Advances in Civil Engineering
Volume 2020 (2020), Article ID 7467608, 15 pages
https://doi.org/10.1155/2020/7467608

Research Article

The Physicomechanical Deterioration Characteristics and Mesoscopic Damage Analysis of Sandstone under Acidic Environment

Runke Huo,1,2 Tian Qiu,1,2 Yanling Liang,1,2 Shuguang Li,1,2,3,4 and Meiting Qian1,2

¹School of Civil Engineering, Xi’an University of Architecture and Technology, Xi’an 710055, China
²Shanxi Key Lab of Geotechnical and Underground Space Engineering, Xi’an 710055, China
³Postdoctoral Research Workstation, China Railway 20th Bureau Group Co., Ltd., Xi’an 710016, China
⁴R&D Center of Plateau Tunnel Construction Technology and Equipment, China Railway 20th Bureau Group Co., Ltd., Xi’an 710016, China

Correspondence should be addressed to Yanling Liang; l18220585037@163.com and Shuguang Li; lssgg2015@163.com

Received 10 February 2020; Revised 21 June 2020; Accepted 30 June 2020; Published 30 July 2020

Academic Editor: Timo Saksala

Copyright © 2020 Runke Huo et al. 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.

Abstract.

The physicomechanical deterioration characteristics of sandstone subjected to H₂SO₄, HCl, and H₂O solutions of different pH values are studied by the method of long-term accelerated immersion. The quantitative relationships between the damage variables based on CT (computer tomographic identification technology) numbers and the immersion time, the uniaxial compressive strength, the peak point strain, and the elastic modulus of rock samples are analyzed. The test results indicate that the pH value of immersion solutions, the dissolution rate of Ca²⁺ and Na⁺, and the quality change of rock samples show visible stage characteristics under acidic environment. With the soaking time extended, the pH value of solutions increases gradually, and the quality change of rock samples decreases gradually. The smaller the pH value of immersion solutions is, the higher the dissolution rate of Ca²⁺ and Na⁺ is. However, the cation dissolution rate under a weak acid environment with a high pH value has little difference with that under the distilled water (pH = 7). With the increase of the soaking time and the acidity, the compaction stage of rock samples becomes longer, the elastic stage becomes shorter, the deterioration degree of mechanical parameters becomes more extensive, and the destruction of sandstone samples shows ductility characteristics increasingly. The corrosion degree of corroded sandstone samples is quantitatively represented by microscopic damage variables based on CT numbers. The regression analysis results show that damage variables of acid-corroded sandstone samples have a power function relationship with soaking time and an exponential function relationship with peak strength, peak point strain, and elastic modulus.

1. Introduction

The worsening of environmental pollution has caused rock and concrete materials to suffer corrosion destruction of varying degrees during their service [1–3]. The action of chemical media in the natural environment causes materials such as rocks to have a performance degradation and even are corroded. Although this process is slow, the cumulative effect of long-term corrosion cannot be ignored.

