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The nutrient retention function of different ecosystems varied significantly.
The nutrient retention function decreased as slope increased.
Specifically, nutrient retention function varied with altitude and slope.
Based on the landscape source-sink theory, this study assessed the nutrient retention function of ecosystems.
The water retention function was expressed by calculating the hydric significance (HS) indicator.
As expected from their pollutant retention function, highway ponds differed in abiotic conditions from surrounding ponds.
The presented approach represents a valid alternative to the shear retention function.
However, few studies exploring the effect of terrestrial ecosystem nutrient retention function on water quality have been conducted to date.
The semi-empirical equation of the soil water retention function had the lowest values of RMSE and RSE and was qualified as "optimal" for the formal description of the shape of the water retention function.
The results showed a significant influence of land-use on retention function; however, this impact could be limited by extreme precipitation or high soil water saturation.
The water retention function is defined as the ability of the landscape to retain water, slow runoff and encourage water infiltration.
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