Ou ZOU, Jian XUE, Na LI, Xin WANG, Rong YANG, Yuqiong LI. Inversion method of soil Mohr-Coulomb parameters based on dynamic cavity expansion model[J]. Optics and Precision Engineering, 2023, 31(5): 565

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- Optics and Precision Engineering
- Vol. 31, Issue 5, 565 (2023)

Fig. 1. Penetrometer and spherical cavity expansion model
![Relationship between penetration resistance Fz and penetration speed square Vz2 [25]](/richHtml/gxjmgc/2023/31/5/565/img_2.jpg)

Fig. 3. Images of surfaces Π 1 and Π 2

Fig. 4. Intersection lines l 1 and l 2 and their intersection point under λ ≠0 and λ ≠3/4

Fig. 5. Lines L 1 and L 2 when λ =3/4 or λ =0
![Relationship between shear strength and average stress[25]](/Images/icon/loading.gif)
Fig. 6. Relationship between shear strength and average stress[25]

Fig. 7. Fitting of the resistance coefficients based on acceleration and velocity curves

Fig. 8. Image of the function f (β's ) and the relationship between penetration depth and initial speed

Fig. 9. Solution domain determined by dynamic cavity expansion model
![Influence of the fitting interval on the inversion results of C and φ[25]](/Images/icon/loading.gif)
![Acceleration curve and the time interval corresponding to the penetration instrument entering different soil layers[25]](/Images/icon/loading.gif)
Fig. 11. Acceleration curve and the time interval corresponding to the penetration instrument entering different soil layers[25]
![Influence of parameters E and η* on the inversion results of C and φ, respectively, where αs=101.48 kN and βs=1.87 kg/m (using the velocity curve[25])](/Images/icon/loading.gif)
Fig. 12. Influence of parameters E and η * on the inversion results of C and φ , respectively, where αs =101.48 kN and βs =1.87 kg/m (using the velocity curve[25])
![Influence of parameters E and η* on the inversion results of C and φ, respectively, where αs=276.92 N and βs=0.30 kg/m (using the penetration depth-initial velocity data[31])](/Images/icon/loading.gif)
Fig. 13. Influence of parameters E and η * on the inversion results of C and φ , respectively, where αs =276.92 N and βs =0.30 kg/m (using the penetration depth-initial velocity data[31])
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Table 1. Soil parameters of Forrestal's experiments[25]
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Table 2. Soil parameters of He Xiang’s experiments[31]
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Table 3. Results of He Xiang’s penetration experiments[31]
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Table 4. Calculation results of the 27 data sets

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