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Geostatistical Analysis of Soil Water Content in Natural and Secondary Forests of Changbai Mountain, China

机译:中国长白山自然和中林土壤含水量的地质统计分析

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Applying a combination of classical and geostatistical analysis, we investigated the distribution properties of soil water contents in broad-leaved Korean Pine forest (A) and secondary Polar-Birch forest (B) in Changbai Mountain, Northeast China. The results showed soil water content was significantly different between plots A and B (P < 0.05). The variation coefficient (CV) for soil water content was lower in plot A than in plot B at 0-10 cm depth, while the CV was higher in plot A than in plot B at 10-20 cm depth. Geostatistical analysis revealed that the exponential models were the optimality models for the soil water content in both plots. The spatial structured variance accounted for the largest proportion of total variance in soil water content in both plots. The autocorrelation range value for the semivariogram of soil water content was 8.9 m at 0-10 cm depth and 12.6 m at 10-20 cm depth in plot A, which was more than those in plot B (8.0 m) at both depths. Maps obtained by kriging showed that soil water contents in both plots exhibited different spatial distribution patterns. It could be conclude that the differences of rain time, precipitation form, topography and forest type may contributed to the distribution of soil water content in Changbai Mountain.
机译:应用古典和地统计学分析的组合,研究了中国东北地区长白山阔叶韩国林(A)和二级北极桦树林(B)土壤水分含量的分布特性。结果显示土壤含水量在曲线A和B之间显着差异(P <0.05)。对于土壤水分含量的变化系数(CV)是曲线A比在0-10厘米深入小区B时,虽然在CV 10-20厘米深度为在曲线A比曲线B更高。地质统计分析表明,指数模型是两块土壤含水量的最优性模型。空间结构方差占两块土壤水含量的总方差比例最大。在0-10cm的深度下,土壤水含量的半烹饪局的自相关范围值为8.9μm,曲线A的10-20cm深度为12.6μm,这比两种深度的曲线B(8.0m)中的10.6米。通过Kriging获得的地图表明,两个绘图中的土壤水含量表现出不同的空间分布图案。可以得出结论,下雨时间,降水形式,地形和森林类型的差异可能导致长白山土壤含水量分布。

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