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Life Science Dictionary

Eutrophication

Ecology · Marine Biology

Say it: yoo-troh-fih-KAY-shun

Eutrophication is the over-enrichment of a lake, river or coastal sea with nutrients, fueling algal blooms that later decay and use up the water's oxygen.

Definition

What is eutrophication?

Eutrophication happens when a body of water receives more nutrients, chiefly nitrogen and phosphorus, than its ecosystem can absorb. It can occur slowly in nature as lakes age, but most cases today are caused by people. Fertilizer washed off farmland, sewage, animal manure and some detergents, along with nitrogen oxides from burning fuels, all end up in rivers, lakes and estuaries.

The extra nutrients act as fertilizer for algae and cyanobacteria, which multiply into dense blooms that turn the water green or brown and shade out seagrasses and other rooted plants. When the bloom dies, bacteria decompose the dead cells and use up dissolved oxygen as they do so. The water becomes hypoxic, meaning very low in oxygen, and fish, crabs and shellfish that cannot move away suffocate. Large areas left in this state are called dead zones. Some blooms also release toxins that harm wildlife and people, and the carbon dioxide given off by decay makes coastal water more acidic.

One of the largest dead zones forms each summer in the Gulf of Mexico, fed by fertilizer carried down the Mississippi River. Cutting runoff, improving sewage treatment and restoring wetlands and filter-feeding oyster beds are the main ways to reverse it.

Word parts

Where does the word “eutrophication” come from?

eu-
well, goodGreek eu
troph-
nourishmentGreek trephein, to nourish

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