首页> 外文期刊>Ecosystems >Impacts of Soil Nitrogen and Carbon Additions on Forest Understory Communities with a Long Nitrogen Deposition History
【24h】

Impacts of Soil Nitrogen and Carbon Additions on Forest Understory Communities with a Long Nitrogen Deposition History

机译:氮素沉积历史悠久的土壤氮和碳的添加对林下群落的影响

获取原文
获取原文并翻译 | 示例
           

摘要

Rates of nitrogen (N) deposition have been historically high throughout much of the northeastern United States; thus, understanding the legacy of these high N loads is important for maintaining forest productivity and resilience. Though many studies have documented plant invasions due to N deposition and associated impacts on ecosystems, less is known about whether invasive plants will continue to increase in dominance with further shifting nutrient regimes. Using soil N and carbon additions, we examined the impact of both increasing and decreasing soil N on native and invasive understory plant dynamics over 4 years in a northeastern deciduous forest with a long history of N deposition. Despite applying large quantities of N, we found no difference in soil nitrate (NO3) or ammonium (NH4+) pools in N addition plots over the course of the study. Indicative of the potential N saturation in these forest soils, resin-available NO3- and NH4+ showed evidence that the added N was rapidly moving out of the soil in N addition plots. Accordingly, we also found that adding N to soil altered neither invasive nor native plant abundance, though adding N temporally increased invasive plant richness. Carbon additions decreased soil N availability seasonally, but did not alter the total percent cover of invasive or native plants. Rather than being suppressed by excess N availability, native plant species in this ecosystem are primarily inhibited by the invasive species, which now dominate this site. In conclusion, understory plant communities in this potentially N-saturated ecosystem may be buffered to future alterations in N availability.
机译:从历史上看,美国东北大部分地区的氮(N)沉积速率一直很高。因此,了解这些高氮负荷的遗产对于维持森林生产力和韧性至关重要。尽管许多研究已经记录了由于氮的沉积以及对生态系统的相关影响而造成的植物入侵,但对于入侵植物是否会随着养分制度的进一步变化而占据主导地位的情况知之甚少。使用土壤氮和碳的添加量,我们研究了氮素沉积历史悠久的东北落叶林中4年内土壤氮素的增加和减少对原生和侵入性林下植物动态的影响。尽管施用了大量的氮,但在研究过程中,我们发现在氮添加区的土壤硝酸盐(NO3)或铵(NH4 +)库中没有差异。这些森林土壤中潜在的N饱和表明,树脂可利用的NO3-和NH4 +表明,在N增加区中,添加的N迅速从土壤中移出。因此,我们还发现,向土壤中添加N不会改变入侵植物和天然植物的丰度,尽管添加N会暂时增加入侵植物的丰富度。碳的添加会季节性降低土壤氮的利用率,但不会改变入侵植物或本地植物的总覆盖率。该生态系统中的本地植物物种并未受到过量氮素供应的抑制,而主要受到了入侵物种的抑制,而入侵物种现已成为该地区的主导。总之,在这个潜在的N饱和生态系统中,地下植物群落可能会被缓冲,以防N可用性的未来变化。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号