Tag Archives: Pollution

Biogeochemistry of Nutrient Pollution

Yuck!

I have used the term biogeochemistry in several blog posts on nutrient pollution and have been asked to explain what this term means and what role biogeochemistry plays in nutrient pollution. Biogeochemistry is a mouth full, but if you dissect the word then you see that there are two prefixes attached to the noun chemistry – bio and geo. Bio is short for biology and geo for geology. Biochemistry refers to the chemical processes taking place within living things, for example the incorporation of nitrogen into a plant’s proteins and chlorophyll. Geochemistry on the other hand is the study of the chemistry of geological processes, such as, the behavior of nitrogen in water and soils. So biogeochemistry is the combination of the two.

 

To explain further, let’s follow through with the example of the biogeochemistry of nitrogen pollution. Did you know earth’s atmosphere is 78 % nitrogen? That’s good right? After all, living organisms on earth need nitrogen for use in daily metabolic functions. But plants including algae can’t directly use the nitrogen in the air. It’s kind of like that old maxim about the ocean – “water, water everywhere but not a drop to drink.” Nitrogen gas has to be converted into ammonia or nitrate in order for plants to be able to use it. Nitrogen fixation and nitrification are the primary processes of conversion.

 

Nitrogen fixation produces ammonia. The chief nitrogen fixers on the planet used to be bacteria. But of course now humans have gotten into the game. Nitrogen fixation occurs as a result of fossil fuels being burned in power plants and during combustion in car engines. The process called nitrification converts ammonia to nitrite and then on to nitrate. Nitrification is pretty much just carried out by single cell organisms like bacteria. Both nitrogen fixation and nitrification require oxygen.

 

These biogeochemical processes occur both in soils and in water. So in water bodies like lakes, rivers, estuaries and oceans, bacteria are busy converting unusable nitrogen into usable forms, which algae – just like terrestrial plants – can use to grow. There’s also another process called denitrification which is going on in soils and water that are oxygen deficient. A group of bacteria which prefer oxygenless environments are busy taking nitrate and converting it back to unusable nitrogen gas. The nitrogen gas formed by denitrification is then cycled back into soils and water where it is once again used in the nitrogen fixation and nitrification process. It’s just one perpetual do-loop and is called the “nitrogen cycle” by scientists.

 

Of course the algae require other nutrients like phosphorous to grow and they depend on sunlight for photosynthesis, but in coastal waters and estuaries, the growth of algae is only limited by the availability of nitrogen. This is because these little algae guys need 16 times more nitrogen than phosphorous to grow and ocean waters are low in biologically usable nitrogen compared to phosphorous. It’s the exact opposite for freshwater lakes and streams.  In general if you add a bunch of man-made forms of nitrogen from fossil fuel combustion, nitrogen fertilizers, farm animal manure, and human waste (from wastewater treatment plants) to estuarine and coastal waters then algae are going to thrive.

 

However there are all sorts of other biogeochemical interactions that can come into play which affect the availability of nitrogen compounds to algae in the water. Take phosphorous, it readily adsorbs onto sediments under normal oxygen conditions and is then not available to the algae floating around in the water. In this case, adding nitrogen to the water won’t result in excessive algae growth. However if a water body is lacking in oxygen then sediments will release adsorbed phosphorous back into the water. This is because adsorption of phosphorous in sediments is strongly dependent on the presence of iron – oxidized iron. Iron forms sulfide compounds in water bodies without oxygen. Phosphorous does not interact in the same way with iron sulfides in sediments as it does with iron oxides. Therefore in low oxygen zones, phosphorous is more available in the water to help algae prosper when there are sources of nitrogen pollution.

 

Iron is also needed by algae for photosynthesis. Iron is not very soluble in water so it has to combine with organic matter to be available to aquatic organisms. The amount of organic matter in low oxygen waters is higher than it is in water with normal oxygen levels, because well, a lot of things are dying down there in the no oxygen zone since most aquatic organisms need oxygen to survive. Increased iron is then available in the water to help algae grow.

