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首页> 外文期刊>Global change biology >Seasonal soil-surface carbon fluxes from the root systems of young Pinus radiata trees growing at ambient and elevated CO2 concentration
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Seasonal soil-surface carbon fluxes from the root systems of young Pinus radiata trees growing at ambient and elevated CO2 concentration

机译:在环境和高CO2浓度下生长的辐射松幼树根系的季节性土壤表面碳通量

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摘要

Elevated atmospheric CO2 concentration may result in increased below-ground carbon allocation by trees, thereby altering soil carbon cycling. Seasonal estimates of soil surface carbon flux were made to determine whether carbon losses from Pinus radiata trees growing at elevated CO2 concentration were higher than those at ambient CO2 concentration, and whether this was related to increased fine root growth. Monthly soil surface carbon flux density (f) measurements were made on plots with trees growing at ambient (350) and elevated (650 mu mol mol(-1)) CO2 concentration in large open-top chambers. Prior to planting the soil carbon concentration (0.1%) and f (0.28 mu mol m(-2) s(-1) at 15 degrees C) were low. A function describing the radial pattern of f with distance from tree stems was used to estimate the annual carbon flux from tree plots. Seasonal estimates of fine root production were made from minirhizotrons and the radial distribution of roots compared with radial measurements of f. A one-dimensional gas diffusion model was used to estimate f from soil CO2 concentrations at four depths. For the second year of growth, the annual carbon flux from the plots was 1671 g y(-1) and 1895 g y(-1) at ambient and elevated CO2 concentrations, respectively, although this was not a significant difference. Higher f at elevated CO2 concentration was largely explained by increased fine root biomass. Fine root biomass and stem production were both positively related to f. Both root length density and f declined exponentially with distance from the stem, and had similar length scales. Diurnal changes in f were largely explained by changes in soil temperature at a depth of 0.05 m. Ignoring the change of f with increasing distance from tree stems when scaling to a unit ground area basis from measurements with individual trees could result in under- or overestimates of soil-surface carbon fluxes, especially in young stands when fine roots are unevenly distributed. [References: 44]
机译:大气CO2浓度升高可能会导致树木增加地下碳的分配,从而改变土壤碳循环。对土壤表面的碳通量进行季节性估算,以确定在高CO2浓度下生长的辐射松树的碳损失是否高于环境CO2浓度下的损失,这是否与增加的细根生长有关。每月土壤表面碳通量密度(f)的测量是在大开顶室中树木生长在环境(350)和升高(650μmol mol(-1))的浓度下进行的。在种植之前,土壤碳含量(0.1%)和f(在15摄氏度下为0.28μmol m(-2)s(-1))较低。用函数描述f的径向模式以及与树茎的距离,可以从树图中估算年碳通量。季节性的细根产量估算是根据小型根际生物进行的,根的径向分布与f的径向测量值进行了比较。一维气体扩散模型用于从四个深度的土壤CO2浓度估算f。对于生长的第二年,在环境浓度和升高的CO2浓度下,该样区的年碳通量分别为1671 g y(-1)和1895 g y(-1),尽管这没有显着差异。在较高的CO2浓度下较高的f可以用细根生物量的增加来解释。细根生物量和茎秆产量均与f呈正相关。根长密度和f都随着距茎的距离呈指数下降,并且具有相似的长度尺度。 f的日变化主要由深度为0.05 m的土壤温度变化解释。当根据单个树木的测量结果缩放到单位地面面积时,忽略f随树根距离的增加而变化的情况可能会导致土壤表面碳通量的估计过低或过高,特别是在幼小的林中,细根分布不均。 [参考:44]

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