logo
Scientific dispute over using sewage to restore Louisiana's wetlands turns political

Scientific dispute over using sewage to restore Louisiana's wetlands turns political

Yahoo13-04-2025

On right, the City of Hammond's assimilation wetland on the northern coast of Pass Manchac. The wastewater effluent flows to the right of the pipeline, labeled for clarity in the image. (Photo: Wes Muller/Louisiana Illuminator)
Opposing views among environmental groups and coastal scientists in Louisiana have spurred intense debates over the use of treated sewage to restore Louisiana's wetlands. The conflicts could jeopardize some decades-long efforts to restore the state's disappearing coast.
Wetlands are sometimes referred to as the kidneys of the earth — and for good reason. They keep water clean by filtering out pollutants and managing the amount of nutrients, such as nitrogen and phosphorus, that can lead to the harmful algae blooms that create 'dead zones' without the oxygen needed to support aquatic life.
Wetlands can even be created to treat wastewater processed from sewage treatment plants. The practice can avoid polluting rivers and streams while providing valuable habitat.
But in Louisiana, the use of natural wetlands for wastewater treatment is a topic rife with controversy.
Originally pitched as a method of coastal restoration, a natural assimilation wetland is typically an area of degraded forested swamp or marshland where disinfected treated sewage water is pumped in an effort to push away saltwater, provide nutrients for the growth of plants and trees, and reverse the sinking and eroding of the land. Louisiana's 3 million acres of wetlands, which include coastal marshes and swamps, are lost at the rate of roughly 75 square kilometers annually and are on pace to disappear entirely within 200 years, according to the U.S. Geological Survey.
Both federal and state regulators permit local wastewater utilities to use natural wetlands for assimilation. One of the sites, located in Breaux Bridge, began in the 1940s as the city's solution to discharging its treated wastewater. But it wasn't until around the 1980s when LSU scientists began using and studying assimilation wetlands as a way to rebuild Louisiana's coast. There are now 15 such assimilation sites across the state.
Local utilities and scientists, led by wetlands ecologist John Day, believe assimilation sites have been largely successful in restoring wetlands. Day is one of the LSU researchers who spearheaded their use for coastal restoration. He founded Comite Resources, a company of environmental scientists who work on coastal restoration projects and currently monitor a few of the assimilation wetland sites.
On the other side of the debate is Eugene Turner, emeritus professor of coastal sciences at LSU, who says assimilation is killing rather than restoring wetlands. Turner has a vocal public following, including organizations such as the Ponchartrain Conservancy and Louisiana Wildlife Federation, that has rallied around his argument: Feeding treated wastewater to Louisiana's wetlands hurts rather than helps.
Such disagreements are a normal and even necessary part of science, but Day and his colleagues say Turner's side is venturing outside the scientific process and lobbying state lawmakers to halt the projects in an 'undemocratic' manner.
On March 18, Turner gave a presentation to the Louisiana House Committee on Natural Resources and Environment, claiming assimilation is a failure. He urged lawmakers to defund work on the South Slough Wetland project, just south of Ponchatoula. Much of the money for it comes from federal grants.
Six out of the nine assimilation areas LDEQ monitors passed their long-term health assessments, according to the agency's 2024 report. Wetland health is determined in the report solely by the amount of vegetation growth at the site, called net primary productivity, evaluated over a period of five years. The South Slough Wetland is one of the six sites that passed its evaluation.
Turner's claims received no pushback at the time because, according to Day, no other coastal scientists were invited to the hearing or even aware that the wetlands projects were up for discussion.
Turner did the same thing at a legislative hearing last year, catching the scientific community by surprise with misleading testimony that no one got a chance to refute, Day said in an interview.
'It's happened twice, and it's undemocratic,' he said. 'They never alert the larger scientific community that's interested in this.'
Turner disputed the idea he's doing anything underhanded and accused Day of trying to protect his funding source. Comite Resources provides the monitoring services for the site, though Day said he hasn't received a paycheck from the company in nearly 20 years.
'What is undemocratic? Testifying at a legislative session? Speaking up with facts?' Turner said in an interview. 'Is publishing in open access scientific journals undemocratic? Democracy includes public discourse in this country.'