 

Complicated right? And I haven’t even touched on the issue of silica and how it impacts the type of algae growing in a water body. The diversity of biogeochemical interactions within a water body is the reason why each one must be studied independently to determine how best to prevent nutrient pollution.

Georgia Coastal Pollution

The world lies east: how ample, the marsh and the sea and the sky!

A league and a league of marsh-grass, waist-high, broad in the blade,

Green, and all of a height, and unflecked with a light or a shade,

Stretch leisurely off, in a pleasant plain,

To the terminal blue of the main.

Oh, what is abroad in the marsh and the terminal sea?

Somehow my soul seems suddenly free

From the weighing of fate and the sad discussion of sin,

By the length and the breadth and the sweep of the marshes of Glynn.

– Sidney Lanier

Marshland in Georgia

 

Georgia has the largest extant marshland along the entire Atlantic coast. Except for the intrusion of Interstate 95 and the growth of the cities of Savannah and Brunswick, the landscape has changed little since Sidney Lanier wrote his poem about the Marshes of Glynn in Georgia during the 1800’s. The reason for the wetland preservation is the forward thinking people of the state of Georgia who back in 1970 supported and passed a law protecting the coastal marshes of Georgia (Georgia Coastal Marshlands Protection Act.) Georgia has around 370,000 acres of estuarine tidal marsh bordering its 100 mile coastline. The state has also protected most of the barrier islands along the coast and they are primarily state and federal parkland. With such little development one might expect nearly pristine water quality off the coast of Georgia. One would be wrong.

Five major rivers flow through the coastal region of Georgia and empty into the Atlantic Ocean – the Savannah, the Ogeechee, the Altamaha, the Satilla, and the St. Mary’s Rivers.  The Satilla and St. Mary’s River are blackwater rivers. Blackwater rivers are named for the color of their water which is a dark tea brown to black. The color results from the decay of the abundant vegetation in the marshes through which the rivers flow. The water in blackwater rivers is usually more acidic than rivers with clear water and it may also have lower dissolved oxygen because of the vegetative decay. The watersheds of all five rivers are large and encompass not only the salt and freshwater marshes along the coast but the upstream woodlands, agricultural lands, and small cities and towns which dot the region. Forests and wetlands are the primary land cover in these watersheds. Farms only make up 8 percent of the land use. The widely dispersed population centers cover 7 percent of the land.

In spite of the near perfect ecological conditions along Georgia’s coast, each of the rivers has impaired water quality. Impaired water quality means that the water in a certain stretch of the river does not meet the pollution standards for the water’s designated use, like fishing or swimming. The Georgia Environmental Protection Division issued a Surface Water Quality Resource Assessment in 2017 which identified 413 miles of impaired waters in the 5 coastal watersheds and impairment of two inlets where the rivers meet the ocean. The major cause of impairment is low dissolved oxygen, which is problematic for aquatic organisms like fish since they (like us) need oxygen to survive. The second cause of impairment is fecal coliform. Fecal coliform is a bacteria produced in the intestines of humans, other mammals, and birds and is discharged with their poo.

If you were a water scientist, you would immediately suspect – based on the fecal coliform levels in the surface water of the rivers – there might be a gigantic wastewater treatment problem in the towns and cities within the watershed. But no, the Coastal Georgia Regional Water Plan issued in June 2017 identified Bryan County wastewater treatment plants as the only ones in the entire area needing upgrades to meet water quality. The main contributors to water pollution, according to both The Surface Water Quality Resource Assessment and the Coastal Georgia Regional Water Plan, are non point sources like urban development in the small towns and cities within the watersheds, agriculture which consists primarily of livestock operations in the upland areas, and silviculture (a fancy name for tree farm operations). Widespread use of septic systems in this rural environment is also probably a major contributor to surface water degradation.

