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Fractal features of soil particle size distribution in newly formed wetlands in the Yellow River Delta

机译:黄河三角洲新建湿地土壤粒径分布的分形特征

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摘要

The characteristic of particle size distribution (PSD) in the newly formed wetlands in coast has seldom been studied. We applied fractal-scaling theory in assessing soil particle size distribution (PSD) features of newly formed wetlands in the Yellow River Delta (YRD), China. The singular fractal dimensions (D) values ranged from 1.82 to 1.90, the capacity dimension (D-0) values ranged from 0.84 to 0.93, and the entropy dimension (D-1) values ranged from 0.66 to 0.84. Constrained corresponding analysis revealed that 43.5% of the variance in soil PSD can be explained by environmental factors, including 14.7% by seasonal variation, 8.6% by soil depth, and 8.0% by vegetation type. The fractal dimensions D and D-1 were sensitive with fine particles with size ranging less than 126 mu m, and D-0 was sensitive with coarse particles with size ranging between 126 mu m to 2000 mu m. Fractal analysis makes full use of soil PSD information, and offers a useful approach to quantify and assess the soil physical attributes in the newly formed wetland.
机译:很少研究沿海新形成的湿地的粒径分布(PSD)的特征。我们应用分形标度理论来评估中国黄河三角洲(YRD)新形成的湿地的土壤粒径分布(PSD)特征。分形维数(D)的范围为1.82至1.90,容量维数(D-0)的范围为0.84至0.93,熵维(D-1)的范围为0.66至0.84。约束相应的分析表明,土壤PSD的43.5%的变化可以由环境因素解释,包括季节变化的14.7%,土壤深度的8.6%和植被类型的8.0%。分形维数D和D-1对尺寸小于126μm的细颗粒敏感,而D-0对尺寸在126μm至2000μm的粗颗粒敏感。分形分析充分利用了土壤PSD信息,并提供了一种有用的方法来量化和评估新形成的湿地中的土壤物理属性。

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