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The Analysis of Characteristic and Spatial Variability for Soil Organic Matter and Organic Carbon around Qinghai Lake

机译:青海湖周边土壤有机质与有机碳的特性和空间变异分析

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The use of geostatistics to explore the spatial distribution and variability of soil properties has become an important tool to recognize soil properties. In this paper, we combined actual field sampling data with geostatistics to study the characteristic and spatial variability of soil organic matter and organic carbon content around Qinghai Lake. The results showed that the mean content of soil organic carbon is 5.95 ± 3.40%, and organic matter is 3.45 ± 1.97%, both are low. The variogram model of semi-variance function graph showed the models of soil organic carbon and matter are the exponential model. Isotropic ratio of nugget to sill of soil organic carbon and organic matter are 82.9% and 83%, both variable range are 9300m,all are in the range, here exists a correlation between organic carbon and organic matter content in the space. Fractal dimension can exhibit the higher spatial heterogeneity of soil organic carbon and organic matter content around Qinghai Lake. Anisotropy semi-variance analysis reveals that there does not exist any anisotropy structural characteristics of soil organic carbon and organic matter content in different directions in the study area; but there is spatial variability in the east-west as for organic matter content, while variability is very small in the other directions.
机译:使用地统计算法探索土壤特性的空间分布和变异性已成为识别土壤性质的重要工具。在本文中,我们将实际的现场采样数据与地统计学相结合,研究了青海湖周边土壤有机质和有机碳含量的特征和空间变异。结果表明,土壤有机碳的平均含量为5.95±3.40%,有机物质为3.45±1.97%,两者都低。半差异函数图的变形仪模型显示了土壤有机碳的型号,物质是指数模型。土壤有机碳和有机物质的块的各向同性比例为82.9%和83%,两个可变范围为9300m,一切都在范围内,这里存在空间中有机碳和有机物质含量之间的相关性。分形尺寸可以表现出青海湖周边土壤有机碳和有机物质含量较高的空间异质性。各向异性半变异分析表明,在研究区中不同方向存在土壤有机碳和有机物质含量的任何各向异性结构特征;但东部有机物质含量存在空间变异性,而可变性在另一个方向上非常小。

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