3.1 Contact modulus
The contact modulus between particles differs from the elastic modulus, which refers to the relationship between the contact force between particles and the amount of overlap between particles. In this section, the influence of the contact modulus on the macro-parameters of the samples is studied by setting different contact modulus for the samples, and the contact modulus is set as 300MPa, 600MPa, 900MPa and 1200MPa, respectively. Other granular mesoscopic parameters are shown in Table 2.
Table 2
Particle mesoscopic parameters
Anti-rotation coefficient
|
Friction coefficient
|
Stiffness ratio
|
0.4
|
0.4
|
2
|
The influence of the contact modulus on the stress-strain curve of the sample is shown in Fig. 4. It can be seen from Fig. 4 that with the continuous increase of the contact modulus, the initial elastic modulus also gradually increases because with the increase of the contact modulus, the tangential and normal stiffness of the particles will also increase. During the loading process, the contact force will also increase, and the elastic modulus will increase with the increase of the contact modulus under the same strain. The peak strength decreases gradually, and when the contact modulus increases to a certain value, the peak strength tends to be the same. Under the same confining pressure, the strain-softening degree of the sample decreases gradually with the increase of the contact modulus.
The coordination number is a micrometric parameter describing the contact number around particles, also known as the average contact number. Thornton [32] proposed that particles with less than two contact numbers bear no stress in the specimen. Excluding these coordination numbers, that is, the mechanical coordination number describes the mechanical property expression expressed by the soil skeleton as follows:
$${C}_{n}=\frac{2{N}_{c}-{N}_{s1}}{{N}_{s}-{N}_{s0}-{N}_{s1}}$$
4
In the formula, \({\text{N}}_{\text{c}}\)is the total number of contact samples, \({N}_{s1}\)and\({N}_{s0}\) are the number of particles whose contact numbers equal 1 and 0, respectively, and \({N}_{s}\)is the total number of particles.
Figure 5 describes the changes in mechanical coordination numbers under different confining pressures when the contact modulus is different. With strain development, the mechanical coordination numbers increase first and then gradually decrease and eventually become stable; under different confining pressures, the coordination numbers gradually decrease with the increase of contact modulus; meanwhile, the coordination numbers under coaxial strain increase with the increase of confining pressure. Compared with the stress-strain curve, it can be seen that the mechanical coordination number also begins to become stable at the corresponding strain point when the peak strength appears, indicating that the sample skeleton particles rearrange after the peak strength to obtain a more stable structure.
The relationship between macroscopic mechanical parameters and the contact modulus of soil under different confining pressures is shown in Fig. 6–7. As the contact modulus increases, the elastic modulus linearly increases, and the peak friction Angle linearly decreases. The elastic modulus and friction Angle can be obtained quickly by changing the contact modulus of particles during the calibration of sand soil, and the calibration efficiency can be improved.
3.2 Friction coefficient
The friction coefficient is a micrometric parameter to characterize the friction characteristics between particles. Under the confining pressure conditions of 100kPa, 300kPa and 500kPa, the friction coefficient is set as 0.2, 0.4, 0.6 and 0.8. Other microscopic parameters of particles are shown in Table 3. The influence of the friction coefficient on the macroscopic parameters of the sample is studied.
Table 3
Particle mesoscopic parameters
Anti-rotation coefficient
|
Contact modulus(Emod)
|
Stiffness ratio
|
0.4
|
0.3GPa
|
2
|
It can be seen from Fig. 8 that with the increasing friction coefficient, the peak strength also increases. This can be explained by the fact that with the increase of the friction coefficient, the occlusion between the particles increases, and the stress required for the particles to slide is also greater, so the peak strength is increased. As can be seen from the observed figure, the degree of strain softening increases with the increasing friction coefficient, and the slope of the curve decreases with the increase of confining pressure under the same friction coefficient.
Figure 9 describes the relationship between the mechanical coordination number and the friction coefficient of the sample under the confining pressure of 100kPa, 300kPa and 500kPa. It can be seen from the figure that the mechanical coordination number firstly increases, then decreases and finally tends to be stable with the increase of strain. With the increase of the friction coefficient, the stable value of the mechanical coordination number gradually decreases, which is because the increase of the friction coefficient increases the biting force between the particles, making it more difficult for the particles to generate relative movement and then produce a larger contact force between the particles. The efficiency of the transmission force is higher, and the contact number is less.