In recent years, the research on the influence of acid corrosion on the physical and mechanical properties of rocks has been valued by relevant scholars at home and abroad. It has become one of the emerging research focuses in the field of rock and environmental geotechnical engineering. Mohtarami et al. [4, 5] studied the effect of chemical solutions on the physical and mechanical properties of rocks and analyzed the chemical effect of rock fracture by the finite element method. Portier and Vuataz [6] studied the response of Enhanced Geothermal System (EGS) reservoir to chemical stimulation by numerical simulation of coupled thermohydraulic-chemical processes. Taron and Elsworth [7] introduced a new methodology and numerical simulator for the modelling of thermal-hydraulic mechanical-chemical processes in dual-porosity media. Chen et al. [8] had carried out microscopic mechanical tests on the uniaxial compression fracture process of rocks under chemical corrosion, discussed the corrosion effect of different chemical solutions on uniaxial compression strength of rocks, and analyzed the microfracture characteristics and corrosion mechanism of rock under chemical etching. Huo et al. [9–12] and Li et al. [13, 14] obtained the evolution laws of physical, chemical, and mechanical properties of acid corrosion sandstone and mortar by the indoor long-term accelerated corrosion test under acidic environment, established the constitutive model of sandstone in acid solutions, deduced the damage variables of acid corrosion sandstone based on CT numbers, and revealed the corrosion mechanism of sandstone under acidic environment. Xu et al. [15] and Li et al. [16] had carried out shear strength tests of sandstone subjected to different water chemical solution erosion. The mechanism of chemical damage of sandstone was discussed, and the relationship between porosity and shear strength was established. The influence of hydrochemical corrosion on the sandstone destruction, crack opening, and expansion direction was obtained. Chen et al. [17], Ding et al. [18], Han et al. [19], and Gao et al. [20] had performed the physical and mechanical tests on the chemical corrosion and freeze-thaw cycles of granite, limestone, sandstone, and red sandstone, respectively. The physical and mechanical damage laws of rock under the combined action of the freeze-thaw cycle and water chemical solution were analyzed. Wang et al. [21, 22] and Han et al. [23] had studied the effect of chemical solution soaking on the mechanical properties of sandstone and sand slate by uniaxial and triaxial compression tests. They found that the mechanical properties of sandstone decrease obviously after chemical corrosion, and it is closely related to the change of porosity. The conclusion that the elastic modulus and compressive strength of rocks decrease with the increase of soaking time and acidity was drawn. He and Guo [24] studied the failure of rock strength affected by different acid solutions from macroscopic and microscopic perspectives through core tests. Ding et al. [25] studied the mechanical damage characteristics and chemical dissolution behaviour of limestone under different chemical solutions. A time-dependent damage equation of the uniaxial compressive strength of limestone was developed under various chemical solutions. Chemical dynamic erosion equations of limestone were developed. Xie et al. [26] had carried out conventional triaxial and rheological tests on natural limestone and chemically etched porous limestone, respectively. They analyzed the effects of chemical corrosion on the pore-changing and aged mechanical properties of limestone. In recent years, the study of microscopic damage to rock by CT nondestructive testing technology is emerging [27, 28]. Yang et al. [29] applied the CT detection techniques for the study of rock damage characteristics, established the mathematical model of CT number distribution in damaged rocks, and deduced the formula for expressing rock damage variables by CT numbers. Fu et al. [30] analyzed the evolution mechanism of the microscopic damage of rock samples under the action of dry-wet cycles through CT scanning tests of sandstone with different initial microstructures. They obtained the damage evolution equation of sandstone.

The current research results mainly focus on the influence of chemical solutions on the macroscopic mechanical properties of rocks, lacking quantitative analysis of the effect of long-term accelerated corrosion and acidic solutions of different chemical compositions on the physical and mechanical properties of rocks. In this paper, the common sandstone in water conservancy and civil engineering is taken as the research object. The physical and mechanical properties of sandstone under acidic environment are systematically studied based on the uniaxial compression test. The quantitative relationship between damage variables and soaking time and mechanical parameters is established, which provides a basis for quantifying the deterioration degree of rocks in the acid environment.

2. Materials and Methods

2.1. Preparation of Sandstone Samples and Chemical Solutions

The sandstone specimen used in the tests were sampled from the water conservancy project in Shanxi Province, China, where the sandstone samples have good integrity and homogeneity. The rock samples were taken from the same rock mass to ensure uniformity. The X-ray diffraction test identified that the name of the sandstone is green-grey fine-grained calcareous feldspar sandstone with fine-grained unequal-grained structure. The particle size of debris is 0.05 mm to 0.45 mm, and the shape of debris is irregular, mainly angular-subangular, and a little subcircular. The detrital components are mainly quartz, feldspar, mica, chlorite, siliceous, and limestone clastic. The sandstone sample composition is shown in Table 1, and the microstructure diagram is shown in Figure 1.

Table 1: Debris components and contents.

Cuttings composition
Content (%)

Quartz
58

Feldspar
11

Calcite
5

Mica
3

Chlorite
1

Siliceous cuttings
6

Limestone cuttings
2

Cement
7

Clay
3

Heavy minerals
Occasionally

Figure 1: Microscopic image of the sandstone sample.

