2012
DOI: 10.1007/s10706-011-9489-7
|View full text |Cite
|
Sign up to set email alerts
|

Re-examination of Undrained Strength at Atterberg Limits Water Contents

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

1
22
0
3

Year Published

2012
2012
2021
2021

Publication Types

Select...
7
1

Relationship

0
8

Authors

Journals

citations
Cited by 60 publications
(30 citation statements)
references
References 38 publications
1
22
0
3
Order By: Relevance
“…Although usually quite sharp for a given material, undrained strength-liquidity index correlations can also vary widely between geomaterials since the strengths mobilised at the Casagrande LL and PL states are not unique (Haigh et al, 2013;Nagaraj et al, 2012;O'Kelly, 2013c). This is compounded by general difficulties in measuring and interpreting consistency limit values for organic soils (O'Kelly, 2013a(O'Kelly, , 2013b(O'Kelly, , 2014a(O'Kelly, , 2016bO'Kelly and Zhang, 2013).…”
Section: With Liquidity Indexmentioning
confidence: 99%
See 1 more Smart Citation
“…Although usually quite sharp for a given material, undrained strength-liquidity index correlations can also vary widely between geomaterials since the strengths mobilised at the Casagrande LL and PL states are not unique (Haigh et al, 2013;Nagaraj et al, 2012;O'Kelly, 2013c). This is compounded by general difficulties in measuring and interpreting consistency limit values for organic soils (O'Kelly, 2013a(O'Kelly, , 2013b(O'Kelly, , 2014a(O'Kelly, , 2016bO'Kelly and Zhang, 2013).…”
Section: With Liquidity Indexmentioning
confidence: 99%
“…Undrained strength against water content correlations for municipal sludge and residue materials: (a) bilinear axes, (b) semi-logarithmic plot and (c) bilogarithmic plots content, with such relationships often incorporating measured LL and PL values in the calculations, with the main ones reviewed by O'Kelly (2013c). Many of them assume a 100-fold strength variation between the water content values corresponding to the LL and PL conditions, but as O'Kelly (2013c) emphasised, there is no theoretical basis for this, with the ratio of the strengths mobilised at the PL and LL conditions varying over a wide range when many different soils are considered (Haigh et al, 2013;Nagaraj et al, 2012;O'Kelly, 2013cO'Kelly, , 2015b. This is particularly true for organic soils, including the municipal water/wastewater sludge and residue materials under consideration in this paper, for which the ratio of the strengths mobilised at the PL and LL has been found to be significantly less than 100 (O'Kelly, 2013c(O'Kelly, , 2014a(O'Kelly, , 2014b(O'Kelly, , 2015b(O'Kelly, , 2016bZentar et al, 2009).…”
mentioning
confidence: 99%
“…To accomplish this, a Table 1. Undrained shear strengths (s u ) at liquid limit (adapted from Kayabali andTufenkci, 2010 andNagaraj et al, 2012 bulk soil sample was mixed with fine sand and commercial powdered bentonite at varying drymass ratios. The final product of this procedure is 60 soil samples with liquid limits ranging from about 30 to 120, which covers the plasticity range of most soils on earth.…”
Section: Methodsmentioning
confidence: 99%
“…The variation of the s u with the water content has been well-documented in the geotechnical literature. A brief summary of such studies was provided by Nagaraj et al (2012).…”
Section: Introductionmentioning
confidence: 99%
“…3, the strength gain factor (R MW ) for the traditionally defined plastic range is generally significantly different (and more often than not substantially less) than the assumed 100-fold increase. Prakash (2005) and Nagaraj et al (2012) cautioned against assigning a fixed strength value at PL. As explained in Haigh et al (2013), the assumption of a 100-fold factor increase derives from the following passage in Schofield & Wroth (1968), who were examining the data of Skempton & Northey (1952) (shown in Fig.…”
Section: Strength-based Approachesmentioning
confidence: 99%