Goddard Earth Sciences, NASA. Science Focus: Dead Zones. August 2, 2010. Accessed March 31st, 2011 from http://disc.sci.gsfc.nasa.gov/oceancolor/additional/science-focus/ocean-color/science_focus.shtml/dead_zones.shtml
Yoon, C.K. A "Dead Zone" Grows in the Gulf of Mexico. The New York Times, January 20th 1998. Accessed online March 31st 2011 from http://query.nytimes.com/gst/fullpage.html?res=9B04E1DD1338F933A15752C0A96E958260
Two elements are limiting agents in plant growth: nitrogen and phosphorus. Phosphorus clings to sediments, but nitrogen mostly dissolves in water. This means on land, phosphorus is typically available in soil, as it doesn’t wash away into streams or oceans. Terrestrial plants are typically limited in their growth by the availability of nitrogen, which can easily wash through soils and into water bodies. As a result, farmers often use nitrogen enriched fertilizers to maximize crop growths.
Unfortunately, the ability of nitrogen to dissolve into and be carried away by water has its downsides. As nitrogen enters the ocean, it fertilizes plants. Algae thrive when they come in contact with nitrogen enriched water, and massive blooms appear. Great, right? Algae use up carbon dioxide, produce oxygen, and act as the base of almost every food web in the ocean, so how is this a bad thing? Well, the algae eventually die, and when they do, they sink to the bottom of the ocean where they are consumed by bacteria through a process called “bacterial respiration”. In bacterial respiration, the bacteria consume oxygen and produce carbon dioxide in the process of decomposing the dead algae.
Being deep in the ocean, far below air and a ready supply of oxygen, it becomes very difficult to replace the oxygen consumed in decomposing bacteria. Such massive algal blooms caused by fertilizer runoff results in so many dead algae sinking to the bottom, that bacteria pull almost or even all the oxygen from the water. Through the process of bacterial respiration, the bacteria create a “dead zone” in which life for oxygen-breathing organisms is impossible to maintain (Goddard Earth Sciences).
Theses dead zones are appearing all over the world. One of the largest dead zones occurs in the Gulf of Mexico. The Mississippi River is formed by headwaters from Canada all through the United States until it empties into the Gulf of Mexico. The Mississippi happens to pass through thousands of acres of prime agricultural land; a considerable amount with nitrogen enriched soil. The resulting runoff from agricultural emptying into the Mississippi and eventually the Gulf of Mexico, has created a dead zone approximately 7,000 square miles (New York Times). Unfortunately, this phenomenon has struck close to home. Saanich, just outside of Victoria, BC, has recorded a dead zone. In the Saanich Inlet, at depths below 100 m, the water becomes anoxic as a result of nitrogen runoff from farmlands on Vancouver Island (Goddard Earth Sciences).
How can we stop this? Many scientists are attempting to fuse nitrogen-fixing bacteria with plants. Their success would make it possible for the plant to pull nitrogen out of the atmosphere rather than have to rely on nitrogen-fixing soil bacteria or fertilizers. Legumes are among the few plants which can do this. Unfortunately, until the scientists can manage this, the only feasible option is to ban nitrogen fertilizers; a choice which would certainly be shot down by governments worldwide.
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