2012
DOI: 10.1007/s11069-012-0252-z
|View full text |Cite
|
Sign up to set email alerts
|

Evaluation of soil collapse potential in regional scale

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
4
1

Citation Types

0
11
0

Year Published

2017
2017
2021
2021

Publication Types

Select...
8
1

Relationship

0
9

Authors

Journals

citations
Cited by 19 publications
(17 citation statements)
references
References 33 publications
0
11
0
Order By: Relevance
“…ere were six survey lines in total (Figure 3), and each survey line was 15 m in length (Table 1). A total of 28 deep markers were laid out in the 6 survey lines, and there were 5 deep markers for survey lines IV, V, VII and IX, while 4 e deep marker (Figure 4) consisted of several mechanically connected galvanized pipes and a 60 mm diameter iron base plate welded vertically. And the location of the subbase reflects the subsidence of the soil beneath it.…”
Section: Test Pit Design and Survey Point Layoutmentioning
confidence: 99%
See 1 more Smart Citation
“…ere were six survey lines in total (Figure 3), and each survey line was 15 m in length (Table 1). A total of 28 deep markers were laid out in the 6 survey lines, and there were 5 deep markers for survey lines IV, V, VII and IX, while 4 e deep marker (Figure 4) consisted of several mechanically connected galvanized pipes and a 60 mm diameter iron base plate welded vertically. And the location of the subbase reflects the subsidence of the soil beneath it.…”
Section: Test Pit Design and Survey Point Layoutmentioning
confidence: 99%
“…When collapsible loess is wetted by water, the internal structure of the loess is destroyed under the joint action of self-weight stress or selfweight stress and external additional stress, and the strength of the loess decreases significantly [1][2][3]. When the remaining strength between loess units is insufficient to resist their stresses, the soil structure is rapidly disrupted, resulting in significant self-weight collapsible deformation of the soil [4][5][6].…”
Section: Introductionmentioning
confidence: 99%
“…Loess deposits cover 640000 km 2 , distributed mainly along the middle reaches of the Yellow River Valley, constituting one of the most important parts of the Chinese regional and physical geography and the Loess Plateau. Because of its collapse behavior and other associated geotechnical engineering issues, such as landslides, hydro-consolidation, and wetting-induced collapse, loess belongs to problematic soils and has been the subject of geotechnical research and practice since the 1960s [4][5][6][7][8][9][10][11][12][13][14]. Following the adoption of "the belt and road" strategy, infrastructure construction in the Loess Plateau will develop more vigorously.…”
Section: Introductionmentioning
confidence: 99%
“…Loess is the dominant soil in Northwest China, accounting for 72.4% of the total loess area in China. In addition, China introduced the conception of the "New Silk Road Economic Belt" in 2013, and most of the soil in this area is loess, which brings great opportunity and challenge to the construction of pile foundation in loess area [16][17][18][19][20][21]. When cast-in-place bored piles are used in loess area, the steel casing is usually used to stabilize the borehole wall or solve the slurry leakage problem of huge caves.…”
Section: Introductionmentioning
confidence: 99%