2019
DOI: 10.1007/s11440-019-00857-z
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Fractal characteristics of pore structure of compacted bentonite studied by ESEM and MIP methods

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Cited by 50 publications
(19 citation statements)
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“…Clayey materials are preferred here for at least two reasons. First, as previously mentioned, clayey soils or rocks often show microstructural patterns that are observed in multiscale materials 37–41,68 . They exhibit a complex hierarchical organization at microstructural levels observed with space scales of several orders of magnitude, typically from nanometers to millimeters 69 .…”
Section: Applicationsmentioning
confidence: 92%
See 1 more Smart Citation
“…Clayey materials are preferred here for at least two reasons. First, as previously mentioned, clayey soils or rocks often show microstructural patterns that are observed in multiscale materials 37–41,68 . They exhibit a complex hierarchical organization at microstructural levels observed with space scales of several orders of magnitude, typically from nanometers to millimeters 69 .…”
Section: Applicationsmentioning
confidence: 92%
“…This construction process leads to a multiscale or “fractal‐like” microstructure constituted by a set of many inclusions of many orders of magnitude. Note that this textural or microstructural feature is typical of clayey materials 37–41 …”
Section: Introductionmentioning
confidence: 92%
“…If the object is a signal, it is denoised before the fractal dimension is calculated by fractal dimension calculation methods for signals (e.g., PSD, correlation dimension and others). In addition, the fractal feature extraction of porous packaging materials can be obtained by mercury intrusion porosimetry [ 32 ] (MIP) and adsorption method [ 33 ], and then the fractal dimension can be acquired. The fractal dimension of packaging materials suitable for small-angle X-ray scattering [ 34 ] (SAXS) analysis can be obtained by the following method.…”
Section: Basic Theory Of Fractalmentioning
confidence: 99%
“…All samples have a bimodal pore size distribution, with two major pore sizes, which can be divided into macroscopic pores (between aggregation and aggregation) and microscopic pores (aggregated interior). The duplicate porosity feature usually also occurs when the soil samples are compressed at the optimal moisture content 43,44 .…”
Section: Mechanism Analysis Of Clay Content Effect On Mechanical Propertiesmentioning
confidence: 99%