From single fields to river basins: Identification of critical source areas for erosion and phosphorus losses at high resolution.

As shown by the highly significant positive linear regression between loads of SS and different P forms (TP and PP), transport of SS governs transport of PP and, more often than not, transport of TP.

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This type of error may be significant locally and should be considered when the results are evaluated at field scale, in case the diverted flow runs across the field.

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