Open access peer-reviewed chapter

Setting Up a Computer Simulation Model in an Arkansas Watershed for the MRBI Program

Written By

Gurdeep Singh and Mansoor Leh

Reviewed: 13 August 2018 Published: 28 November 2018

DOI: 10.5772/intechopen.80902

From the Edited Volume

Water and Sustainability

Edited by Prathna Thanjavur Chandrasekaran

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Abstract

The Mississippi River Basin Healthy Watersheds Initiative (MRBI) program launched by the USDA Natural Resources Conservation Service (NRCS) aims to improve the water quality within the Mississippi River Basin. Lake Conway Point Remove (LCPR) watershed, being one of the MRBI watersheds, is a potential candidate for evaluating the effectiveness of MRBI program. Recommended best management practices (BMPs) for LCPR watershed are pond, wetland, pond and wetland, cover crops, vegetative filter strips, grassed waterways, and forage and biomass planting. Before simulating these practices, it is essential to prepare the data needed for model setup to avoid the issue of garbage in, garbage out. This chapter focuses on detailed steps of preparing the data for model setup along with the calibration and validation of the model. The calibration and validation results were within the acceptable bounds. The results from this study provide the data to help simulate the MRBI best management practices effectively and prioritize monitoring needs for collecting watershed response data in LCPR.

Keywords

  • best management practices
  • modeling
  • water quality
  • SWAT
  • MRBI

1. Introduction

The Mississippi River Basin Healthy Watersheds Initiative (MRBI) program aims at implementing best management practices (BMPs) to control water quality. Quantifying the impacts of BMPs is important to demonstrate the worth of the MRBI program. Out of various MRBI-selected watersheds, the Lake Conway Point Remove (LCPR) watershed is the one listed in the 2011–2016 priority watershed by the Arkansas Natural Resources Commission (ANRC) [1, 2].

Field studies can be laborious and time-consuming; therefore, watershed modeling technique is generally used for analyzing the effects of BMPs on water quality. The Soil and Water Assessment Tool (SWAT, [3]) model was selected for this study. The SWAT model has been widely applied across the globe to assess the impact of various BMPs [4]. SWAT has also been applied to various watersheds in Arkansas—L’Anguille River Watershed [5, 6], Cache River Watershed [7], and Illinois River Watershed [8]. SWAT allows modifications of various parameters to simulate BMPs [9] and was applied at various spatial and temporal scales [10]. SWAT has been used to simulate impacts of land uses and BMPs [11, 12], develop maximum daily load plans [13, 14], and evaluate impacts on water quality [15, 16]. However, before simulating BMPs, it is essential to acquire and process the data needed for setting up a good model.

The goal of this chapter is to describe the steps in detail for acquiring and processing the data needed to set up, calibrate, and validate the SWAT model for the LCPR watershed.

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2. Methodology

2.1. Study area

The Lake Conway Point Remove (LCPR) watershed is a 2950 km2 (1140 miles2) watershed located in central Arkansas within the counties of Conway, Faulkner, Perry, Pope, Pulaski, Van Buren, and Yell (Figure 1). The watershed has mixed land uses of forest, pasture, urban, and cropland. An increase in urbanization, in parts of the watershed, has occurred since 1999. The subwatersheds within LCPR along with the area and hydrological unit codes (HUC) can be seen in Table 1.

Figure 1.

Lake Conway Point Remove watershed.

