The protocol describes procedures to acquire high-spatial resolution computed tomography (CT) images of a granular soil during triaxial compression, and to apply image processing techniques to these CT images to explore the grain-scale mechanical behavior of the soil under loading.
The rapid development of X-ray imaging techniques with image processing and analysis skills has enabled the acquisition of CT images of granular soils with high-spatial resolutions. Based on such CT images, grain-scale mechanical behavior such as particle kinematics (i.e., particle translations and particle rotations), strain localization and inter-particle contact evolution of granular soils can be quantitatively investigated. However, this is inaccessible using conventional experimental methods. This study demonstrates the exploration of the grain-scale mechanical behavior of a granular soil sample under triaxial compression using synchrotron X-ray micro-tomography (μCT). With this method, a specially fabricated miniature loading apparatus is used to apply confining and axial stresses to the sample during the triaxial test. The apparatus is fitted into a synchrotron X-ray tomography setup so that high-spatial resolution CT images of the sample can be collected at different loading stages of the test without any disturbance to the sample. With the capability of extracting information at the macro scale (e.g., sample boundary stresses and strains from the triaxial apparatus setup) and the grain scale (e.g., grain movements and contact interactions from the CT images), this procedure provides an effective methodology to investigate the multi-scale mechanics of granular soils.
It is widely recognized that the macro-scale mechanical properties of granular soil, such as stiffness, shear strength and permeability, are critical to many geotechnical structures, for example, foundations, slopes and rock-fill dams. For many years, on-site tests and conventional laboratory tests (e.g., one-dimensional compression tests, triaxial compression tests and permeability tests) have been used to evaluate these properties in different soils. Codes and standards for testing soil mechanical properties have also been developed for engineering purposes. While these macro-scale mechanical properties have been intensively studied, the grain-scale mechanical behavior (e.g., particle kinematics, contact interaction and strain localization) that governs these properties has attracted much less attention from engineers and researchers. One reason is the lack of effective experimental methods available to explore the grain-scale mechanical behavior of soils.
Until now, most of the understanding of the grain-scale mechanical behavior of granular soils has come from discrete element modeling1 (DEM), because of its ability to extract particle-scale information (e.g., particle kinematics and particle contact forces). In earlier studies of using DEM techniques to model granular soil mechanical behaviors, each individual particle was simply represented by a single circle or sphere in the model. The use of such over-simplified particle shapes has led to the over-rotation of particles and thereby a lower peak strength behavior2. To achieve a better modeling performance, many investigators have used a rolling resistance model3,4,5,6 or irregular particle shapes7,8,9,10,11,12 in their DEM simulations. As a result, a more realistic understanding of particle kinematic behavior has been acquired. Aside from particle kinematics, DEM has been increasingly used to investigate grain contact interaction and to develop theoretical models. However, because of the requirement to reproduce real particle shapes and the use of sophisticated contact models, DEM requires extremely high computational capability in the modeling of granular soils with irregular shapes.
Recently, the development of optical equipment and imaging techniques (e.g., the microscope, laser-aided tomography, X-ray computed tomography (CT) and X-ray micro-tomography (μCT)) has provided many opportunities for experimental examination of the grain-scale mechanical behavior of granular soils. Via acquisition and analysis of soil sample images before and after triaxial testing, such equipment and techniques have been utilized in the investigation of soil microstructures13,14,15,16,17,18,19. More recently, in situ tests with X-ray CT or μCT have been increasingly used to investigate the evolution of void ratio20, strain distribution21,22,23,24, particle movement25,26,27,28, inter-particle contact29,30,31 and particle crushing32 of granular soils. Here, “in situ” implies X-ray scanning conducted at the same time as loading. In contrast to general X-ray scanning, in situ X-ray scanning tests require a specially fabricated loading apparatus to deliver stresses to soil samples. With the combined use of the loading apparatus and X-ray CT or μCT device, CT images of the samples at different loading stages of the tests can be acquired non-destructively. Based on these CT images, particle-scale observations of granular soil behavior can be acquired. These CT image-based particle-level observations are extremely helpful to verify numerical findings and to gain novel insights into the grain-scale mechanical behavior of granular soils.
