TY - JOUR
T1 - Cyclic Response and Reconsolidation Volumetric Strain of Sand under Repeated Cyclic Shear Loading Events
AU - Le, Trung Tri
AU - Park, Sung Sik
AU - Woo, Seung Wook
N1 - Publisher Copyright:
© 2022 American Society of Civil Engineers.
PY - 2022/12/1
Y1 - 2022/12/1
N2 - Many regions of the world have witnessed repeated earthquakes that have caused repeated liquefaction of soil. Therefore, the effect of repeated earthquakes on the dynamic behavior of soil is an important aspect that must be considered. In this study, a series of cyclic shear loading events and consolidation phases was repeated for loose sand to investigate the cyclic stress-strain response and postcyclic reconsolidation volumetric strain that are usually induced by repeated earthquakes. After an initial consolidation, samples were subjected to repeated cyclic shear loading events and subsequent reconsolidations in a cyclic direct simple shear (CDSS) device with various cyclic stress ratios (CSRs) under undrained conditions for nonliquefied and liquefied stages. Based on the test results, the number of cyclic shear events (Nev), built-up excess pore water pressure ratio (ru), CSR, and maximum double amplitude shear strain (γmaxDA) were shown to be the factors influencing the behavior of samples. For the samples that were not subjected to any prior liquefaction stage, the reliquefaction resistance continuously increased as Nev increased. For those subjected to repeated liquefaction, the samples presented cyclic liquefaction accompanied by high flow shear strain in the first event. The reliquefaction resistance drastically decreased in the second cyclic shear loading event as a result of the critical anisotropy induced by the first cyclic shear loading event when the contraction tendency prevailed. The samples showed cyclic mobility behavior from the fourth event onward, corresponding to the predominance of the dilation tendency. The obtained γmaxDA and ϵrcV increased as CSR and/or ru increased and decreased as Nev increased. The relative density (Dr) was not a major factor affecting the reliquefaction resistance; however, it might have promoted a lower induced anisotropy level, lower induced γmaxDA, lower ϵrcV, and the change in behavior of samples from cyclic liquefaction (contraction tendency) to cyclic mobility (dilation tendency). A higher contraction tendency in samples resulted in a higher γmaxDA and ϵrcV. The shear strain induced in the immediate-past cyclic shear loading event was found to be the main factor affecting ϵrcV. From the γmaxDA-ϵrcV relationship, two separate zones were observed, namely (1) noninduced flow shear strain; and (2) induced flow shear strain, regardless of CSR and Nev. Additionally, a relationship between γmaxDA and ϵrcV was proposed for practical applications.
AB - Many regions of the world have witnessed repeated earthquakes that have caused repeated liquefaction of soil. Therefore, the effect of repeated earthquakes on the dynamic behavior of soil is an important aspect that must be considered. In this study, a series of cyclic shear loading events and consolidation phases was repeated for loose sand to investigate the cyclic stress-strain response and postcyclic reconsolidation volumetric strain that are usually induced by repeated earthquakes. After an initial consolidation, samples were subjected to repeated cyclic shear loading events and subsequent reconsolidations in a cyclic direct simple shear (CDSS) device with various cyclic stress ratios (CSRs) under undrained conditions for nonliquefied and liquefied stages. Based on the test results, the number of cyclic shear events (Nev), built-up excess pore water pressure ratio (ru), CSR, and maximum double amplitude shear strain (γmaxDA) were shown to be the factors influencing the behavior of samples. For the samples that were not subjected to any prior liquefaction stage, the reliquefaction resistance continuously increased as Nev increased. For those subjected to repeated liquefaction, the samples presented cyclic liquefaction accompanied by high flow shear strain in the first event. The reliquefaction resistance drastically decreased in the second cyclic shear loading event as a result of the critical anisotropy induced by the first cyclic shear loading event when the contraction tendency prevailed. The samples showed cyclic mobility behavior from the fourth event onward, corresponding to the predominance of the dilation tendency. The obtained γmaxDA and ϵrcV increased as CSR and/or ru increased and decreased as Nev increased. The relative density (Dr) was not a major factor affecting the reliquefaction resistance; however, it might have promoted a lower induced anisotropy level, lower induced γmaxDA, lower ϵrcV, and the change in behavior of samples from cyclic liquefaction (contraction tendency) to cyclic mobility (dilation tendency). A higher contraction tendency in samples resulted in a higher γmaxDA and ϵrcV. The shear strain induced in the immediate-past cyclic shear loading event was found to be the main factor affecting ϵrcV. From the γmaxDA-ϵrcV relationship, two separate zones were observed, namely (1) noninduced flow shear strain; and (2) induced flow shear strain, regardless of CSR and Nev. Additionally, a relationship between γmaxDA and ϵrcV was proposed for practical applications.
KW - Induced anisotropy
KW - Induced shear strain
KW - Postcyclic settlement
KW - Reconsolidation
KW - Reliquefaction
KW - Repeated earthquakes
UR - http://www.scopus.com/inward/record.url?scp=85139510728&partnerID=8YFLogxK
U2 - 10.1061/(ASCE)GT.1943-5606.0002919
DO - 10.1061/(ASCE)GT.1943-5606.0002919
M3 - Article
AN - SCOPUS:85139510728
SN - 1090-0241
VL - 148
JO - Journal of Geotechnical and Geoenvironmental Engineering - ASCE
JF - Journal of Geotechnical and Geoenvironmental Engineering - ASCE
IS - 12
M1 - 04022109
ER -