Abstract
Particle breakage is a theme of great focus on affecting the behavior of granular soil. This paper presents an experimental investigation on the influence of particle breakage on the isotropic compressibility of the precrushed sands using a number of drained isotropic consolidation tests. Particle breakage resulted in movement of the compression lines followed by the rebound lines towards a decrease in the void ratio, implying that particle breakage caused a more contractive soil. Particle breakage impaired the bulk deformation modulus by increasing the compression coefficient for the compression behavior of the precrushed sands, but showed a complex effect on the bulk deformation modulus and rebound coefficient for the rebound behavior of the precrushed sands. However, particle breakage caused an increase in the compression indexes of the precrushed sands but showed a complex effect on the rebound indexes of the precrushed sands. In the e−p′ plane and the e−logp′ plane, the compression lines and rebound lines of the precrushed sands were curved. A generalized model was proposed to straighten the compression and rebound lines of the precrushed sands in the e − (p′/pa)α plane. Particle breakage resulted in a general rotation and translation of the linear compression and rebound lines of the precrushed sands in the e−(p′/pa)α plane. The critical state line and isotropic consolidation line on the loosest state of silica sand no. 5 were curved in the e−logp′ plane but straightened in the e − p′α=0.7 plane. In the e− p′α=0.7 plane, a reasonable linear critical state line of silica sand no. 5 was proposed by adjusting it to match the isotropic consolidation line on the loosest state.
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Abbreviations
- a c :
-
Compression coefficient of soil
- a r :
-
Rebound coefficient of soil
- a i :
-
Compression or rebound coefficient of soil, subscript i=c or r
- B r :
-
Relative breakage of soil, Br = Bt/Bp (Hardin 1985)
- B p :
-
Breakage potential of soil (Hardin 1985)
- B t :
-
Total breakage of soil (Hardin 1985)
- CSL:
-
Critical state line of soil
- ICL:
-
Isotropic consolidation line of soil
- C co :
-
Coefficient of curvature of soil
- C i :
-
Compression or rebound index of soil, subscript i=c or r
- C c :
-
Compression index of soil
- C r :
-
Rebound index of soil
- C u :
-
Coefficient of uniformity of soil
- e :
-
Void ratio of soil
- e0 :
-
Initial void ratio of soil
- e max :
-
Maximum void ratio of soil
- e min :
-
Minimum void ratio of soil
- F c :
-
Fines content of soil (%)
- G s :
-
Specific gravity of soil particles
- K 0 :
-
Initial consolidated stress ratio
- K i :
-
Bulk deformation modulus of soil, subscript i=c or r
- K c :
-
Bulk deformation modulus for compression response of soil
- K r :
-
Bulk deformation modulus for rebound response of soil
- p a :
-
A reference pressure
- p′ :
-
Mean effective stress of soil
- SP:
-
Poorly-graded sand (JGS 0051 2015)
- σ c0 :
-
Initial confining stress
- α :
-
A model constant of soil
- λ :
-
A model constant of soil
- Δe :
-
Difference in the void ratio e of soil
- Δe i :
-
Difference in the void ratio e of soil at the i condition
- Δ(i):
-
Difference in the (i), i=(p′/pa), log(p′/pa) or (p′/pa)α
- dε v :
-
Volumetric strain increment of soil
- dp′ :
-
Mean effective stress increment of soil
- Λ:
-
A set of constants of soil
- C A:
-
set of constants of soil
- f():
-
Function of relative breakage Br and a set of constants of soil Λ
- g():
-
Function of relative breakage Br and a set of constants of soi C
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Acknowledgements
This work was supported by the National Natural Science Foundation of China (Grant no. 41807268) and the Youth Innovation Promotion Association of the Chinese Academy of Sciences — China (Grant no. 2018408). A special acknowledgement should be expressed to the Geotechnical Engineering Laboratory of the University of Tokyo, Japan that supported the implementation of the tests in this paper.
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Yu, Fw., Su, Lj. & Peng, Xz. Influence of particle breakage on the isotropic compressibility of sands. J. Mt. Sci. 19, 2086–2099 (2022). https://doi.org/10.1007/s11629-022-7390-x
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DOI: https://doi.org/10.1007/s11629-022-7390-x