Use of a gradient of N-deposition to calculate effect-related soil and vegetation measures in deciduous forests

被引:36
作者
Falkengren-Grerup, U
Diekmann, M
机构
[1] Lund Univ, Dept Ecol Plant Ecol, SE-26362 Lund, Sweden
[2] Univ Bremen, FB 2, Dept Ecol & Evolutionary Biol, DE-28359 Bremen, Germany
关键词
N deposition; N mineralisation; nitrification; life history traits; critical loads;
D O I
10.1016/S0378-1127(02)00605-9
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
Deposition of N and S has increased since the 1950s in most European countries and N accumulates in ecosystems that are not N saturated. This study shows long-term effects of a (modelled) N deposition of 7-17 kg N ha(-1) per year on biological and chemical processes in soil, vegetation composition, and functional types of field-layer plant species in deciduous forests. Soil pH largely determined the response of the soil processes, emphasising the importance to compare soils of similar acidity regarding the effects of N deposition. The most pronounced effects were demonstrated for the most acid study plots. When we compared regions with a deposition of 7 and 17 kg N ha(-1) per year we found a 40-80% higher soil N mineralisation rate, 2-90% higher nitrification rate and 10-25% lower C:N ratio in the region with the highest deposition. Similar but smaller differences were indicated when regions with a deposition of 7 and 10 kg N ha(-1) per year were compared. Number of species was lower in the regions with the highest deposition. Literature data for plants on N concentration, nitrate reductase activity (NRA), growth rates, morphology and height were calculated on a site basis. They varied to different extent between the regions. The N concentration was 7-24% higher in the regions with the highest N deposition. We argue that the effect-related critical load based on our results should be set to a N deposition of 7-10 kg N ha(-1) per year. Critical loads for a subdivision of deciduous forests would give lower critical loads for the most acid soils compared to less acid soil. (C) 2002 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:113 / 124
页数:12
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