HR: 1340h
AN: H23D-1448    [Abstracts]
TI: Influence of Hydrological Flow Paths on Rates and Forms of Nitrogen Losses from Mediterranean Watersheds
AU: * Lohse, K A
EM: klohse@asu.edu
AF: Arizona State University, International Institute for Sustainability, Box 873211, Tempe, AZ 85287-3211 United States
AU: Sanderman, J
EM: jsandman@nature.berkeley.edu
AF: University of California, Berkeley, Department of Environmental Science, Policy and Management 137 Mulford Hall, Berkeley, CA 94720 United States
AU: Amundson, R G
EM: earthy@nature.berkeley.edu
AF: University of California, Berkeley, Department of Environmental Science, Policy and Management 137 Mulford Hall, Berkeley, CA 94720 United States
AB: Patterns of precipitation and runoff in California are changing and likely to influence the structure and functioning of watersheds. Studies have demonstrated that hydrologic flushing during seasonal transitions in Mediterranean ecosystems can exert a strong control on nitrogen (N) export, yet few studies have examined the influence of different hydrological flow paths on rates and forms of nitrogen (N) losses. Here we illuminate the influence of variations in precipitation and hydrological pathways on the rate and form of N export along a toposequence of a well-characterized Mediterranean catchment in northern California. As a part of a larger study examining particulate and dissolved carbon loss, we analyzed seasonal patterns of dissolved organic nitrogen (DON), nitrate and ammonium concentrations in rainfall, throughfall, matrix and preferential flow, and stream samples over the course of one water year. We also analyzed seasonal soil N dynamics along this toposequence. During the transition to the winter rain season, but prior to any soil water displacement to the stream, DON and nitrate moved through near-surface soils as preferential flow. Once hillslope soils became saturated, saturated subsurface flow flushed nitrate from the hollow resulting in high stream nitrate/DON concentrations. Between storms, stream nitrate/DON concentrations were lower and appeared to reflect deep subsurface water flow chemistry. During the transition to the wet season, rates of soil nitrate production were high in the hollow relative to the hillslope soils. In the spring, these rates systematically declined as soil moisture decreased. Results from our study suggest seasonal fluctuations in soil moisture control soil N cycling and seasonal changes in the hydrological connection between hillslope soils and streams control the seasonal production and export of hydrologic N.
DE: 0469 Nitrogen cycling
DE: 0486 Soils/pedology (1865)
DE: 1804 Catchment
DE: 1871 Surface water quality
DE: 1875 Vadose zone
SC: Hydrology [H]
MN: Fall Meeting 2005