scholarly journals Validation of an elastoplastic model to predict secant shear modulus of natural soils by experimental results

Author(s):  
A Gomes Correia ◽  
J Santos ◽  
F Lopez-Caballero ◽  
R Carrilho Gomes ◽  
A Modaressi
2015 ◽  
Vol 20 (2) ◽  
pp. 609-622 ◽  
Author(s):  
Rui Carrilho Gomes ◽  
Jaime A. Santos ◽  
Arézou Modaressi-Farahmand Razavi ◽  
Fernando Lopez-Caballero

1947 ◽  
Vol 14 (4) ◽  
pp. A281-A284
Author(s):  
Alice Winzer ◽  
W. Prager

Abstract In a recent paper A. A. Ilyushin drew attention to the remarkable simplicity which the theory of plastic deformation assumes when the secant shear modulus is taken as a power of the octahedral shearing stress. In the present paper Ilyushin’s results are discussed in connection with a specific example and it is shown that great caution is indicated in the use of such power laws.


2019 ◽  
Vol 56 (12) ◽  
pp. 1743-1755
Author(s):  
Hirofumi Toyota ◽  
Susumu Takada

Many reports describe overestimation of liquefaction resistance based on sounding data related to ground materials containing coarse particles such as gravel and cobbles. Better methods of liquefaction potential estimation must be developed using investigation data other than those from sounding. Gathering perfect and undisturbed samples is difficult, but using seismic methods such as PS logging might be effective for assessing liquefaction potential. For this study, bender element (BE) tests and local small strain (LSS) tests were conducted, respectively, to measure the dynamic and static shear moduli of gravel – mixed sand specimens. Subsequently, relations between liquefaction strength and secant shear moduli were examined to provide reliable estimation of liquefaction in gravel – mixed sand. Although the liquefaction resistance increased considerably with overconsolidation, the initial shear modulus exhibited only a slight change with the same overconsolidation. The experimentally obtained results elucidated that the important shear strain level, for which secant shear modulus has a strong relation with liquefaction strength, was not a linear elastic region of 0.001%: it was about 0.01%.


In this chapter, the obtained experimental results are presented and analyzed from the thermal experiments that have been achieved on the different samples of natural soils. These soils can be used as backfill soil in buried cables. The obtained results are used to study the drying out phenomena and its effects on the cable insulation. These experiments study the temperature against heat flux density at infinity Pf value and the specification of the soil. An instrument simulates a real power buried cable is used. This apparatus was described in chapter five in detail.


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