27 acres of land by 2050. Made by silt diverted from the Mississippi River in Plaquemines Parish. There are articles both for and against the Mid-Barataria Diversion.
Picture an hourglass lying on its side, the top resting in the Mississippi River to capture the sands of time floating downstream from the Midwest. The sand flows through the neck of the hourglass and empties into Barataria Basin, where scientists predict it will create and nourish freshwater marshes and saltwater wetlands to stave off an expected dramatic loss of Louisiana’s coast over the next 50 years. That’s the concept behind the Mid-Barataria Sediment Diversion project, a $2 billion proposal to rebuild a basin that has been eroding for more than a century because of natural subsidence, erosion by hurricanes and storms, construction of hundreds of miles of oil and gas canals and navigation channels and, more recently, increasing rates of human-accelerated sea level rise.
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It is expensive. The alternative is the potential loss of 20 parishes in south Louisiana.
It’s enormously expensive, the second costliest project in Louisiana’s coastal Master Plan, the state’s 50-year, $50 billion bid to keep the Gulf of Mexico from swallowing the 20 parishes along the coast and protecting them from hurricane storm surge. It’s controversial, and it’s risky, too, for while scientists are confident in their work and their predictions, hardly anything has ever been attempted on this scale. “The intent of the project is to change things. We know the trajectory the Barataria Basin is on right now and it’s not a good one,” said Bren Haase, executive director of the Coastal Protection and Restoration Authority. “Literally, there are tons of sediment passing through our river every day, every week and every year,” he said. “So the idea behind this project is to tap that resource, tap that sediment being moved by the Mississippi River, and introduce it into the Barataria Basin to help restore some of those wetlands that are in the basin and all those functions that are so important associated with those wetlands.”
The Army Corps of Engineers released its draft environmental impact statement on the project in March. The public comment period ends Thursday. Then the project is revised and, hopefully, will be released in 2023 and construction can begin. It just might work and produce what is needed down here – land.
Modeling conducted for the state indicates the Mid-Barataria Sediment Diversion will build more new wetlands than if no project is built. These five maps show the difference in land gained (blue) and lost (red), compared to no action, at the end of each of the first five decades of of the diversion’s operation. IMAGES FROM LOUISIANA TRUSTEE IMPLEMENTATION GROUP
In 2020, the Barataria Basin contained only 509 square miles of wetlands, marsh and land, according to the Army Corps of Engineers. While that’s an area almost as large as Phoenix, Arizona, consider that in 1935 the basin contained more than 935 square miles of wetlands, almost the size of the state of Rhode Island. The Corps says the diversion will create 27 square miles of new marsh and wetlands by 2050. Additional sea level rise is likely to reduce that to 21 square miles through 2070. The Corps says the diversion will create 27 square miles of new marsh and wetlands by 2050. Additional sea level rise is likely to reduce that to 21 square miles through 2070. But without the diversion, the basin’s wetlands will shrink to only about 81½ square miles, or 16% of its 2020 size, according to computer modeling conducted for the environmental assessment. Even with the diversion, only about 133⅔ square miles will remain in the basin by 2070.
This model is what the Mississippi did to build South Louisiana, especially New Orleans!. Silt left the river to build land. Then we built levees and straightened the river for easier commerce and the land building stopped. We will not be letting the river do what the river wants to do, which for nature would be the best option, but being still constrained the diversion will only gather 7.5% of the river flow. The Corps of Engineers first had to pick a site, determine opening and closing and deciding the amounts of sediment, nutrients and other environmental contaminants would be allowed. The kinds of sediment and the best time of year were also considered.
The project would be built at river mile marker 60.7, just downriver from the Phillips 66 Alliance oil refinery and the proposed Plaquemines Liquids Terminal and just upriver of the Ironton and Myrtle Grove communities. “We actually sited the diversion based on the ability of that site to capture sediment loads, specifically sand loads,” said Wes LeBlanc, a coastal resources scientist at the Coastal Protection and Restoration Authority and manager for the project. The largest grains would be captured as the river begins to rise as a result of winter and spring floodwaters moving down from the Midwest. Researchers determined that those large grains, mostly sand, would likely drop out of the water near the diversion’s outlet, while smaller sand grains, organic material and mud particles would be carried farther south and west in the basin by the freshwater. Some of it would eventually settle out on or near existing wetlands, helping to assure their survival.
The location is also just below three sandbars the river passes over giving the possibility of more sand to be gathered through the diversion.
