2020
DOI: 10.1007/s12665-020-08933-4
|View full text |Cite
|
Sign up to set email alerts
|

Failure characteristics of sandstone specimens with randomly distributed pre-cracks under uniaxial compression

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
4
1

Citation Types

0
10
0

Year Published

2021
2021
2023
2023

Publication Types

Select...
6

Relationship

2
4

Authors

Journals

citations
Cited by 26 publications
(10 citation statements)
references
References 45 publications
0
10
0
Order By: Relevance
“…The contact bond reflects the normal and tangential interactions (forces) between particles (see Figure 2(a)), while the parallel bond transmits both the force and the moment (see Figure 2(b)). It is widely accepted that these two kinds of bonds both exist in the interior of rock and soil [7], so they are used in this paper.…”
Section: Numerical Model Of Cracked Sandstone Specimenmentioning
confidence: 99%
See 4 more Smart Citations
“…The contact bond reflects the normal and tangential interactions (forces) between particles (see Figure 2(a)), while the parallel bond transmits both the force and the moment (see Figure 2(b)). It is widely accepted that these two kinds of bonds both exist in the interior of rock and soil [7], so they are used in this paper.…”
Section: Numerical Model Of Cracked Sandstone Specimenmentioning
confidence: 99%
“…The basin sediments are about 100~200 m thick and are of continuous transversal cycles, consisting of beds about 2 m thick. The cracks and joints there caused by the long-time affection of low temperature and ocean erosion have been extremely developed [4][5][6][7], as shown in Figure 1. The existence of cracks not only reduces the material strength of the rock but also accelerates the damage process, which poses safety hazards to the construction of slopes and underground projects [2,5,7,8].…”
Section: Introductionmentioning
confidence: 99%
See 3 more Smart Citations