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Quantitative microstructure characteristics of landslide soil affected by Three Gorges Reservoir with using ERDAS

机译:基于ERDAS的三峡水库滑坡土壤定量微观结构特征

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The study on soil microstructure has transferred from qualitative description to quantitative analysis as the improvement of image processing technology. However, it is difficult that how to apply the quantitative technology to solve practical problems. We used ERDAS to quantify microstructure images of landslide soil in the Three Gorges Reservoir area, and then analyzed the variations of diameter and distribution dimension of particle and those of pore during the unsaturated and 1 to 3 water-saturated processes. Using ERDAS to quantify the 1500 times magnification microstructure image after the treatment of threshold value of 120, is effective for the analysis of impacts of fluctuated water level on the landslide soil structure. With the increase of water-saturated process, the average particle diameters increased from 0.2um to 0.33um while there were few changes of the average pore diameters, at the same time, the distribution dimensions of particles and pores became smaller.
机译:随着图像处理技术的进步,对土壤微观结构的研究已从定性描述转向定量分析。但是,如何应用定量技术来解决实际问题是困难的。我们利用ERDAS对三峡库区滑坡土的微观结构图像进行了定量,然后分析了非饱和和1至3个水饱和过程中颗粒直径和分布尺寸以及孔隙的直径和分布尺寸的变化。在阈值120处理后,使用ERDAS量化1500倍放大的微观结构图像,对于分析水位波动对滑坡土壤结构的影响是有效的。随着水饱和过程的增加,平均粒径从0.2um增加到0.33um,平均孔径变化不大,同时,颗粒和孔的分布尺寸变小。

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