y.
,
Zhang
H.
&
Li
F.
2019
Effects of reservoir operation on phosphorus transport and retention in a river system: a case study of the Daning River, China
.
Science of the Total Environment
662
,
319
330
.
Du
W.
,
Wu
W.
,
Chen
X.
,
Zhang
J.
&
Liu
M.
2018
Improving the simulation of hydrological processes in a loess plateau catchment using the SWAT model with the modified SWAT Soil Water Assessment Tool
.
Hydrology Research
49
(
3
),
888
905
.
Fath
B. D.
,
Patten
B. C.
&
Choi
J. S.
2017
Systems ecology as a framework for sustainability in water ecosystems
.
Ecological Modelling
363
,
137
145
.
Fu
G.
,
Charles
S. P.
,
Montas
H. J.
&
Fang
X.
2016
A review of SWAT studies in the world
.
Journal of Hydrology
535
,
1
13
.
Fu
Q.
,
Wang
Y.
,
Chen
W.
,
Zhao
X.
&
Wang
Z.
2019
Application of WQMN model in water quality prediction for a reservoir in China
.
Journal of Water and Environment Technology
17
(
6
),
233
243
.
Gassman
P. W.
,
Reyes
M. R.
,
Green
C. H.
&
Arnold
J. G.
2007
The soil and water assessment tool: historical development, applications, and future research directions
.
Transactions of the ASABE
50
(
4
),
1211
1250
.
Guo
H.
,
Wang
H.
,
Li
W.
,
Han
L.
&
Yu
G.
2018
Quantifying the contributions of point sources and non-point sources to riverine nutrient loads: a case study in the Huai river basin, China
.
Science of the Total Environment
639
,
52
63
.
Hadjisolomou
E.
,
Agapiou
A.
,
Michaelides
S.
,
Papadavid
G.
&
Themistocleous
K.
2021
Modelling freshwater eutrophication with limited limnological data using artificial neural networks
.
Water
13
(
11
),
1590
.
Huang
Q.
&
Wang
Q.
2019
Water demand and supply in China: past, present, and future
.
Journal of Environmental Management
250
,
109473
.
Huang
Q.
,
Chen
Y.
,
Xu
H.
,
Yin
C.
&
Li
Z.
2021
Assessment of total phosphorus pollution and source apportionment in a drinking water reservoir: a case study in Eastern China
.
Environmental Science and Pollution Research
28
(
21
),
27388
27400
.
Jin
Q.
,
He
Y.
,
Chen
L.
&
Chen
X.
2019
Multi-objective optimization for water pollution control based on pollutant reduction and economic cost in a river basin
.
Science of the Total Environment
658
,
461
469
.
Li
R.
,
Chen
Y.
,
Wang
Z.
&
Li
Y.
2019a
Assessing spatial-temporal variability of water quality in the Xiangxi River using multivariate statistical analysis and geostatistics
.
Science of the Total Environment
660
,
649
658
.
Li
Z.
,
Chen
Y.
,
Li
X.
,
Chen
X.
&
Xu
Y.
2019b
Improving SWAT model performance by incorporating new algorithms for baseflow separation and flow routing
.
Journal of Hydrology
568
,
677
689
.
Li
H.
,
Jia
Y.
,
Wu
W.
&
Zhu
H.
2020b
Assessing the impacts of climate change and land use on streamflow in a typical mountainous watershed using SWAT
.
Hydrology Research
51
(
5
),
981
998
.
Li
M.
,
Xiong
L.
,
Yu
M.
,
Li
X.
&
Wang
S.
2020c
Application of statistical models in water quality prediction: a review
.
Water
12
(
4
),
999
.
Liu
J.
,
Mooney
H.
,
Hull
V.
,
Davis
S. J.
,
Gaskell
J.
,
Hertel
T.
,
Lubchenco
J.
,
Seto
K. C.
,
Gleick
P.
,
Kremen
C.
&
Li
S.
2015
Sustainability. Systems integration for global sustainability
.
Science
347
(
6225
),
1258832
.
doi:10.1126/science.1258832
.
Liu
D.
,
Shi
Y.
,
Wang
H.
,
Li
Y.
&
Wang
X.
2020a
Assessment of total phosphorus pollution and sources in a typical agricultural watershed of North China
.
Environmental Science and Pollution Research
27
(
6
),
5844
5856
.
Liu
X.