According to the provisions of international rock mechanics, the sample was processed into a cylinder with a diameter of 50 mm and a height of 100 mm. The basic dimensions and machining accuracy were in line with the Standard for Tests Method of Engineering Rock Masses [31]. Before the test, the samples were sonic tested, and the samples with a significant difference in wave velocity were excluded. The sandstone samples were grouped according to the longitudinal wave velocity. Considering the complexity of the acidic environment in nature, two acids (sulfuric acid and hydrochloric acid) were chosen to simulate the acidic environment. And, taking into account the strong acid, the medium-strong acid, and the weak acid, the pH values were set to 1, 3, and 5. Therefore, hydrochloric acid and sulfuric acid solutions (pH = 1, 3, and 5) and distilled water solution (pH = 7) were prepared, as shown in Figure 2. A total of 60 samples were selected and divided into four groups. There are 8 rock samples in each solution with pH = 1, 3, 5, or 7. Grouping and soaking of sandstone samples are shown in Table 2. Sandstone samples were soaking in the above solutions for the corrosion test.

Figure 2: Preparation of acidic solutions.

Table 2: Sandstone samples grouping.

Group number
pH value
Soaking state
Sample number
Wave velocity range (m/s)
Mass range

1

Natural rock samples
#1∼4
2467∼2775
529.67∼534.8

2
1, 3, 5
Sulfuric acid
#5∼28
2416∼2477
523.93∼533.08

3
1, 3, 5
Hydrochloric acid
#29∼52
2941∼2973
522.69∼528.92

4
7
Distilled water
#53∼60
2487∼2546
522.41∼529.26

2.2. Test Apparatus

The pH test equipment and ion concentration test equipment used in the experiment are Leica PHS-3C and Metrohm 792 Basic IC, respectively. The weighing instrument is an electronic balance JA12002 with a division value of 0.01 g. The oven is WGL-30B with a temperature range of room temperature plus 5∼300°C. The uniaxial compression tests were conducted in the LETRY electrohydraulic rock pressure testing machine (Figure 3). The maximum axial load was 2000 KN. Philips Brilliance 16 spiral CT machine (Figure 4) was used to obtain the CT images of the samples. The spatial resolution was 0.208 mm × 0.208  mm. The density contrast resolution was 0.3% (Hu). The image storage matrix was 1024 × 1024. The CT number range was minus 1024∼plus 3071.

Figure 3: Uniaxial compression test.

Figure 4: CT scanning test.

2.3. Test Methods

In this paper, hydrochloric acid solutions, sulfuric acid solutions with pH = 1, 3, and 5, and distilled water solution with pH = 7 were used to simulate the hydrochemical environment. The sandstone specimens were soaked and corroded at room temperature and atmospheric pressure. The experiment was divided into six stages (S1–S6), every 30 days for a stage. In order to observe obvious changes of corrosive sandstone samples in a relatively short time, the soaking solution was renewed every 30 days during the test (the type and pH of the replacement solution were unchanged). Before the experiment, the numbered sandstone samples were photographed, and the initial mass was weighted (Table 2). Then, the rock samples were placed in the prepared solutions, and the soaking container was a ground glass beaker. During the soaking process, the beaker was sealed to prevent carbon dioxide from entering, and the pH value and ion concentration of solutions and the mass of samples were measured. When the soaking time reached 30, 60, 90, and 180 days, the samples were taken out for the uniaxial compression test, and the CT scanning test was carried out on sandstone samples at 0, 30, 90, and 180 days.

3. Results and Discussion

3.1. Relative Change Law of Masses of Sandstone Samples

During soaking, the samples were taken out from the solution every 10 days. First, the surface water of the samples was wiped off with a cotton cloth, so that there was no dripping liquid. Then, the samples were left in the air for 5 minutes to ensure that the liquid is volatilized and dried. They were weighed in an electronic scale, and the values were recorded; after that, they were kept in an oven for drying (24 h, 105°C), and then they were taken out and weighed. The average values of the weight of samples were taken as the test result. The mass loss rate L is defined as the ratio of the mass loss of the sandstone samples after acid corrosion to its initial mass. The formula is as follows:

where M₀ and Mt are the weight of the samples in natural state and weight of the dry samples after soaking for t days (g), respectively.

The relative mass change rate curves can reflect the extent of interaction of acid and sandstone indirectly. As can be seen from Figure 5, we have the following.

Figure 5: Mass loss rate curves of sandstone samples in different pH solutions.

