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Recovery of soil properties and functions in different rainforest restoration pathways

机译:不同雨林恢复途径中土壤性质和功能的恢复

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摘要

Rainforests in the tropics and subtropics are declining rapidly, leading to significant changes in soil physical and chemical characteristics and biochemical cycles that connect vegetation and soil. Effects of such changes on soil carbon (C) and nitrogen (N) pools are still poorly understood and contradictory results have been reported in different studies. We studied changes in C and N dynamics associated with deforestation and reforestation in the Big Scrub region of subtropical eastern Australia, where over 99% of the former rainforest cover was converted by European settlers for pasture or agriculture. In this area, the most common reforestation pathways are tree-planting for ecological restoration purposes, autogenic regrowth dominated by the invasive tree species camphor laurel (Cinnamomum camphora), and management of this regrowth to accelerate the development of a more native tree community. Nineteen soil properties were measured at 25 sites, five within each of: remnant rainforest, pasture, ecological restoration plantings 10-15-year old, camphor laurel regrowth 20-40-year old, and rainforest regrowth 3-6 years after poisoning of camphor trees within older regrowth. Of eight components of N cycling measured, four differed significantly between site-types: nitrate-N, plant-available nitrate-N and nitrification rates were highest in rainforest and lowest in pasture, with revegetated sites showing intermediate levels; while plant-available ammonium-N showed a reverse pattern. Among revegetated sites, camphor-dominated regrowth showed slightly less regeneration of N dynamics than treated camphor and replanted sites. Among soil attributes related to the soil C cycle and soil microbial activity, there was little variation with deforestation or reforestation. Four of five other soil attributes (pH, bulk density, fine root biomass, and plant-available phosphate-P) showed significant variation among site-types, with specific patterns varying. All three reforestation pathways were able to restore soil properties to varying degrees, although the rate of recovery was lowest in untreated camphor regrowth.
机译:热带和亚热带的雨林正在迅速减少,导致土壤物理和化学特征以及连接植被和土壤的生化循环发生了重大变化。这种变化对土壤碳(C)和氮(N)库的影响仍然知之甚少,并且在不同的研究中报道了矛盾的结果。我们研究了与亚热带东部澳大利亚大灌木丛地区森林砍伐和再造林相关的碳和氮动态变化,那里超过99%的前雨林覆盖物是由欧洲定居者转换为牧场或农业的。在该地区,最常见的造林途径是植树造林以恢复生态,以入侵性树种樟脑(Cinnamomum camphora)为主导的自生再生,以及对该再生的管理以加速建立更原生树木社区的发展。在25个地点测量了19个土壤特性,每个地点中有五个:残余雨林,牧场,生态恢复种植园10-15年,樟树月桂树再生20-40年以及雨林在樟脑中毒后3-6年再生。较旧的再生树。在测量的N循环的八个组成部分中,四个站点类型之间存在显着差异:硝酸盐-N,植物有效的硝酸盐-N和硝化率在雨林中最高,在牧场中最低,重新植被的站点显示中等水平。而植物可用的铵态氮则显示相反的模式。在植被恢复的地点中,以樟脑为主的再生长区比处理过的樟脑和重新种植的地点显示出较少的N动态再生。在与土壤碳循环和微生物活动相关的土壤属性中,森林砍伐或再造林几乎没有变化。其他五种土壤属性(pH,堆密度,细根生物量和植物有效的磷酸盐-P)中的四种显示出位点类型之间的显着差异,具体模式有所不同。尽管未经处理的樟脑再生的恢复速度最低,但所有三种造林途径均能够不同程度地恢复土壤特性。

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