,
Liu
H.
,
Yu
Z.
&
Xue
J.
2020b
Impacts of climate change on streamflow in the Donghe River Basin, China
.
Journal of Hydro-Environment Research
30
,
100639
.
Liu
Z.
,
Li
J.
&
Xu
Z.
2020d
Water quality assessment and source identification of a river basin using the improved fuzzy comprehensive evaluation method: a case study in the Luanhe River Basin, China
.
Journal of Cleaner Production
276
,
124076
.
Moriasi
D. N.
,
Arnold
J. G.
,
Van Liew
M. W.
,
Bingner
R. L.
,
Harmel
R. D.
&
Veith
T. L.
2007
Model evaluation guidelines for systematic quantification of accuracy in watershed simulations
.
Transactions of the ASABE
50
(
3
),
885
900
.
Neitsch
S. L.
,
Arnold
J. G.
,
Kiniry
J. R.
&
Williams
J. R.
2005
Soil and Water Assessment Tool Theoretical Documentation Version 2005
.
Neitsch
S. L.
,
Arnold
J. G.
,
Kiniry
J. R.
&
Williams
J. R.
2011
Soil and Water Assessment Tool Theoretical Documentation Version 2009
.
Texas Water Resources Institute
.
Panday
A.
&
Huyck
C. K.
2004
Incorporating expert knowledge in calibration of SWAT model: case study of Upper Narmada River Basin
.
Journal of Hydrologic Engineering
9
(
6
),
492
501
.
Park
S. J.
,
Park
N. W.
&
Jun
M. J.
2013
Application of the SWAT model to a mountainous watershed located in the semi-humid region of South Korea
.
Water
5
(
1
),
369
389
.
Peng
Y.
,
Fu
G.
,
Fang
X.
,
Li
C.
&
Zheng
Y.
2018
Application of WQMN model in water quality prediction for a river in China
.
Environmental Science and Pollution Research
25
(
31
),
31467
31478
.
Safi
G. M.
,
Motamedi
M.
&
Barzegar
R.
2020
Water quality simulation in a river system using CE-QUAL-W2 model: a case study of the Jajrood River, Iran
.
Environmental Monitoring and Assessment
192
(
2
),
1
15
.
Shamshirband
S.
,
Ismail
Z.
,
Khoshnevisan
B.
,
Anuar
N. B.
&
Hashim
R.
2019
Ensemble models with uncertainty analysis for multi-day ahead forecasting of chlorophyll a concentration in coastal waters
.
Engineering Applications of Computational Fluid Mechanics
13
(
1
),
91
101
.
Shoemaker
L. K.
&
Brua
R. B.
2018
Evaluation of land use change impacts on streamflow and water quality using the HSPF model
.
Journal of Environmental Management
215
,
1
11
.
Shrestha
S.
&
Chen
X.
2019
Modelling the impacts of land use and climate change on hydrology and water quality in a watershed using the HSPF model
.
Water Science and Engineering
12
(
4
),
256
264
.
Sun
Z.
,
Chen
X.
,
Wang
Z.
,
Li
X.
&
Li
J.
2020b
Hydrological response to climate change in the upper Yellow River basin during 1960–2017
.
Journal of Hydrology
589
,
125068
.
Tsai
W. Y.
,
Chen
W. J.
&
Yang
H.
2018
Simulating the impacts of climate change on water quality in a subtropical reservoir using the AQUATOX model
.
Journal of Hydrology
566
,
162
174
.
Vamvakeridou-Lyroudia
L. S.
&
Karatzas
G. P.
2017
Water resources management models: a review of their role in the decision-making process
.
Water Resources Management
31
(
13
),
4249
4273
.
Duan, Q. Y., Sorooshian, S. & Gupta, V. K. 1994 Optimal use of the SCE-UA global optimization method for calibrating watershed models. Journal of Hydrology 158(3-4), 265–284.
Wang
S.
,
Xie
P.
,
Liang
X.
,
Chen
Y.
&
Zhu
M.
2019a
Simulation of water quality dynamics in a large shallow lake using the AQUATOX model: a case study of Lake Taihu, China
.
Science of the Total Environment
655
,
679
689
.
Wang
F.
,
Wu
J.
,
Zhang
J.
,
Wang
X.
&
Li
Y.
2019b
Urbanization and water quality: a review of the impacts of urban development on water quality changes in China
.