Representatives from the Ponchartrain Conservancy and Louisiana Wildlife Federation also attended the March 18 meeting and gave testimony supporting Turner's position to pull money back from wetland assimilation projects. While the organizations supported the idea in the past, they have since changed their stance.
Ponchartrain Conservancy executive director Kristi Trail said she thinks Louisiana should stop issuing permits for new assimilation projects.
Both organizations cite many of Turner's arguments and are calling for treatment plants associated with assimilation projects to improve the quality level of the water they discharge into manufactured wetland areas. They also argue that the water may need to be mixed between assimilation wetlands and an open water body in an effort to protect wetlands against long periods of exposure to extra nutrients.
Ponchatoula state Rep. Kim Coates asked Louisiana Department of Equality Secretary Aurelia Giacometto, who was also at the March hearing, to respond to Turner's claims. Giacometto told Coates the agency could get back to her later if she submits her questions in writing.
Coates expressed some frustration with Giacometto's lack of response during the hearing. She reiterated that in a phone interview several days later, saying she was 'disappointed' LDEQ came to the hearing unprepared to discuss the work it has been doing.
Giacometto was at the hearing to discuss the agency's waste tire program. No one from the committee had asked LDEQ to prepare for a discussion on wastewater wetlands, the agency's communications division said in an email. Coates had not yet sent questions to the agency as of April 13, according to LDEQ.
Coastal researchers say one of Louisiana's greatest environmental threats is coastal erosion. The state has experienced significant deterioration of wetlands along its coast, eroding barrier islands that provide natural hurricane protection, threatening vital habitat for fish and wildlife and losing an ecosystem that absorbs greenhouse gases and is one of the earth's greatest carbon sinks.
Researchers have found geological evidence that the Mississippi River went through natural cycles of flooding and course meandering prior to the construction of levees. Like the tail of a snake, the river would frequently whip back and forth, changing its position and forming new deltas across the coast roughly every millennium.
These natural cycles created the wetlands along Louisiana's coast. The building of levees locked the Mississippi River in place, preventing it from depositing its nutrient-rich freshwater and sediments across the region's natural coastal plain, according to studies by LSU coastal scientists Harry Roberts and Irv Mendelssohn.
Through their research, Day and Turner have made significant contributions to science's general consensus on Louisiana's land loss, which points to climate change, sea-level rise, hurricanes and various human activities such as oil drilling, canal dredging and perhaps most significantly, the building of levees.
However, Turner agrees with only part of this theory and has spent much of his research arguing that canal dredging, above all else, is the primary cause of land loss. He points to more than 35,000 canals that have lacerated Louisiana's coastal wetlands, with massive amounts of soil dredged away for oil and gas operations and shipping lanes.
Turner has positioned himself against the consensus' view of how to solve Louisiana's coastal crisis, criticizing river diversion and wetland assimilation projects as costly and ignorant. He has published papers pointing out the large amounts of taxpayer money spent on such work and arguing that backfilling dredged canals is an easier and more cost-effective solution to restore the coast.
Day agrees that canal dredging has had a detrimental effect on the coast, but he said Turner has taken an extreme position by dismissing all the other causes of wetland loss.
Part of the controversy surrounding Louisiana's wetland assimilation projects lies in the difference between natural wetlands and artificial ones constructed for sewage assimilation.
Constructed wetlands are usually contained within a perimeter of concrete walls, making it easier for people to control the exact amount of water and nutrients that enters and exits a system. These engineered areas are used much more commonly around the world to treat wastewater.
Louisiana is one of few places that sends wastewater effluent to natural wetlands. Florida has a similar program intended to reuse wastewater and, in some capacity, restore wetland health. Both constructed and natural wetlands are used to treat the wastewater, but natural wetlands have stricter monitoring rules and allow smaller amounts of nutrients to be discharged.