With the increase of soaking time, the change laws of the mass loss rate of sandstone samples soaked in different pH solutions are the same basically. The growth rate is faster in the early stage of immersion and gradually tends to be stable later. In the early stage of acid rock reaction, the erosion of the solution is mainly concentrated on the rock surface, and the chemical reaction rate is fast. With the extension of the penetration corrosion path, the acid rock reaction rate tends to be stable gradually. The smaller the pH value of the soaking solution is, the more violent the reaction between the soaking solution and the rock is, the higher the change rate and amplitude of the mass loss rate are, and the more bubbles and flocs are produced during the soaking process. When the soaking time reaches 180 days, the mass loss rates of the samples in HCl and H₂SO₄ solutions with pH = 1, 3, and 5 are 1.28% and 1.09%, 0.84% and 0.72%, and 0.61% and 0.59%, respectively. The mass loss rate of samples in distilled water with pH = 7 is 0.58%.

There are significant differences in the mass loss rate of sandstone samples in different types of soaking solutions with different pH values. Under the same conditions, the change amplitude and change rate of the mass loss rate in HCl solution are higher than those in H₂SO₄ solution during the initial soaking stage, and the change rate is basically the same in the later period of soaking. The mass loss rate of sandstone samples in HCl solution is slightly higher than that in H₂SO₄ solution after soaking, indicating that the HCl solution is more corrosive to sandstone than the H₂SO₄ solution. This is because the H₂SO₄ solution produces more water film and cement than the HCl solution during the acid rock reaction. The microsolutes such as calcium sulfate are adsorbed inside the sandstone samples, which causes the insoluble matter to block parts of pores and hinders the progress of the chemical reaction.

3.2. The Change Law of pH Value of the Soaking Solution

Figure 6 shows the curves of the pH value change of sandstone samples soaked in different pH solutions for different days. As can be drawn from Figure 6, we have the following:

(1)The pH values of acidic solutions with pH = l, 3, and 5 (Figures 6(a) and 6(b)) increase rapidly at the initial stage of each soaking period (0∼5 days). The pH values still increase after 5 days, but the growth rate slows down gradually. For example, the pH values of hydrochloric acid and sulfuric acid solutions are 2.12 and 2.02 on the 5th day of the first soaking stage (0∼30 days) and reach 3.24 and 3.12 after the first soaking stage. The acidic solution with pH = l changes from strong acid to medium-strong acid at the end of each soaking stage. The acidic solution with pH = 3 changes from medium-strong acid to weak acid at the end of each soaking stage. The acidic solution with pH = 5 shows weak alkalinity at the end of each soaking stage. Under the action of distilled water with pH = 7 (Figure 6(c)), the water rock reaction is slight. The pH value of the solution increases gradually at each soaking stage. After the end of each soaking stage, the pH value of the solution is between 7.28 and 7.86, which shows slightly alkaline.(2)Overall, the pH values of the hydrochloric acid solution increase slightly faster than those of the sulfuric acid solution with the same initial pH values under the same soaking period. The higher the pH value of solution after acid rock reaction is, the more the hydrogen ions are consumed during corrosion soaking, and the more violent the acid rock reaction is. The experimental data show that the hydrochloric acid solution is more corrosive on sandstone than sulfuric acid solution under the same conditions.(3)The acid rock interaction is intense in the early stage. The smaller the pH value of the solution is, the larger the change of value is, indicating that the chemical corrosion is stronger. In a limited enclosed space, the acid rock reaction has a time effect that the reaction rate gradually decreases with the extension of soaking time. Sandstone samples have an acid corrosion reaction with H⁺ in the acidic solution and the hydrolysis and ion exchange with distilled water. At the initial stage of soaking, the acid corrosion reaction is mainly on the surface of the sandstone. After a certain period of reaction, H⁺ in the solution continuously penetrates the sandstone to cause the chemical action between water and rock. Therefore, the pH value of the solution changes greatly at the initial soaking stage, and H⁺ is consumed gradually in the later stage of the reaction, which makes the pH value of the solution changeless.

(a)

(b)

(c)

Figure 6: The change law of pH with time in different chemical solutions: (a) H₂SO₄ solution, (b) HCl solution, and (c) distilled water.