Blame for some of the dissolved oxygen problems also can be laid on the nutrients – nitrogen and phosphorous, but the lack of widespread dead zones such as the ones in the Gulf of Mexico caused by fertilizer runoff into the Mississippi River and the ones in the Chesapeake Bay caused by fertilizer run-off and overdevelopment in the watershed don’t exist off the coast of Georgia. Nutrients cause algae blooms. The algae die and their decay depletes the water of oxygen. The lack of widespread nutrient related dead zones off the coast of Georgia can be attributed to the lack of development and limited agricultural operations, but also to the existence of abundant marshlands. All wetlands remove nutrients from water. This has been documented in a number of scientific studies over the last thirty years. The soils in wetlands are called hydric soils because they are saturated. These types of soils are full of organic matter from all the decaying wetland vegetation. Denitrifying microbes love these soils and provide a substantial removal system which locks up the nitrogen and keeps it from flowing out of the wetland. The marsh plants also like the excess nutrients because it helps them to grow, so they suck up as much of it as they can get. Waters leaving a marsh are substantially cleaner than those which entered, so much so, that environmental scientists often construct artificial wetlands just to treat nutrients. Georgia’s preservation of their coastal wetlands has helped save them from the nightmare conditions which other aquatic environments are undergoing.

The Coastal Georgia Regional Water Plan is part of another forward thinking effort by the Georgia state government to engage in state wide water planning efforts to sustainably manage water resources throughout the state. State wide water planning began in 2009 and the first coastal plan was issued in 2011. The 2017 plan is an update. The goal of water planning on the Georgia Coast is to meet water demands while protecting ecosystems dependent on clean water such as Georgia’s significant offshore commercial and recreational fisheries.

The Coastal Regional Water Plan recognizes the sources of contamination and the impairments identified in the 2017 Surface Water Assessment and has established specific actions to be taken to reduce pollution including replacing and upgrading the wastewater treatment plants in Bryan County or moving their discharge locations. Also identified in the plan is a monitoring program to determine the sources of the persistent fecal coliform contamination, establishment of best management practices for stormwater runoff such as retention ponds and erosion controls, providing silviculture operations with incentives for restoring wetlands, and supporting implementation of agricultural runoff controls such as manure management, conservation tillage, and planting of cover crops.

Most actions under the plan are anticipated to be implemented by the year 2025. Little future development is anticipated along the coast because of the protections the state of Georgia has provided for their marshlands. These protections will limit the surface water degradation which is found in other states like Louisiana ( https://waterblogger.org/water-quality/gulf-of-mexico-pollution/) and Maryland (https://waterblogger.org/water-quality/chesapeake-bay-pollution/ ) where wetlands have been destroyed and as a consequence there has been serious water degradation from nutrient pollution.

This is the fourth blog post in a series concerning nutrient pollution.

Gulf of Mexico Pollution

Can you imagine an area of pollution in the ocean which is the size of the state of New Jersey and where no marine life can live because there is too little oxygen in the water? You would think if such a place existed then it would be featured on the nightly television news and be in the newspapers on a regular basis. After all journalists flocked to the Gulf of Mexico when the oil spill from the Deep Water Horizon occurred in 2011 and it was reported in the media on a daily basis. But indeed such a large polluted area in the ocean does exist and it is located off the coast of Louisiana in the Gulf of Mexico. Perhaps journalists ignore its’ existence because there aren’t dramatic photos to show on the television like flowing oil from a borehole on the ocean floor or multiple oiled seabirds. In fact if you sailed right through this huge polluted zone on a boat, you would not even notice it, unless of course you tried to catch a fish.

 

The lack of oxygen in this area of the Gulf of Mexico is caused by “nutrient” pollution. Essentially water flowing down the Mississippi River is full of sediment, phosphorous, and nitrogen washed off the abundant farmlands in the central part of the United States. Phosphorous and nitrogen are called nutrients because they are used by living things for growth and metabolic functions. When all those nutrients in the freshwater river flow into the salty waters of the Gulf of Mexico, two things happen. Number one, the freshwater forms a lighter layer on top of the heavier salty water in the near shore environment of the Gulf. Number two, all those nutrients in the freshwater feed the algae living at the Gulf’s surface where the sunlight is abundant. This causes the growth of massive algal blooms. When the algae eventually die, they drop to the salty bottom layer of water. The decay of the algae uses up the oxygen in the bottom salty layer of water and produces a hypoxic or dead zone. (For more information on nutrient pollution follow this link https://waterblogger.org/water-quality/nutrient-pollution/ ).