Assimilation wetlands are similar to river diversions but on a smaller and less expensive scale, proponents say. In theory, both methods rebuild wetlands by introducing freshwater, nutrients and sediment into a degrading marsh, encouraging more plants to take root and allowing soil to accumulate over time.
Day and other supporters of natural assimilation wetlands argue resources shouldn't be spent on expensive artificial wetland systems when those resources can be used to save the state's natural wetlands.
With the Mississippi River delta sinking and the sea level rising, Louisiana's wetlands need to rise at at least the same rate to stop from disappearing, Day said.
Dr. Rachel Hunter, a wetlands ecologist with Comite Resources, said the method provides nutrients and freshwater to a hydrologically isolated wetland.
'So normally, where that water may be stagnant, you're getting water flowing through the area, and those nutrients and that fresh water will stimulate primary productivity,' Hunter said.
If regulators were to require sewage treatment plants to provide cleaner water for assimilation wastewater, proponents say it could cause the projects to fail. Increasing treatment reduces the amount of sediment pumped into a site to rebuild the land.
One of the most controversial assimilation sites is the South Slough Wetland just north of Pass Manchac, in Coates' district. Owned by the city of Hammond, it opened in 2006 and almost immediately generated public suspicion because marsh deterioration occurred at the site the following year, leaving mostly standing water in the area.
The initial deterioration at the Hammond site was attributed to nutria eating the vegetation, but the site rebounded after the project managers killed more than 2,000 nutria there, Day said.
Turner, a natural assimilation wetlands critic, argues wastewater overloaded with nutrients inundates the marsh. That weakens its soil strength and speeds up the rate of plant decomposition, causing wetlands to break apart, he said.
He dismissed claims that nutria are responsible for destroying new wetlands and doubled down on the unpredictability of a natural wetland making it hard to manage nutrient overload.
'It's very undefined,' Turner said, adding that without restraints on how effluent enters and leaves the marsh, wastewater nutrients have overloaded the system.
In his presentation to lawmakers on March 18, he displayed a photo of the site that showed what he said were dying trees and vegetation. Healthier looking vegetation was growing in the adjacent area north of the discharge pipe that does not receive any effluent.
The picture was taken in 2009, however, and Day accused Turner of using an outdated photograph and said he hasn't cited any data to show that effluent or nutrients are being affected by a lack of artificial containment structures.
The Illuminator visited the South Slough Wetland on March 20 and 25 and took drone photographs that show what appears to be thriving vegetation in the assimilation site, in contrast to mostly brown vegetation in the area north of the pipeline that does not receive wastewater. Proponents say this is a sign of the project's success.
Those on either side of the issue can present convincing arguments, but often lost in the debate is what might happen if the projects are shuttered.
Charles Borchers IV, Hammond's director of administration, said the opponents of the assimilation site never talk about alternatives for disposing the city's treated wastewater.
'A lot of people don't understand where wastewater goes after they flush their toilet … It has to go somewhere,' Borchers said. 'It's not like it just sits at the wastewater treatment plant and just goes away.'
If not for the assimilation wetland, the city would be discharging its wastewater into a river, lake or some other body of water, he said.
Borchers was also upset when he learned lawmakers had a hearing in which Hammond's project was criticized and no one was there to defend it. Like Day and Hunter, city officials only learned about the hearing when they received calls from the Illuminator.
'The city's position is that the science is on our side,' Borchers said.
He considers the site healthy and growing and said the city has its own scientist who monitors the water quality and reports the data to LDEQ on a regular basis.
'You can go to Google Earth and look at that area evolve over time,' Borchers said. 'It's got more vegetation, and it's more green now than it was in 2005.'
Turner, the Louisiana Wildlife Federation and Ponchartrain Conservancy called for a full review of the natural wetland assimilation program at the legislative meeting in March, urging LDEQ to discontinue permits for natural wetlands assimilation projects. Day supported the idea of a review, saying the science supports the projects.
'I'm all in favor of it, but let's have full involvement of everybody in there,' Day said.
SUPPORT: YOU MAKE OUR WORK POSSIBLE

