PS 1-17 - An Isotopic view of water and nitrogen transport through the vadose zone in Oregon's southern Willamette Valley’s Groundwater Management Area

Monday, August 7, 2017
Exhibit Hall, Oregon Convention Center
J. Renée Brooks, Western Ecology Division, NHEERL, US EPA, Corvallis, OR, Susanna L. Pearlstein, Matanuska Experiment Farm, University of Alaska Fairbanks, Palmer, AK, Stephen R. Hutchins, Ground Water and Ecosystems Restoration Division, USEPA National Risk Management Research Laboratory, Ada, OK, William Rugh, Western Ecology Division, US EPA, Corvallis, OR, Kenneth Willard, Student Services Contract, Oak Ridge Associate Universities, Corvallis, OR, Barton R. Faulkner, Office of Research and Development, United States Environmental Protection Agency, Ada, OK, Robert A. Coulombe, CSS, Covallis, OR and Jana E. Compton, US EPA, NHEERL, Western Ecology Division, Corvallis, OR

Groundwater nitrate contamination affects thousands of households in Oregon's southern Willamette Valley and many more across the Pacific Northwest. The southern Willamette Valley Groundwater Management Area (SWV GWMA) was established in 2004 due to nitrate levels in the groundwater exceeding the human health standard of 10 mg nitrate-N L-1. Much of the nitrogen inputs to the GWMA comes from agricultural nitrogen use, and thus efforts to reduce N inputs to groundwater are focused upon improving N management. However, the effectiveness of these improvements on groundwater quality is unclear because of the complexity of nutrient transport through the vadose zone and long groundwater residence times. Our objective was to focus on vadose zone transport and understand the dynamics and timing of N and water movement below the rooting zone in relation to N management and water inputs. Stable isotopes are a powerful tool for tracking water movement, and understanding nitrogen transformations within the vadose zone. In partnership with local farmers, and state agencies, we established lysimeters and groundwater wells in multiple agricultural fields in the GWMA, and have monitored nitrate, nitrate isotopes, and water isotopes weekly for multiple years


Our results indicate that vadose zone transport is highly complex, and the residence time of water collected in lysimeters was much longer than expected. While input precipitation water isotopes were highly variable over time, lysimeter water isotopes were surprisingly consistent, more closely resembling long-term precipitation isotope means rather than recent precipitation isotopic signatures. However, some particularly large precipitation events with unique isotopic signatures revealed high spatial variability in transport, with some lysimeters showing greater proportions of recent precipitation inputs than others. In one installation where we have lysimeters at multiple depths and groundwater wells, nitrate/nitrite concentrations decrease with depth, and within a depth, lower N concentrations are associated with higher δ15N values, indicating some denitrification is associated with the variation in concentration. However, these relationships show spatial and temporal complexity not explained by simple denitrification processes. We are exploring how these vadose zone complexities can be incorporated into practical understand of N management on groundwater inputs.