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River systems are impacted by nutrient inputs from the landscape.
These nutrient inputs are comparable to or even higher than those supplied by local rivers.
All the above systems are open atmospherically, and often have some water and nutrient inputs.
In this catchment, nutrient inputs from agricultural land represent the main instream eutrophication sources.
The significance of nutrient inputs at the watershed scale is best expressed in terms of in-stream processes, compared to evaluating simple field measurements of nutrient inputs.
This acceleration of nutrient inputs to surface waters is termed cultural eutrophication.
The "high intensity (HI)" cultural treatment included even greater nutrient inputs and complete sustained competition control.
Wetlands with fewer nutrient inputs or in cold climates have lower primary productivity.
The "low intensity (LI)" cultural treatment included relatively high nutrient inputs and early competition control.
The forcing variables are discharge, river morphology, water temperature, available light and nutrient inputs.
The causes of hypoxia are associated with excess nutrient inputs from both point and non-point sources.
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