2016
DOI: 10.12988/ces.2016.6687
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On the fractal characteristics of loess subsidence

Abstract: Loess soils may be considered as a discrete medium. Under increasing humidity subsidence degradation occurs as a result of the slow disintegration of microaggregates into free particles, repackaging and porosity changes. The volumetric porosity of the formed new structure and the volumetric porosity changes can be quantified from the position of the fractal theory. The main aim of this paper is to show that the fractal dimension of the particle size distribution function has important role in the description o… Show more

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Cited by 4 publications
(3 citation statements)
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References 11 publications
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“…It needs to be pointed out that the values of dry density and particle size distribution index employed for experiments fall into the normal range of loess in the studied area, and that the employed illuminance values are typical of light conditions controlled in the laboratory studies of the image analysis method. Considering the fractal characteristics of soil particle size distribution of natural loess [38][39][40], the mass fractal dimension D is used as a target indicator when preparing specimens with different particle size distribution. The mass fractal dimension D is calculated using the following equation:…”
Section: Sample Preparationmentioning
confidence: 99%
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“…It needs to be pointed out that the values of dry density and particle size distribution index employed for experiments fall into the normal range of loess in the studied area, and that the employed illuminance values are typical of light conditions controlled in the laboratory studies of the image analysis method. Considering the fractal characteristics of soil particle size distribution of natural loess [38][39][40], the mass fractal dimension D is used as a target indicator when preparing specimens with different particle size distribution. The mass fractal dimension D is calculated using the following equation:…”
Section: Sample Preparationmentioning
confidence: 99%
“…All of the specimens have a diameter of 61.8 mm and a height of 5 mm and are fully saturated using the vacuum saturation method prior to the testing. Considering the fractal characteristics of soil particle size distribution of natural loess [38][39][40], the mass fractal dimension D is used as a target indicator when preparing specimens with different particle size distribution. The mass fractal dimension D is calculated using the following equation:…”
Section: Sample Preparationmentioning
confidence: 99%
See 1 more Smart Citation