According to Barbara Juncosa, dead zones are not a new thing; they form seasonally in economically viral ecoystems worldwide, including, but not limited to the Gulf of Mexico and Chesapeake Bay. Agricultural runoff sparks many of these die-offs; increased use of nitrogen fertilizers has doubled the number of lifeless pockets every decade since the 1960s, resulting in 405 dead zones now dotting coastlines globally (1) One area of major concern in the United States is the Mississippi River Basin. Due to the fact that it drains nearly 40% of the entire United States and is in the center of the largest area of cropland in the nation puts it right inline for big ecological problems. The use of monoculture crop raising in this region is particularly dangerous. Soybeans and corn have become the two major crops and dominate the landscape in this area. Fertilizers are the most abundant source of nutrients for crops like soybeans and corn which generally cannot sustain themselves in the same ground two years in a row without the aid of nutrients. "Agricultural inputs of nitrogen and phosphorus are the largest source of nutrients in most affected areas." (Cleaner Production and Environmentally Sound 4) This area of the country is also a large producer of grains grown for domestic livestock feed and that production is fueled with fertilizer as well. In Simon D. Donner's article "Surf and Turf" he cites that the data shows that corn and soybeans are the predominant feed crops in the Mississippi Basin, comprising 94% of the total production. Corn alone receives the majority of the nitrogen (73%), phosphorus (62%), potash (64%) and herbicide (62%) because of the extensive cultivation and typically high application rates (2). This relationship with the earth is having profound impacts that can't be seen from the places that they start. A bit more agricultural runoff in Missouri might be a mere annoyance to a farmer there, but that same runoff could be adding more and more nitrogen into the ocean at the outlet of the Mississippi River, devastating the plants and animals of the delta and further on out into the Gulf of Mexico. As stated by Goolsby, Battaglin, Aulenbach, and Hooper the direct relationship between concentration and streamflow indicates that most of the nitrate in streams studied in their paper is from non-point sources. If the nitrate was predominantly from point sources, concentrations would decrease as streamflow increased due to dilution. Instead nitrate concentrations in streams increase in response to rainfall or snowmelt that leaches nitrate that has accumulated in the soil (5).
Our relationship with nature has changed in the last 50 years in quite a drastic way in the United States. We have moved from a family farm producer society to a city dwelling mega farm production society. This has had many benefits and many costs as well. One of the major costs to the environment from this mega farming production system is the clearing of huge areas of land for raising crops and consequently the massive amount of water runoff that this cleared land produces. Major water runoff is a problem on its own, producing large quantities of topsoil erosion and runoff into waterways that become choked with sediment. More importantly though, this runoff oftentimes carries with it the chemicals and bi-products of our massive scale crop production.
Heller and Keoleian cite that commercially manufactured chemical fertilizers are the major source of plant nutrients in the US. Fertilizer accounted for 6.4% of total farm production expenses in 1997, and was applied to 25% of the total farmland (total farmland includes pastureland, rangeland, etc., which typically receives little to no fertilizer) (3) Fertilizers are used to enhance the viability of soil that has been farmed too extensively, or in soil that is of the wrong composition for specific target crops that a farmer is planting. These fertilizers are used in heavier concentrations in conjunction with the spring and summer growing seasons, which is the time of the largest mass of dead zones.
In the Mississippi River Basin in particular, Turner, Rabalais and Justic cite that the increased production of corn has come at the expense of cotton, the conservation reserve program, and soybean acreage, which is a crop more efficient in retaining nitrogen once applied (2323). Our addiction to cheap corn sweeteners and the rise of use of ethanol based bio-fuels has only spurred more growth in this sector of the agricultural industry.
The process by which high concentrations of nitrogen are turned into a dead zone is a cycle of boom and bust. When the large concentrations of nitrogen enter the warmer estuary waters of a delta or gulf they cause an algae bloom. The life cycle of these algae blooms includes sinking to the bottom of the body of water to decompose with the aid of bacteria. This process consumes oxygen though, and in the massive scale that is required for breaking down these super algae blooms, it is faster than it can be naturally replaced in the water. This process depletes the water of life giving oxygen and creates what we call a dead zone. Booth and Campbell point out that the natural stratification of the Gulf, whereby lighter river water overlies heavier salt water, impedes overturn and oxygen recharge at depth (5410). These dead zones are called hypoxic zones which means low oxygen. When oxygen concentrations in a body of water reach down to 2 parts per million, an area is considered to be hypoxic. To sum up this idea as described by ScienceDaily dead zones are caused by farm fertilizers and other chemicals, and their runoff into rivers creating a large amount of plankton, which in turn depletes oxygen as it sinks down into the water. Without sufficient oxygen, marine life on and close to sediment dies (2),
Effects from hypoxia on fisheries is huge, fish that are able to will leave an area will, but many more get trapped by expanding pockets of hypoxic water and have mass die offs. Some other creatures like shellfish and crustaceans aren't able to move as quickly and can not get out of the hypoxic area in time and have die offs as well. This is pushing fisheries farther off shore and leaving large portions of ocean barren of life.
