Nitrogen Saturation and Carbon Sequestration in a Coniferous Forest Catchment: 32 years of Nitrogen Additions at Gårdsjön, Sweden

被引:0
|
作者
Moldan, F. [1 ]
Jutterstrom, S. [1 ]
Oulehle, F. [2 ,3 ]
Chuman, T. [2 ,3 ]
Hruska, J. [2 ,3 ]
Tahovska, K. [4 ]
Wright, R. F. [5 ]
机构
[1] IVL Swedish Environm Res Inst, Box 53021, S-40014 Gothenburg, Sweden
[2] Czech Geol Survey, Klarov 3, Prague 1, Czech Republic
[3] Czech Acad Sci, Global Change Res Inst, Belidla 986-4a, Brno 60300, Czech Republic
[4] Univ South Bohemia, Fac Sci, Dept Ecosyst Biol, Branisovska 31, Ceske Budejovice 37005, Czech Republic
[5] NIVA Norwegian Inst Water Res, Okernveien 94, N-0579 Oslo, Norway
关键词
Soil; Runoff chemistry; Boreal; Ecosystem experiment; Repeated samplings; Mass budgets; TEMPERATE FOREST; GARDSJON; DEPOSITION; NITREX; ECOSYSTEMS; GROWTH; RUNOFF;
D O I
10.1007/s11270-025-07848-9
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
At G & aring;rdsj & ouml;n, Sweden, a long-term experiment has been conducted in which a 5250-m2 coniferous-forested catchment (G2 NITREX) receiving 8 kg N ha-1 yr-1 ambient N deposition has been given an additional 40 kg N ha-1 yr-1 in 20 small portions yearly. Catchment inputs and outputs of N have been monitored. The soils were systematically sampled in 1990 and 2016. Over 26 years (1991-2016) cumulative inputs were 1290 kg N ha-1 (deposition 230, additions 1030, nitrogen fixation 30). Cumulative outputs were 231 kg N ha-1 (runoff dissolved inorganic N 89, runoff dissolved organic N 55, denitrification 87). The ecosystem retained about 80% (1060 kg N ha-1) of the incoming N in the biomass and soils. About 80% of the retained N was found in the soil, mostly in the mineral horizons. The C/N ratio of the organic soil decreased from 32 to 29. The remaining 20% of the retained N went to plant biomass. The enhanced N deposition has resulted in sequestration of 44 t C ha-1. The C sequestered in the ecosystem had a C/N ratio of 34. The ecosystem has moved towards N saturation; the fraction of N added that is leached to runoff has increased from about 1% in 1991 to nearly 30% in 2022, 32 years later. As the N leaching and denitrification increase, less of the incoming N is available for C sequestration.
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页数:16
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