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    Cyclic Degradation and Pore-Water Pressure Response of High-Plasticity Compacted Clay

    Source: Journal of Geotechnical and Geoenvironmental Engineering:;2021:;Volume ( 147 ):;issue: 011::page 04021113-1
    Author:
    Naman Kantesaria
    ,
    Ajanta Sachan
    DOI: 10.1061/(ASCE)GT.1943-5606.0002630
    Publisher: ASCE
    Abstract: This experimental study focused on cyclic degradation and cyclic pore-water pressure response of high-plasticity compacted clay under different dynamic loading and initial static shear stress conditions. The strain-controlled undrained cyclic simple shear tests were performed at different initial static shear stress ratios (τs/Su=0, 0.45, 0.65, 0.79, and 0.87), cyclic strain amplitudes (γc=0.5%, 1.5%, 2.5%, and 3.75%), and frequencies (f=0.1, 0.5, 1, and 2 Hz). The results revealed that the initial static shear stress significantly increased the magnitude and rate of stiffness degradation and cyclic pore-water pressure generation. The mobilized shear stress under cyclic loading decreased below the static shear strength within only five loading cycles. The shear modulus increased and the damping ratio decreased with the increase in frequency and decrease in cyclic strain amplitude. The enhanced rate of stiffness degradation followed a power-law functional relationship with cyclic strain amplitude, and its trend was dependent on the magnitude of the initial static shear stress ratio and the cyclic strain-reversal conditions. The experimental results clearly demonstrated the coupling between cyclic degradation and pore-water pressure generation. A strain-based model was formulated for the risk assessment of compacted high-plasticity clay (CH soil) subjected to combined static and cyclic loading.
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      Cyclic Degradation and Pore-Water Pressure Response of High-Plasticity Compacted Clay

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    contributor authorNaman Kantesaria
    contributor authorAjanta Sachan
    date accessioned2022-02-01T21:55:59Z
    date available2022-02-01T21:55:59Z
    date issued11/1/2021
    identifier other%28ASCE%29GT.1943-5606.0002630.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4272313
    description abstractThis experimental study focused on cyclic degradation and cyclic pore-water pressure response of high-plasticity compacted clay under different dynamic loading and initial static shear stress conditions. The strain-controlled undrained cyclic simple shear tests were performed at different initial static shear stress ratios (τs/Su=0, 0.45, 0.65, 0.79, and 0.87), cyclic strain amplitudes (γc=0.5%, 1.5%, 2.5%, and 3.75%), and frequencies (f=0.1, 0.5, 1, and 2 Hz). The results revealed that the initial static shear stress significantly increased the magnitude and rate of stiffness degradation and cyclic pore-water pressure generation. The mobilized shear stress under cyclic loading decreased below the static shear strength within only five loading cycles. The shear modulus increased and the damping ratio decreased with the increase in frequency and decrease in cyclic strain amplitude. The enhanced rate of stiffness degradation followed a power-law functional relationship with cyclic strain amplitude, and its trend was dependent on the magnitude of the initial static shear stress ratio and the cyclic strain-reversal conditions. The experimental results clearly demonstrated the coupling between cyclic degradation and pore-water pressure generation. A strain-based model was formulated for the risk assessment of compacted high-plasticity clay (CH soil) subjected to combined static and cyclic loading.
    publisherASCE
    titleCyclic Degradation and Pore-Water Pressure Response of High-Plasticity Compacted Clay
    typeJournal Paper
    journal volume147
    journal issue11
    journal titleJournal of Geotechnical and Geoenvironmental Engineering
    identifier doi10.1061/(ASCE)GT.1943-5606.0002630
    journal fristpage04021113-1
    journal lastpage04021113-19
    page19
    treeJournal of Geotechnical and Geoenvironmental Engineering:;2021:;Volume ( 147 ):;issue: 011
    contenttypeFulltext
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