Effect of nitrogen input on carbon accumulation of boreal forest soils and ground vegetation

被引:54
作者
Makipaa, R
机构
[1] Finnish Forest Research Institute, FIN-01301 Vantaa
关键词
nitrogen; carbon sink; understorey vegetation; mosses;
D O I
10.1016/0378-1127(95)03601-6
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
The effects of nitrogen deposition on the carbon balance of forest soils and ground vegetation were estimated in long-term fertilization experiments. The experiments were established during 1958-1962. They were situated on 36- to 63-year-old Scots pine (Pinus sylvestris L.) and Norway spruce (Picea abies Karst.) stands of different levels of fertility. The experiments received nitrogen fertilization five to seven times over a 30-year period, and the total input of nitrogen was 596-926 kg ha(-1). Nitrogen input increased the amount of carbon in the humus layer and mineral soil. With one exception, the carbon storage of the humus layer was increased by 14-87%, and carbon storage of the mineral soil by 15-167%. The humus layer was thicker on the fertilized plots due to accumulation of organic matter during the study period. In the changing environment, nitrogen deposition reinforces the accumulation of organic matter in forest soils, and may enhance carbon accumulation in boreal forests. On the other hand, both the biomass and the amount of carbon in the ground vegetation were decreased by the addition of nitrogen. The ground vegetation under a closed canopy does not have the potential to respond positively to addition of nitrogen, because the vegetation is dominated by slow-growing mosses and dwarf shrubs. Thus, the ground vegetation of the boreal forests is not a sink for carbon in the changing environment.
引用
收藏
页码:217 / 226
页数:10
相关论文
共 52 条
[1]   NITROGEN SATURATION OF TERRESTRIAL ECOSYSTEMS [J].
AGREN, GI ;
BOSATTA, E .
ENVIRONMENTAL POLLUTION, 1988, 54 (3-4) :185-197
[2]   SUCCESSIONAL STATUS, SEED SIZE, AND RESPONSES OF TREE SEEDLINGS TO CO2, LIGHT, AND NUTRIENTS [J].
BAZZAZ, FA ;
MIAO, SL .
ECOLOGY, 1993, 74 (01) :104-112
[3]   THE SENSITIVITY OF SOME HIGH-LATITUDE BOREAL FORESTS TO CLIMATIC PARAMETERS [J].
BONAN, GB ;
SHUGART, HH ;
URBAN, DL .
CLIMATIC CHANGE, 1990, 16 (01) :9-29
[4]  
CAJANDER A. K., 1949, ACTA FOREST FENNICA, V56, P1
[5]   POSSIBLE EFFECTS OF RISING CO2 ON CLIMATE [J].
CRANE, AJ .
PLANT CELL AND ENVIRONMENT, 1985, 8 (06) :371-379
[6]  
ELLENBERG H, 1988, CRITICAL LOADS SULPH, P375
[7]   CLIMATIC-CHANGE AND THE BROAD-SCALE DISTRIBUTION OF TERRESTRIAL ECOSYSTEM COMPLEXES [J].
EMANUEL, WR ;
SHUGART, HH ;
STEVENSON, MP .
CLIMATIC CHANGE, 1985, 7 (01) :29-43
[8]  
FORTELIUS C, 1994, FINNISH RES PROGRAMM, P45
[9]   CARBON BALANCE IN TUSSOCK TUNDRA UNDER AMBIENT AND ELEVATED ATMOSPHERIC CO2 [J].
GRULKE, NE ;
RIECHERS, GH ;
OECHEL, WC ;
HJELM, U ;
JAEGER, C .
OECOLOGIA, 1990, 83 (04) :485-494
[10]   NITROGEN DEPOSITION AND THE FOREST NITROGEN-CYCLE - ROLE OF DENITRIFICATION [J].
GUNDERSEN, P .
FOREST ECOLOGY AND MANAGEMENT, 1991, 44 (01) :15-28