Investigative team finds river spillway flooding caused new land formation in Louisiana

July 23, 2012 by Bob Yirka report
Map overview of survey location. Image: Nature Geoscience (2012). doi:10.1038/ngeo1525

( -- A team of geologists, civil engineers and one representative from the US Army Corp of engineers has found that when a spillway was opened last year to prevent flooding of the Mississippi river from drowning New Orleans, new land was created. The team, which has had their paper on the topic printed in the journal Nature Geoscience, says that this is the first time new land formation has been documented this way and now the technique might be used in the future to build up eroded lands.

In the spring of 2011, the became engorged as record amounts of snow melted along its northern route. The result was record flooding over a period of a month as news media marked its ominous march south. But because it took awhile for the extra water to reach areas in the south, planners had time to take action to best protect the most populated areas. They opened levees allowing water to spill over farmlands, enraging , but saving many villages, towns, and even cities such as New Orleans, which of course was flooded in the aftermath of hurricane Katrina just seven years ago.

Oblique aerial photograph of a dune field in the Bonnet Carré Spillway. Sand deposits were worked into trains of dunes when flood water flowed in the spillway. Once the flood subsided and the spillway was closed, the water drained and dried from the spillway, thereby exposing the dunes. Trees and shrubs near the top of the photograph provide scale.

 Credit: Jeffrey Nittrouer

To save New Orleans, engineers opened levees (using dynamite) allowing water to enter the Bonnet Carré Spillway, which was dug for just that purpose after a massive flood back in 1927. The tactic worked, sparing New Orleans from what might have been a fatal blow. But another unexpected positive outcome appears to have been the formation of new land in some of the areas that had been flooded. It was a surprise because just ten to fifteen percent of the water volume from the river was diverted, which was mostly surface water, yet some thirty to forty percent of the silt load it was carrying managed to make its way into the spillway. The result was new land development adjoining the river and massive silt deposits left behind on the farmlands that had been covered. The research team says that until now, such land development has only been theorized, never documented.

Now, because it’s been seen in action, engineers and conservation groups can study areas that might benefit from temporary flooding, and perhaps dig spillways to make it happen. One idea is to use such spillways to restore delta lands that have eroded due to farming over many years. Another is to build up lands around areas that tend to flood regularly to build up natural barriers.

Explore further: Mississippi diverted to revive Delta wetlands

More information: Mitigating land loss in coastal Louisiana by controlled diversion of Mississippi River sand, Nature Geoscience (2012). doi:10.1038/ngeo1525

After the 1927 flood of record on the Mississippi River, the Bonnet Carré Spillway in Louisiana was constructed as a flood control operation. When it is opened, the spillway diverts floodwaters from the Mississippi River to Lake Pontchartrain1, to reduce the water discharge flowing past New Orleans. During the 2011 Mississippi River flood, which had the highest peak discharge since 1927, the Bonnet Carré Spillway was opened for 42 days, from 9 May to 20 June. During this period, the average spillway discharge of 6,010 m3 s−1 amounted to 10–20% of the total river flood discharge. Here we present measurements of the areal extent and thickness of new sediments in the floodway, following the 2011 Mississippi flood. Only the upper 10–15% of the river water column was skimmed into the floodway. Yet, we conservatively estimate that 31–46% of the total sand load carried by the Mississippi River during the period of spillway opening was diverted. We find that local river conditions led to increased concentrations of suspended sand in the upper water column and thus led to diversion of sand from the river into the spillway. We conclude that an appropriate design of engineered river diversions in Louisiana can help mitigate coastal wetland loss.

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4.3 / 5 (3) Jul 23, 2012
A picture's worth a thousand words. Is it possible to increase the size of the 'Enlarge?' picture?
1 / 5 (2) Jul 24, 2012
What is amazing is Deltas naturally do this all the time., yet somehow they need proof that this will happen?
Jason C_
not rated yet Jul 24, 2012
This article is quite misleading. Levees do not have to be opened (particularly with dynamite) for water to flow through the Bonne Carre spillway. There is no levee between the river and the spillway; in fact, the fore-bay area is frequently flooded in the spring even though the spillway itself is rarely opened. The spillway is a wall with a series of wooden pins to keep water in the fore-bay area. To open the spillway a crane moves along the top of the structure and removes the pins.
not rated yet Jul 24, 2012
Doesn't look like they know much about anything.
What is new is that they believe that 40% or more silt was carried into a spillway with 15% of the water from the top few inches. A number of things are not necessarily accurate. But the silt dropped is easily measured and is one of the good side benefits of regular flooding.

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