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Permanent Deformation of Track-Bed Materials at Various Inclusion Contents under Large Number of Loading Cycles

Identifiers
URI: http://hdl.handle.net/20.500.12020/1270
ISSN: 19435606
ISSN: 10900241

DOI: https://doi.org/10.1061/(ASCE)GT.1943-5606.0001911
Author/s
Wang, Han-Lin; Cui, Yu-Jun; Lamas López, Francisco; Dupla, Jean-Claude; Canou, Jean; [et al.]
Date
2018-05-19
Document type
article
Área/s de conocimiento
Ciencias de la Naturaleza
Ingenierías
Matemáticas y Física
Materia/s Unesco
3323 Tecnología de Los Ferrocarriles
2205.09 Mecánica de Sólidos
25 Ciencias de la Tierra y del Espacio
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Abstract
In the French conventional railway substructure, the interpenetration of ballast grains and subgrade fine soils that occurred over years of operation has created a new layer, namely, an interlayer. The in situ investigation on this interlayer showed that the content of ballast grains decreases over depth, with the lower part characterized by a matrix of fines with inclusions of coarse grains. In this study, the permanent deformation of a material simulating the lower part of interlayer soil was investigated at six different volumetric inclusion contents fv (volumetric ratio of the inclusion grains to the total sample) by performing cyclic triaxial tests. The results indicate that at a given cycle, the permanent deformation decreases with the increase of fv, and the evolution of permanent deformation is strongly influenced by the loading history. To further investigate the effect of inclusion content, a method that allows eliminating the influence of loading history and estimating the end-stage permanent deformations at different stress levels was applied. Quadratic polynomial and bilinear fitting methods were used to fit the variations of the estimated end-stage permanent deformations with fv, showing a proper similarity between the two methods at high loading amplitudes (higher than 15 kPa). Furthermore, the testing results revealed the existence of a characteristic volumetric inclusion content fv-cha by bilinear fitting method, separating two zones with different inclusion effects. This observation is strongly supported by the X-ray microcomputed tomography (μCT) scans performed on the as-compacted samples. When fv ranges from 0 to 20% (smaller than fv-cha), the fines constitute the skeleton of the sample, and the permanent deformation decreases rapidly with the increase of fv. By contrast, when fv increases up to 35–45% (larger than fv-cha), the inclusions dominate the skeleton of the sample, leading to a slight decrease of permanent deformation with fv.
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