I recently did a nutrient-drip (NH4 and PO4) experiment in a high-altitude stream in the Andes.  The stream had quite low background N, and quite high P (probably an N-limited system).  We did the drip for 24 hours during which time turbidity fluctuated along with discharge.  Any thoughts on why the mass-transfer coefficient (Vf) for NH4 would increase with increasing turbidity?

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