Sciences in Cold and Arid Regions ›› 2021, Vol. 13 ›› Issue (5): 450-462.doi: 10.3724/SP.J.1226.2021.21023.

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Study on mechanical properties of soil-rock mixture of various compactness subjected to freeze-thaw cycles

Zhong Zhou(),HaoHui Ding,WenYuan Gao,LinRong Xu   

  1. School of Civil Engineering, Central South University, Changsha, Hunan 410075, China
  • Received:2021-04-19 Accepted:2021-10-11 Online:2021-10-31 Published:2021-12-03
  • Contact: Zhong Zhou E-mail:369144091@qq.com

Abstract:

The soil-rock mixture, a collection of soil particles and rock blocks, is inherently heterogeneous and anisotropic due to significant particle size and material strength differences. This study conducts triaxial tests on soil-rock mixture samples of various compactness subjected to varying freeze-thaw cycles. A mesoscopic simulation is carried out by particle flow code (PFC) to analyze the effects of freeze-thaw cycles on the mechanical properties of soil and rock particles. The results show that the mechanical properties of the soil-rock mixture under freeze-thaw cycles are greatly affected by the initial compaction. In general, when the degree of compaction is higher, the influence of freeze-thaw cycles on the soil-rock mixture is greater. The stress-strain curves of the samples with different compactness demonstrate strain-softening behavior. The freeze-thaw cycles greatly influence the failure strength of the samples with a higher degree of compaction but have little impact on the samples with a lower degree of compaction. On the microscopic level, during freeze-thaw cycles, the pore volume in the highly compacted sample is too small to accommodate the volume expansion from ice crystal formation, causing significant strength loss among the soil and rock particles and deterioration of the macroscopic properties of the soil-rock mixture.

Key words: soil-rock mixtures, freeze-thaw cycle, degree of compaction, particle flow code

Figure 1

Particle size distribution of the soil rock mixture with 45% stone blocks"

Figure 2

Sample preparation"

Table 1

Relationship between dry density and moisture content of the soil-rock mixture by the compaction test"

Moisture contentDry density (g/cm3)
0.97%2.186
2.96%2.212
4.14%2.293
5.24%2.341
6.21%2.354
7.17%2.345
9.02%2.309

Figure 3

Large-scale triaxial apparatus and test sample"

Table 2

Key technical specifications of the TAJ-2000 triaxial apparatus"

Sample size

(mm)

Max axial load

(kN)

Max confining pressure (MPa)

Axial deformation

velocity (mm/min)

Max axial

displacement (mm)

Volume change measure range (mL)
Φ 300×6002,0005.00.01-10030010,000

Table 3

Summary of sample groups and testing parameters"

Sample groupNumber of freeze-thaw cyclesDegree of compactionConfining pressure
03610
1#1-11-21-31-487%50 kPa, 100 kPa, 200 kPa
2#2-12-22-32-490%
3#3-13-23-33-495%

Figure 4

Stress-axial strain curves from triaxial compression tests of samples with various compactness with or without freeze-thaw cycling"

Figure 5

Static strength of samples subjected to freeze-thaw cycles"

Table 4

Loss of static strength due to freeze-thaw cycles"

Relative compaction

Confining pressure

(kPa)

Static strength before freeze-thaw cycles

(kPa)

Static strength after ten

freeze-thaw cycles

(kPa)

Static strength loss ratio
87%5086.9978.719.51%
100115.50108.675.91%
200184.20175.791.85%
90%50108.6793.8113.67%
100145.71123.7815.05%
200224.40200.7710.53%
95%50220.99169.1023.48%
100304.56250.9617.60%
200518.97401.7722.58%

Figure 6

Modulus of elasticity of samples subjected to freeze-thaw cycles"

Figure 7

Variation in the cohesion with the number of freeze-thaw cycles"

Table 5

Cohesion of samples with different compactness"

Degree of compactionFreeze-thaw cyclesCohesion (kPa)Cohesion loss ratio
87%024.860.00%
320.2318.62%
618.3126.35%
1017.9527.80%
90%030.170.00%
325.8714.25%
625.0916.84%
1024.1819.85%
95%041.130.00%
336.9510.16%
635.4913.71%
1034.4316.29%

Figure 8

Variation in internal friction angle with the number of freeze-thaw cycles"

Table 6

Variation in internal friction angles of samples with different compactness and freeze-thaw cycles"

Degree of compactionFreeze-thaw cyclesInternal friction angle (kPa)Internal friction angle loss ratio
87%018.820.00%
315.9815.09%
614.5522.69%
1015.7316.42%
90%027.390.00%
321.6820.85%
618.4332.71%
1017.5935.78%
95%035.750.00%
328.9319.08%
625.4528.81%
1022.9135.92%

Table 7

Parameters for particle flow simulation"

Particle parametersWall parameters

Normal contact stiffness

(kn/Pa)

Tangential contact stiffness

(ks/Pa)

Frictional coefficientDamping coefficient

Normal

stiffness of loading wall

(kn/Pa)

Tangential

stiffness of loading wall

(ks/Pa)

Normal stiffness of side wall (kn/Pa)

Tangential

stiffness of

side wall (ks/Pa)

Frictional coefficient
5?× 1061?× 1060.50.71?× 1071?× 1061?× 1061?× 1060.5

Table 8

Relationship between the bond strength and number of freeze-thaw cycles in PFC"

Rock block content

Degree of

compaction

Freeze-thaw cycles

Normal bond strength

(TF/Pa)

Tangential bond strength

(SF/Pa)

Bond strength decay ratioAverage bond strength decay ratio
45%87%02242240.00%0.00%
90%2212210.00%
95%2302300.00%
87%318718716.52%15.24%
90%19219213.12%
95%19319316.09%
87%616216227.68%25.95%
90%16216226.70%
95%17617623.48%
87%1015315331.70%31.57%
90%14914932.58%
95%16016030.43%

Figure 9

Particle flow models with different compactness"

Figure 10

Comparison of simulated and experimental stress-strain relationship for samples subjected to ten freeze-thaw cycles at confining pressure of 50 kPa"

Figure 11

Fracture distribution of samples with different compactness"

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