首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Spatial variability of organic carbon and total nitrogen in the soils of a subalpine forested catchment at Mt. Taiyue, China
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Spatial variability of organic carbon and total nitrogen in the soils of a subalpine forested catchment at Mt. Taiyue, China

机译:山坡苏联森林集水区土壤中有机碳和总氮的空间变异性。

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Soil organic carbon (SOC) and total nitrogen (TN) are critical indicators of soil quality and play a pivotal role in key biogeochemical process (i.e. soil carbon and nutrient cycling). Many studies have assessed soil organic matter and nutrients individually in different ecosystems. However, appropriate sampling density for accurate estimation of the spatial distribution of SOC in subalpine forests and quantification of the relative importance of influencing factors remains uncertain. In this study, a combination of conventional analytical and geostatistical methods was used to analyze the spatial variability and patterns of SOC and TN along a soil profile. A total of 444 soil samples, taken from three layers down to 60 cm, were collected from the Jieshigou catchment area (5.64 km(2)) of Mount Taiyue in northern China. Results show that a large spatial variability of SOC and TN appears in upper 40 cm along an elevation and vegetation gradient, while strong spatial autocorrelation is present below 40 cm (40-60 cm). Range and degree of spatial autocorrelation for SOC were slightly larger than those of TN; All the same, both showed clustered spatial distribution. A distribution map of Kriging revealed that both SOC and TN concentrations in the Jieshigou catchment area decreased from west to east along the direction of the valley, which coincides with the overlay of topographic features. More than 40% of the variance in SOC and TN contents could be explained by topographical indices and normalized difference vegetation index (NDVI). SOC and TN significantly increased (from 23.6 to 56.8 g kg(-1)) with age of larch plantations in the surface layer. Our results suggest that a stratified random sampling was proved a sufficiently reliable way for estimating the spatial distribution of SOC and TN. (C) 2017 Elsevier B.V. All rights reserved.
机译:土壤有机碳(SOC)和总氮(TN)是土壤质量的关键指标,并在关键生物地球化学过程中发挥关键作用(即土壤碳和营养循环)。许多研究在不同生态系统中分别评估了土壤有机物和营养素。然而,用于精确估计SoC在血乃顺森林中的空间分布的适当采样密度和影响因素的相对重要性的量化仍然不确定。在该研究中,常规分析和地质统计方法的组合用于分析沿土壤剖面的空间变异性和SOC和TN的模式。从吉斯海沟集水区(5.64 km(2))在中国北部的泰岳山山山山山山区(5.64 km(2))收集了444个土样。结果表明,沿着高程和植被梯度,SOC和TN的大量空间可变性出现在高40厘米中,而强烈的空间自相关40厘米(40-60厘米)。 SOC的空间自相关的范围和空间自相关的程度略大于TN;所有相同,两者都显示了集群空间分布。 Kriging的分布图显示,杰希沟集水区中的SOC和TN浓度沿着山谷的方向从西向东减少,这与地形特征的覆盖相一致。可以通过地形指标和归一化差异植被指数(NDVI)来解释SOC和TN内容的40%以上的SOC和TN内容的差异。 SOC和TN显着增加(从23.6到56.8g kg(-1)),表面层中的落叶松人工植物年龄。我们的研究结果表明,已经证明了分层随机抽样是一种足够可靠的方法来估计SOC和TN的空间分布。 (c)2017 Elsevier B.v.保留所有权利。

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