Subwatershed Subwatershed name Area (km2) HUC no.
1 Trimble creek-west fork point remove creek 77.0 111102030102
2 Brock creek 113.1 111102030101
3 Devils creek-west fork point remove creek 88.2 111102030107
4 Barns branch-east fork point remove creek 102.7 111102030204
5 Galla creek 118.0 111102030303
6 Whig creek-Arkansas river 106.3 111102030302
7 Mountain view-east fork point remove creek 97.8 111102030201
8 Upper clear creek 120.4 111102030103
9 Rock creek-west fork point remove creek 156.2 111102030105
10 Sunny side creek-east fork point remove creek 100.9 111102030202
11 Lower clear creek 106.5 111102030104
12 Prairie creek-east fork point remove creek 106.9 111102030203
13 Gum log creek 130.4 111102030106
14 Portland bottoms-Arkansas river 90.9 111102030503
15 Headwaters rocky Cypress creek 100.1 111102030501
16 Jim creek-Palarm creek 92.4 111102030402
17 Little creek-Palarm creek 106.8 111102030403
18 Beaverdam creek-Arkansas river 88.0 111102030507
19 Little Palarm creek-Palarm creek 89.9 111102030405
20 Taylor creek-Arkansas river 65.1 111102030506
21 Tupelo bayou 110.8 111102030505
22 Outlet rocky cypress creek 70.5 111102030502
23 Pierce creek-Palarm creek 100.0 111102030404
24 Little cypress creek-Palarm creek 53.4 111102030401
25 Overcup creek 81.1 111102030205
26 Khun Bayou-Arkansas River 131.1 111102030304
27 Long Lake-Harris creek 148.2 111102030301
28 Point remove creek 80.2 111102030206
29 Miller Bayou-Arkansas river 116.4 111102030504

Table 1.

List of HUC 12 subwatersheds and area in LCPR watershed.

2.2. Data preparation

The objective of this task was to collect and organize all data needed for the SWAT model setup at a 12-digit hydrological unit code within the LCPR watershed. Geospatial, watershed management, water quantity, and point source data that were available and usable at the time of modeling were collected and reorganized in a consistent format for use in the SWAT model.

2.2.1. Elevation

The elevation dataset was retrieved at a 5 m resolution from GeoStor. This 5 m dataset was resampled to a 10 m resolution to reduce the size of huge files and increase the computation efficiency. The elevation map for LCPR can be seen in Figure 2.

Figure 2.

Lake Conway Point Remove watershed elevation.

2.2.2. Soils

The soil data were acquired from the Soil Survey Geographic (SSURGO) database for all LCPR counties in Arkansas and combined to make a soil map for the entire watershed. The SSURGO is the most comprehensive and detailed soil dataset available for LCPR. The soil map for LCPR can be seen in Figure 3.

Figure 3.

Soil map of Lake Conway Point Remove watershed, Arkansas, showing major soil series.

2.2.3. Land use/land cover

Land use and land cover data were acquired for 1999, 2004, and 2006 from GeoStor. Forest area was observed to be the most dominant land use and cover in the LCPR watershed. All land use and land covers were reclassified to make it compatible with the SWAT model. The land use and land cover map for LCPR can be seen in Figure 4.

Figure 4.

Land use and land cover in the Lake Conway Point Remove watershed.

2.2.4. Climate

Climatic data specifically daily precipitation and maximum and minimum temperature data were obtained from 90 climate stations from the NOAA’s National Climatic Data Center (NCDC). Data are available from 1980 to 2012 for at least one of the climatic parameters. The procedure recommended by USDA-ARS in developing SWAT-formatted climate data were followed. Daily climate data were obtained using an inverse distance-weighted interpolation algorithm. The average data were calculated for each subwatershed using a pseudo-weather station. NCDC validation results at each calibration station using leave-one-out cross-validation technique can be seen in Table 2. NEXRAD data were obtained from the Arkansas Basin River Forecasting Center (ABRFC).

