GIS in Water resources: CEE 6440
Using GIS to show the temporal –spatial variation of
Phosphorus in Wellsville City Sewage Lagoons as simulated by a water quality
model
Background and
justification of study
The Little Bear River TMDL identifies
Wellsville City Sewage Lagoons as a point source for Total phosphorus on the river’s
segment below the Hyrum reservoir to the East Fork Little Bear confluence. As a
result of the increased P loadings from the lagoons, this segment of the LBR is
impaired for its Class 3A beneficial use. In order to improve the receiving
water quality, the State in 2007 issued a UPDES permit to Wellsville City
Lagoons limiting the total P discharges from the Lagoons to 72 kg of TP /season
(warm season, June – September) and 360 kg of TP/season (cool season, October –
May).
Since discharge from the lagoons is
determined by the operators, it is important for them to know which cell has
the least P and when this occurs so that they can maximum discharge from the
Lagoon without violating the limit. This process would optimize the performance
of the lagoons and at the same time preserve the environment.
A water quality model helps describe and simulate complex
dynamic processes that are occurring within a water system. The modeling
process can however be greatly enhanced by the use of GIS which has very
powerful tools for spatial discretization and
visualization of data.
Figure 1: Wellsville City Wastewater
Treatment Facility schematic by J.U.B engineers
Objective
To determine and show the amount and distribution of
phosphorus in the Wellsville City Lagoons
Methodology
Process model
In order to
model P in the lagoons, a number of assumptions were made;
1. Each lagoon was assumed to be
completely mixed reactor
2. Non point sources into the lagoon were
considered negligible
3. P
was only taken out of the water column by precipitation/attachment to sediment and discharge
into LBR
4. Volume in each reactor was considered
constant
5. First order settling rate and
settling velocity was assumed to be 10 m/yr (Chapra,
2007)
6. No P recycle from sediments
Model set up
Reactor 1 Reactor
2
Reactor 3 Reactor
4
Where:
C-concentration of P (mg/m3), t-time (day), Q-discharge (m3/d),
h-time step (day), Vs-settling velocity (md-1),
Excel and GIS
The model was run in excel using
numerical methods (Heun’s method) and the results
obtained exported into GIS and displayed for analysis and interpretation.
Data used
Table 1: Hydro-geometric properties of the
Lagoons from J.U.B engineers report
Lagoon Cell |
Lagoon SA (acres) |
Depth (ft) |
Volume (Mgal) |
1 |
15.6 |
6 |
29.1 |
2 |
20.1 |
6 |
37.6 |
3 |
11.2 |
6 |
20.6 |
4 |
9.6 |
6 |
17.7 |
Total |
56.5 |
105 |
Field effluent phosphorus values,
discharge values from operators monthly report for the years 2004 – 2007, Bear
River Watershed data, and NHDPlus data. Temporal
visualization was done by use of Tracking Analyst tool, and Time slider.
Model output from excel and input into arcGIS
From the operators’ report, only
monthly effluent P concentrations, daily inflow and outflow discharge values
were available. Consequently, the discharge values were averaged to monthly
values inorder to have a uniform time step for the
model. The model was used to predict the P concentrations in each of the
lagoons based on the known effluent concentration. The model output was
tabulated and exported to arcGIS as a table
containing the temporal P data. This was done by using a table to table tool
that converted the excel table into a geodatabase
table.
It is important to note that the
model used was not very accurate because of the inherent assumptions but it did
give reasonable results for the purpose at hand. Also I could not verify the
results obtained because a lack of P data for the three lagoon cells (P values
are recorded for only the effluent out of the 4th lagoon cell).
The Study area is found within the
Little Bear River watershed specifically the Logan –Bear segment. Using the Bear River Watershed and NHDPlus data, a shape file of the lagoons was created and Little
Bear River located as shown in Figure 2.
Figure 2: Wellsville City Sewage Lagoons and the discharge point into the LBR
The attribute table for the lagoon
cells shape file contained the spatial reference data. A cell ID field was
added to the both tables containing the temporal data and spatial data and used
as a unique identifier to join the two tables in ARCGIS. Given that the join
had a one - many relationship, the make query table command was used to
successfully execute the join.
Table 2: Illustration of the one- many
relationship
Visualizing temporal data
Two types of data were displayed in ArcGIS i.e. time instant data (variation of P for each
month within each lagoon cell) and time extent data (Average P values for each
season with in each lagoon cell) using the tracking analyst tool and the time
slider respectively. This was done as an illustration on how the two tools
work.
Using tracking analyst tool
The query table containing both the
spatial and temporal data was exported into the geodatabase
as a layer. The add button on the tracking analyst toolbar was used to open the
add data wizard and input the spatial –temporal data contained in the layer.
The symbology of the event (TP) was changed to
graduated colors for better visualization. The play back manager properties
were set to one month and the visualization enabled using the play button.
Using the time slider
The query table was exported into the
geodatabase as a table. The time properties in the
table were enabled by checking “Enable time on this layer” under the time tab
in the layer properties. The time extent was set by specifying the start and
end time. I used 3 months for each season (winter, spring, summer and fall) for
uniformity and simplicity. The time slider was opened and its options changed
accordingly to give the desired output. Visualization was enabled by the play
button.
Results
Figure 3 illustrates the use of
tracking analyst tool to show P variation in the different lagoon cells for the
month of April 2004.
Figure 3: Temporal –spatial variation of P
(mg/L) within ponds for 04/30/2004 using tracking analyst tool
The graphs below illustrate the use
of the time slider to show the variation of P in the lagoons for the year 2004 in
kg/season. Discharge is from the fourth lagoon cell; therefore in an ideal
situation it should always have the lowest P concentration. This is not always
the case as shown in Figure 5. If the lagoon operators are provided such
information on a seasonal basis then it would be easy for them to determine the
quantity of P discharge required and from what cell. This information can be
provided by modifying the model to predict P concentrations given the desired
effluent limit, incoming P concentrations and discharge values. The lagoon
piping system already has the capacity to bypass effluent from the preceding
cells to cell 4.
Figure 4: Temporal –spatial variation of P
(kg/season) within lagoon cells for winter 2004
Figure 5: Temporal-spatial variation of P
(kg/season) within lagoon cells for spring 2004
Figure 6: Temporal-spatial variation of P
(kg/season) within lagoon cells for summer 2004
Figure 7: Temporal - spatial variation of P
(kg/season) within lagoon cells for fall 2004
Conclusions
GIS tools can be used to enhance
visualization of data from process models
Recommendations
Other than the demonstrated use, spatial temporal
visualization of data in ArcGIS can enable scientists
or researchers who have years of data to visualize how the data evolved or trace
progression trends. The tracking analyst tool is also a useful for real time
data.
References
NHDPlus http://www.horizon-systems.com/NHDPlus/
Watershed boundary
Dataset http://www.ncgc.nrcs.gov/products/datasets/watershed/
TMDL Little Bear River
J.U.B. Engineers
Report: Wellsville City Wastewater Treatment Facilities Plan (2008)
Chapra S.
(2007): Surface Water Quality modeling
ArcGIS professional library help (Tracking
Analyst tool)
ESRI video: Working
with temporal data in ArcGis http://video.esri.com/watch/93/working-with-temporal-data-in-arcgis
assessed on 11/01/2010.