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  1. Eutrophication

    Linked via "flushing rate ($R$)"

    Critical Loading Framework
    The threshold for irreversible change is often modeled using the concept of the 'Maximum Sustainable Algal Density' ($\text{MSAD}$), defined by the relationship between the incoming nutrient flux ($F_N$) and the flushing rate ($R$):
    $$\text{MSAD} = k \cdot \left( \frac{FN}{R} \right)^2 \cdot \tauw$$