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Fine root dynamics of trees and understorey vegetation in a chronosequence of Betula platyphylla stands

机译:白桦(Betula platyphylla)林分按时序排列的树木和林下植被的精细根系动态

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Despite the recognized importance of fine roots in influencing forest carbon and nutrient cycling, knowledge of how fine root biomass, production and turnover rates change with stand age is still limited. In this study, we applied both sequential soil coring and ingrowth cores techniques to assess the influence of stand age on fine root biomass, live/dead ratio, production and turnover rates of trees and understorey vegetation in 20-, 36-, 57- and 82-year-old Betula platyphylla stands in northeastern China. A total of 1440 sequential cores and 288 ingrowth cores were collected from three soil depths (0-10, 10-20, and 20-30 cm) during 2009-2010. Fine root biomass of trees increased from 20- to 36-year-old stands, and decreased thereafter in 57- and 82-year-old stands, while the distribution of understorey fine roots differed from that of tree fine roots. Fine root biomass of the understorey vegetation accounted for 49%, 12%, 31% and 60% of total fine root biomass in 20-, 36-, 57- and 82-year-old stands, respectively. Total biomass of fine roots (trees and understorey vegetation) increased with stand age. The live/dead ratio decreased with stand age, indicating that the older the stands, the greater the proportion of fine root necromass. Furthermore, our results showed that the mean tree basal area could explain 67% of the variation in tree fine root biomass and 53% of that in the total fine root biomass at the tree level. These tree-level analyses may be of great value in predicting fine root biomass values in B. platyphylla stands at the stand and/or tree level. Fine root production and turnover rates based on both sequential soil coring and ingrowth cores techniques exhibited similar age-related patterns, strengthening the results that fine root production and turnover rates increased with stand age in the B. platyphylla chronosequence we studied. (C) 2015 Elsevier B.V. All rights reserved.
机译:尽管公认细根在影响森林碳和养分循环中的重要性,但是关于细根生物量,产量和周转率如何随着林龄的变化而变化的知识仍然有限。在这项研究中,我们应用顺序土壤取芯和向内生长的核心技术来评估林分年龄对20、36、57和57的细根生物量,生/死比,树木和林下植被的生产和周转率的影响。 82岁的白桦(Betula platyphylla)站在中国东北。在2009-2010年期间,共从三个土壤深度(0-10、10-20和20-30 cm)收集了1440个连续岩心和288个向内岩心。树木的细根生物量从20岁到36岁的林分增加,然后在57和82岁的林分中减少,而下层细根的分布与树木细根的分布不同。在20、36、57、57和82年的林分中,底层植被的细根生物量分别占总细根生物量的49%,12%,31%和60%。细根(树木和林下植被)的总生物量随树龄的增加而增加。生死比随林分年龄而降低,表明林分越老,细根坏死的比例越大。此外,我们的结果表明,在树木水平上,平均树根面积可以解释67%的细根生物量变化和53%的细根总生物量变化。这些树级别的分析对于预测白桦在林分和/或树水平上的细根生物量值可能具有重要价值。基于连续土壤取芯和向内生长核技术的细根产量和周转率表现出相似的年龄相关型态,加强了我们研究的白僵菌年代序列中细根产量和周转率随林龄的增加而增加的结果。 (C)2015 Elsevier B.V.保留所有权利。

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