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Ju-yun Zhai, Xiang-yong Cai, "Strength Characteristics and Slope Stability of Expansive Soil from Pingdingshan, China", Advances in Materials Science and Engineering, vol. 2018, Article ID 3293619, 7 pages, 2018. https://doi.org/10.1155/2018/3293619
Strength Characteristics and Slope Stability of Expansive Soil from Pingdingshan, China
By analyzing the characteristics of expansive soil from Pingdingshan, China, the shear strength parameters at different water contents, dry densities, and dry-wet cycles of expansive soil are obtained. It is found that, at higher soil-water content, the internal friction angle is 0° and the shallow layer of expansive soil slope will collapse and destroy; this has nothing to do with the height of the slope and the size of the slope. The parameters of soil influenced by atmosphere are the ones which have gone through dry-wet cycles, and the parameters of soil without atmospheric influence are the same as those of natural soil. In the analysis of slope stability, the shear strength parameters of soil can be determined by using the finite element method, and the stability coefficient of the expansive soil slope can be calculated.
Disasters, such as deformation and destruction, occur to natural slopes, roads, mounds, foundation pits, and artificial slopes of underground engineering excavation, resulting in great economic losses . Especially, a series of disasters, such as crack, landslide, and slump, are more apt to occur to expansive soil because of the water sensitivity [2–4]. The strength of expansive soil slope shallow layers is greatly affected by climatic conditions [5–7]. The study on the strength and slope stability of expansive soil is of great significance to control and prevent the natural disasters [8–10].
Much work has been done on the expansive soils. Experimental study on drying and wetting cycles of undisturbed expansive soil in Nanning area has been done in . Tang and Shi studied the deformation on drying and wetting cycles of the pukou area in nanjing . Wei and Wang studied the expansion and shrinkage deformation mechanism of solidified expansive soil . Zhai et al. studied the permeability and intensity characteristics of expansive soil from Pingdingshan . There are few reports on the stability of the Pingdingshan expansive soil slope under the influence of the atmosphere.
This paper simulates the effects of the atmosphere. Based on the analysis of the different water contents, dry densities and strength characteristics of the expansive soil in Pingdingshan, the stability of the Pingdingshan expansive soil slope under the influence of the atmosphere is studied. It could provide a reference for engineering design.
2. Brief Introduction to Expansive Soil from Pingdingshan
The expansive soil from Pingdingshan is meanly montmorillonite. The humidity coefficient is 0.7–0.8, the depth of atmospheric influence is generally <4 m, and the sharp depth of the atmospheric influence is 1.5∼1.8 m. Parameters of natural soil samples that have been tested are as follows: natural water content of 20%∼26%, natural density of 1.8∼2.0 g/cm3, dry density of 1.5∼1.7 g/cm3, pore ratio of 0.69∼0.81, compression index of 0.08∼0.15, cohesive force of 35∼85 kPa, internal friction angle of 9∼27°, and free expansion rate of 51–71.
3. The Characteristics of the Expansive Soil from Pingdingshan
3.1. The Selection of Expansive Soil Samples
The disturbed soil samples of expansive soil taken for experiment are at the intersection of the construction road and the Dongfeng road in Pingdingshan city. Through the indoor soil test, the plastic limit of the expansive soil is 22.85%, the 17 mm liquid limit is 45.72%, and the free expansion rate is 55%. The chemical composition and content of expansive soil are shown in Table 1.
3.2. Deformation Parameters of Expansive Soil
To the representative expansion soil which was air-dried, grounded, and sieved by a 2 mm sieve was added appropriate amount of water, stirred evenly, and was finally made into remolding soil samples of different water contents and dry densities. After compaction, the diameter of the samples is 61.8 mm and the height is 20 mm. Furthermore, by studying the expansion-shrinkage deformation, the deformation parameters were obtained. The relation curves of the expansion rate with vertical pressure are shown in Figure 1.
The relation curves of the shrinkage rate with water content were obtained by shrinkage test at three different dry densities of expansive soils, as shown in Figure 2.
The following can be found: The dry density: 1.67 g/cm3; the water content: 21%; the fitting equation: y = −0.5144x + 10.522; and R2 = 0.977. The dry density: 1.63 g/cm3; the water content: 21%; the fitting equation: y = −0.4692x + 9.4898; and R2 = 0.999. The dry density: 1.70 g/cm3; the water content: 20%; the fitting equation: y = −0.4474x + 8.7071; and R2 = 0.9688.
