TY - JOUR
T1 - Strength and deformation behavior of the Yellow River silt under triaxial drained condition considering characteristic states
AU - Chen, Yu yuan
AU - Wang, Yu ke
AU - Hazarika, Hemanta
AU - Wan, Yong shuai
N1 - Funding Information:
The work present in this paper was supported by National Natural Science Foundation of China (Grant Nos. 52178369; 52109140); Key Projects of High Schools of Henan province of China (20A560021); Natural Science Foundation of Henan Province of China (202300410424); Youth Talent Promotion Project of Henan Province of China (2021HYTP016); Key Specialized Research and Development Breakthrough in Henan Province of China (212102310977); China Postdoctoral Science Foundation (2019M662533).
Publisher Copyright:
© 2023, Science Press, Institute of Mountain Hazards and Environment, CAS and Springer-Verlag GmbH Germany, part of Springer Nature.
PY - 2023/1
Y1 - 2023/1
N2 - Currently, the application of the Yellow River silt in subgrade, especially in expressway subgrade, has not been widely promoted. The main reason is that the research on the mechanical characteristics of the Yellow River silt used for subgrade filling is extremely limited. In this study, the static shear test of the Yellow River silt under drained condition was carried out using Global Digital Systems (GDS) triaxial apparatus, and the effects of confining pressure, relative density and shear rate on the strength and deformation behavior of the Yellow River silt were investigated. The cohesive force of the Yellow River silt is low, and the friction angle is the main factor determining the shear strength. Friction angle at phase transformation state φpt, friction angle at peak state φps, friction angle at critical state φcs, were obtained via the observation on the evolution law of mobilized friction angle during the whole shearing process. The friction angles corresponding to three different characteristic states have the following magnitude relationship, namely φps > φcs > φpt. The strength parameters for low-grade subgrade and highgrade subgrade were chosen to be 29.33° and 33.75°. The critical state line (CSL), envelop of phase transformation (EOP), and envelop of dilatancy (EOD) for three different characteristic states were determined. The critical stress ratio M, the phase transformation stress ratio Mpt and the dilatancy stress ratio Md of the Yellow River silt are 1.199, 1.235, 1.152, respectively. These results provide a basis for the mechanical analysis of the Yellow River silt subgrades and the subsequent establishment of dynamic constitutive model of the Yellow River silt.
AB - Currently, the application of the Yellow River silt in subgrade, especially in expressway subgrade, has not been widely promoted. The main reason is that the research on the mechanical characteristics of the Yellow River silt used for subgrade filling is extremely limited. In this study, the static shear test of the Yellow River silt under drained condition was carried out using Global Digital Systems (GDS) triaxial apparatus, and the effects of confining pressure, relative density and shear rate on the strength and deformation behavior of the Yellow River silt were investigated. The cohesive force of the Yellow River silt is low, and the friction angle is the main factor determining the shear strength. Friction angle at phase transformation state φpt, friction angle at peak state φps, friction angle at critical state φcs, were obtained via the observation on the evolution law of mobilized friction angle during the whole shearing process. The friction angles corresponding to three different characteristic states have the following magnitude relationship, namely φps > φcs > φpt. The strength parameters for low-grade subgrade and highgrade subgrade were chosen to be 29.33° and 33.75°. The critical state line (CSL), envelop of phase transformation (EOP), and envelop of dilatancy (EOD) for three different characteristic states were determined. The critical stress ratio M, the phase transformation stress ratio Mpt and the dilatancy stress ratio Md of the Yellow River silt are 1.199, 1.235, 1.152, respectively. These results provide a basis for the mechanical analysis of the Yellow River silt subgrades and the subsequent establishment of dynamic constitutive model of the Yellow River silt.
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U2 - 10.1007/s11629-021-7289-y
DO - 10.1007/s11629-021-7289-y
M3 - Article
AN - SCOPUS:85146596327
SN - 1672-6316
VL - 20
SP - 273
EP - 284
JO - Journal of Mountain Science
JF - Journal of Mountain Science
IS - 1
ER -