The researchers also had to determine the best time of year to open and close the diversion, based on records of the amount of sediment in river water during a 50-year period from 1964 through 2013. “At low flow, there’s no sand in suspension in the river,” said Ioannis Georgiou, director of coastal and deltaic systems modeling at The Water Institute of the Gulf and formerly director of the University of New Orleans’ Pontchartrain Institute for Environmental Sciences. “The sand gets trained [in the water] as the flow transitions from low to high.” The trigger delivering the most large sand grains is when the river’s flow reaches 450,000 cubic feet per second upstream at Belle Chasse. At that point, the diversion gates are opened and 25,000 cfs of water and sediment will flow into Barataria Basin. As the river speeds to 1 million cfs, the amount diverted will increase to a maximum of 75,000 cfs.
At its highest flow, the diversion will deliver an average 50,000 metric tons of sand and soil per day into the basin. But it’s more likely that the average flow when the gates are open will be about 33,636 metric tons per day. That’s enough sediment to fill the Louisiana Superdome in 92 days, or fill 198 Superdomes over 50 years. However, the larger grain sizes best suited for land building, between 63 and 250 microns, represent only about 26 percent of the sediment load. That translates into filling the equivalent of 52 Superdomes over 50 years. The lighter sediment, a combination of sand, organic material and mud particles, isn’t lost, though, Georgiou said. As it moves farther out in the basin, many of these particles will be caught by marsh and wetland grasses, or deposited on the grasses during high tides or storms, with the remainder slowly settling into open water.
The 50-year sediment load modeling was combined with detailed bathymetry, the mapping of water depths, of the present mix of wetlands and open water. That let scientists estimate the amount and location of new land built over 50 years, said Jim Pahl, a senior coastal resources scientist with the coastal authority. Included in the estimates are assumptions of the rate of sea level rise and land subsidence, and other natural conditions that might affect the way land builds, he said. The state predicts the Gulf of Mexico will rise almost 5 feet in Barataria Basin by 2100. That’s based on expected increases in the worldwide release of greenhouse gases such as carbon dioxide through the remainder of this century. Subsidence rates, the natural sinking of land, near the diversion site is averaging about 5 millimeters a year, the equivalent of another 10 inches of sinking through 50 years. Thus the combined effect of rising seas and sinking land is that the water in the basin could be 5 feet, 10 inches deeper by 2100.
If we can reduce greenhouse gases then sea rising might not be as much. Efforts are being done to make this reduction a reality and Gov. John Bel Edwards’ proposed reduction in Louisiana’s releases to 2005 levels by 2050 is a good starting point.
“What we’re providing are not absolute predictions that in year 5, it’s going to be this, year 10 is going to be this,” Pahl said. “It gives us an order of magnitude of estimation of what we believe is going to be the outcome.” The modeling included some runs with the proposed Mid-Breton Sediment Diversion in operation on the river’s east side and a bit upstream. It also included some runs that assumed the state would indeed build separate marsh creation projects it is planning within the basin. The modeling also looked at the effects of nutrients carried by river water into the basin. The nutrients include fertilizer that is used on farms throughout the river’s huge watershed and flows downstream during spring and summer months. Some nutrients come from untreated or inadequately treated sewage.
These nutrients are important to the diversion in two ways. First they help grow the plants and then when the plants die their organic matter will be dropped to the bottom building land. The model also looked a where sediment including nitrogen and phosphorus would be carried to. Monitoring these nutrients is also important as they end up in the Gulf and cause the annual summertime low-oxygen dead zone along the state’s coastline. The federal-state Mississippi River/Gulf of Mexico Hypoxia Task Force has been working with farmers to voluntarily reduce the amount of fertilizer used in farming with little success.
Pahl said the modeling of nutrients diverted from the river to the basin assumes that the amount of nutrients carried by the river doesn’t change from levels measured during the past 50 years. In the basin, nutrients might still impair oxygen in the water, but not to levels violating state Department of Environmental Quality standards, the Corps’ environmental statement concludes. Another area of uncertainty is the potential for block faulting: Whether the weight of sediment in newly built wetlands could cause the geologic blocks of the underlying earth to sink rapidly. Pahl said the environmental statement acknowledges there’s a chance that would happen, but assumes it will not. “Just because there’s a fault somewhere, what is our level of certainty that we can say that if we have a diversion layering new sediment on top of that marsh where the fault is, is that going to induce a slump in an isolated geologic block?” he said. “I don’t think anybody can say with certainty that is going to happen or not. “We’ll be monitoring that as best we can and hoping that at some point the state of the science catches up to provide something more appropriate to use as an advisory,” he said.
In short, the models show progress can be made but, as usual, nature will have the final say. What is known, though, is that this is only one part of the solution to save South Louisiana and we also have a part to play.