 

Scientists have been measuring the extent of the dead zone in the Gulf of Mexico for over thirty years. The size of the dead zone has gotten larger and larger and in 2017 it grew to be the largest size ever – 8776 square miles. You are probably thinking, why isn’t someone doing something about this huge dead zone in the Gulf of Mexico, like the U.S. Environmental Protection Agency (EPA), isn’t that their job? Yes it is, and the agency does have the regulatory tools under the Clean Water Act to require waters of the United States to meet Water Quality Standards. But so far, and despite recommendations to EPA in 2007 by the National Academy of Science for the agency to use their regulatory tools, the EPA instead has decided to improve water quality in the Gulf through the use of a voluntary watershed effort among the states with drainages entering the Mississippi River. A Hypoxia Task Force was established in 1997 which includes several federal agencies and the states of Iowa, Illinois, Minnesota, Wisconsin, Kentucky, Tennessee, Arkansas, Ohio, Missouri, Mississippi and Louisiana. This may seem like a lot of states, but in reality, it is not even all the states which have drainage into the Mississippi River, after all the entire Mississippi River basin covers 1,245,000 square miles – 41 percent of the lower 48 states of the United States. However, the states involved in the Task Force are the biggest contributors of nutrients to the river.

 

The Hypoxia Task Force regularly reports on progress being made to reduce nutrient pollution. The Task Force set itself a goal of reducing the hypoxic zone in the Gulf to less than 3100 square miles by the year 2035. In order to reduce the hypoxic zone to this size, the amount of nutrients entering the Gulf of Mexico must be reduced by 45 % from the average amount of nutrients measured between1980 and1996.  An interim reduction goal of 20 % has been set for the year 2025, just seven years from now. The Task Force is relying on individual state strategies to achieve these nutrient reductions. At this point all states involved with the Hypoxia Task Force have drafted or completed strategies. Each state has set very different methodologies and plans for achieving nutrient reduction goals. Other than some targeted improvements to reduce nutrients from wastewater treatment plants, most of the actions in the state strategies are voluntary.

 

The Hypoxia Task Force knows where most of the nutrient pollution is coming from, after all this problem has been studied for a long time. The U.S. Geological Survey (USGS) has been able with the help of the Natural Resource Conversation Service (NRCS) to define where the greatest amount of nutrient pollution is coming from in the Mississippi River Basin. Below is a map showing the main sources of nutrient pollution to the Gulf. The map was put together by the USGS for the EPA’s 2017 Biennial Report to Congress.

Nutrient Sources to the Mississippi River from the EPA 2017 Report to Congress

As you can see from the map, the states with the greatest nutrient contributions to the Gulf are in the northern basin of the Mississippi River. So states like Minnesota, Iowa, Illinois, Wisconsin and Indiana, which are all over a thousand miles from the Gulf of Mexico, are the biggest polluters. Most of the pollution is coming from agricultural lands. Some of the causes are over fertilization of crops, uncontrolled manure at farm animal operations, and even the growing of certain types of crops, such as soybeans, which can produce excess nitrate in the soil. According to EPA, there are numerous conservation methods identified by the Department of Agriculture which can vastly reduce these sources of pollution. Studies conducted by the NRCS on conservation practices already being implemented in the upper Mississippi River Basin show reductions of nutrients can be achieved in the order of 5 to 34 % for nitrogen and 1 – 10 % for phosphorous. The NRCS studies attribute these conservation practices within the whole Mississippi River Basin to an 18 % reduction in nitrogen and a 20 % reduction of phosphorus in the surface water entering the Gulf of Mexico.

