Terrestrial
eutrophication means a state of increased nutrient availability in soil as a result of input of plant nutrients.
The most common use of the term
eutrophication is related to inputs of mineral nutrients, primarily nitrogen and phosphorus, to coastal waters.
Water managers aiming to control
eutrophication in Latn America lakes are advised to use the OECD predictive equations with utmost caution.
Eutrophication may be defined as the sum of the effects of the excessive
The increase in nutrients in lakes ultimately cause the
eutrophication is anthropogenic, and a result of increasing population (for instance, more agricultural and urban waste runoff).
They found that the European Union (EU) drives the largest global non-food
eutrophication displacements, to the Asia-Pacific region for marine
eutrophication and to Africa for freshwater
eutrophication.
The forestry department said that, in cooperation with the WDD, they will carry out further analyses to examine the effects of
eutrophication on the quality of the lake water.
These increased anthropogenic activities have increased the N deposition rate and aggravated
eutrophication [26-39].
However, quantitative analyses of the effects of high crop yield and high nutrient use efficiency on coastal
eutrophication are lacking.
Changes in coastal diatom species assemblages from sediment sequences have been successfully used to study, e.g., the
eutrophication and changes in turbidity, salinity and freshwater input, and the possible reasons for the observed palaeoenvironmental changes (Battarbee 1986; Cooper et al.