Orange background

Try Our AI Features

Explore what Daily8 AI can do for you:

Comments

No comments yet...

Related Articles

Colorado just had an earthquake. Is that normal? Here's what to know
Colorado just had an earthquake. Is that normal? Here's what to know

Yahoo

timea day ago

  • Yahoo

Colorado just had an earthquake. Is that normal? Here's what to know

A 2.9 magnitude earthquake near Dacono provided a jarring wakeup for some Coloradans, with the shaking reported some 20 miles away into the Denver area. The U.S. Geological Survey said the temblor had an epicenter about 3 miles southwest of Dacono. The quake was not the largest in Colorado in 2025 — that honor goes to a 3.2 quake that rumbled about 21 miles west of Delta on April 3. But the Dacono quake likely stood out because it was relatively close to a large population center. Reports of people feeling the jolts stretched into Thornton and over to Erie. While minor, the event was a reminder along the Front Range that Colorado can have earthquakes, and good preparation is important in the event of more significant shaking. Somewhat. There have been 20 reported in the past year on Earthquake Track, a website that logs seismic activity around the world. They're just not that large and not usually close to cities. The largest in the 365 days prior to the Dacono quake was a 3.4 earthquake near Salida on Oct. 26, 2024, according to the USGS. More: What cities are most at risk of a strong earthquake? Here's what USGS map shows Colorado has thousands of faults, but only five have been studied enough and determined to be active enough to end up on the USGS's National Seismic Hazard Map. They are the Cheraw Fault in southeastern Colorado, Northern Sangre de Cristo Fault in south central Colorado, the Williams Fork Mountains Fault in southwestern Colorado, the Sawatch Fault in central Colorado and the Gore Range Frontal Fault, the closest major fault near the Denver area. The Colorado Geological Survey says it is likely that more faults have similar potential but have not been studied closely enough. In all, it says, it is impossible currently to predict the time or location of the next big Colorado earthquake. It has never had one recorded, based on seismologists' definition of a major earthquake having a 7.0 or greater magnitude. The strongest earthquake ever reported in Colorado was on Nov. 7, 1882, estimated as a 6.6 magnitude temblor. The epicenter has been difficult to pin down based on historical data, although estimates put it roughly 60 miles away from Denver in the northern Front Range. The Denver area accidentally became one of the most seismically active areas in the country in the 1960s. An attempt to dispose of chemicals from the Rocky Mountain National Arsenal by injecting them deep into the ground is believed to have triggered several years of seismic instability that caused property damage throughout the area. More than 1,500 earthquakes emanated along the Derby Fault from 1961 to 1967, including multiple quakes of 5.0 or greater magnitude. The largest quake recorded since then had a 5.3 magnitude on Aug. 22, 2011, with an epicenter about 15 miles southwest of Salida. Shaking is usually very brief, meaning you don't have a lot of time to react when an earthquake hits. Colorado Emergency Management has several recommendations of what to do when an earthquake starts: When you feel and earthquake, drop and cover under a desk or sturdy table and hold on to it. If it moves, move with it. Stay away from windows and objects like bookcases or display shelves that could fall. If you are in a crowded public place, do not rush for an exit. If you are in a theater or stadium, stay in your seat, protect your head with your arms or get under the seat. Do not leave until the shaking stops. If you are outdoors, move to a clear area away from trees, signs, buildings or downed electrical wires and poles. If you are on a sidewalk near a tall building, get into a building's doorway or lobby to protect yourself from falling bricks, glass and other debris If you are driving, slowly pull over to the side of the road and stop. Avoid overpasses, power lines and other hazards. Stay inside the vehicle until the shaking stops. If you are in a wheelchair, stay in it. Move to safe cover if possible, lock your wheels and protect your head with your arms. There are several steps you can take to prepare for an earthquake. Anchor appliances and tall, heavy furniture that might fall. Put latches on cabinet doors to keep contents from spilling out. Establish an 'out-of-area' contact family members should call if you are separated, particularly if local phone or internet service is not working well. Keep emergency supplies in one place in the home. The Great Colorado ShakeOut, billed as the state's largest earthquake drill, is scheduled for Oct. 16. It is a coordinated day for individuals, businesses, public spaces and more to practice what to do in the event of an earthquake. Interested parties can sign up at the event's website. Nate Trela covers trending news in Colorado and Utah for the USA TODAY Network. This article originally appeared on Fort Collins Coloradoan: Colorado earthquake: How common are they and when was the last one?