3.3. The Change Law of Cation Dissolution Rate

Define the cation dissolution rate in the solution as

where is the dissolution rate of cation, is the initial concentration of cation , is the concentration of cation after soaking t days , is the time difference before and after corrosion reaction , and is the volume of the soaking solution .

Figure 7 shows the variation curves of Ca²⁺ and Na⁺ with soaking time in different pH solutions and different periods for sandstone samples. As can be drawn from Figure 7, we have the following.

(a)

(b)

(c)

(d)

Figure 7: The change law of cation dissolution rate with time in different chemical solutions: (a) Ca²⁺ in sulfuric acid solution, (b) Ca²⁺ in hydrochloric acid solution, (c) Na⁺ in sulfuric acid solution, and (d) Na⁺ in hydrochloric acid solution.

The cation dissolution rate has a significant stage response over time. The smaller the pH value of the soaking solution is, that is, the stronger the acidity is, the more obvious the stage characteristic is. Under the same pH values of the soaking solution, the change law of the cation dissolution rate in each soaking stage (30 days) shows a downward trend as a whole. Under different pH values of the same soaking solution, during the initial to intermediate stage of soaking, the dissolution rate of Ca²⁺ and Na⁺ decreases due to the increase of infiltration paths. During the middle to the late stage of soaking, the acid solution diffuses to the uncorroded area inside the rock sample, causing the dissolution rate to rise and then it continues to decrease.

Different soaking solutions have a great influence on the cation dissolution rate. Under the same conditions, the water film and cement produced by the reaction of H₂SO₄ and rock block the pores, resulting in the dissolution rate of Ca²⁺ under the action of the sulfuric acid solution which is lower than that under the action of hydrochloric acid solution. The dissolution rates of Na⁺ in the two acidic solutions are approximately the same. When clay minerals such as montmorillonite and illite in sandstone are in an acidic environment, the action of dissolution, hydrolysis, and ion exchange affects the precipitation of ions contained therein. So, when the pH value is high, the dissolution degree of clay minerals is similar to that in distilled water solution. This is also the reason why the dissolution rate of the cation under the action of the acidic solution with pH = 5 (Figure 7) is not much different from that under the action of distilled water with pH = 7.

3.4. The Effect of Acidic Environment on Rock Mechanical Parameters

After soaking in the acid solution for 30, 60, 90, and 180 days, two sandstone samples were taken out for the uniaxial compression test. Because the effect of two samples under uniaxial pressure was similar, and the mechanical data were close, the experimental data of either of the two was selected as a result in the paper. The test results and stress-strain curves are shown in Table 3 and Figure 8, respectively.

(1)As can be seen from Figure 8, the stress-strain curve of sandstone can be divided into the following four stages: compaction phase, elastic phase, plastic phase, and failure phase. The concave length of the natural specimen is short, and the degree of deformation is small. Then, it enters the elastic phase quickly. However, the compaction phase of the samples attacked by acid solution increases obviously. With the increases of axial pressure, the rock samples enter the elastic stage from the compaction stage. As can be seen from Table 3, the elastic modulus of acid-corroded sandstone samples all decreases to different extents compared with the sandstone in a natural state. The plastic deformation stage of the samples is not obvious. As can be seen from Table 3, the axial strain at the peak point of the sandstone samples increases gradually with the increase of the acidity of the chemical solution. Because of the strong brittleness of rock samples selected in the test, the destruction of rock samples was often accompanied by a crisp sound, and the stress drops rapidly after the failure of samples. Therefore, the postpeak stage has not been obtained.(2)For different kinds of soaking solutions with different pH values, the characteristic of sandstone changes from brittleness to ductility with the increase of soaking time. The micropores in acid-corroded rock increase, and the rock becomes soft. The deformations of the compaction stage, the elastic stage, and the plastic stage all increase to varying extents, and the compaction stage and the elastic stage increase significantly. In the same soaking solution, the smaller the pH value is, the greater the effect on deformation is. After soaking for 180 days, the peak strains of rock samples in H₂SO₄ solution with pH = 1, 3, and 5 are 0.0198, 0.0132, and 0.0118, respectively, which are 4.92, 3.27, and 2.92 times of the initial peak strains. Under the same conditions, the corrosion degree of HCl solution is slightly greater than that of H₂SO₄ solution at all stages.(3)The deterioration laws of strength parameters of rock samples soaking in different chemical solutions are basically the same. Under the same conditions, the pH value has a great influence on rock strength. After soaking for 180 days, the peak strength of sandstone samples in H₂SO₄ solution with pH = 1, 3, and 5 decreases by 48.2%, 38.4%, and 31.78%, respectively. After soaking for 30 days, the peak strength of samples in hydrochloric acid and sulfuric acid solutions with pH = 1 decreases by 35.7% and 34.1%, respectively, indicating that the strength mainly decreases in the early stage of the reaction. Under the same conditions, the peak strength of rock samples corroded by the hydrochloric acid solution is lower than that of samples corroded by the sulfuric acid solution, which indicates that the hydrochloric acid solution has a greater effect of deterioration on sandstone and sulfate radical has a slight inhibition effect on corrosion. The elastic modulus of acid-corroded sandstone decreases gradually with the extension of soaking time, and its variation range is more uniform than that of peak strength. Under the same conditions, the smaller the pH value is, the greater the change of elastic modulus of rock samples is. And the variation of elastic modulus of rock samples in HCl solution is slightly larger than that in H₂SO₄ solution. Because of the strong brittleness of sandstone samples, the destruction of sandstone samples is often accompanied by a crisp sound and the stress dropped rapidly after the failure of the samples, so the postpeak stage has not been obtained.