 

With such large nutrient pollution reductions from existing conservation practices, one wonders exactly why the hypoxic zone in the Gulf is getting larger. There are a couple of reasons. Poor nutrient controls have been in place for multiple years. A lot of the old nutrients which washed off farmland years ago are now contained within the sediment of the streams and rivers forming the Mississippi River watershed. This sediment in the stream and river channels is a continuing source of nutrient pollution into the Gulf. Every time there’s a big storm or there’s lots of precipitation then sediments containing nutrients are scoured from the river and stream channels and washed further down the river toward the Gulf. Even if you were to eliminate all the nutrients in farm runoff from now into the future, there are still these legacy nutrients over which one has to worry.

 

I’m afraid we always tend to blame the farmers for all our nutrient pollution problems. Farmers are probably unfairly targeted to shoulder most of the nutrient reductions when many of the causes of the long term pollution problem in the Gulf are really a result of the over engineering and channelization of the Mississippi River to provide transportation and to reduce flooding. These activities have resulted in loss of streamside vegetation, including forests and wetlands that would have helped buffer the nutrient pollution. (Here’s a link to more reading on the problems of the Mississippi River https://waterblogger.org/water-quantity/dams-and-their-impacts-on-wetlands/  .) Scientists also blamed the increased size of the dead zone on the larger and more dispersed freshwater flow resulting from the channelization and diversion of the river into the Gulf through the lower portion of the Mississippi Delta because it has spread the nutrients and the stratification in the coastal waters over a much larger area then would have otherwise occurred.

 

So whatever pollution reduction methods are implemented by the states through their strategies, it is unlikely to produce immediate reductions in the size of the dead zone in the Gulf even by 2035. Unless of course other options like stream and river restoration activities are also incorporated into the Hypoxia Task Force’s plans.

Nutrient Pollution

My recent post on the Bloede Dam removal in Maryland prompted me to dwell a little bit on the nutrient pollution that continues to plague our water resources. Nutrients are the chief polluter of our river systems, lakes and coastal waters. It is such an old problem, but it just never gets resolved. When scientists talk about nutrient pollution, they are referring to phosphorous and nitrogen entering our waterways through surface run-off and groundwater discharge (referred to as “non-point sources”) and through direct discharges from wastewater treatment plants and other end of pipe sources (commonly called “point sources.”) Scientists are alarmed about the ever increasing amount of nutrients in our waters. So much so that a few years ago, the U.S. Environmental Protection Agency (EPA) commissioned a Nutrient Innovation Task Group composed of water managers and scientists from state governments, federal agencies and universities to define the problem. The Task Groups Report was issued in late 2009 and was actually entitled “An Urgent Call to Action.” It is a source of amazing statistics.

 

Just a refresher in case you don’t remember, but the problem with nutrients in our waterways is the resulting algal blooms. Scientists don’t call phosphorus and nitrogen nutrients for no reason. Both nitrogen and phosphorous are needed by living organisms for cell growth. This is why farmers spread it on their crops as fertilizer. It is why homeowners use it on their lawns. So when you have a lot of nutrients going into the water, it is like fertilizing the algae. Add sunshine and you get a bumper crop. Not really what anyone wants, because when the algae inevitably die off, the decay of their little dead algae corpses uses up the dissolved oxygen in the water through a process called eutrophication. Eutrophication produces “dead zones” or what scientists refer to as hypoxic zones. The quantity of floating algae (called phytoplankton) can increase so much that their mass actually blocks sunshine into deeper waters, depriving beneficial grasses and other vegetation that are to be found in the bottom of water bodies of the light they need for growth.

 

The Nutrient Innovation Task Group’s report states nutrient pollution along with the consequent overgrowth of algae and other nuisance aquatic plants as well as decreases in dissolved oxygen impairs 31% of assessed rivers and streams in the U.S., 30% of our lakes, and 50% of our bays and estuaries. The word “impairs” simply means that the function of the water resource is diminished. An example of an impaired water body would be an estuary which once supported a vital fishing industry but now has large “dead zones” where there is so little oxygen that fish can’t breathe and they have either died or vacated the area.

