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Temporal patterns of net soil N mineralization and nitrification through secondary succession in the subtropical forests of eastern China

机译:中国东部亚热带森林次生演替过程中净土壤氮矿化和硝化的时间格局

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摘要

Linking temporal trends of soil nitrogen (N) transformation with shifting patterns of plants and consequently changes of litter quality during succession is important for understanding developmental patterns of ecosystem function. However, the successional direction of soil N mineralization and nitrification in relation to species shifts in the subtropical regions remains little studied. In this study, successional patterns of net soil N mineralization and nitrification rates, litter-fall, forest floor litter, fine root and soil properties were quantified through a successional sequence in the subtropical forests of eastern China. Net N mineralization rate was ‘U-shaped’ through succession: highest in climax evergreen broad-leaved forest (CE: 1.6 ± 0.2 mg-N kg−1 yr−1) and secondary shrubs (SS: 1.4 ± 0.2 mg-N kg−1 yr−1), lowest in conifer and evergreen broad-leaved mixed forest (MF: 1.1 ± 0.1 mg-N kg−1 yr−1) and intermediate in conifer forest (CF: 1.2 ± 0.1 mg-N kg−1 yr−1) and sub-climax forest (SE: 1.2 ± 0.2 mg-N kg−1 yr−1). Soil nitrification increased with time (0.02 ± 0.1, 0.2 ± 0.1, 0.5 ± 0.1, 0.2 ± 0.1, and 0.6 ± 0.1 mg-N kg−1 yr−1 in SS, CF, MF, SE and CE, respectively). Annual production of litter−fall increased through succession. Fine root stocks and total N concentration, soil total N, total carbon (C) and microbial biomass C also followed ‘U−shaped’ temporal trends in succession. Soil bulk density was highest in MF, lowest in CE, and intermediate in SS, CF and SE. Soil pH was significantly lowest in CE. Temporal patterns of soil N mineralization and nitrification were significant related to the growth of conifers (i.e. Pinus massoniana) and associated successional changes of litter-fall, forest floor, fine roots and soil properties. We concluded that, due to lower litter quality, the position of Pinus massoniana along the succession pathway played an important role in controlling temporal trends of soil N transformation. Keywords Evergreen broad-leaved forest - Fine roots - Forest floor litter - Litter-fall - Soil incubation - Soil N availability - Soil properties Responsible Editor: Per Ambus.
机译:将土壤氮(N)转化的时间趋势与植物的转移模式联系起来,从而将演替过程中的凋落物质量变化联系起来,对于理解生态系统功能的发展模式非​​常重要。然而,关于亚热带地区土壤氮矿化和硝化作用与物种迁移相关的演替方向仍然很少研究。在这项研究中,通过演替序列对中国东部亚热带森林的净土壤氮矿化和硝化速率,凋落物下降,林地凋落物,细根和土壤特性的演替模式进行了定量。净氮矿化率通过演替呈“ U”形:在高潮常绿阔叶林中最高(CE:1.6±0.2 mg-N kg -1 yr -1 )和次生灌木(SS:1.4±0.2 mg-N kg −1 yr −1 ),在针叶树和常绿阔叶混交林中最低(MF:1.1± 0.1 mg-N kg -1 yr -1 )和针叶林中间产物(CF:1.2±0.1 mg-N kg -1 yr -1 )和次高潮森林(SE:1.2±0.2 mg-N kg -1 yr -1 )。土壤硝化随时间增加(0.02±0.1、0.2±0.1、0.5±0.1、0.2±0.1和0.6±0.1 mg-N kg -1 yr -1 SS,CF,MF,SE和CE)。凋落物的年产量逐年增加。细根种群和总氮浓度,土壤总氮,总碳(C)和微生物生物量碳也相继遵循“ U型”时间趋势。土壤容重在MF最高,在CE最低,在SS,CF和SE中等。 CE中的土壤pH值最低。土壤氮矿化和硝化的时间格局与针叶树(即马尾松)的生长以及凋落物,林地,细根和土壤特性的连续演替密切相关。我们得出的结论是,由于凋落物质量较低,马尾松沿演替途径的位置在控制土壤氮转化的时间趋势中起着重要作用。关键词常绿阔叶林-细根-森林地面凋落物-凋落物-土壤温育-土壤氮素供应-土壤特性责任编辑:Per Ambus。

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