Sammanfattning

Increased atmospheric deposition of inorganic nitrogen (N) may lead to increased leaching of nitrate (NO(3)(-)) to surface waters. The mechanisms responsible for, and controls on, this leaching are matters of debate. An experimental N addition has been conducted at Gardsjon, Sweden to determine the magnitude and identify the mechanisms of N leaching from forested catchments within the EU funded project NITREX. The ability of INCA-N, a simple process-based model of catchment N dynamics, to simulate catchment-scale inorganic N dynamics in soil and stream water during the course of the experimental addition is evaluated. Simulations were performed for 1990-2002. Experimental N addition began in 1991. INCA-N was able to successfully reproduce stream and soil water dynamics before and during the experiment. While INCA-N did not correctly simulate the lag between the start of N addition and NO 2 3 breakthrough, the model was able to simulate the state change resulting from increased N deposition. Sensitivity analysis showed that model behaviour was controlled primarily by parameters related to hydrology and vegetation dynamics and secondarily by in-soil processes.

Nyckelord

acidification; experimental nitrogen addition; Gardsjon; nitrogen leaching

Publicerad i

Hydrology research
2009, Volym: 40, nummer: 2-3, sidor: 187-197
Utgivare: IWA PUBLISHING

SLU författare

• Futter, Martyn

  • Institutionen för vatten och miljö, Sveriges lantbruksuniversitet
    

UKÄ forskningsämne

Miljövetenskap


Publikationens identifierare

DOI: https://doi.org/10.2166/nh.2009.076

Permanent länk till denna sida (URI)

https://res.slu.se/id/publ/83803