Eutrophication describes the enrichment of an ecosystem with chemical nutrients (nitrates, phosphates, etc.)
The nutrients can be introduced into waterways via leaching from soil by rainfall or released as part of sewage
Eutrophication is common around agricultural lands where the use of artificial fertilisers are prevalent
An increase in nutrient supply within aquatic and marine ecosystems will result in several ecological consequences:
A rapid growth in algal populations will occur (algal blooms) as a result of the increased availability of nutrients
As the algae die, there will be a subsequent spike in the numbers of saprotrophic microbes (decomposers)
The high rate of decomposition will result in an increased biochemical oxygen demand (BOD) by saprotrophic bacteria
The saprotrophs will consume available quantities of dissolved oxygen, leading to deoxygenation of the water supply
Eutrophication will also increase the turbidity of the water, which will reduce oxygen production by photosynthetic seaweeds
This will stress the survival of marine organisms, potentially leading to a reduction in biodiversity within the ecosystem
Eutrophication