首页> 外文OA文献 >Fine Root Biomass And Root Length Density In A Lowland And A Montane Tropical Rain Forest, Sp, Brazil [biomassa De Raízes Finas E Densidade Do Comprimento Radicular Em Uma Floresta Tropical Chuvosa De Terras Baixas E Montana, Sp, Brasil]
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Fine Root Biomass And Root Length Density In A Lowland And A Montane Tropical Rain Forest, Sp, Brazil [biomassa De Raízes Finas E Densidade Do Comprimento Radicular Em Uma Floresta Tropical Chuvosa De Terras Baixas E Montana, Sp, Brasil]

机译:巴西Sp低地和山地热带雨林的细根生物量和根长密度[巴西Sp低地和山地雨林中的细根生物量和根长密度]

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摘要

Fine roots, <2 mm in diameter, are responsible for water and nutrient uptake and therefore have a central role in carbon, nutrient and water cycling at the plant and ecosystem level. The root length density (RLD), fine root biomass (FRB) and vertical fine root distribution (VRD) in the soil profile have been used as good descriptors of resource-use efficiency and carbon storage in the soil. Along altitudinal gradients, decreases in temperature and radiation inputs (depending on the frequency of fog events) may reduce decomposition rates and nutrient availability what might stimulate plants to invest in fine roots, increasing acquisition of resources. We evaluated the seasonal variation of fine root parameters in a Lowland and Montane forest at the Atlantic Rain Forest. We hypothesized that, due to lower decomposition rates at the Montane site, the FRB and RLD at soil surface will be higher in this altitude, which can maximize the efficiency of resource absorption. FRB and RLD were higher in the Montane forest in both seasons, especially at the 0-5 layer. At the 0-5 soil layer in both sites, RLD increased from dry to wet season independently of variations in FRB. Total FRB in the top 30 cm of the soil at the Lowland site was significantly lower (334 g.m -2 in the dry season and 219 g.m -2 in the wet season) than at the Montane forest (875 and 451 g.m -2 in the dry and wet season, respectively). In conclusion, despite the relevance of FRB to describe processes related to carbon dynamics, the variation of RLD between seasons, independently of variations in FRB, indicates that RLD is a better descriptor for studies characterizing the potential of water and nutrient uptake at the Atlantic Rain Forest. The differences in RLD between altitudes within the context of resource use should be considered in studies about plant establishment, seedling growth and population dynamics at the Atlantic Rain Forest. At the ecosystem level, RLD and it seasonal variations may improve our understanding of the Atlantic rain forest functioning in terms of the biogeochemical fluxes in a possible scenario of climate change and environmental changes.
机译:直径小于2毫米的细根负责水分和养分的吸收,因此在植物和生态系统一级的碳,养分和水循环中起着核心作用。土壤剖面中的根长密度(RLD),细根生物量(FRB)和垂直细根分布(VRD)已被用作土壤资源利用效率和碳储量的良好描述。沿着海拔梯度,温度和辐射输入的减少(取决于雾事件的发生频率)可能会降低分解速率和养分利用率,这可能会刺激植物投资于细根,从而增加资源获取。我们评估了大西洋雨林的低地和山地森林细根参数的季节性变化。我们假设,由于Montane地点的分解速率较低,在此高度下,土壤表面的FRB和RLD会更高,从而可以最大程度地利用资源。在两个季节中,山地森林中的FRB和RLD都较高,尤其是在0-5层。在两个地点的0-5土层,RLD从干季到湿季都增加,与FRB的变化无关。低地站点顶部30厘米土壤的总FRB明显低于山地森林(旱季为334 gm -2,湿季为219 gm -2)(蒙大拿州为875和451 gm -2)。旱季和雨季)。总之,尽管FRB可以描述与碳动力学相关的过程,但季节之间的RLD的变化与FRB的变化无关,表明RLD是表征大西洋雨水和养分吸收潜力的更好的描述符森林。在关于资源利用的背景下,海拔高度之间的RLD差异应在有关大西洋雨林植物的建立,幼苗生长和种群动态的研究中加以考虑。在生态系统层面,RLD及其季节性变化可能会改善我们对大西洋雨林在气候变化和环境变化的可能情况下生物地球化学通量方面的功能的了解。

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