HR: 09:10h
AN: H21F-05 [Abstracts]
TI: The Influence of Watershed Properties on the Large-Scale Transport of Nitrogen
AU: * Alexander, R B
EM: ralex@usgs.gov
AF: U.S. Geological Survey, 12201 Sunrise Valley Drive
413 National Center, Reston, VA 20192
United States
AU: Smith, R A
EM: rsmith1@usgs.gov
AF: U.S. Geological Survey, 12201 Sunrise Valley Drive
413 National Center, Reston, VA 20192
United States
AU: Schwarz, G E
EM: gschwarz@usgs.gov
AF: U.S. Geological Survey, 12201 Sunrise Valley Drive
413 National Center, Reston, VA 20192
United States
AU: Boyer, E W
EM: boyer@nature.Berkeley.EDU
AF: University of California
Dept. of Environmental Science, Policy, and Management, 137 Mulford Hall #3114, Berkeley, CA 94720
United States
AU: Scott, D T
EM: dscott4@unlnotes.unl.edu
AF: University of Nebraska
Dept. of Geosciences, 214 Bessey Hall, Lincoln, NE 68588
United States
AU: Harvey, J W
EM: jwharvey@usgs.gov
AF: U.S. Geological Survey, 12201 Sunrise Valley Drive
430 National Center, Reston, VA 20192
United States
AB:
Considerable advances have been made in understanding the hydrological and biogeochemical processes that control nitrogen
cycling and transport in soils, ground waters, and the riparian and hyporheic areas of streams. This includes expanded
knowledge of the dynamic coupling of these processes and their influence on flow paths and residence times of nitrogen
through landscapes. Much of the progress reflects improved understanding at small spatial scales. Less progress has been
made in 'scaling-up' these processes to assess their large-scale effects on the downstream
transport of nitrogen. Modeling techniques are viewed as essential scaling tools, but questions have emerged about how
accurately complex mechanistic models describe the large-scale effects of processes on nitrogen cycling and transport. One
area of increased modeling research emphasizes the use of less complex model structures to identify the principle controls at
catchment and watershed scales. Here, we illustrate the use of spatially referenced, statistical models to identify major
terrestrial and aquatic properties that influence nitrogen transport across a range of stream and watershed sizes. We use
the Spatially Referenced Regression on Watershed Attributes (SPARROW) model of mean-annual total nitrogen loads, applied to
major streams of the conterminous United States. The SPARROW model relates in-stream measurements of total nitrogen loads to
geographic data on nitrogen sources and properties of the landscape that influence transport. The model employs mechanistic
components and mass balance constraints within a formal parameter-estimation structure to empirically quantify the sources,
attenuation rates, and transport of nitrogen through terrestrial and aquatic ecosystems. We identified the influence of
topography, soils, climate, reservoirs, and in-stream and riparian properties on the long-term and long-distance transport of
nitrogen. Nitrogen transport is best described by nonlinear interactions with these properties; the interactions only
partially scale with catchment size. Progress in evaluating and scaling-up these relations is currently limited to watershed
properties with well defined spatial attributes. We discuss the types of experimental and spatial data needed to further
advance the use of models to describe nitrogen transport across broad temporal and spatial scales.
DE: 0469 Nitrogen cycling
DE: 0470 Nutrients and nutrient cycling (4845, 4850)
DE: 1847 Modeling
DE: 1871 Surface water quality
SC: Hydrology [H]
MN: Fall Meeting 2005