Science of the Total Environment
649
,
186
194
.
Wang
C.
,
Wang
P.
,
Liu
W.
,
Yang
W.
&
Li
Y.
2020a
Influences of hydrological factors on the transport of phosphorus in a large river basin
.
Science of the Total Environment
729
,
138772
.
Wang
J.
,
Wu
P.
,
Zhao
Y.
,
Xie
D.
&
Zhou
X.
2020b
Evaluation and source apportionment of nitrogen and phosphorus pollution in a typical rural watershed on the North China Plain
.
Journal of Hydrology
588
,
125073
.
Wang
X.
,
Zou
Z.
,
Li
X.
,
Xu
D.
&
Zhu
H.
2020c
Water quality prediction using an improved back-propagation neural network model in a eutrophic lake
.
Environmental Monitoring and Assessment
192
(
12
),
1
14
.
Wu
L.
,
Wei
Y.
,
Li
Y.
&
Zhang
M.
2017
Evaluating the applicability of SWAT model in a small mountainous catchment on the Loess Plateau of China
.
Environmental Earth Sciences
76
(
15
),
530
.
Xie
H.
,
Shi
X.
&
Tang
Q.
2019
Impacts of low-flow conditions on nutrient dynamics and transport in a typical agricultural river basin
.
Science of the Total Environment
659
,
898
908
.
Xu
D.
,
Li
X.
,
Zou
Z.
,
Zhang
Z.
&
Zhu
H.
2020
Evaluating the applicability of SWAT model for water quality simulation in a eutrophic lake watershed
.
Science of The Total Environment
711
,
134566
.
Yin
H.
,
Jin
L.
&
Li
W.
2017
Water quality assessment and modeling of a river using the QUAL2K model: a case study in the Huai River Basin, China
.
Environmental Science and Pollution Research
24
(
34
),
26689
26699
.
Zeng
Y.
,
Li
Z.
&
Chen
Y.
2019
A hybrid optimization approach for calibrating water quality models considering model structural uncertainty
.
Journal of Environmental Management
245
,
165
174
.
Zhang
Q.
,
Xu
C. Y.
,
Chen
Y. D.
&
Zhang
Z. X.
2009
Spatial and temporal variations of annual precipitation during 1960–2005 in Haihe River basin, China
.
Journal of Hydrology
377
(
1–2
),
35
42
.
Zhang
Y.
,
Yu
Z.
,
Li
B.
,
Zhang
Q.
&
Li
Y.
2017b
Advances in water quality prediction models: a review
.
Water Science and Technology
76
(
10
),
2513
2535
.
Zhang
Y.
,
Wang
Y.
&
Wang
Y.
2018a
Water pollution control policies in China: a historical and institutional analysis
.
Environmental Science and Pollution Research
25
(
16
),
15197
15209
.
Zhang
Y.
,
Sun
G.
,
Liu
H.
,
Yu
X.
&
Wu
L.
2019a
Spatial-temporal characteristics and source apportionment of total phosphorus in a typical Plateau Lake, China
.
Ecological Indicators
99
,
249
257
.
Zhang
Y.
,
Yu
Z.
,
Huang
G.
,
Wang
X.
&
Zhao
Z.
2019b
A review of statistical models for water quality assessment and prediction
.
Environmental Science and Pollution Research
26
(
8
),
7413
7428
.
Zhang
H.
,
Wu
Y.
,
Liu
C.
&
Wang
X.
2020
Water quality modeling and assessment of a river using the QUAL2K model: a case study in the middle reach of the Yangtze River, China
.
Environmental Monitoring and Assessment
192
(
10
),
1
16
.
Zhang
Y.
,
Yu
Z.
,
Wang
L.
,
Li
L.
&
Zhang
X.
2021a
Modeling non-point source pollution in the Daliao River Basin using the SWAT model
.
Water
13
(
1
),
100
.
Zhang
Z.
,
Zheng
F.
&
Yang
W.
2021b
Data-driven modeling of hydrological responses to land use change in a mesoscale mountainous watershed using SWAT
.
Science of the Total Environment
767
,
144679
.
Zhu
B.
,
Zhang
Y.
,
Tang
J.
,
Huang
Q.
&
Li
C.
2017
Assessment of nonpoint source pollution under dry and wet weather conditions in a mountainous watershed
.
Environmental Monitoring and Assessment
189
(
12
),
645
.
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/).