2020
DOI: 10.1007/s11771-020-4290-5
|View full text |Cite
|
Sign up to set email alerts
|

3D stability assessment of stepped slopes in inhomogeneous soils

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1

Citation Types

0
3
0

Year Published

2020
2020
2024
2024

Publication Types

Select...
6
1

Relationship

0
7

Authors

Journals

citations
Cited by 13 publications
(3 citation statements)
references
References 22 publications
0
3
0
Order By: Relevance
“…It can be seen from Figure 9 that from 14 August 2018 and 9 November 2019, a total of four rockfall disasters occurred at the wide cracks on the surface of the slope; the overall deformation of the slope was small with a maximum value of 0.183 m and occurred at the middle of the wide tension crack in the upper part of the slope. According to Li et al [13] and Li et al [56], the slope will continue to maintain a stable state without special inducing factors such as earthquake, heavy rainfall, and artificial excavation.…”
Section: Calculation Resultsmentioning
confidence: 99%
“…It can be seen from Figure 9 that from 14 August 2018 and 9 November 2019, a total of four rockfall disasters occurred at the wide cracks on the surface of the slope; the overall deformation of the slope was small with a maximum value of 0.183 m and occurred at the middle of the wide tension crack in the upper part of the slope. According to Li et al [13] and Li et al [56], the slope will continue to maintain a stable state without special inducing factors such as earthquake, heavy rainfall, and artificial excavation.…”
Section: Calculation Resultsmentioning
confidence: 99%
“…According to the analysis, this action was due to the large number of polar groups in GO, which occurred due to the hydrogen bonds in GO, SA, and AKP . These hydrogen bonds absorbed within a certain wave‐number range . To explore and regulate the effect of the hydrogen bonds in the SA–AKP composite system after different mass fractions of GO were added, the broad peak at 3000–3700 cm −1 was smoothed, and the peak area ratio (i.e., the ratio of different types of hydrogen bonds) was calculated after we subtracted the straight line and the Gauss peak fitting of the peak analyzer.…”
Section: Resultsmentioning
confidence: 99%
“…The geological body formed by combining the intermediate bridge and slope of an adjacent open pit has a special spatial shape and structure as well as a significant 3D effect. Currently, the 2D limit equilibrium method is widely used for analyzing slope stability [10][11][12][13] , and the existing 3D limit equilibrium method is only limited to analyzing regular landslide mass stability [14][15][16][17] . However, it is difficult to quantitatively understand the stability of irregular slopes under the support effect of an intermediate bridge in adjacent open pits.…”
Section: Introductionmentioning
confidence: 99%