PS 14-134
Hydrologic and chemical connectivity in urban accidental wetlands: Implications for nitrate removal

Monday, August 10, 2015
Exhibit Hall, Baltimore Convention Center
Amalia M. Handler, School of Life Sciences, Arizona State University, Tempe, AZ,
Amanda K. Suchy, School of Life Sciences, Arizona State University, Tempe, AZ,
Nancy B. Grimm, School of Life Sciences, Arizona State University, Tempe, AZ, USA
Monica M. Palta, School of Earth and Space Exploration, Arizona State University, Tempe, AZ, USA
Daniel L. Childers, School of Sustainability, Arizona State University, Tempe, AZ, USA
Juliet C. Stromberg, School of Life Sciences, Arizona State University, Tempe, AZ, USA
Background/Question/Methods

Accidental wetlands have emerged in the urban Salt River channel of Phoenix, Arizona. Stormwater pipes collect urban runoff that drains directly into the dry river channel, providing a new perennial water source that sustains wetlands. These systems were not planned nor are they actively managed by any group, hence the ‘accidental’ designation. Water delivered by storm drains is enriched in nitrogen, particularly nitrate (NO3), a common surface-water pollutant. We investigated the chemical and hydrological connectivity between surface water and subsurface porewater to evaluate potential for nitrogen attenuation by microbial NO3 transformation. Microbially mediated NO3 reduction requires low oxygen and high organic carbon availability, conditions common in wetland soils. For microbial NO3 reduction to occur in the Salt River wetlands, the NO3-enriched surface water must be connected to the subsurface soils and sediments. Surface–subsurface connectivity also may be expected to vary with surface vegetation cover and type. To evaluate hydrochemical connectivity, we measured surface water and subsurface porewater electrical conductivity and chloride (Cl) concentration as inert tracers. We measured dissolved oxygen and NO3 concentrations across three wetland vegetation cover types to test for spatially explicit differences in potential for NO3 reduction between the surface and subsurface zones.

Results/Conclusions

Results suggest that wetland surface water and subsurface porewater exchange dissolved constituents. Electrical conductivity and Cl concentrations were indistinguishable both vertically across surface and subsurface water samples as well as horizontally across vegetation cover types, indicating high chemical connectivity between zones. Dissolved oxygen concentration was significantly lower in the subsurface at 1.7 ± 0.69 mg L-1 (mean ± SD) compared to the surface water at 4.4 ± 2.6 mg L-1, indicating high potential for NO3 reduction under subsurface conditions. Nitrate concentration was an order of magnitude higher in the surface water than in the subsurface porewater, but there were no concentration differences between the wetland vegetation patch types. Given the chemical connectivity indicated by electrical conductivity and Cl concentration, the difference in NO3 between the surface and subsurface hint that the wetland soils act as a sink for NO3 delivered from stormwater drains. Thus these unplanned, unmanaged urban wetland systems may have high capacity to attenuate nitrogen delivered from the urban landscape.