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Fine-root dynamics in mixed boreal conifer-broad-leafed forest stands at different successional stages after fire

机译:北方针叶阔叶混交林火后不同演替阶段的细根动态

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摘要

Fine-root (diameter ≤ 10 mm) standing biomass, length, distribution, production, and decomposition were studied in mixed conifer broad-leafed forest stands 48, 122, and 232 years after fire on clay soils in the southern boreal forest of Quebec. A combination of ingrowth bags, soil cores, and root litter bags was used. Forest composition changed from trembling aspen- (Populus tremuloides Michx.) dominated stands in the youngest stage to balsam fir (Abies balsamea (L.) Mill.), and then to eastern white-cedar (Thuja occidentalis L.) stands in the oldest stage. The fine- and small-root standing biomass did not differ significantly between the forest successional stages. However, the total root length was significantly more developed in the 48-year-old successional stand than in the 232-year-old stand. Within the investigated soil profile (depth = 30 cm) most roots (>80%) were found in the 5 to 8 cm thick organic layer and the top 10 cm of the mineral soil. Root biomass in the organic layer increased significantly after fire, and a simultaneous increase in thickness of the organic layer was observed. The ingrowth of roots into ingrowth bags during one and two growing seasons was more than twice as high m the youngest stand as in the oldest one. However, the differences were not statistically significant because of high variation. Fine roots of aspen decomposed significantly faster than those of balsam fir and cedar in all forest stands. The results suggest that root production, the rate of decomposition, and presumably the rate of turnover are higher in forest stands dominated by early successional broad-leafed species such as aspen than in stands composed of late successional coniferous species such as fir, spruce, and cedar. Differences in root dynamics may contribute significantly to the change in the carbon and nutrient cycling often reported with succession in the boreal forest.
机译:细针叶林(直径≥10 mm)的站立生物量,长度,分布,生产和分解在南方针叶阔叶林的黏土上火后48、122和232年对混合针叶阔叶林林分进行了研究。魁北克向内生长袋,土壤芯和根垃圾袋结合使用。森林组成从最年轻阶段的颤抖白杨(Populus tremuloides Michx。)为主的林分转变为香脂冷杉(Abies balsamea(L.)Mill。),然后变为东部白雪松(Thuja occidentalis L.)最老的林分。阶段。在森林演替阶段之间,细根和小根生物量没有显着差异。但是,在48岁的演替林中,总根长明显比在232岁的演林中更发达。在所调查的土壤剖面(深度= 30厘米)内,大多数根系(> 80%)位于5至8厘米厚的有机层和矿物土壤的顶部10厘米处。火灾后,有机层中的根生物量显着增加,并且观察到有机层的厚度同时增加。在一个生长季节和两个生长季节中,根系向内生长的生长比最小的林分高出两倍。但是,由于差异很大,因此差异在统计上并不显着。在所有森林林分中,白杨细根的分解速度都明显快于香脂冷杉和雪松的分解速度。结果表明,由早期演替阔叶树种(如白杨)主导的林分中的根系生成,分解速率和推定的周转率要高于由冷杉,云杉和松木等后期演替针叶树种组成的林分。雪松。根系动力学的差异可能极大地促进了北方森林中经常报告的碳和养分循环的变化。

著录项

  • 作者单位
  • 年度 1997
  • 总页数
  • 原文格式 PDF
  • 正文语种 {"code":"en","name":"English","id":9}
  • 中图分类
  • 入库时间 2022-08-20 20:19:12

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