Solutions to this problem are needed, and fast. With alarming news of global climate change and precipitation, evapo-transpiration and runoff expected to increase globally, and hydrologic extremes such as floods and droughts becoming more common and more intense (Coupling Between Climate 1) we need to decide on a decisive way to approach this issue. While there are no silver bullets that would knock out dead zones completely, industry will have to settle with some terms on fertilizer use eventually and a managed approach to dealing with wastewater. The reintroduction of sustainable farming practices would be a good start for limiting nitrogen release and runoff into waterways. In Russia, harmful algae blooms declined in the 1990s coinciding with a decrease in nutrient loading. This was due to reduced fertilizer usage following the breakup of the former Soviet Union and termination of its agricultural subsidies (Harmful Algal Blooms 4). Conventional wisdom has led us astray in the type of agriculture that we have been practicing. As we become more and more dependant on fertilizers to keep up our production of crops like corn, we are destroying ecosystems that we cant even see. Replanting riparian ecosystems, or even just allowing them to regrow could make a huge impact on this problem by allowing the ground to absorb more of the runoff water that would be drained right away without it. In the subject of wastewater runoff, treatment has begun in some parts of the world to remove the high levels of nitrogen, Olguin, Sanchez and Mercado state that high-rate anaerobic treatment for industrial wastewater was first applied on a large commercial scale in the Mexican sugar industry in the mid 1970s. This has a wide ranging potential in developing countries since most current mainstream technologies for wastewater treatment (e.g., activated sludge) are too costly and time-consuming (5). This brings with it hope that at some point there will be a time when it is recognized that biological treatment of high nitrate wastewater is a cost effective solution to keep larger problems at bay.
In conclusion, ocean dead zones are an ecological nightmare that are slowing destroying our oceans ability to support life in certain areas. Without action, these dead zones will only increase in size and volume.
Works Cited
Anderson, Donald M., et al., "Harmful Algal Blooms And Eutrophication: Examining Linkages From Selected Coastal Regions of the United States", Harmful AlgaeIn Press, 6 September 2008.
ScienceDirect University of Alaska Fairbanks, Fairbanks, AK. 28 Oct. 2008 www.sciencedirect.com
Booth, M.S. and Campbell, C. "Spring Nitrate Flux in the Mississippi River Basin: A Landscape Model with Conservation Applications" Environmental Science Technology, 41, 15, 5410 - 5418, 2007, 10.1021/es070179e
Academic Search Premier.
EBSCO. University of Alaska Fairbanks, Fairbanks, AK. 28 Oct. 2008
http://dx.doi.org/10.1021/es070179e
Justic, Dubravkom, Rabalais, Nancy N. , Turner, R. Eugene "Coupling Between Climate Variability and Coastal Eutrophication: Evidence and Outlook for the Northern Gulf of Mexico", Journal of Sea Research Volume 54, Issue 1, , Contrasting Approaches to Understanding Eutrophication Effects on Phytoplankton, July 2005, Pages 25-35.
ScienceDirect University of Alaska Fairbanks, Fairbanks, AK. 28 Oct. 2008 www.sciencedirect.com
Olguin, Eugenia J., Sanchez, Gloria, Mercado, Gabriel "Cleaner Production and Environmentally Sound Biotechnology for the Prevention of Upstream Nutrient Pollution in the Mexican Coast of The Gulf of Mexico", Ocean & Coastal Management Volume 47, Issues 11-12, , Integrated Coastal Management in the Gulf of Mexico Large Marine Ecosystem, 2004, Pages 641-670.
ScienceDirect University of Alaska Fairbanks, Fairbanks, AK. 28 Oct. 2008 www.sciencedirect.com doi:10.1016/j.ocecoaman.2004.12.006
Goolsby, Donald A., Battaglin, William A., Aulenbach, Brent T., Hooper, Richard P., "Nitrogen Flux and Sources in the Mississippi River Basin", the Science of the Total Environment Volume 248, Issues 2-3, Pages 75-86, 5 April 2000
ScienceDirect University of Alaska Fairbanks, Fairbanks, AK. 28 Oct. 2008 www.sciencedirect.com doi:10.1016/S0048-9697(99)00532-X
Juncosa, Barbara. "Suffocating Seas." Scientific American 299.4 (Oct. 2008): 20-22. Academic Search Premier.
EBSCO. University of Alaska Fairbanks, Fairbanks, AK. 28 Oct. 2008
http://libapps.uaf.edu:2059/ehost/detail?vid=4&hid=13&sid=5f8bbecf-6dcb-4329-ac6a-54ac2bae1066%40SRCSM2&bdata=JnNpdGU9ZWhvc3QtbGl2ZQ%3d%3d#db=aph&AN=34236087
Heller, Martin C., Keoleian, Gregory A. "Assessing the Sustainability of the US Food System: A Life Cycle Perspective", Agricultural Systems Volume 76, Issue 3, , June 2003, Pages 1007-1041.
ScienceDirect University of Alaska Fairbanks, Fairbanks, AK. 28 Oct. 2008 www.sciencedirect.com doi:10.1016/S0308-521X(02)00027-6
Donner, Simon D. "Surf Or Turf: a Shift From Feed to Food Cultivation Could Reduce Nutrient Flux to the Gulf of Mexico," Global Environmental Change Volume 17, Issue 1, Pages 105-113, February 2007,
ScienceDirect University of Alaska Fairbanks, Fairbanks, AK. 28 Oct. 2008 www.sciencedirect.com doi:10.1016/j.gloenvcha.2006.04.005
Texas A&M University. "Into the Dead Zone: Galveston Researcher Examines Loss of Marine Life."
ScienceDaily 7 May 2004. 28 October 2008
http://www.sciencedaily.com/releases/2004/05/040507082408.htm
Turner, R. Eugene, Rabalais, Nancy N., and Justic, Dubravko. "Gulf of Mexico Hypoxia: Alternate States and a Legacy" Environmental Science Technology, 10.1021/es071617k: 42, 7, 2323 - 2327,
http://dx.doi.org/10.1021/es071617k
