1991
DOI: 10.1061/(asce)0733-9410(1991)117:4(540)
|View full text |Cite
|
Sign up to set email alerts
|

Stability Evaluation during Staged Construction

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

21
180
0
15

Year Published

2008
2008
2023
2023

Publication Types

Select...
4
4

Relationship

0
8

Authors

Journals

citations
Cited by 424 publications
(216 citation statements)
references
References 66 publications
21
180
0
15
Order By: Relevance
“…Furthermore, ðs u DSS =s 0 vc Þ NC is 0·46 for Booneschans fibrous peat and 0·47 for Uitdam sedge-reed peat (Zwanenburg and Jardine, 2015), with s u DSS =s 0 vc ¼ 0Á46 for Taylor River peat with w o = 500% (Foott and Ladd, 1981). These s u DSS =s 0 vc values are remarkably consistent and considerably greater than the range of 0·20-0·27 reported for NC clay or silt materials (Ladd, 1991). Other limited published s u DSS =s 0 vc data for Polish, Irish and Swedish peats (after Carlsten (2000), Farrell andHebib (1998), Farrell et al (1999) and Lechowicz (1994)) show much scatter in the range of 0·38-0·55.…”
Section: Geotechnical Research Volume 4 Issue Gr3supporting
confidence: 68%
See 1 more Smart Citation
“…Furthermore, ðs u DSS =s 0 vc Þ NC is 0·46 for Booneschans fibrous peat and 0·47 for Uitdam sedge-reed peat (Zwanenburg and Jardine, 2015), with s u DSS =s 0 vc ¼ 0Á46 for Taylor River peat with w o = 500% (Foott and Ladd, 1981). These s u DSS =s 0 vc values are remarkably consistent and considerably greater than the range of 0·20-0·27 reported for NC clay or silt materials (Ladd, 1991). Other limited published s u DSS =s 0 vc data for Polish, Irish and Swedish peats (after Carlsten (2000), Farrell andHebib (1998), Farrell et al (1999) and Lechowicz (1994)) show much scatter in the range of 0·38-0·55.…”
Section: Geotechnical Research Volume 4 Issue Gr3supporting
confidence: 68%
“…Correlating with consolidation stress leads to normalised undrained strength ratio, s u TC =s 0 vc , values ranging 0·47-0·78 for conventionally sized triaxial specimens of fibrous peats (see Table 2), indicating that significant strength gains are achieved with consolidation, compared with the typical range of 0·30-0·35 for NC clay and silt materials (Ladd, 1991). (Ajlouni, 2000), with s u TC defined at the phase transformation point on the ESP trace described earlier, whereas ðs u fTC =s 0 vc Þ NC values of 0·62 for CK 0 UC (see Figure 11), 0·61 for CIUC and 0·59 (±22%) for CIUC (Zwanenburg and Jardine, 2015) were deduced based on estimated s u fTC values for Marken peat, Booneschans fibrous peat and Uitdam sedge-reed peat materials, respectively, where s 0 vc is the vertical consolidation stress at the start of the compression stage in the CU TC tests.…”
Section: Cu Tc Testingmentioning
confidence: 98%
“…(Ladd, 1991). For SS tests, s u-SS /σ' v values vary from 0.38 to 0.55, with one point lying outside this range.…”
Section: Laboratory Testingmentioning
confidence: 97%
“…6. Undrained strength ratios were evaluated using the SHANSEP technique (Ladd, 1991) using triaxial testing, with the results shown in Figure 7. Those results were used to estimate pre-earthquake shear strengths beneath the affected structures, with the results in Figure 6.…”
Section: Laboratory Testingmentioning
confidence: 99%
“…Based on the ICU triaxial compression test results as indicated in Figure 7, the averaged undrained shear strength (s u ) of the upper 10 m clay is approximately 68 kPa. Considering the effects of anisotropy, the averaged undrained shear strength (s u-ave ) can be taken as 80% of the triaxial compression s u (Ladd, 1991), which is about 55 kPa. Using Vesic (1973) bearing capacity theory, the ultimate bearing capacity for the mat foundation is 350 kPa.…”
Section: Bearing Capacity Failure Potential Evaluationmentioning
confidence: 99%