The process of eutrophication is driven by the enrichment of water with nutrients, particularly those high in nitrogen and/or phosphorus, which causes an increase in the growth, primary production, and biomass of algae as well as changes in the organismal balance and degradation of water quality. Eutrophication's effects are unfavorable if they significantly reduce ecosystem health, biodiversity, and/or the sustainable production of products and services.
The main inorganic nutrients that cause the
eutrophication of marine waters are nitrogen and phosphorous. Marine waters
naturally include nitrogen and phosphorus, which are transported there from the
land by streams, rivers, and runoff from rainfall as well as by the breakdown
of organic matter already present in the water. The amount of nitrogen and
phosphorus in the oceans has increased due to human nutrient inputs into the
environment.
The
Main Sources of Eutrophication
On land, particularly in agricultural areas,
diffuse sources account for the majority of the nitrogen load. Aquaculture,
wastewater treatment facilities, industrial water, nearby oceans, and nitrogen
emissions (such as ammonium from manure and nitrogen oxides from ships, which
are transmitted via the atmosphere to oceans by precipitation) are some other
sources of nitrogen.
The primary source of phosphate introduced by
humans is found in domestic and industrial wastewater and sewage. Although
phosphate is a component of fertilizers its run-off from land is also a
significant source of phosphate.
Effects
of Eutrophication on Aquatic Ecosystem
The term "eutrophication" is broad
and refers to a significant problem in the nation's estuaries. The process of
eutrophication, which happens when the environment becomes enriched with
nutrients, increases the quantity of plant and algae production in estuaries
and coastal waters, is what causes harmful algal blooms, dead zones, and fish
kills. According to a study, excessive nitrogen imports have moderately to
severely deteriorated 65 per cent of the contiguous U.S.'s estuaries and
coastal waters. A surplus of nutrients causes algal blooms and hypoxic
conditions, which can kill fish and seagrass and diminish vital fish habitats.
Bivalve mollusc populations (such as those of oysters, clams, and scallops) are
also common in many of these estuaries, and they naturally remove nutrients
through filter-feeding.
An excess of algae and plants is the first
sign of eutrophication, which then triggers a chain reaction in the ecosystem.
As the surplus algae and plant stuff finally break down, it releases a lot of
carbon dioxide. This results in ocean acidification, a process where seawater's
pH decreases. The production of shells in bivalve molluscs can be prevented by
acidification, which also retards fish and shellfish growth. This results in
smaller harvests and more expensive seafood for both commercial and
recreational fisheries due to the decreased harvest.
Eutrophication can cause a decrease in the
quantity of sunlight that bottom waters receive, which can affect the
distribution of macroalgae and seagrasses by depth. Oxygen deficit in bottom
waters can be caused by an increase in the decomposition of organic materials
(dead algae). Reduced oxygen levels may therefore affect fish and benthic fauna
(animals that live on the bottom of lakes or oceans), causing them to leave the
area or perish. Moreover, eutrophication has the potential to alter
biodiversity and ecosystem balance.
It also has socio-economic impacts such as the
negative impact on the fish industry, degradation of water quality with foul
smell and toxins from blooms affecting the tourism industry.
In conclusion, eutrophication is recognized as
a toxic and pollution problem and a threat to water quality, marine life,
tourism and economic growth.
About the Author: Muhammad Tahir is a
postgraduate scholar in environmental sciences and deeply passionate about
environmental studies and eager to pursue opportunities to deepen his knowledge
and engagement in this area to make positive changes in this world.
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