Keywords

1 Introduction

It has been extensively studied how loading frequency (f) affects liquefaction resistance of sand; however, the issue is highly controversial. In several studies, liquefaction resistance of sandy soil was found to be small or unaffected by loading frequency. Peacock et al. [1] applied several cyclic simple shear tests (CSS) with the range from 1/6 to 4 Hz of f and noted that the frequency effects were small. The same conclusions have been reached by other studies [2, 3]. More recently, Zhu et al. [4] performed cyclic triaxial tests to highlight the effect of f on the sand liquefaction response. Medium dense and dense samples were subjected to a various f (in both stress-controlled mode and strain-controlled mode). It was found that the effect of the f was insignificant for dense sand in stress-controlled mode.

Moreover, numerous researchers [5, 6] reported that the sand exhibited a higher cyclic strength at the higher loading frequencies. A series of CSSs was conducted on Nakdong sand with a wide range of f (0.05–1 Hz) by Nong et al. [6] to examine the f effects on the cyclic strength. It showed that an increase in the f resulted in increasing liquefaction resistance, regardless of the vertical effective stress or relative density.

In contrast, other researchers [7, 8] found that varying the frequency resulted in a decrease in cyclic strength. Dash et al. [8] observed that cyclic liquefaction resistance decreased as f increased in range of 0.1–0.5 Hz, due to an increase in the excess pore water pressure.

Therefore, the relationship between the loading frequency and liquefaction resistance of sand remains unclear and requires more investigation. In this study, CSS tests on poorly graded medium density sand samples are conducted with various f (0.03, 0.05, 0.1, 0.2, and 0.5 Hz) to evaluate the influence of f on the liquefaction resistance of sand.

2 CDSS Tests

2.1 Material

The characteristic and particle size analysis of the silica sand are shown in Table 1 and Fig. 1, respectively. The specific gravity (GS) is 2.60, the maximum void ratio (emax) and minimum void ratio (emin) are 1.02 and 0.63, respectively. Based on the Unified Soil Classification System, the sand is classified as poorly graded sand (SP).

Table 1 Physical properties of testing samples
Fig. 1
A graph of percent finer by weight versus grain size represents the particle size distribution curve. 0.64, 5.31, and 0.87 are the poorly graded values of the 3 different sand samples.

Grain size distribution curve

2.2 Testing Condition and Sample Preparation

The CSS device used in this study is described in Fig. 2. The system includes a shear box, a lateral load cell, a vertical load cell, and a horizontal and vertical LVDT. In the CSS tests, typical cylindrical samples have initial diameter of 63.5 mm and height of 25 mm, respectively. The dry funnel deposition technique is used to prepare the sample in this study. All dry sand samples are conducted with a relative density of 60%, consolidated under the initial vertical effective stress (σ′) of 100 kPa. The cyclic stress ratio (CSR) is defined as the ratio between the cyclic shear stress (τcyc) and the initial vertical effective stress (σ′). Upon the consolidation stage, the cyclic stage is conducted with CSR values (0.1, 0.12, 0.15, and 0.18), as well as f (0.03, 0.05, 0.1, 0.2, and 0.5 Hz).

Fig. 2
A photograph of a C D S S device. 1. The shear box, 2. lateral load cell, 3. soil sample, 4. vertical load cell, 5. horizontal L V D T, and 6. vertical L V D T are the labeled parts.

CDSS device

3 Result and Discussion

3.1 Test Results

The details of CSS test results, including CSR, f and average number of cycles to liquefaction (Ncyc), are shown in Table 2. Figure 3 presents the typical result for the case CSR = 0.1 and f = 0.1 Hz. To determine the cyclic resistance of silica sand, at least three CSS distinct test cases with various CSRs are conducted for a given f.

Table 2 CDSS test results
Fig. 3
A set of 4 graphs represent the results of the C D S S test. For a, b, c, and d the values of C S R = 0.1 and frequency = 0.1 hertz. For a and b, the number of cycles = 68.

CDSS test results for the case CSR = 0.1, f = 0.1 Hz, a shear strain and N, b excess pore pressure and N, c shear stress versus shear strain, and d shear stress versus normal stress

3.2 Liquefaction Resistance of Poorly Graded Sand

Effect of f on cyclic behavior of poorly graded sand with various CSRs is shown in Fig. 4. The figure describes the undrained cyclic simple shear response of poorly graded silica sand with various fs (f = 0.03, 0.05, 0.1, 0.2, and 0.5 Hz) at different CSRs ((a) CSR = 0.1, (b) CSR = 0.12, and (c) CSR = 0.15). The shear strain is accumulated continuously and nearly the same with low f (f = 0.03, 0.05, and 0.1 Hz). The double amplitude of the shear strain exceeds 7.5% at the same number of cycles (Ncyc = 71 with CSR = 0.1, Ncyc = 31 with CSR = 0.12, and Ncyc = 15 with CSR = 0.15). With higher f, the shear strain accumulation is different. When f increases from 0.1 to 0.5 Hz, the number of cycles to liquefaction increases from 71 to 111 with CSR = 0.1, from 31 to 69 with CSR = 0.12, and from 15 to 18 with CSR = 0.15.