Trump administration cuts could impact efforts to shrink Gulf ‘dead zone'
Trump administration cuts could impact efforts to shrink Gulf ‘dead zone'

Yahoo

time2 days ago

  • Yahoo

Trump administration cuts could impact efforts to shrink Gulf ‘dead zone'

An aerial view of Plaquemines Parish, Louisiana, on June 7, 2024. Nutrients from throughout the Mississippi River basin wash down into the Gulf of Mexico, creating an annual 'dead zone' of low oxygen conditions. Aerial support provided by SouthWings. Credit: La'Shance Perry, The Lens Annual forecasts for the Gulf 'dead zone' at the mouth of the Mississippi River predicts the section of water with low oxygen levels will be about average in size this year. What's less certain is whether government efforts to reduce its size will falter as the Trump administration scales back agencies involved in the process. The National Oceanic and Atmospheric Administration predicts the dead zone will be around 5,500 square miles this summer. Some estimates suggest it will be a little smaller, including those from LSU research scientists Nancy Rabalais and R. Eugene Turner. Their study predicts the hypoxic zone to be around 4,800 square miles, taking into account how warmer water temperatures have altered the Gulf's complex food web, helping reduce the dead zone. The different models share one key element: their predicted size is about three times bigger than experts would like to see it. SUBSCRIBE: GET THE MORNING HEADLINES DELIVERED TO YOUR INBOX When nitrogen and phosphorus from farming fertilizers upriver washes down to the Gulf, the excess nutrients can cause algae to bloom near the surface of the water. When the algae dies and decomposes, it sinks into the water and depletes the oxygen fish and other aquatic life need to survive. The hypoxic conditions affect commercial and recreational fishing as well as cause ecological harm. Efforts to reduce nutrient runoff into the Gulf are largely outlined in the Environmental Protection Agency's Hypoxia Task Force Action Plan. Long-term, its goal is to reduce the dead zone to about 1,900 square miles by 2035. Its short-term objective is to drop the amount nitrogen and phosphorus emptying into the Gulf by 20%. Data from the U.S. Geological Survey (USGS), an integral agency in predicting the annual size of the dead zone, found the river's phosphorus load was up 31% but its nitrate levels were about 24% below average in May. That's just a snapshot from a single month, said Doug Daigle, an LSU coastal research scientist and coordinator for the Louisiana Hypoxia Working Group, a state-based organization working to address the Gulf's dead zone. He emphasized that multi-year data will give the most accurate picture into whether the U.S. is on target to meet its goals. 'Obviously, you don't like it to be bigger in the years when it's bigger, but then we also need to keep it in perspective in years when it's smaller. It's the trend over time that we're looking at,' he said. 'And we're not at square one.' Whether key federal agencies such as the USGS and the National Oceanic and Atmospheric Administration (NOAA) will have sufficient funding and manpower to gauge if reduction goals are even being met is uncertain, Daigle said. 'There's a lot of question marks about what's happening to the federal agencies and their capacity … between the mass firings and all the other things that are happening,' he said. Large sections of NOAA staff have been reduced, and USGS research and data collection funding faces millions of dollars in cutbacks. Daigle added there's supposed to be a meeting of the EPA's Hypoxia Task Force later this year, but with all of the federal changes, its members might not have the bandwidth to assess whether reduction goals are being met. 'That's all tentative at this point,' he said. An EPA spokesperson said in an email that the agency 'takes this initiative very seriously' and will continue its progress. They did not respond to specific questions over staffing capacity and funding resources. NOAA's communications staff declined to comment on staffing capacity, saying it 'remains dedicated to providing timely information, research and resources.' Several federal task force positions remain vacant as of June 12, with only 'TBD' listed on the EPA's website for spots reserved for its own representatives, the Geological Survey, the U.S. Army Corps of Engineers and other federal agencies. NOAA predicts the size of the dead zone at the beginning of the summer using an aggregate of models from various partner universities, including LSU and the University of Michigan. The agency will monitor and survey the dead zone throughout the summer and review its estimates against the size of the actual dead zone in August. 'It's about human behavior. There's both a watershed issue and a global climate change issue here,' Turner said. Turner and Rabalais agreed the problem isn't with the EPA's plan but a need for greater efforts to reduce nitrogen runoff upstream. Solutions such as cover crops and crop rotation strategies help farmers keep fertilizer in their soil for better plant growth and reduce hypoxia-causing runoff. 'Every place is going to be a little different, but there are ways to reduce this,' Turner said. Whether funding will continue to support these programs is unknown. Aside from some Inflation Reduction Act money and funds from previous federal farm bills, financial support for nutrient reduction has been 'modest,' Daigle said. 'There's a lot of questions about what's going to happen,' he added. This upstream uncertainty affects industries that depend on the Gulf, such as commercial seafood harvesting, according to Daigle. 'They're under a lot of stress' from hurricanes and the influx of cheap, foreign shrimp saturating the market, he said. Reducing the hypoxic zone before it becomes the final nail in the coffin for shrimping in the Gulf is part of the Task Force's plan, and now is the time to drive home these reduction strategies, Daigle said 'The idea was that you wouldn't wait for that to happen. You start reducing the loading, you reverse the trend,' he said. SUBSCRIBE: GET THE MORNING HEADLINES DELIVERED TO YOUR INBOX This story is a product of the Mississippi River Basin Ag & Water Desk, an independent reporting network based at the University of Missouri in partnership with Report for America, with major funding from the Walton Family Foundation.