Station Parameter DRAIN1 DNO_RAIN2 ME3 d4 PBIAS5% R26 NSE7 MAE8 RMSE9
Center Ridge, 4.S, AR, USA PRCP 0.94 0.86 −0.12 0.95 −0.3 0.83 0.83 15.48 45.03
Conway, AR, USA PRCP 0.91 0.79 −0.64 0.87 −1.9 0.59 0.58 23.53 63.56
Dardanelle, AR, USA PRCP 0.95 0.79 0.51 0.85 1.5 0.54 0.52 24.55 71.4
Hattieville, AR, USA PRCP 0.95 0.82 0.08 0.92 0.2 0.74 0.73 18.13 57.15
Morrilton, AR, USA PRCP 0.90 0.82 0.97 0.9 2.8 0.69 0.68 19.84 59.78
North Little Rock Airport, AR, USA PRCP 0.90 0.81 0.23 0.85 0.7 0.56 0.55 24.37 69.37
Perry, AR, USA PRCP 0.90 0.82 −1.19 0.89 −3.3 0.65 0.64 21.71 64.82
Russellville Municipal Airport, AR, USA PRCP 0.68 0.84 1.85 0.67 5.9 0.24 0.03 34.7 99.07
Conway, AR, USA TMAX 0.45 0.99 0.2 0.95 0.95 14.49 22.31
Dardanelle, AR, USA TMAX −5.02 0.99 −2.2 0.95 0.94 15.14 22.95
Morrilton, AR, USA TMAX −1.9 0.99 −0.8 0.94 0.94 17.39 23.86
North Little Rock Airport, AR, USA TMAX 4.05 1 1.8 0.99 0.99 9.03 11.83
Russellville Municipal Airport, AR, USA TMAX 2.42 0.99 1 0.95 0.95 13.71 22.57
Conway, AR, USA TMIN −7.55 0.98 −7.1 0.95 0.94 15.59 22.75
Dardanelle, AR, USA TMIN −7.89 0.99 −7.8 0.95 0.95 14.18 21.36
Morrilton, AR, USA TMIN 5.27 0.98 5.7 0.94 0.94 15.89 23.35
North Little Rock Airport, AR, USA TMIN −9.94 0.99 −8.3 0.97 0.95 14.79 19.68
Russellville Municipal Airport, AR, USA TMIN 6.76 0.99 6.9 0.96 0.95 13.11 20.5

Table 2.

NCDC precipitation and minimum and maximum temperature validation results at each calibration station using leave-one-out cross-validation.

NEXRAD detection conditioned on exceeding a given threshold gauge observations (DRAIN).


NEXRAD detects no rainfall event (DNO_RAIN).


Mean error (ME).


Index of agreement (d).


Percent bias (PBIAS).


Coefficient of determination (R2).


Nash-Sutcliffe efficiency (NSE).


Mean absolute error (MAE).


Root-mean-square error (RMSE).


2.2.5. Streamflow

The flow data are available for the West Fork Point Remove Creek near the Hattieville monitoring station from the US Geological Survey (USGS). This monitoring station is located in subwatershed 3 and covers approximately 20% of LCPR. The flow data were split between surface and baseflow using the baseflow filter program by [17].

2.2.6. Point sources

Point source data were obtained from the Arkansas Department of Environmental Quality (ADEQ) and was processed in the SWAT-compatible format. Point source data were available for flow, total suspended solids, organic nitrogen, organic and mineral phosphorus, nitrate nitrogen, ammonia nitrogen, and carbonaceous biochemical oxygen demand (CBOD). Locations for active point source facility that was incorporated in the SWAT model can be seen in Table 3.

