Case Studies
New Orleans, LA - August 2001
Geographic and Bathymetric Features of the Lake Pontchartrain
Estuarine System. View
AVI movie (3.45 MB)
Ioannis Georgiou works at the University of New Orleans,
Department of Civil and Environmental Engineering as a doctoral candidate
in Engineering and Applied Science.
Ioannis' work includes 2- and 3-D numerical modeling of the Lake Pontchartrain
System – simulating hydrodynamics, transport, and water quality processes.
This effort involves the collection of field data, analysis, construction
of laboratory scaled physical models, and implementation of numerical
hydrodynamic and transport models.
These models serve mainly to investigate the flow exchange and dynamics
of impeding salt water currents and the water quality impact these density
currents have on the Lake Pontchartrain ecosystem.
Data
visualisation plays a big part in applying his numerical models. Viewing
animated time steps during the execution of the solution is invaluable.
The ability to slice 3-D plots and volumes enable Ioannis to look inside
a process and discover hidden details.
Our Image of the Month is geographic and bathymetric (depth) features
of the Lake Pontchartrain Estuarine System. The data was collected during
the summer of 1998 with acoustic instruments that measure depth by reading
reflected signals off the bottom, and from digitised hydrologic maps provided
by the National Oceanic and Atmospheric Administration (NOAA).
The plot was generated by loading the depth data file, which included
a longitude, latitude and the corresponding depth, and then triangulating
the data points to create a surface plot. The contour option was checked
to show the depth contours. Value-blanking was used on the depth variable
to block out points falling on land. Additional contour levels were used
to show more detail in the areas where the depth did not vary significantly.
Finally, the map showing the location of Lake Pontchartrain was loaded
into a different frame, made transparent and popped to the front.
Bathymetric features shown in this plot are of specific importance in
constructing a mesh for the three-dimensional model. The intrusive high
density saltwater currents sink to the bottom waters of the lake – thus
depth variability would significantly affect the dynamics of the flow.
Ioannis is specifically investigating the impacts of saltwater intrusion
from the Inner Harbor Navigation Canal (IHNC) on the south shore of Lake
Pontchartrain. The IHNC is part of the Mississippi River Gulf Outlet (MRGO),
which connects Lake Pontchartrain with the Gulf of Mexico. The connection
between the MRGO and Lake Pontchartrain is achieved via the IHNC.

Map showing the Mississippi River Gulf Outlet (MRGO),
the Inner Harbor Navigation Canal (IHNC), and adjacent areas.
"The Mississippi
River Gulf Outlet system, built in 1963 as a shortcut for oceangoing
ships that were headed to New Orleans to upload and receive cargo, has
resulted in tremendous environmental damage such as salt water intrusion
and wetland loss, along with weather and flooding threats."
For Lake Pontchartrain this intrusion has led to the endangerment of fresh
water marshes that surround the lake. When the high salinity water is
pushed into fresh water marshes it eventually destroys the habitat. High
saline water causes the fresh and brackish (slightly salty) water dependent
plants and animals to die. Plants and invertebrates such as clams are
typically affected most. Birds and fish are able to swim out of the low
oxygen water, but ultimately driven out of the area due to salinity changes.
When the plants are destroyed in a marsh, the area becomes more susceptible
to wetland loss. The roots no longer hold soil together, allowing the
soil to wash away with the tide and storms.
There are no specified acceptable levels of salinity, but depending on
what you are investigating, a certain limit is apparent. Biologists discovered
that clam concentrations in Lake Pontchartrain were diminished not by
high salt content in the water column, but by low dissolved oxygen resulting
from the salt intrusion. In the case of the freshwater marshes, the Cypress
trees that dominate the area cannot tolerate salt concentrations exceeding
six parts per thousand (ppt for fresh water is sero ppt, and ocean water
is variable around 30-32 ppt).
The
contour plot above shows salinity concentration contours (top) and the
dissolved oxygen concentration contours (bottom). This field data obtained
in Lake Pontchartrain is to be used for calibrating the numerical model.
The image shows the density current originating from the navigation canal
(left) as it moves into Lake Pontchartrain (right). A depth irregularity
near the canal, consisting of a scour hole and a dredge hole, normally
fills up with higher salinity water from the canal. Once these irregularities
fill, this higher salinity water proceeds into Lake Pontchartrain as as
a thin layer in the bottom waters as shown in the plot. This thin layer
of higher salinity water is often associated with low dissolved oxygen,
as seen in the bottom plot. The goal is to investigate the dynamics of
this density current and the associated water quality impacts, and try
to calibrate numerical models to be used as predictive tools in the future.
After establishing hydrodynamics in Lake Pontchartrain, Ioannis and his
research team will attempt to relate circulation patterns, temperature
and salinity to dissolved oxygen, by solving additional equations. Once
this step is successfully completed, they will have a complete picture,
allowing them to address possible solutions such as structural modifications
to the canal, or additional structural components to help control the
intrusion.

XY plot showing salinity gradients (bottom salinity
minus surface salinity). The data is from the field surveys obtained using
a digital handheld YSI instrument.
TECPLOT TIP: If you want your
contour legend not to look overloaded with floating numbers add more contours
from the menu, then use the skip option to show fewer numbers but all
the colors. If your legend looks very small, enlarge it by increasing
the legend line spacing.
|