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Evidence of plant biodiversity changes as a result of nitrogen deposition in permanent pine forest plots in central Russia

机译:由于俄罗斯中部的永久性松树林地块中的氮沉积导致植物生物多样性的证据

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This study examines the influence of the increased atmospheric nitrogen (N) deposition observed in central Russia between 1960 and 2010 (with a peak in 1990) on biodiversity and the availability of N in soil in pine forests. Shifts in N availability in soils of 3 pine plots were analyzed using presence/absence chronosequence records of the dynamics of ground vegetation plants and a set of specialist plant species with a narrow range of tolerance as bioindicators of soil richness. We assumed that changes in plant communities might be caused by increased atmospheric N input. To examine this assumption, (i) the species composition of forest ground vegetation was analyzed using the Ellenberg N scale and the Tsyganov N scale, which was developed for forest vegetation in European Russia, and (ii) the dynamics of the main N pools were examined using simulation models of forest growth and elements cycling in the forest-soil system. Our results confirm that changes in the ground vegetation communities experiencing eutrophication occurred in all plots. The number of indicators of N-rich conditions for these plots reached a maximum in 1990, the year N deposition reached its maximum in this area. The decline in the number of oligotrophic species indicated that N-poor soils decreased over the monitoring period. Model simulations showed an increase in labile N compounds in the soil and in the total N pool in forest ecosystems. Our results demonstrate an acceleration of natural succession due to atmospheric nitrogen deposition in this region.
机译:本研究探讨了1960年至2010年期间在俄罗斯中部观察到的大气氮(N)沉积增加的影响(1990年的高峰)对松林中土壤中N的生物多样性以及N的可用性。使用地面植被植物动态的存在/缺席的计量记录和一系列专科植物物种的存在/缺席计量记录分析了3个松树的土壤中的偏移,以及土壤丰富性的生物inderation的宽度较窄。我们假设植物群落的变化可能是由增加的大气N输入引起的。为了检查这个假设,(i)使用Ellenberg N规模分析森林地面植被的物种组成,并为欧洲俄罗斯的森林植被而开发,(ii)主要N池的动态用森林生长与森林 - 土壤系统循环的仿真模型研究。我们的结果证实,在所有地块中发生了体验富营养化的地面植被社区的变化。这些地块的N-Rich条件的指标数量在1990年达到了最大值,这一年份沉积在该地区最大值达到其最大值。寡营养物种数量的下降表明,在监测期内,N差的土壤下降。模型模拟显示土壤中不稳定的氮素化合物的增加,并在森林生态系统中的N总库中增加。我们的结果表明,由于该地区的大气氮沉积,自然继承的加速。

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