No. Subbasin Facility NPDES_ID Latitude Longitude
1 5 City of Pottsville AR0048011 35.23 −93.05
2 6 City of Dardanelle AR0033421 35.19 −93.14
3 6 Dardanelle water treatment plant ARG640149 35.21 −93.15
4 6 Tyson Foods Inc., Dardanelle AR0036714 35.22 −93.16
5 6 Russellville Water and Sewer System, City Corporation AR0021768 35.25 −93.12
6 6 Freeman Brothers, Inc., d/b/a Bibler Brothers Lumber Company AR0044474 35.25 −93.13
7 7 SEECO, Inc., J and R Farms SE1 AR0052221 35.43 92.56
8 7 Hamilton Aggregates ARG500026 35.44 −92.54
9 8 Dover Water Works ARG640148 35.40 −93.12
10 9 Quality Rock/Jerusalem Quarry ARG500039 35.39 −92.80
11 10 KT Rock LLC ARG500031 35.41 −92.67
12 11 SEECO, Inc., Campbell Thomas SE1 AR0052141 35.40 −92.83
13 13 City of Atkins AR0034665 35.25 −92.92
14 14 Environmental Solutions and Services, Inc. AR0051357 35.09 −92.71
15 14 Green Bay Packaging, Inc., Arkansas Kraft Division AR0001830 35.10 −92.74
16 16 Rogers Group, Inc., Beryl Quarry AR0047520 35.07 −92.25
17 16 Roy Nunn ARG550322 35.07 −92.37
18 16 Waste Water Management, Inc. d/b/a Oak Tree Subdivision AR0050792 35.08 −92.35
19 16 Fritts Construction, Inc., Hayden’s Place Subdivision AR0050253 35.09 −92.34
20 16 BHT Investment Company, Inc. AR0044997 35.09 −92.33
21 16 Rolling Creek POA AR0042536 35.11 −92.33
22 16 Genesis Water Treatment, Inc. AR0051152 35.11 −92.34
23 17 Faulkner County Public Facility Board, d/b/a Preston Community WW Utility AR0050571 35.03 −92.41
24 17 Wilhelmina Cove property owner AR0048682 34.93 −91.11
25 17 City of Conway, Stone Dam Creek AR0033359 35.05 −92.44
26 17 Coreslab Structures (ARK), Inc. AR0050474 35.06 −92.43
27 17 MAPCO Express, Inc. #3059 AR0045071 35.07 −92.42
28 17 Flushing Meadows Water Treatment, Inc. AR0048879 35.06 −92.37
29 17 Jesse Ferrel d/b/a Jesse Ferrel Rental Development AR0049832 35.09 −92.37
30 18 City of Mayflower AR0037206 34.95 −92.45
31 18 Carla Knight ARG550430 34.97 −92.48
32 19 Construction Waste Management, Inc. Class IV Landfill AR0051764 34.93 −92.44
33 19 Grassy Lake Apartments AR0050334 34.94 −92.43
34 20 City of Bigelow AR0049999 35.00 −92.61
35 20 City of Conway, Tucker Creek WWTP AR0047279 35.07 −92.50
36 21 Conway Corporation, Tupelo Bayou WWTP AR0051951 35.05 −92.54
37 22 City of Oppelo AR0047643 35.08 −92.76
38 24 Faulkner County POID, Seven Point Lake Project AR0050903 35.02 −92.18
39 25 Rogers Group, Inc. ARG500066 35.24 −92.65
40 26 Lentz Sand and Gravel, LLC ARG500072 35.12 −92.76
41 26 City of Atkins, South WWTP AR0034673 35.22 −92.93
42 29 Rogers Group, Inc., Toad Suck Quarry AR0047104 35.11 −92.56
43 29 City of Morrilton ARG160001 35.13 −92.70
44 29 City of Menifee AR0049361 35.14 −92.55
45 29 Gericorp, Inc. AR0048623 35.15 −92.72

Table 3.

Active point source facility location incorporated into the SWAT model.

2.2.7. Cattle grazing, manure deposition, and poultry litter application

The detailed method for estimating pastures that should be receiving litter applications can be seen below.

Detailed methods for estimating pastures that received litter application:

  1. Create buffer of a random radius around the active poultry houses.

  2. Extract pasture areas under the buffer.

  3. Assuming a grazing density of 1 cow/0.8 ha of litter amended pasture, calculate the number of cows that can fit the buffer.

  4. Compare the calculated number of cows to the number of cows in the subwatershed.

  5. Repeat steps 1–4 to obtain the best agreement between estimated numbers of cows.

  6. Apply litter to pasture HRUs that fall under the best buffer radius.

The SWAT compatible data for cattle grazing, manure deposition, and poultry litter application can be seen in Table 4.

Subbasin Cattle grazing rate (kg/day/ha) Cattle manure deposition rate (kg/day/ha) Litter application/grazing
1 14.38 5.59 Yes
2 12.59 4.90 Yes
3 9.16 3.57 Yes
4 11.46 4.46 Yes
5 6.11 2.38 Yes
6 5.83 2.27 Yes
7 13.18 5.13 Yes
8 6.27 2.44 Yes
9 11.43 4.45 Yes
10 11.46 4.46 Yes
11 7.34 2.86 Yes
12 11.46 4.46 Yes
13 6.11 2.38 Yes
14 10.51 4.09 Yes
15 9.05 3.52 Yes
16 12.03 4.68 No
17 12.03 4.68 No
18 11.98 4.66 No
19 12.44 4.84 No
20 6.44 2.51 No
21 12.03 4.68 No
22 9.24 3.60 Yes
23 12.03 4.68 No
24 12.03 4.68 Yes
25 11.46 4.46 Yes
26 7.84 3.05 Yes
27 4.50 1.75 Yes
28 9.15 3.56 Yes
29 10.70 4.16 Yes

Table 4.