Lava seen soaring from Kilauea's latest eruption
Lava seen soaring from Kilauea's latest eruption

Yahoo

time3 days ago

  • Yahoo

Lava seen soaring from Kilauea's latest eruption

HONOLULU, Hawaii – The eruption of one of the world's most active volcanoes continued on Wednesday with the U.S. Geological Survey reporting that lava reached as high as 1,000 feet in the air on Hawaii's Big Island. The USGS said a build-up of intermittent gas led to the twenty-fifth episode located along one of the mountain's northern vents. Cameras focused on the shield volcano showed a speculator stream of lava shooting out of the eruption site, with all activity safely confined within the boundaries of Hawaii Volcanoes National Park. The agency noted that no other significant changes in terrain or seismic activity were observed along Kīlauea's East or Southwest Rift Zones, which are areas of concern due to their closer proximity to infrastructure outside of the park. Live: Watch Kilauea Erupt As Lava Fountains Shoot Nearly 1,000 Feet Into The Air The latest episode is part of a broader series of events that have occurred around Halemaʻumaʻu crater since late 2024. "Episode 25 was preceded by intermittent gas-pistoning in the north vent, with associated small spatter fountains and lava flows which began before dawn on June 10. This activity, which occurred at a rate of about 5-10 gas piston events per hour, continued to increase in intensity until 11:57 a.m. on June 11, when a small sustained dome fountain began to feed lava flows onto the crater floor. As of 12:30 p.m. HST, fountains from the north vent are reaching about 165 feet (50 meters) high and feeding multiple lava streams. Fountains heights are likely to increase in the coming hours," the Hawaiian Volcano Observatory said in a statement. Volcanologists say any one particular event has typically lasted less than a day, followed by an extended period of relative calm. The last significant episode ended just last week with lava fountains reportedly reaching heights of up to 1,000 feet. Hazards associated with the eruptive episodes include the release of toxic volcanic gasses and strands of volcanic glass known as Pele's hair; however, all potential impacts were expected to remain in and around the national park site. Experts said rockfalls can also be enhanced in the immediate region, but the area surrounding the Halemaʻumaʻu crater has been closed to the public since 2007. 4 Classic Types Of Volcanoes The active shield volcano has been continuously erupting since 1983 and is among the most active in the world. In 2018, an eruption destroyed hundreds of buildings and forced the evacuation of thousands of residents, as a series of explosive fissure eruptions article source: Lava seen soaring from Kilauea's latest eruption

DOWNLOAD THE APP

Get Started Now: Download the App

Ready to dive into the world of global news and events? Download our app today from your preferred app store and start exploring.
app-storeplay-store