首页> 外文期刊>Forest Ecology and Management >Soil C:N:P dynamics during secondary succession following fire in the boreal forest of central Canada
【24h】

Soil C:N:P dynamics during secondary succession following fire in the boreal forest of central Canada

机译:加拿大中部北方森林火灾后次生演替过程中的土壤C:N:P动态

获取原文
获取原文并翻译 | 示例

摘要

Measures of soil nutrient availability such as concentrations of nitrogen and phosphorus ([N] and [P]) are important indicators of terrestrial productivity. Optimal plant growth and ecosystem functioning are also strongly correlated with nutrient ratios in soils. Long-term trends in soil [C], [N], [P], and their stoichiometric ratios during secondary succession in the fire-driven boreal forest remain unclear. We used replicated 7- to 209-year chronosequences to examine the influence of stand age and overstory composition on [C], [N], and [P] and their ratios in the forest floor, surface (0-15 cm), and subsurface (15-30 cm) mineral soil in the boreal forest of central Canada. In the forest floor, [C] and [N] increased rapidly during the first three decades following fire, after which they fluctuated, but remained larger than in the youngest stands. Surface soil [C] and [N] increased from young to intermediate-aged stands, but decreased in the oldest stands. Subsurface [C] and [N] followed a similar trend, but was higher in the 7-year-old stands. Forest floor [P] followed a gradual, linear increase throughout stand development but of smaller magnitude than [C] and [N]. The temporal pattern of [P] in both mineral soil layers was lower in the 33-year-old stands of all overstory types, suggesting that P resources may be outpaced by their demand during this highly competitive stage of advanced stem exclusion during forest succession. In the forest floor and surface soil, C:N differed not only with stand age but also with overstory type, due to higher C:N in intermediate-aged conifer stands. Forest floor C:P and N:P were higher in the 33- to 146-year-old stands in all overstory types and soil layers, but particularly so in the conifer stands. In the mineral layers, C:N, C: P, and N:P all followed a similar trend. Our results demonstrate the important influence of stand age, overstory composition (as influenced by succession), and soil depth on forest soil nutrient dynamics in boreal forest ecosystems. (C) 2016 Elsevier B.V. All rights reserved.
机译:土壤养分有效性的量度,例如氮和磷的浓度([N]和[P])是陆地生产力的重要指标。最佳的植物生长和生态系统功能也与土壤中的养分比密切相关。在火驱动的北方森林中,次生演替过程中土壤[C],[N],[P]的长期趋势及其化学计量比仍不清楚。我们使用重复的7到209年的时间序列,研究了林分年龄和林分组成对[C],[N]和[P]的影响,以及它们在森林地面,地表(0-15厘米)和加拿大中部北方森林中的地下(15-30厘米)矿质土壤。在森林地面,[C]和[N]在大火后的前三十年迅速增加,此后波动,但仍比最小的林分更大。表层土壤[C]和[N]从年轻到中年林分增加,但在最老林分中减少。地下[C]和[N]遵循相似的趋势,但在7岁的林分中较高。林分[P]在整个林分发育过程中呈逐渐线性增长,但幅度小于[C]和[N]。在所有具有故事情节类型的33岁的林分中,两个矿质土壤层中[P]的时空模式都较低,这表明在森林演替过程中,这种高级竞争性的高级茎排阻阶段中,P资源的需求可能会超过其需求。在森林地表和表层土壤中,C:N不仅因林分年龄而异,而且随着林木类型的变化而不同,这是由于中年针叶林林分的C:N较高。在33至146年的林分中,所有地上类型和土壤层的林地C:P和N:P均较高,但在针叶林中尤为如此。在矿物层中,C:N,C:P和N:P都遵循相似的趋势。我们的研究结果表明,林分年龄,树桩组成(受演替影响)和土壤深度对北方森林生态系统中森林土壤养分动态的重要影响。 (C)2016 Elsevier B.V.保留所有权利。

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