Cattle grazing, manure deposition, and poultry litter application data incorporated into the SWAT model.

2.2.8. Urban pasture management

The pasture management schedule relating to specific operation and crop can be seen in Table 5.

Date End No. of days Operation Comment Crop
Cool-season grass (fescue)
1-Apr Fertilizer Poultry litter@1 ton/acre of auto-fertilize BERM
1-May Planting Warm-season grass (Bermuda) BERM
15-May 31-Oct 170 Grazing BERM
15-Jun Hay cutting 85% removal BERM
15-Jul Hay cutting 85% removal BERM
15-Aug Hay cutting 85% removal BERM
15-Sept Hay cutting 85% removal BERM
15-Oct Hay cutting 85% removal BERM
1-Mar Fertilizer Poultry litter@1 ton/acre of auto-fertilize BERM
15-May 30-Oct 170 Grazing BERM
15-Jun Hay cutting 85% removal BERM
15-Jul Hay cutting 85% removal BERM
15-Aug Hay cutting 85% removal BERM
15-Sept Hay cutting 85% removal BERM
15-Oct Hay cutting 85% removal BERM
1-Apr Fertilizer Poultry litter@1 ton/acre of auto-fertilize BERM
Warm-season grass (Bermuda)
31-Aug Fertilizer Poultry litter@1 ton/acre of auto-fertilize FESC
1-Sept Planting Cool-season grass (fescue) FESC
15-Mar 1-Jun 79 Grazing FESC
15-May Hay cutting 85% removal FESC
15-Jun Hay cutting 85% removal FESC
1-Sept Fertilizer Poultry litter@1 ton/acre of auto-fertilize FESC
1-Oct Grazing FESC
15-Oct Hay cutting 85% removal FESC
21-Feb Fertilizer Poultry litter@1 ton/acre of auto-fertilize FESC
15-Mar 1-Jun 79 Grazing FESC
15-May Hay cutting 85% removal FESC
15-Jun Hay cutting 85% removal FESC
1-Sept Fertilizer Poultry litter@1 ton/acre of auto-fertilize FESC
1-Oct 30-Nov 61 Grazing FESC
21-Feb Fertilizer Poultry litter@1 ton/acre of auto-fertilize FESC

Table 5.

Pasture management schedule incorporated into the SWAT model.

2.2.9. Ponds and wetlands

SWAT input parameters relating to ponding were PND_FR, PND_PSA (ha), PND_PVOL (104 m3), PND_ESA, PND_EVOL, and PND_VOL. These ponding parameters can be seen in Table 6. SWAT input parameters relating to wetland were WET_FR, WET_NSA (ha), WET_NVOL 104 (m3), WET_MXSA (ha), WET_MXVOL 104 (m3), and WET_VOL 104(m3). These wetland parameters can be seen in Table 7.

Subwatershed PND_FR PND_PSA (ha) PND_PVOL (104 m3) PND_ESA PND_EVOL PND_VOL
1 0.068 30 30 40 40 30
2 0.007 4 4 6 6 4
3 0.290 146 146 195 195 146
4 0.330 194 194 258 258 194
5 0.066 45 45 60 60 45
6 0.090 55 55 73 73 55
7 0.138 77 77 103 103 77
8 0.062 43 43 57 57 43
9 0.064 57 57 76 76 57
10 0.059 34 34 45 45 34
11 0.080 49 49 65 65 49
12 0.088 54 54 71 71 54
13 0.087 65 65 87 87 65
14 0.126 65 65 87 87 65
15 0.072 41 41 55 55 41
16 0.102 54 54 72 72 54
17 0.098 60 60 80 80 60
18 0.068 34 34 45 45 34
19 0.200 103 103 137 137 103
20 0.225 84 84 112 112 84
21 0.067 42 42 56 56 42
22 0.097 39 39 52 52 39
23 0.096 55 55 73 73 55
24 0.111 34 34 45 45 34
25 0.128 60 60 79 79 60
26 0.109 82 82 109 109 82
27 0.087 74 74 98 98 74
28 0.053 24 24 33 33 24
29 0.190 126 126 168 168 126

Table 6.