Table 3: Uniaxial compressive test results of sandstone samples subjected to acid corrosion.

Corrosion time
Soak solution
Peak stress (MPa)
(%)
Peak strain (10⁻³)
(%)
Elastic modulus E (GPa)
(%)

30

58.14
34.12
5.37
33.25
14.79
38.76

60
pH = 1
52.37
40.66
9.33
131.51
7.36
69.52

90
H₂SO₄
49.06
44.41
12.01
198.01
5.71
76.36

180

45.71
48.20
19.82
391.81
3.50
85.51

30

64.04
27.43
5.11
26.80
15.63
35.28

60
pH = 3
59.86
32.17
8.39
108.19
9.11
62.28

90
H₂SO₄
57.67
34.65
10.64
164.02
7.03
70.89

180

54.39
38.37
13.17
226.80
6.01
75.11

30

69.7
21.02
4.95
22.83
19.13
20.79

60
pH = 5
65.04
26.30
7.61
88.83
11.51
52.34

90
H₂SO₄
62.02
29.72
9.48
135.24
8.13
66.34

180

60.20
31.78
11.78
192.31
7.24
70.02

30

56.78
35.66
5.23
29.78
14.53
39.83

60
pH = 1
51.74
41.37
9.68
140.20
6.96
71.18

90
Hcl
46.91
46.84
12.65
213.90
5.08
78.96

180

41.73
52.71
20.78
415.63
2.38
90.14

30

65.55
25.72
5.03
24.81
15.88
34.24

60
pH = 3
58.17
34.08
8.96
122.33
8.54
64.64

90
Hcl
54.25
38.53
10.17
152.36
7.35
69.57

180

49.53
43.88
13.65
238.71
5.06
79.05

30

68.89
21.94
4.93
22.33
18.02
25.38

60
pH = 5
64.24
27.21
7.72
91.56
11.42
52.71

90
HCl
62.13
29.60
9.71
140.94
8.74
63.81

180

59.85
32.18
12.32
205.71
6.73
72.13

30

75.26
14.72
4.68
16.13
20.45
15.32

60
pH = 7
71.18
19.34
5.85
45.16
16.18
33.00

90
H₂O
67.73
23.25
6.88
70.72
12.82
46.92

180

63.52
28.02
9.05
124.57
8.418
65.14

Nature

88.25

4.03

24.15

Note that in this table, , , and are, respectively, peak strength, peak point axial strain, and elastic modulus of sandstone samples in a natural state.

(a)

(b)

(c)

(d)

Figure 8: Uniaxial compressive stress-strain curves for sandstone samples attacked by acid solutions for different days: (a) soaking for 30 days, (b) soaking for 60 days, (c) soaking for 90 days, and (d) soaking for 180 days.

The relationships between the peak stress and elastic modulus of acid-corroded sandstone samples and the soaking time can be fitted by the following formula:

where y is the peak strength () or elastic modulus (), is soaking time (d), and a, b, and c are the fitting parameters, as shown in Table 4. The relationships between the peak strength and elastic modulus and soaking time are shown in Figures 9(a) and 9(b).

