首页> 外文期刊>Geoderma: An International Journal of Soil Science >Soil organic carbon stock is closely related to aboveground vegetation properties in cold-temperate mountainous forests
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Soil organic carbon stock is closely related to aboveground vegetation properties in cold-temperate mountainous forests

机译:温带山区森林土壤有机碳储量与地上植被特性密切相关

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摘要

The soils of cold-temperate mountainous forest ecosystems contain large carbon pools that may respond quickly to changes in climate and land use. A better understanding of the temporal-spatial distribution of soil organic carbon (SOC) stock is the first step toward quantifying its potential responses to global changes in climate or land use. The primary objective of this study was to understand the spatial distribution of SOC within a representative mountainous landscape in the cold-temperate zone in Japan. The two dominant tree species in this region are beech (Fagus crenata, a climax species in this zone), and birch (Betula ermanii). In 15 permanent plots located along an altitudinal gradient on the Mount Naeba and Mount Yakio, relationships were determined between SOC and climate (as represented by mean annual temperature), topography (aspect, slope, and altitude), aboveground vegetation properties (stand age, leaf area index, aboveground biomass, mean tree height, tree diameter, stand density, tree basal area, litter depth, and site index), and soil properties (soil bulk density, soil hardness, soil water content, soil root content). Our results indicated that SOC stocks in Japanese cold-temperate forest ecosystems are relatively high, ranging from 12 to 20 kg m super(- 2) in the top 30 cm of soils. Correlation analysis that included data from all 15 plots (and therefore data from both beech and birch forest and both mountains) suggested that the aboveground vegetation properties, such as aboveground biomass, mean tree height, and stand density, were strongly correlated with the SOC stock. In contrast, topographic factors (aspect and slope) explained SOC spatial distribution for the plots within the same mountain but not for plots from both mountains. Regression models based only on aboveground vegetation properties explained 76.7% of the variability in SOC stocks in beech ecosystems (represented by 10 plots) and 74.9% of the variability in all 15 plots. The strong correlation between aboveground vegetation properties and SOC suggests that measurement of vegetation properties by remote sensing could represent a feasible and rapid method for estimating SOC distribution in a rugged terrain.
机译:温带山区森林生态系统的土壤含有大量的碳库,这些碳库可能会对气候和土地利用的变化做出快速反应。更好地了解土壤有机碳(SOC)储量的时空分布是量化其对全球气候或土地利用变化的潜在反应的第一步。这项研究的主要目的是了解日本冷温带代表性山地景观中SOC的空间分布。该地区的两个主要树种是山毛榉(山毛榉(Fagus crenata),该区域的高潮树种)和桦木(Betula ermanii)。在沿苗场山和亚基奥山的海拔梯度分布的15个永久性地块中,确定了SOC与气候(以年平均温度表示),地形(纵横比,坡度和高度),地上植被特性(林分年龄,叶面积指数,地上生物量,平均树高,树木直径,林分密度,树木基础面积,枯枝落叶深度和站点指数)和土壤特性(土壤容重,土壤硬度,土壤含水量,土壤根含量)。我们的结果表明,日本冷温带森林生态系统中的SOC储量相对较高,在土壤的前30 cm范围内为12至20 kg m super(-2)。相关分析包括所有15个样地的数据(因此也包括山毛榉,桦木和两个山地的数据)表明,地上植被特性(例如地上生物量,平均树高和林分密度)与SOC量密切相关。 。相反,地形因素(坡度和坡度)解释了同一山脉内各样地的SOC空间分布,但不能解释两个山脉中各地的SOC空间分布。仅基于地上植被特性的回归模型解释了山毛榉生态系统中SOC种群的76.7%的变异性(由10个样地表示)和所有15个样地的74.9%的变异性。地上植被特性与SOC之间的强相关性表明,通过遥感测量植被特性可以代表一种估计崎a地形中SOC分布的可行且快速的方法。

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