3.3. Strength Characteristics of Expansive Soils
The representative expansive soil that was sieved by a 2 mm sieve was made into a sample of dry soil with the dry density of 1.5 g/cm3 and 1.6 g/cm3 and water content of 30%, 31%, and 33%. The shear strength curve could be obtained through direct shear test at room temperature as shown in Figure 4.
The shear strength of the expansive soil under a high water contentunder the same pressure decreases significantly with the increase of water content (Figure 4). And the internal friction angle decreases to 0, when the water content increases over a certain degree. Meanwhile, the value of cohesion decreases significantly with the increase in water content. The collapse of slope is unconcerned about slope height and slope foot size, on a heavy rainfall condition. Therefore, the effective measure of slope protection is to handle slope waterproofing and drainage well.
The shearing testing of the expansive soil of water content of 26%, 24%, 20%, dry density of 1.5 g/m3, 1.6 g/m3 is carried out. The curve is shown in Figure 5.
The internal friction angle of the expansive soil decreases with the increase of water content, under a low water content. And the shear strength changed with the density of soil obscurely, when the water content of soil is the same, as shown in Figure 5.
The equation of soil shear strength iswhere is the shear strength (kPa), φ is the angle of internal friction (°), and C is the cohesive force (kPa).
Comparing the shear strength curve fitting equation of multiple water content, the shear strength characteristics of the expansive soil at the dry density of 1.5 g/cm3 are shown in Table 2.
The shear strength characteristics of the expansive soil at the dry density of 1.6 g/cm3 are shown in Table 3:
3.4. The Characteristics of Expansive Soil during Drying and Wetting Cycles
Samples of Pingdingshan expansive soil were remolded, and the attenuation law of shear strength after drying and wetting cycles was studied in the test. The shear strength sharply reduced in the first 2∼4 cycles and then tended to be stable. The stable strength parameters should be taken during the construction of the project.
Take the expansive soil sample with initial water content of 24% as an example. The soil sample passes through 1, 2, 3, 4, and 5 times dry-wet cycles. The water content ranges from 24.0% to 16.6%. And then, samples of the same water content was made, which is called the control of water content. The characteristic curve of the shear strength of 20% is shown in Figure 6.
In the same way, by testing the expansive soil shear strength of other water contents under dry-wet cycles, the shear strength of the control water contents 20% and 25% is obtained. With the linear fitting of expansive soil stable strength, the strength parameters are obtained, as shown in Tables 4 and 5.
4. Calculation of Slope Stability of Expansive Soil
4.1. The Selection of the Computational Model
The stability calculation of the expansive soil slope is based on the Swedish method. The safety factor could be calculated, and the position of the most unfavorable center could be searched by Lizheng software, as shown in Figure 7. In the figure, b = 1 m is the width of the earth bar and q = 30 kPa is the overload size.
Shear strength parameters of slope soil are different at different positions. The slope is divided into multiple units, as shown in Figure 8.
In the shallow layer of the soil, the shear strength parameters within 2 m from the soil surface are the same as those after dry-wet cycles. The shear strength parameters deeper than 2 m are the same as those of the initial soil.
4.2. Calculation of Slope Safety Factor
The horizontal projection of the expansive soil slope is 10 m and the vertical projection is 6 m. The coordinates of each node calculation unit are shown in Table 6.
Soil slopes are divided into multiple areas by the nodes. The density of the soil is 20 kN/m3. The water content of each area is determined by the indoor tests. The shear strength parameters of shallow soil are the stable parameters, which after the dry-wet cycles are C = 40 kPa and φ = 11°. The parameters of inner area are the same as natural soil strength parameters: C = 40 kPa and φ = 17°.
With the horizontal projection of 10 m, the slope safety factor and the most unfavorable center position at different slope heights are calculated by the Lizheng software, as shown in Table 7.
4.3. Analysis of Safety Factor of Expansive Soil at Different Slope Heights
The safety factor at different slope heights of 6 m, 8 m, 9 m, and 10 m, with the abscissa of level projection and the ordinate of safety factor, is shown in Figure 9.
In this paper, the physical and mechanical characteristics of expansive soils from Pingdingshan are analyzed, which provide a reliable basis for engineering design and they can be used in the calculation of slope stability. The finite element method is used to calculate the different positions of the soil slope layers and select the corresponding strength parameters.
Conflicts of Interest
No potential conflicts of interest were reported by the authors.
This research was supported by the Science and Technology Planning Project of Henan (no. 152192310091), the Innovation Talent Project of Pingdingshan (no. 2017010(10.3)), and the Key Scientific Research Projects in Henan colleges and universities (no. 18B560001).
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Copyright © 2018 Ju-yun Zhai and Xiang-yong Cai. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.