 

All of the excess nutrients entering our water bodies are from just a few sources, but they are large sources. Much of it comes from agricultural production. If there are no runoff controls on agricultural fields, excess fertilizer applied to crops can be washed into local streams. Manure from chicken and cows are also a big source of nitrogen and phosphorous to local waterways if not managed and controlled adequately. Urban storm water is another big source of nutrients as a result of all that lawn fertilizer we apply. Then there’s all the nitrogen and phosphorous coming out of wastewater treatment plants and septic systems. Humans in the U.S. produce about 18 million pounds of poop annually which is treated somewhat inadequately at our wastewater treatment plants. In 2009 when “An Urgent Call to Action” was published only 4% of the 16,500 wastewater treatment plants in the U.S. had limits for nitrogen in their permits and only 10% had limits for phosphorous. Then there are the 20% of homes in the U.S. which are on septic systems and are contributing nutrients to our surface waters via groundwater flow.

 

Oh wait a minute; I nearly forgot to mention another major source of nitrogen. It is from atmospheric deposition. When fossil fuels are burned in cars and power plants, it results in nitrogen oxides being emitted into the air. As they say, what goes up eventually comes down. And it comes down directly into our water resources or it is washed off our urban centers during storms and eventually makes its way into our waterways as well.

 

There are two well known, well studied water bodies where nutrients have caused major problems – the Gulf of Mexico and the Chesapeake Bay. The 2009 report cites that hypoxic zones cover 7900 square miles of the Gulf of Mexico and over 40% of the Chesapeake Bay. The report had a very interesting chart which I’m going to share here. It is the estimated sources of phosphorous and nitrogen going into these two water bodies.

 

Source: An Urgent Call to Action. Report of the State-EPA Nutrient Innovations Task Group. August 2009.

As you can see the source of most of the nutrients going into the Gulf of Mexico are from agricultural production, while nutrients going into the Chesapeake Bay are about equally split between agricultural production and urban sources.

Nutrient pollution is not a stagnant problem, because the population continues to grow. In the report by the EPA Nutrient Innovations Task Group, the chief cause cited for the escalation of nutrient pollution in water is the increase in the U.S. population. In addition, the report predicts the U.S. population will grow by 135 more million people by 2050, exacerbating the amount of nutrients flowing into our waters. The report written almost eight years ago now, states that current controls to reduce nutrient pollution of our water resources are totally inadequate. In response, the U.S. EPA and state environmental regulators developed a “Framework for State Nutrient Reductions” in 2011. The framework reflects a partnership effort to reduce nitrogen and phosphorous in U.S. waterways by prioritizing watersheds for reduction efforts and then setting actual goals such as strengthening permits for waste water treatment plants and other point sources, establishing strong programs to promote land stewardship practices for agricultural lands, and improving storm water management in urban areas.

As part of this effort states are being asked to establish numeric goals in priority watersheds for reduction of nutrients. When water scientists talk about the amount of nutrients entering a water body, they call it a load. So these efforts are aimed at reducing nutrient loads into water resources. EPA guidance in the past allowed for narrative or numerical criteria for establishing pollution concentrations below which a water body would be able to achieve its full designated use – such as commercial fishing or swimming. Narrative criteria have been mostly used by state water managers and have been rather useless in achieving improvements. Narrative criteria simply state what condition you want to achieve. Numerical criteria establish what nutrient loads must be imposed for both point sources and non-point sources entering a water body. As you can imagine numerical criteria are much harder to establish than a simple statement of what you’d like to achieve.

 

With the proposed framework and a call by EPA to provide numeric criteria as opposed to narrative criteria for attaining the water quality goals for a water body, I would expect to see some improvements over the last six years. After all as the old adage says, what gets measured gets done. So as a follow-up to this blog post, I will be examining over the next few months whether improvements have been achieved in the two largest hypoxic water systems in the U.S. – the Chesapeake Bay and the Gulf of Mexico.