Table 4: Fitting parameters of relationship between the peak stress and the elastic modulus and soaking time.

Mechanical parameters
Soaking solution
a
b
c
R²
Soaking solution
a
b
c
R²

Peak stress (MPa)
pH = 1 H₂SO₄
40.916
−0.040
47.154
0.994
pH = 1 HCl
44.057
−0.035
43.783
0.986

pH = 3 H₂SO₄
32.189
−0.042
55.909
0.991
pH = 3 HCl
37.846
−0.028
50.125
0.996

pH = 5 H₂SO₄
27.477
−0.035
60.648
0.997
pH = 5 HCl
27.541
−0.038
60.607
0.996

pH = 7 H₂O
24.431
−0.021
63.477
0.992
—
—
—
—

pH = 1 H₂SO₄
21.534
−0.023
2.857
0.992
pH = 1 HCl
22.677
−0.022
1.717
0.992

Elastic modulus (GPa)
pH = 3 H₂SO₄
19.151
−0.024
5.256
0.991
pH = 3 HCl
19.989
−0.022
4.427
0.988

pH = 5 H₂SO₄
19.307
−0.017
5.552
0.960
pH = 5 HCl
19.082
−0.018
5.477
0.986

pH = 7 H₂O
20.604
−0.009
3.858
0.994
—
—
—
—
—

(a)

(b)

(c)

Figure 9: Relationship between (a) the peak stress, (b) the elastic modulus, and (c) the peak stain of sandstone samples and soaking time.

The relationship between the peak stain and soaking time can be fitted by the following formula:

where is the peak stain (mm) and a, b, and c are the fitting parameters, as shown in Table 5. The relationships between the peak stain and soaking time are shown in Figure 9(c).

Table 5: Fitting parameters of relationship between peak strain and soaking time.

Mechanical parameters
Soaking solution
a
b
c
d
R²
Soaking solution
a
b
c
d
R²

Peak strain (10⁻³)
pH = 1 H₂SO₄
0.994
22.038
83.858
45.153
0.996
pH = 1 HCl
1.377
22.463
82.427
40.169
0.995

pH = 3 H₂SO₄
3.072
13.205
60.410
25.065
0.996
pH = 3 HCl
1.823
13.899
56.229
34.521
0.980

pH = 5 H₂SO₄
3.149
11.845
61.572
26.602
0.996
pH = 5 HCl
3.098
12.411
63.538
27.143
0.996

pH = 7 H₂O
3.015
9.534
73.119
42.502
0.999
—
—
—
—
—
—

4. Quantitative Damage Analysis of Acid-Corroded Sandstone Based on CT

The main cause of the nonlinearity of mechanical properties of sandstone is the heterogeneity of the microstructure of rocks. Therefore, based on the damage variables defined by the microstructure of rocks, the macroscopic mechanical effect can be better analyzed. The chemical reaction between the rocks and the acid solution causes the internal micropores to expand and penetrate. The cohesive force between the particles decreases, resulting in a decrease in the effective bearing area, a decrease in mechanical parameters, and a deeper deterioration. Computer tomographic identification technology (CT) can describe the physical parameters of rocks quantitatively by CT number. Through the observation of CT images and the quantitative analysis of CT numbers, the change in the formation, permeability depth, and the path of microvoids of rock samples can be obtained, and the mechanical characteristics of corrosion damage of sandstone can be more intuitively linked with the change of internal microstructures.

Figure 10 shows CT scanning images of the middle layer of sandstone samples subjected to two different solutions. The corrosion damage degree of samples subjected to the solution with the same pH value is obviously different in different stages, and the smaller the pH value of the solution is, the more seriously the rock samples are corroded. The author had carried out a detailed analysis of the damage of acid-corroded sandstone based on CT histogram technology in [12, 13]. According to the literature in [13], the formulas for calculating damage variables of acid-corroded sandstone are as follows:

where is the damage variable of acid-corroded sandstone, and are the damage variable of corroded and noncorroded rocks, and and are the density of corroded and noncorroded rocks, respectively .

