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Microtomographic analysis of pore space in a virgin soddy-podzolic soil

机译:原始大豆-土壤中孔隙空间的显微断层分析

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The method of X-ray microtomography was applied to study pore space of a virgin soddy-podzolic soil at the natural soil water content. The morphometric parameters of the pores of more than 100 mu m in diameter were determined in the vertically oriented undisturbed soil monoliths (d = 3 cm, h = 3-4 cm) from the genetic horizons of the most differentiated part of the soil profile (the AY, AEL, EL, BEL, BT1, and BD cent 2 horizons). A tendency for the horizontal orientation of these pores was found in all the horizons, except for the humus (AY) horizon. Isolated vesicular pores of different sizes were abundant in the eluvial part of the profile. Numerous recent and relict phytogenic channels were found in the intraped mass of the BT2 horizon. Differently directed interfaces of structural units in the soil horizons were visualized. Cluster analysis was applied to estimate differences between the genetic horizons with respect to their textures, aggregate sizes, and shapes of pores as seen in vertical two-dimensional X-ray images.
机译:运用X射线显微照相法研究了天然土壤水含量下原始水田土壤的孔隙空间。从土壤剖面最分化部分的遗传视野(d = 3 cm,h = 3-4 cm),在垂直定向的未扰动土壤整料中确定直径超过100μm的孔的形态参数( AY,AEL,EL,BEL,BT1和BD分2级)。除了腐殖质(AY)层外,在所有层位中都发现了这些孔隙水平取向的趋势。不同大小的孤立的囊泡孔在剖面的凹陷部分富集。在BT2层位的被埋物中发现了许多最近的和遗留的植物通道。可视化了土壤层中结构单元的不同定向界面。应用聚类分析来评估遗传视野之间的差异,如垂直二维X射线图像中所见,它们的质地,聚集体大小和孔的形状有关。

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