This article aims to share the details of how an X-ray in situ scanning test of a soil sample can be carried out, using an exemplary experiment that observes particle kinematics, strain localization and inter-particle contact evolution within a soil sample. The results show that X-ray in situ scanning tests have a great potential to explore the grain-level behavior of granular soils. The protocol covers the choice of X-ray μCT device and the preparation of a miniature triaxial loading apparatus, and detailed procedures to carry out the test are provided. In addition, the technical steps for using image processing and analysis to quantify the particle kinematics (i.e., particle translation and particle rotation), strain localization, and inter-particle contact evolution (i.e., contact gain, contact loss and contact movement) of the soil are described.
1. Designing the experiment well in advance
2. Carrying out in situ triaxial compression testing
3. Image processing and analysis
4. CT image-based exploration of grain-scale mechanical behavior of soils
NOTE: The following image-based analysis is not applicable to idealistically spherical particles or samples with very narrow grading ranges (i.e., monodisperse samples). However, for particles with high roundness and poor grading (e.g., 0.3~0.6 mm glass beads), the methodology yields good results (see Cheng and Wang31).
Figure 5 depicts the particle kinematics results of a Leighton Buzzard sand (LBS) sample at a 2D slice during two typical shear increments, I and II. Most of the particles are successfully tracked and their translations and rotations are quantified following the above protocol. During the first shear increment, neither particle displacements nor particle rotations show clear localization. However, a localized band is developed in both the particle displacement map and particle rotation map during the second shear increment. Figure 6 shows the octahedral and volumetric strain maps of the sample during the two shear increments. A clear localization zone is observed in the strain maps at the second shear increment, demonstrating the capability of the method to visualize sand failure under triaxial shearing. Figure 7 depicts the normalized orientation frequency of branch vectors of gained contacts and lost contacts in the sample during the two shear increments. The lost contacts exhibit a clear directional preference towards the minor principal stress direction (i.e., the horizontal direction) during both shear increments.
Figure 1: X-ray micro CT setup and triaxial loading device. (A) A triaxial apparatus used in conjunction with an X-ray micro CT setup. (B) An enlarged view of the installation of the triaxial apparatus during triaxial testing. (C) Triaxial apparatus from a different angle. This figure has been modified from Cheng and Wang28. Please click here to view a larger version of this figure.
Figure 2: The process of making a sample. (A) Installation of a porous stone and a membrane on the base plate, (B) installation of a sample maker, (C) creation of suction inside the sample maker, (D) dropping sand particles into the sample maker, (E) installation of another porous stone and a cushion plate on top of the sand sample, and (F) removal of sample maker from the base plate. Please click here to view a larger version of this figure.
Figure 3: Image processing of CT images. (A) Raw CT projection, (B) the CT projection after phase retrieval, (C) a reconstructed horizontal CT slice, (D) the CT slice after image filtering, (E) the CT slice after image binarization, and (F) the CT slice after particle separation. Please click here to view a larger version of this figure.
Figure 4: Illustration of the extraction of inter-particle contacts of LBS in 2D slices. (A) Implementation of a logical operation AND between the binary image of a CT slice and the binary image of watershed lines, and (B) a typical contact of two LBS particles in 3D space (particles are shown in green and blue and contact is shown in red). Please click here to view a larger version of this figure.
Figure 5: Typical particle kinematics results of an LBS sample during two shear increments. (A) Stress–strain curve of the sample under triaxial compression, (B) particle displacements and particle rotations of the sample during shear increment I, and (C) particle displacements and particle rotations of the sample during shear increment II. This figure has been modified from Cheng and Wang24. Please click here to view a larger version of this figure.
Figure 6: Typical strain fields of LBS during two shear increments.
(A) Octahedral shear strain and volumetric strain of the sample during shear increment I. (B) Octahedral shear strain and volumetric strain of the sample during shear increment II. This figure has been modified from Cheng and Wang24. Please click here to view a larger version of this figure.
Figure 7: Typical inter-particle contact evolution results of LBS during two shear increments. (A) Normalized orientation frequency of branch vectors of gained contacts and lost contacts of LBS during shear increment I. (B) Normalized orientation frequency of branch vectors of gained contacts and lost contacts of LBS during shear increment II. Please click here to view a larger version of this figure.