Pond input parameters for each subwatershed.

Subwatershed WET_FR WET_NSA (ha) WET_NVOL 104 (m3) WET_MXSA (ha) WET_MXVOL 104 (m3) WET_VOL 104(m3)
1 0.0000 0.00 0.00 0.00 0.00 0.00
2 0.0000 0.00 0.00 0.00 0.00 0.00
3 0.0249 65.97 32.99 219.90 109.95 6.60
4 0.0151 46.43 23.22 154.78 77.39 4.64
5 0.0004 1.38 0.69 4.61 2.30 0.14
6 0.0040 12.62 6.31 42.06 21.03 1.26
7 0.0001 0.15 0.08 0.50 0.25 0.02
8 0.0000 0.00 0.00 0.00 0.00 0.00
9 0.0000 0.00 0.00 0.00 0.00 0.00
10 0.0000 0.00 0.00 0.00 0.00 0.00
11 0.0000 0.00 0.00 0.00 0.00 0.00
12 0.0000 0.00 0.00 0.00 0.00 0.00
13 0.0018 7.18 3.59 23.92 11.96 0.72
14 0.0146 39.90 19.95 133.01 66.51 3.99
15 0.0093 27.84 13.92 92.79 46.39 2.78
16 0.0003 0.96 0.48 3.20 1.60 0.10
17 0.0000 0.00 0.00 0.00 0.00 0.00
18 0.0142 37.57 18.79 125.24 62.62 3.76
19 0.0058 15.53 7.77 51.78 25.89 1.55
20 0.0019 3.77 1.89 12.57 6.28 0.38
21 0.0052 17.23 8.62 57.45 28.72 1.72
22 0.0331 70.06 35.03 233.53 116.76 7.01
23 0.0017 5.04 2.52 16.79 8.40 0.50
24 0.0040 6.33 3.16 21.09 10.54 0.63
25 0.0000 0.00 0.00 0.00 0.00 0.00
26 0.0081 31.88 15.94 106.25 53.13 3.19
27 0.0002 0.81 0.41 2.70 1.35 0.08
28 0.0060 14.39 7.20 47.97 23.99 1.44
29 0.0364 127.13 63.56 423.75 211.88 12.71

Table 7.

Wetland input parameters for each subwatershed.

2.3. Model setup

SWAT divides a watershed into subwatersheds and further subwatersheds into hydrological response units. User-defined approach for delineating subwatersheds was used. ArcSWAT was used to develop the SWAT2012 model with a revision number 635. A threshold of 0% for land use, 5% for soil, and 0% for slope was used to delineate HRUs resulting in 3402 HRUs. Some past studies reported the relationship between watershed response and HRU delineation approach [18, 19].

2.4. Calibration and validation

Before calibrating a model, sensitivity analysis is usually performed to reduce the number of parameters. Latin hypercube (LH) one-at-a-time (OAT) method [20] was used to identify the sensitive parameters that might affect the output results. A total of 22 flow parameters were tested, and the following 12 were found sensitive: SOL_AWC, CN2, ALPHA_BF, SOL_K, CH_N2, CH_K2, CANMX, RCHRG_DP, SURLAG, GW_DELAY, OV_N, and GW_REVAP.

The model calibration period was from 1987 to 2006 and the validation period was from 2007 to 2012. The first 3 years of calibration period were selected as a warm-up period so that the model parameters can be initialized. The calibration started with baseflow followed by surface flow adjusting related parameters affecting baseflow and surface flow. The SWAT Check tool [21] was used before calibration to make sure that the simulated outputs were within the reasonable ranges. The Load Estimator (LOADEST) tool [22] was used on a water quality dataset available from Sept 2011 to Dec. 2012 at Hattieville and Apr. 2012 to Dec. 2012 at Morrilton. The regression coefficients were found to be statistically significant (p < 0.05) at Hattieville and Morrilton for sediment, total phosphorus, and nitrate nitrogen. The performance of the model was determined mainly using the coefficient of determination (R2).

