CEE 6640 Term Paper
Prepared by Lindsey DeBoer
Pineview Reservoir, shown in Figure
1, is situated in the Wasatch Front region, approximately eight miles east of
Figure 1. Pineview Reservoir Watershed dominates the eastern half of
The majority of the watershed is dominated by rangeland in the upper elevations that is subject to minimal human impact. In contrast, the valley floor near the reservoir encompasses many uses such as agriculture, residential, and recreation and has been subject to many changes in recent years. Hydrologically, this watershed is impacted by snowfall and runoff events. Export coefficients based on land use can vary orders of magnitude (Lin 2004) based other factors such as soil type, geography, and climate. As such, there is a need to quantify the location-specific nutrient export rates. Future studies will focus on the hydrologic and chemical sampling and analyses required while this study presents a preliminary step in determining the sampling locations on one main tributary which will enable the quantification of the desired export coefficients.
The purpose of this project was to:
1) Identify the dominant landscape types under the categories of irrigated lands, impervious surfaces, and rangeland, and quantify their prevalence in the watershed draining to the reservoir,
2) Determine the areas for which non-point pollution can be attributed to two separate stream reaches using a bracketing technique,
3) Using literature values for the export coefficients, calculate the nutrient load per year of total phosphorus (TP) and nitrogen (TN) to the reservoir, and
4) Compare the two evaluated stream reaches to determine which monitoring sites will be the most efficient to quantify anthropogenic nutrient loads.
In order to conduct the geospatial analyses required to complete these tasks, the tools made available through ArcGIS 9 version 9.3.1 (ESRI Inc. 1999-2009) were utilized including the Arc Hydro (ESRI Inc. 2009) and TauDEM (Tarboton 2009) tools.
The approximate coordinates of
sampling sites of interest were obtained in the field using a handheld
GPS. Monitoring sites are located on one
of the main tributaries to the reservoir, the South Branch of the
The datasets were added to ArcMap and projected as necessary to Albers Equal Area Conic (USGS version) to preserve the accuracy of the land surface area and unify the spatial reference. The geographic coordinates of the proposed sampling sites were imported and converted to a feature class sharing the same spatial reference. Figure 2 shows the result of these steps.
Figure 2: Pineview Reservoir Watershed with Irrigated Lands, Impervious
Surfaces, NHD Flowlines and Waterbodies,
and Monitoring Sites
Watershed processing tools were employed on the DEM. First, the NHD Flowlines were burned in and the pits were filled using Terrain Processing (ESRI Inc. 2009). The D8 flow directions and slopes were calculated using TauDEM (Tarboton 2009). In order to determine the fraction of upstream area associated with a specific land use, weight grids were created for each of the specific land cover categories within the irrigated lands raster and for impervious surfaces with a value greater than one. This was achieved by using the Raster Calculator to isolate desired values and then reclassifying the selected feature as one and ‘no data’ values as zero. The D8 contributing area was calculated and recalculated for each land use using the values determined previously with the weighted grid. Dividing the D8 contributing area by each weighted contributing area yielded the fraction of upstream contributing area associated with the respective land use. An example of this procedure using impervious surfaces is shown in Figures 3, 4, and 5.
Figure 3: Impervious Surfaces Weight Grid
Figure 4: Impervious Surfaces D8 Contributing Area
Figure 5: Fraction of Upstream Area Occupied by Impervious Surface
Examining the outflow of the reservoir under natural conditions, total Pineview Reservoir Watershed area is approximately 79,000 hectares. The contributing land uses associated with this upstream area is summarized in Table 1. Area not classified under the categories of irrigated land (hay, alfalfa, pasture, idle, grain, and fruit) and impervious is attributed to rangeland.
Table 1: Land Uses Upstream of Reservoir
Outlet
Land Use |
Fraction |
0-Grass Hay |
0.0087 |
1-Alfalfa |
0.0203 |
2-Pasture |
0.0131 |
3-Idle |
0.0026 |
4-Grain |
0.0039 |
5-Fruit |
0.0000 |
Other (Rangeland) |
0.9401 |
Impervious |
0.0112 |
As shown in
Figure 6, the North and South Branches of the South Fork of the
Figure 6: North and South Branch of the
The drainage area by land use associated with each site was determined and Figures 7 and 8 compare the upstream and downstream sites, respectively.
Figure 7: Comparison of Land Uses Draining to Sites 5 and 4
Figure 8: Comparison of Land Uses Draining to Sites 6 and 7
Using export values reported by Lin (2004), Reckow et al. (1980), and Porcella and Sorensen (1980) (see Appendix A), the anticipated nutrient load per year at each site was calculated. By subtracting the load at the upstream site from the load at the downstream site, the corresponding load from each isolated reach was determined. Table 2 displays the results for each reach according to land use and as a total.
