Estimating Load and Concentration of
Total Nitrogen by Non Point Source in Nooksack
watershed
Joon Hee, Lee
Department of Civil and Environmental
Engineering
Introduction/Method/Results/Conclusion/Future work/References
In recent
years, water supplies have increased in watersheds of
Nitrogen
is the most important constituent in water quality issue because nitrogen
causes eutrophication. Therefore, in this study, total nitrogen
(T-N) load and concentration from non-point source in Nooksack
watershed were estimated. In addition,
the effect of landuse change was evaluated.
In
order to estimate total nitrogen (T-N) annual load, export coefficient approach
was used. The export coefficient is a
pollutant loading rate for some land use in unit area and unit time period
(EPA, 2000). The load is calculated by
following equation.
LP = S (LPU
x AU)
Where LP= Total
nitrogen annual load (lb/yr)
LPU= export coefficient
(lb/ac/yr)
AU=Area of land use type
(ac)
The export coefficient
depends on landuse.
For example, the total nitrogen export coefficients for agricultural and
urban area are higher than forest (Table1).
Table 1. T-N export coefficient
Landuse
type* |
LEVEL 2 ** |
T-N Export coefficient (lb/ac/yr)* |
Low density residential |
Mixed urban or built-up Other urban or built-up |
4.43 |
Multi family residential |
Residential |
7.07 |
Commercial |
Commercial and service
area Industrial commercial
complex |
9.48 |
Highway |
Transport, Commercial,
Utility |
6.25 |
Industrial |
Industrial |
9.93 |
Open Land |
Shrub & Brush range
land |
2.32 |
Wetlands |
Forested wetland Non forested wetland |
4.90 |
Pasture |
Cropland and pasture |
5.60 |
Agriculture |
Orchard, Grove etc. |
15.65 |
Woodland |
Deciduous forestland Evergreen forestland Mixed forestland |
2.78 |
|
Others |
2.20 |
* Supplied by North Florida
Water Management district in EPA, PLOAD User manual.
**In this study, landuse shape file with LEVEL2 was used. Therefore, T-N export coefficient values
supplied for 10 landuse type were matched to LEVEL2.
In this study, annual run
off was calculated by following equation
R= P-ET-U
Where R= Annual run off (in)
P= Precipitation (in)
ET= Evaporate transportation (in)
U= Water use
After calculation of annual
load and run off, total nitrogen concentration is calculated by following
equation.
C= (LP x 454000)/(R x 0.0254x AU)
Where C= Total nitrogen concentration (mg/L)
LP= Total
nitrogen annual load (lb/yr)
R=Run off (in)
AU=Area of land use type (m2)
454000= conversion
factor (mg/lb)
0.0254= conversion
factor (m/in)
The T-N concentration from
non-point source at outlet of each sub-watershed was estimated by following
equation.
S L
T-N
concentration at outlet (mg/L) =
---------
S Q
Where L= T-N load from each
land use in a watershed (or sub-watershed) in mg/yr
Q= Run off from each land use in a
watershed (or sub-watershed) in L/yr
In order to estimate annual average T-N load and
concentration, run off data, export coefficient data and a shape file including
landuse data were used (Figure 1). Run off data came from the water balance
table by Utah Water Research Laboratory.
Averaging run off in inch for each sub watershed was used to calculate
run off in m3. Export
coefficient data came from PLOAD user manual by EPA (EPA, 2000). Land use shape file including area of each
land use type was downloaded form EPA BASINS web site (EPA, 2002). Runoff data and export coefficient data are
inserted to the table of shape file for land use. After inserting runoff data and export
coefficient data, annual average total nitrogen load and concentration for each
land use of each sub watershed were calculated by calculation function of the
table in Arc Map (Figure2).
Figure 1. Linking data to estimate T-N load and concentration
In order to study the effect of landude
change, It was
assumed that deciduous forest area at western part of North fork Nooksack sub watershed was converted to agricultural
area. After export coefficient for this
area was change, the T-N load and
concentration at outlet of North fork Nooksack sub
watershed were recalculated.
