Effects of Ammonium-rich Wastewater Effluent on Phytoplankton Productivity in Experimental Mesocosms from the northern San Francisco Estuary
Abstract:
Mesocosm (10 L enclosure) experiments were conducted in conjunction with the USGS California Water Science Center study (Nitrogen Dynamics along the Sacramento River and Links to Phytoplankton Dynamics), a large scale field manipulation in which WWTF discharge was halted for extended periods (~15 hours) in October 2013 and May of 2014. Whole water mesocosm experiments included comparisons of various nitrogen sources (effluent-NH4, NH4Cl and NO3), and were incubated in ambient light conditions and water temperatures. Development of phytoplankton communities was monitored by measuring Chl-a biomass, nutrient draw-down, function group identification and isotope N-uptake rates.
The reduction of NH4-rich effluent in situ did not alter total phytoplankton biomass, however uptake of NO3 was able to occur when NH4-effluent was reduced. Enclosures from upstream of effluent discharge (low DIN) were nitrogen limited and accumulated very little Chl-a over the study period, while amending with nitrogen (NH4Cl, NO3, NH4-effluent) resulted in high Chl-a, and similar N-uptake and nutrient drawdown. Enclosures did not show differences between growth on effluent-based NH4 and NH4Cl solution at ~40µM NH4, however river data revealed a depression in N-uptake rates at high NH4-effluent concentrations. Elevated NH4 itself has been shown to impact phytoplankton communities, but we must also consider the potential toxicity of other constituents when studying systems with wastewater-based nitrogen pollution.