The relationship between macroscopic mechanical parameters and the friction coefficient of soil under different confining pressures is shown in Fig. 10–11. As the friction coefficient increases, the elastic modulus and the peak friction Angle show an increasing trend. When calibrating sand soil, the target elastic modulus can be quickly obtained by adjusting the friction coefficient to improve the calibration speed.
3.3 Stiffness ratio
The stiffness ratio refers to the ratio of normal stiffness and tangential stiffness. Under the conditions of confining pressure of 100kPa, 300kPa and 500kPa, the stiffness ratio is set as 2,6,10,14, respectively. Other microscopic parameters of particles are shown in Table 4 to study the influence of stiffness ratio on the macroscopic parameters of samples.
Table 4
Particle mesoscopic parameters
Anti-rotation coefficient
|
Contact modulus(Emod)
|
Friction coefficient
|
0.4
|
0.3GPa
|
0.4
|
It can be seen from Fig. 12 that with the increasing stiffness ratio, the slope gradually decreases; that is, the initial elastic modulus gradually decreases. This is because when the stiffness comparison is small when the normal stiffness is similar to the tangential stiffness, the sample has higher tangential deformation resistance, smaller particle displacement, larger overlap, and greater elastic modulus due to the change of axial stress. The degree of strain softening decreases with the increase in stiffness ratio. Moreover, the peak strength becomes smaller; that is, the tangential stiffness gradually decreases, which reduces the tangential resistance to deformation of the material and causes the specimen to gradually change from shear failure to tangential failure. The stress-strain curves all show a downward trend after the peak strength, showing a strain softening trend, and under higher confining pressure, the strain softening trend is more obvious.
Fig. 13-15 shows the changes in mechanical coordination number with stiffness ratio under confining pressure of 100kPa, 300kPa and 500kPa, and the trend of first increasing, then decreasing, and finally stabilizing with the development of shear strain, that is, the number of particle contacts changes from less to more and then to less. Samples under low confining pressure are more stable after reaching peak strength than those under high confining pressure.
Fig. 14-15 shows the relationship between macroscopic coefficients and microscopic parameters of the samples. It can be seen from the figure that both the elastic modulus and friction Angle of the samples show a linear trend of decrease with the increase of the stiffness ratio, and the changes of the elastic modulus and friction Angle under low confining pressure are lower than those under high confining pressure.
3.4 Anti-rotation coefficient
Under the confining pressure of 100kPa, 300kPa and 500kPa, the anti-rotation coefficients were set as 0.2, 0.4, 0.6 and 0.8, respectively. Other granular mesoscale parameters were shown in Table 5 to study the influence of anti-rotation coefficients on the macro-parameters of the samples.
Table 5
Particle mesoscopic parameters
Stiffness ratio
|
Contact modulus(Emod)
|
Friction coefficient
|
2
|
0.3GPa
|
0.4
|
The anti-rotation coefficient will significantly affect the peak strength of the sample. As can be seen from Fig. 16, with the increase of the anti-rotation coefficient, the resistance to be overcome by the relative rotation of the particles becomes larger, and the peak strength of the sample gradually increases. However, it can be observed that the increased range is decreasing continuously; that is, the coefficient value has an effect range, within which the peak strength and residual strength will increase with the increase of the anti-rotation coefficient. The increased range will become smaller and smaller. At the same time, the stress-strain curve will remain unchanged after the threshold because the increase of the anti-rotation coefficient leads to relatively large particle rotation resistance and small particle rotation. The strain-softening tendency of the sample increases with the increase of the anti-rotation coefficient, and the strain-softening conforms to the properties of medium-dense sand.
Figure 17 shows the relationship between the anti-rotation coefficient and the mechanical coordination number. It can be seen from the figure that with the increase of the anti-rotation coefficient, the stable value of the mechanical coordination number will decrease accordingly. As the rotational impedance makes it more difficult for the particles to rotate, the contact force between the particles increases, and the effective contact decreases.
Fig. 18-19 shows the relationship between macroscopic coefficients and microscopic parameters of the sample. It can be seen from the figure that both the elastic modulus and friction Angle of the sample tend to increase with the increase of the stiffness ratio.