Figure 2. Table of landuse shapefile inserting export coefficient and run off data
1) Area and landuse pattern
The total area of Nooksack watershed is 1935 Km2. Five sub watershed, which are north fork Nooksack, middle fork Nooksack,
south fork Nooksack, Nooksack
river and Sumas river, were delineated (Figure 3). North fork Nooksack is biggest sub-watershed and sumas river is smallest sub watershed in Nooksack watershed (Figure 4). In three eastern watershed ,
north fork, south fork and middle fork Nooksack
sub-watershed, much area are forestland
and just small areas are agricultural and urban land (Figuer
5). However, in western part, 52% of
Nook sack river sub watershed and 86% of Sumas river sub watershed are
Agricultural land. Also, 12% of Nooksack river sub watershed and 6% of Sumas river
sub-watershed are urban land (Figure 6)
Figure
3. Sub watershed in Nooksack watershed
Figue 4. Distribution area
for each sub watershed
Figure 5. Landuse in Nooksack watershed
Figure 6. Landuse distribution for each sub watershed
2) Estimated annual average
T-N load from non-point source
Total
annual average T-N load caused by non-point source of entire Nooksack watershed was 1,537,029 lb/yr. Even though Nooksack river and Sumas river
sub-watershed occupied just 31% of entire Nooksack
watershed area, 45% of total Non-point source T-N release were caused by Nooksack river and Sumas river sub watershed (Figure
7). This is because these two western
sub watershed has high export coefficient due to agricultural activity such as
use of fertilizer and urban activity.
Figure 7. T-N load distribution for each sub watershed
3) Run off
North
fork, middle fork and south fork Nooksack sub
watershed have much higher precipitation than Nook sack river
and Sumass river sub watershed (Figure 8). Therefore,
these three eastern sub watershed have higher runoff
than western two sub watershed (Figure 9).
Figure 8. Annual average precipitation, 1961-1990 (USDA, 2002)
Figure 9. Average annual run off
4)
Estimated annual average T-N concentration from non-point source
Almost Sumass river sub watershed
and western part of Nooksack River had over 1.0mg /L
T-N concentration from non-point source while T-N concentrations are below 0.6
mg N/L in almost north fork, middle fork and south fork Nooksack
sub watershed (Figure 10). This because
Sumas river and western Nooksack
river sub watershed have high T-N export coefficient due to agricultural landuse and low runoff. Estimated T-N concentration at
outlet of Sumas river sub watershed was 1.2 mg N/L. Therefore, even though estimated T-N
concentration at outlets of three up stream sub watersheds are 0.16 – 0.22 mg
N/L, the estimated T-N concentration at outlet of entire Nooksack
watershed was 0.35 mg N/L (Figure 11).
Figure 10. Estimated T-N concentration from non-point source
Figure 11. Estimate T-N concentration at outlet of each sub watershed
5)
The effect of land use change
After the deciduous forest land at western north fork Nooksack sub watershed was converted to agricultural area,
the T-N load from non-point source of north fork Nooksack
sub watershed increased 10.8 % from 428,105 lb/yr to 474,388 lb/yr (Figure
12). Since it was assumed that run off
was not changed after landuse change, the T-N
concentration also increased 10.8 % from 0.18 mg/L to 0.20 mg/L at outlet of
north fork Nooksack sub watershed. Since landuse
changing area was small (22.2 km2, 3.5% of north fork Nooksack sub watershed area), land use change did not give
large effect in T-N concentration.
Figure 12. Area of Landuse change
1. EPA, BASINS,2002, http://www.epa.gov/waterscience/ftp/basins/gis_data/huc
2. EPA, 2000, PLOAD user
manual
3.
USDA, 2002, climate and map data, http://www.ftw.nrcs.usda.gov/prism/prism.html
4. USGS, WRIA 1, 2002.
Watershed management project, http://wa.water.usgs.gov/wria1/Intro/intro.html
5. Watcom county, 2000,The watershed management act
6. USGS, 2002, Obtaining
NHD, http://edcnts14.cr.usgs.gov/Website/nhdserver/viewer.htm