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3. Results and discussion

3.1. Calibration and validation results

Various SWAT parameters that were calibrated along with their parameter ranges and final calibrated values can be seen in Table 8. The annual calibrated R2 for the total, surface, and baseflow was 0.83, 0.85, and 0.16. The validated R2 was 0.91, 0.93, and 0.60 for the total, surface, and baseflow. The monthly calibrated R2 was 0.73, 0.73, and 0.54 and validated R2 was 0.84, 0.78, and 0.76 for the total, surface, and baseflow, respectively. The calibration and validation scatter plots for total flow, surface flow, and baseflow can be seen in Figure 5. The validated R2 for water quality was 0.5–0.7 at Hattieville and 0.7–0.87 at Morrilton. The results are within acceptable limits of other modeling studies relating to limited data availability [24, 25].

File/parameter Definition MIN MAX Units Calibrated value Notes
.bsn
ESCO Soil evaporation compensation factor 0 1 0.95 Based on water balance
EPCO Plant uptake compensation factor 0 1 1 Based on water balance
.gw
GW_DELAY Groundwater delay 0 500 2 Calibrated value
ALPHA_BF Baseflow alpha factor 0 1 Days 0.0932 Baseflow separation factor
GW_REVAP Groundwater “revap” coefficient 0.02 0.2 0.072 Calibrated value
REVAPMN Threshold depth of water in the shallow aquifer for “revap” to occur 0 1000 750 Calibrated value
RCHRG_DP Deep aquifer percolation fraction 0 1 0.06 Calibrated value
GWQMN Threshold depth of water in the shallow aquifer required for return flow to occur 0 5000 mm 800 Calibrated value
.rte
CH_N2 Manning’s “n” value for the main channel −0.01 0.3 0.014 Calibrated value
CH_K2 Effective hydraulic conductivity −0.01 500 mm/hr 6
.hru
CANMX-Forest Maximum canopy storage 0 100 mm 6 Wu et al., [23]
CANMX-Ag Maximum canopy storage 0 100 mm 2.8
CANMX-Pasture Maximum canopy storage 0 100 mm 4
CANMX-Urban Maximum canopy storage 0 100 mm 0.1
SURLAG Surface runoff lag time 1 24 Days 2 Calibrated value
HRU_SLP Average slope steepness 0 1 m/m Reduce by 10% Based on identified high sediment yield on high-slope agricultural HRUs
.mgt
CN2 SCS runoff curve number for moisture condition II 35 98 CN + 1 Calibrated value
.sol
SOL_AWC Soil available water capacity 0 1 mm/mm SOL_AWC × 1.13 Calibrated value

Table 8.

SWAT model parameter ranges and the final calibrated values.

Figure 5.

Calibration [left] and validation [right] scatter plots for total flow, surface flow, and baseflow.

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4. Conclusions

Modeling studies are gaining popularity due to rapidness of insight generation before actually performing field experiments. The initiative led by the Mississippi River Basin focused on analyzing the water quality benefits from intended best management practices with the help of modeling studies. However, merely simulating best management practices will not be able to provide reliable results unless the model has been set up correctly and robust. This chapter focused on the detailed discussion for setting up the model to a point where the model setup procedure can be replicated. The model was set up with all relevant information, and each data preparation step has been explained in detail. The model was calibrated and validated for flow at Hattieville. Due to limited water quality data, the model was validated for sediment, total phosphorus, and nitrate nitrogen at Hattieville and Morrilton. The results were satisfactory and within the ranges reported by previous studies. Results from this study can be used to evaluate the relative effectiveness of MRBI-recommended agricultural BMPs for analyzing pollutant load reductions and improving water quality in similar data-limited watersheds.

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Conflict of interest

The authors declare no conflict of interest.

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Written By

Gurdeep Singh and Mansoor Leh

Reviewed: 13 August 2018 Published: 28 November 2018