Nutrient attenuation dynamics in effluent dominated watercourses.

In-stream attenuation of dissolved and particulate forms of carbon, nitrogen and phosphorus are a crucial ecosystem service, especially in watercourses downstream of chemical pollution point-sources (i.e. wastewater treatment plants). Most chemical-fate models assume that attenuation is directly proportional to the concentration of available dissolved organic carbon, and inorganic nitrogen and phosphorus compounds in watercourses, but there are multiple evidences of saturation and even inhibition of attenuation at higher concentrations. Our current comprehension of nutrient attenuation kinetics in streams remains a limiting factor for the development and calibration of predictive models of the chemical fate of these compounds in rivers, thus hindering the development and implementation of more effective regulatory strategies. Here, we assessed the in-stream attenuation of dissolved organic carbon, inorganic nitrogen (NH4+, NO2-, NO3-) and phosphorus (PO43-) compounds at increasing concentrations of these compounds, and analyzed the interaction between attenuation kinetics and biofilm structure and function. Specifically, the net balances of these compounds were assessed in artificial streams exposed to eight treatments following the gradient of WWTP contribution to the river flow (0, 14, 29, 43, 58, 72, 86, and 100% of WWTP effluent water). Results indicate that biological in-stream attenuation by a given biofilm of an effluent dominated watercourse might be saturated if exposed for short periods to high nutrient concentrations such as during combined sewer overflow events, but that communities can adapt if exposed long enough to high concentrations, therefore avoiding or at least minimizing saturation. More attention should be therefore given to the management of effluent-dominated watercourses, as reductions in the temporal variability of the discharged wastewater by WWTP might enhance attenuation and thus reduce water quality issues downstream.

Phosphorus use by planktonic communities in a large regulated Mediterranean river.

The regulation of large rivers to meet human requirements (e.g. hydroelectricity production, flood prevention, recreation activities) alters the longitudinal distribution of plankton communities and may affect their capacity to use nutrients and organic matter. Here we analyzed phosphorus (P) availability and use by phytoplankton and bacterioplankton in 6 upstream and 5 downstream sites from a reservoir system in the Ebro River (N Spain). Alkaline phosphatase activity (APA) was related to nutrient availability and biomass of both phytoplankton and bacterioplankton. During dry periods phytoplankton and bacterioplankton APA was inversely correlated to P availability in the water, but these patterns became less clear during wet periods. The phosphorus-APA patterns were more consistent in the upstream sites and especially during dry periods. Although phytoplankton APA was 6-40 times greater than that of bacterioplankton, APA per unit of biomass suggested that bacterioplankton was more efficient at utilizing dissolved organic phosphorus (DOP) in the upstream section during dry periods. Imbalanced N:P ratios in the particulate (N:P ranging 133-170) and dissolved (N:P ranging 301-819) water fractions confirmed the strong P limitation in these upstream communities. The phosphorus-APA patterns were weaker in the downstream section and during wet periods. The reservoirs caused a change in the downstream dynamics, where bacterioplankton biomass was positively correlated to APA but APA per unit of biomass decreased. Our findings reveal that river regulation drives changes in plankton use of organic phosphorus, especially during extreme dry periods.