Experimental study on strain rate effect of strength characteristics of unsaturated silty clay
Source abstract
Abstract
Strain rate is a key factor affecting the strength characteristics of soil. The intrinsic mechanism of the strain rate effect was investigated through a case study on unsaturated compacted silty clays, where triaxial tests with elven strain rates and six confining pressures ranging from 5×10−7∼1×10−3s−1 and 50∼400 kPa, respectively, were conducted. Then, the effects of strain rate on multiple strength and deformation parameters of the sample, including the stress-strain relationship, failure mode, peak strength, peak strain, and elastic modulus, were analyzed to clarify the inherent mechanism of the strain rate effect. The results showed that there were two types of critical strain rate values, which caused the peak strength to first decrease and then increase with strain rate under low confining pressures. However, under high confining pressures, the peak strength first followed the same trend as low confining pressure, but then it decreased with increased strain rate. Additionally, the elastic modulus increased monotonically with strain rate under low confining pressures, but while under high confining pressures it first decreased and then increased. Finally, linear functions and quadratic polynomials were derived to describe the effect of strain rate on the strength and deformation parameters of silty clay to facilitate engineering applications.
Source: openalex_inverted_index · Quality: baseline
Research context
OpenAlex topics: Soil and Unsaturated Flow · Geotechnical Engineering and Soil Mechanics · Landslides and related hazards
SciVX discovery tags are terminology-based. OpenAlex topics are source-provided classifications.
References (32)
Show source-provided references
1. James · 2005
2. Romer · 2018 · 9 · e00199
3. Long term performance of gravel base course layers in asphalt pavements
4. Progress and trend of experimental investigation on rate-dependent behavior of soft clays
5. Effects of strain rate on instability of granular soils
6. Strain-rate dependent stress-strain behavior of over-consolidated Hong Kong marine clay10.1139/t00-054 ↗
7. Rate-dependent undrained shear behavior of a resedimented clay10.1061/(ASCE)0733-9410(1996)122:2(99) ↗
8. Analysis of the shearing rate effect on anisotropic undrained strength of clays
9. Effect of strain rate on undrained shear strength of clays
10. Compression and shear test of structured clay
11. Effects of shear rate on mechanical behavior of structured loess
12. Loading rate effect on deformation and strength characteristics of undisturbed loess
13. Effects of shear strain rate on mechanical behavior of Zhanjiang strong structured clay
14. Fredlund · 1993
15. Strain-rate dependent behaviors of K0 consolidated clays
16. Various viscosity types of geomaterials in shear and their mathematical expression10.3208/sandf.48.41 ↗
17. Analysis of influence of shear rate on shear strength of sand under high stress
18. Zhang · 2014 · 1 · 74
19. Characteristic of triaxial compressive strength of grading macadam considering loading velocity
20. In-situ and laboratory stress-strain relationships10.1680/geot.1988.38.1.83 ↗
21. Ministry of construction, P.R. China · 2008
22. Mechanical characterization and parameter identification of geological deformation of subgrade compacted soil
23. Time-dependent shear deformation characteristics of geomaterials and their simulation10.3208/sandf.42.2_103 ↗
24. Viscosity coefficient of structural soft clay
25. Recent development of consolidation theories of unsaturated soils
26. Fredlund · 2012
27. Xie · 2015
28. Shear strength equations for unsaturated soil under drying and wetting10.1061/(ASCE)GT.1943-5606.0000261 ↗
29. Coupling of hydraulic hysteresis and stress–strain behavior in unsaturated soils10.1680/geot.2003.53.1.41 ↗
30. Static pore water pressure and excess pore water pressure-A discussion with Mr. CHEN Yu-jiong
31. Lu · 2012
32. Estimation of soil-water characteristics curves in mutiple-cycles using membrane and TDR systems10.3390/ma9121019 ↗