Table 2: Nutrient Load from each Proposed
Monitoring Reach
Monitoring
Site |
Land Use |
Area (ha) |
TP (kg/yr) |
TN (kg/yr) |
North Branch
(6-5) |
Grass Hay |
13.77 |
14.87 |
71.47 |
Alfalfa |
26.82 |
28.97 |
139.20 |
|
Pasture |
33.12 |
49.68 |
286.49 |
|
Idle |
19.44 |
1.94 |
66.10 |
|
Grain |
0.00 |
0.00 |
0.00 |
|
Fruit |
0.00 |
0.00 |
0.00 |
|
Other (Rangeland) |
50.85 |
4.07 |
45.77 |
|
Impervious |
4.32 |
8.25 |
43.07 |
|
Total |
148.32 |
107.78 |
652.08 |
|
South Branch
(7-4) |
Grass Hay |
108.09 |
116.74 |
560.99 |
Alfalfa |
278.10 |
300.35 |
1,443.33 |
|
Pasture |
87.48 |
131.22 |
756.70 |
|
Idle |
41.76 |
4.18 |
141.99 |
|
Grain |
22.41 |
24.20 |
116.29 |
|
Fruit |
0.00 |
0.00 |
0.00 |
|
Other (Rangeland) |
6,463.80 |
517.10 |
5,817.42 |
|
Impervious |
14.76 |
28.20 |
147.18 |
|
Total |
7,016.40 |
1,121.98 |
8,983.90 |
Figures 9 and 10 show the distribution of the sources contributing to the nutrient loads for the North and South Branches, respectively.
Figure 9: Land Uses Contributing to
Nutrient Load of North Branch Monitoring Reach
Figure 10: Land Uses Contributing to
Nutrient Load of South Branch Monitoring Reach
A similar procedure was used to determine the estimated nutrient export from the entire watershed under natural flow conditions (no inundation). The rate of total phosphorus export was approximately 12,000 kg per year and the total nitrogen rate was 99,000 kg per year.
Overall, the dominant landscape for this area is rangeland. It is roughly approximated in Table 2 as 94%; however, Figure 2 shows that anthropogenic impacts on land use are realized more frequently on the valley floor near the reservoir.
Examining Figure 7 shows that at
the upstream sites (5 and 4), the North Branch is dominated by rangeland and
the South Branch is split between alfalfa and rangeland. In contrast, Figure 8 shows the downstream
sites at which the South Branch is dominated by rangeland. There is currently minimal influence due to
impervious surfaces reflecting the large amount of open space still available
in this valley. Comparing the loads of
Figures 9 and 10 reveals that the North Branch will exemplify nutrient loads
more dominantly attributed to irrigated lands while the South Branch will be
more dominated by the loads from rangeland.
TP and TN represent estimates since the actual values will depend on the
local export coefficients which remain to be quantified and do not account for
any in-stream processes. As such, this
estimates the combined load from the North and South Branches of the
The dominant landscape in the Pineview Reservoir Watershed is rangeland; however, land use patterns change near the reservoir. Drainage areas were determined according to land use and nutrient loads were estimated using available export coefficients. Two reaches on a main tributary were proposed for monitoring and associated loads were calculated for the sites and associated reaches. By designating loads based on land use, it was found that the North Branch reach would exemplify loads from human impacts such as irrigated lands and the South Branch would be more characteristic of loads from rangeland. While this is a main tributary hydrologically, it only accounts for approximately 10% the nutrient export from the Pineview Reservoir Watershed under natural flow conditions.
ESRI Inc. (1999-2009).
ArcMap 9.3.1. ArcGIS Desktop Evaluation Edition 9.3.1 .
ESRI Inc. (2009). Index
of ftp://RiverHydraulics@ftp.esri.com/ArcHydro/. Retrieved October 16,
2009, from ftp://ftp.esri.com/ArcHydro/
ESRI Inc. (n.d.). Layers
containing online data. Retrieved November 26, 2009, from ArcGIS Resource
Centers: http://resources.esri.com/arcgisdesktop/index.cfm?fa=content&tab=Layers
Horizon Systems
Corporation. (n.d.). NHDPlus Data. Retrieved November 02, 2009, from
National Hydrography Dataset Plus:
http://www.horizon-systems.com/nhdplus/data.php
Lin, J. P. (2004,
September). Review of Published Export Coefficient and Mean Concentration
(EMC) Data. Retrieved November 28, 2009, from Wetland Regulatory Assistance
Program: http://el.erdc.usace.army.mil/elpubs/pdf/tnwrap04-3.pdf
Porcella, D. B., &
Sorensen, D. L. (1980). Characteristics of
Reckhow, K. H., Beaulac,
M. N., & Simpson, J. T. (1980). Modeling phosphorous loading and lake
response under uncertainty: a manual and compilation of export coefficients.
Tarboton, D. G. (2009). Terrain
Analysis using Digital Elevation Models (TAUDEM). Retrieved October 09,
2009, from Utah State University Hydrology Research Group: David Tarboton:
http://hydrology.neng.usu.edu/taudem/
Land Use |
Mean
(kg/ha/yr) |
Range
(kg/ha/yr) |
Sample Size |
|||
TP |
TN |
TP |
TN |
TP |
TN |
|
Row Crops1 |
4.46 |
16.09 |
0.26-18.6 |
2.1-79.6 |
26 |
11 |
Non-Row Crops1 |
1.08 |
5.19 |
0.10-2.90 |
0.97-7.82 |
13 |
10 |
Pasture1 |
1.50 |
8.65 |
0.14-4.90 |
1.48-30.85 |
14 |
13 |
Idle2 |
0.1 |
3.4 |
|
|
|
|
Rangeland3 |
0.08 |
0.9 |
|
|
|
|
Urban1 |
1.91 |
9.97 |
0.19-6.23 |
1.48-38.47 |
23 |
19 |
|
|
|
|
|
|
|
1 |
(Lin 2004) |
|
|
|
|
|
2 |
(Reckhow, Beaulac, & Simpson 1980) |
|
|
|||
3 |
(Porcella &
Sorensen 1980) |
|
|
|