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On soil textural classifications and soil-texture-based estimations

机译:土壤纹理分类与土壤纹理估计

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摘要

The soil texture representation with the standard texturalfraction triplet sand–silt–clay is commonly used to estimate soilproperties. The objective of this work was to test the hypothesis that otherfraction sizes in the triplets may provide a better representation of soiltexture for estimating some soil parameters. We estimated the cumulativeparticle size distribution and bulk density from an entropy-based representationof the textural triplet with experimental data for 6240 soil samples. The resultssupported the hypothesis. For example, simulated distributions were notsignificantly different from the original ones in 25 and 85 % of cases whenthe sand–silt–clay and very coarse+coarse + medium sand − fine + very finesand − silt+clay were used, respectively. When the same standard andmodified triplets were used to estimate the average bulk density, thecoefficients of determination were 0.001 and 0.967, respectively. Overall,the textural triplet selection appears to be application and data specific.
机译:土壤纹理表示与标准纹理级分三胶砂砂淤泥常用于估计土壤特性。这项工作的目标是测试其他其他人的假设三胞胎中的分数尺寸可以提供更好的土壤表示估计一些土壤参数的纹理。我们估计了累积基于熵的表示的粒度分布和散装密度具有6240个土壤样品的实验数据的纹理三重态。结果支持假设。例如,模拟分布不是与原始的25%和85%的情况有显着不同沙淤泥和非常粗+粗+中沙 - 细+非常好分别使用沙淤硅+粘土。当相同的标准和改进的三胞胎用于估计平均堆积密度,测定系数分别为0.001和0.967。总体,纹理三联选择似乎是应用程序和特定于数据。

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