High-spatial resolution X-ray micro-CT and advanced image processing and analysis techniques have enabled the experimental investigation of the mechanical behavior of granular soils under shear at multi-scale levels (i.e., at macro-scale, meso-scale and grain-scale levels). However, CT image-based meso- and grain-scale investigations require the acquisition of high-spatial resolution CT images of soil samples during loading. The most challenging aspect of this process is perhaps the fabrication of a miniature triaxial loading apparatus that can be used in conjunction with an X-ray micro CT device. One should make an overall consideration of the required sample size, loading stresses and rates, in addition to the restrictions of X-ray micro CT devices such as the spatial resolution, scanning area and the load capacity of the rotation stage.
The determination of optimum X-ray energy and exposure time can be time-consuming but is crucial to the acquisition of high-quality CT images. It is recommended that users try different energies and exposure times during their first scan and determine an appropriate energy and exposure time according to the quality of the reconstructed slices. Besides, samples with different initial porosities can be produced during sample preparation by dropping sand particles into the sample mold from different heights. However, because of the small sample size, producing a sample with a specific initial porosity is more difficult in comparison to conventional triaxial tests. To produce a sample with an initial porosity that is close to a specific value for triaxial testing with CT scanning, users are recommended to practice producing samples in advance.
Compared to conventional triaxial testing, miniature in situ triaxial testing has the advantage of being able to explore the grain-scale mechanical behavior of granular soils, including grain kinematics, strain localization and inter-particle contact interaction, etc. Currently, a popular alternative method to investigate the grain-scale mechanical behavior of granular soils is DEM. Although this technique enables the modeling of sand mechanical behavior under complex loading conditions, grain shapes and contact models are generally over-simplified to achieve high computing efficiency in most DEM studies. In this situation, the grain-scale information extracted from real sand using this protocol is needed for improved validation of DEM models at multi-scale levels. Another advantage of the introduced method for CT image-based strain calculation is the incorporation of particle rotation in the strain calculation. The strain calculation method was shown to produce more reliable strain results than a mesh-base method without considering the effects of particle rotations24.
Even with its many advantages, using X-ray micro CT to study the inter-particle contact evolution of granular soils may suffer from over-detection of inter-particle contacts. The accuracy of inter-particle detection results relies strongly on the spatial resolution of the X-ray micro-CT. This is due to the partial volume effect of the X-ray micro-CT, in which two isolated particles having a distance smaller than the size of a voxel may be identified as two contacting particles. Fortunately, the general trend of inter-particle contact evolution within granular soils was found to be unaffected by the over-detection of inter-particle contacts. Meanwhile, the inability to extract inter-particle contact forces within granular soils is another disadvantage of X-ray micro-CT compared to DEM studies43,44,45,46,47 and photo-elastic studies48,49. Furthermore, because of the above-mentioned CT image-based grain-scale investigation required to correctly identify and extract individual particles from CT images, the application of this method to soils with highly irregular particle shapes or highly crushable soils containing irregular intra-particle voids is very challenging.
In the future, in situ triaxial testing providing ample data on grain shape and grain kinematics will facilitate the incorporation of real particle shapes in DEM modeling. Subsequently, CT image-based DEM modeling will provide a better understanding of the grain-scale mechanical behavior of granular soils under loading. Meanwhile, given the ability to extract inter-particle contact forces50, a combination of X-ray diffraction with X-ray micro-CT for in situ triaxial testing will be helpful for the extraction of full grain-scale information (i.e., both grain kinematics and grain contact forces) from granular soils under shearing.
The authors have nothing to disclose.
This study was supported by the General Research Fund No. CityU 11213517 from the Research Grant Council of the Hong Kong SAR, Research Grant No. 51779213 from the National Science Foundation of China, and the BL13W beamline of the Shanghai Synchrotron Radiation Facility (SSRF).
Confining pressure offering device | GDS | STDDPC | |
De-aired water | N/A | N/A | Water de-aired in the lab |
Leighton Buzzard sand | Artificial Grass Cambridge | Drained Industrial Sand 25 kg | Can be replaced with different soils |
Miniature triaxial loading device | N/A | N/A | The miniature loading device is specially fabricated by the authors |
Silicon grease | RS company | RS 494-124 | |
Synchrotron radiation X-ray micro CT setup | Shanghai Synchrotron Radiation Facility Center (SSRF) | 13W1 | The triaxial testing is carried out at the BL13W beam-line of the SSRF |
Vacuum pump | Hong Kong Labware Co., ltd. | Rocker 300 |