Fig. 4
A set of 3 graphs of excess pore pressure versus the number of cycles represent the ranges of frequency for different values. Frequency = 0.033, 0.05, 0.1, 0.2, and 0.5 hertz.

Effect of f on the shear strain accumulation (medium sand and σ′ = 100 kPa): a CSR = 0.1, b CSR = 0.12, and c CSR = 0.15

Figure 5 shows the change of the excess pore pressure with N with different f when CSR changes between 0.1, 0.12, and 0.15.

Fig. 5
Three graphs of shear strain versus the number of cycles expose the ranges of frequency for different values. The number of cycles for a = 71, 77, and 111, b = 31, 35, 55, and 69, and c = 15, 17, and 18.

Effect of f on the excess pore pressure accumulation (medium sand and σ′ = 100 kPa): a CSR = 0.1, b CSR = 0.12, and c CSR = 0.15

The relationship between f and number of cycles to liquefaction is shown in Fig. 6. Accordingly, when the f increases, the number of cycles to liquefaction remains unchanged. However, after a certain optimum loading frequency (fopt), the increasing in f increases the number of cycles to liquefaction. The fopt is the one at which the liquefaction resistance remains unchanged with decreasing f and increases with increasing f. When f is less than 0.1 Hz, the number of cycles to liquefaction is not influenced by the f at a constant CSR (Ncyc = 15 at CSR = 0.15, Ncyc = 35 at CSR = 0.12, and Ncyc = 71 at CSR = 0.1). The increasing in f corresponds to the increasing trend of the liquefaction resistance. Ncyc increases from 71 to 111 at CSR = 0.1, from 31 to 69 at CSR = 0.12, and from 15 to 18 at CSR = 0.15 when f increases from 0.1 to 0.5 Hz. Moreover, the fopt (fopt = 0.1 Hz) is the same for three cases of CSRs. Therefore, it can be stated that the fopt does not depend on the CSR.

Fig. 6
A graph of the number of cycles to liquefaction versus cyclic loading frequency represents the trends for 3 different values of C S R. C S R = 0.1, 0.12, and 0.15.

Relationship between f and number of cycles to liquefaction

Figure 7 shows the cyclic resistance curves of poorly graded sand for various f. The trend curves shown in Fig. 7 define the relationship between CSR and Ncyc. The liquefaction resistance of sand, expressed in terms of the cyclic resistance ratio (CRR), is defined as the cyclic stress ratio at 15 cycles based on the cyclic resistance curves. In this study, the coefficients of determinations (R2) are quite high, with values of 0.972, 0.993, and 0.985, respectively, indicating that CSR and number of cycles have a good relationship.

Fig. 7
A graph of cyclic stress ratio versus cycle represents the ranges of frequency for different values. The values of C R R = 0.1532, 0.1476, and 0.1413.

Comparison of cyclic resistance curve at medium density states for σ’ = 100 kPa

The change of CRR with f is shown in Fig. 8 for medium sand (Dr = 60%) and σ′ = 100 kPa. CRR remains initially unchanged at low f (CRR = 0.1413 at f ≤ 0.1 Hz). This finding is consistent with some previous research [1,2,3]. Besides that, when f increases from 0.1 to 0.5 Hz, CRR increases from 0.1413 to 0.1532. This phenomenon could result from a slippage or rearrangement of grain structure.

Fig. 8
A graph of cyclic resistance ratio versus cyclic loading frequency represents the values of frequency and C R R. Frequency = 0.033, 0.05, 0.1, 0.2, and 0.5 hertz. C R R = 0.1413, 0.1476, and 0.1532.

Effect of loading frequency on cyclic resistance

4 Conclusion

In this study, the influence of f on cyclic liquefaction resistance of poorly graded sand has been investigated. Numerous CSSs were conducted on silica sand with various f (f = 0.03, 0.05, 0.1, 0.2, and 0.5 Hz). Based on the test results, the cyclic liquefaction resistance of sand was unchanged at low f (f = 0.03 and 0.05 Hz). In this study, the optimum loading frequency was about 0.1 Hz. When the loading frequency was greater than the optimum loading frequency, the increasing of loading frequency increased the liquefaction resistance of sand.