(a)

(b)

(c)

(d)

(e)

(f)

(g)

(h)

Figure 10: CT images of the middle layer of sandstone specimens subjected to different solutions for different stages: (a) pH = 3 H₂SO₄ (0 days), (b) pH = 3 H₂SO₄ (30 days), (c) pH = 3 H₂SO₄ (90 days), (d) pH = 3 H₂SO₄ (180 days), (e) pH = 1 HCl (0 days), (f) pH = 1 HCl (30 days), (g) pH = 1 HCl (90 days), and (h) pH = 1 HCl (180 days).

According to the literature in [28], the relationship between the CT number and the rock density is as follows:

where is the CT number of the damaged sandstone, is the CT number of sandstone matrix material, and is the density of sandstone matrix material.

Equations (5) and (6) can solve the damage variables of the scanned cross section of the acid-corroded sandstone based on the CT number. The calculated damage variables at different corrosion stages of the middle scanning layer of sandstone samples attacked by the hydrochloric acid and sulfuric acid solution with different pH values are shown in Table 6. It can be seen from Table 6 that the chemical damage of rock samples in different acidic solutions in different soaking stages is different. With the increase of acidity of soaking solution and soaking time, the damage variables of rock sample increase, and the stronger the acidity, the greater the increase of damage variable.

Table 6: Damage variables of the intermediate scanning layer of rock samples at different time intervals in different solutions.

Soaking time
Corrosion time (days)
Damage variables (D)

pH = 1 H₂SO₄
30
0.1935

60
0.2825

90
0.3416

180
0.5038

pH = 3 H₂SO₄
30
0.1412

60
0.2135

90
0.2614

180
0.3507

pH = 5 H₂SO₄
30
0.1308

60
0.1754

90
0.2097

180
0.2813

pH = 1 HCl
30
0.2123

60
0.3014

90
0.3602

180
0.5184

pH = 3 HCl
30
0.1685

60
0.2310

90
0.2732

180
0.3713

pH = 5 HCl
30
0.1385

60
0.1886

90
0.2301

180
0.2988

The relationship between the damage variable of acid-corroded sandstone samples and the soaking time can be fitted by the following formula:

where is the soaking time (d); a and b are the fitting parameters, as shown in Table 5. The relationship between the damage variables and soaking time is shown in Figure 11.

Figure 11: Relationship between the damage variables of the sandstone samples and soaking time.

The relationship between the damage variables of the acid-corroded sandstone and peak strength, peak strain, and elastic modulus can be fitted by the following formula:

where is the damage variable, y is the peak strength (), peak strain, and elastic modulus (), and a, b, and c are the fitting parameters, as shown in Tables 7 and 8. The relationships between the damage variables and peak strength, peak strain, and elastic modulus are shown in Figures 12(a)–12(c).

Table 7: Regression parameters of the relationship between the damage variables and soaking time.

Soaking solution
a
b
R²

pH = 1 H₂SO₄
0.031
0.534
0.999

pH = 3 H₂SO₄
0.030
0.472
0.996

pH = 5 H₂SO₄
0.031
0.428
0.996

pH = 1 HCl
0.039
0.499
0.999

pH = 3 HCl
0.038
0.438
0.999

pH = 5 HCl
0.034
0.422
0.997

Table 8: Fitting parameters of relationship between damage variable and peak strength.

Mechanical parameters
Soaking solution
a
b
c
R²
Soaking solution
a
b
c
R²

Peak stress (MPa)
pH = 1 H₂SO₄
97.182
−10.989
3.201
0.998
pH = 1 HCl
99.241
−9.709
1.801
0.998

pH = 3 H₂SO₄
80.707
−14.706
5.463
0.999
pH = 3 HCl
160.863
−15.873
4.792
0.994

pH = 5 H₂SO₄
251.895
−22.727
6.616
0.994
pH = 5 HCl
101.375
−15.151
5.652
0.999

Peak strain (10⁻³)
pH = 1 H₂SO₄
−136.857
−0.359
133.024
0.999
pH = 1 HCl
−96.811
−0.615
90.179
0.999

pH = 3 H₂SO₄
−25.711
−3.484
20.779
0.997
pH = 3 HCl
−30.601
−4.808
18.731
0.994

pH = 5 H₂SO₄
−26.029
−6.711
15.758
0.998
pH = 5 HCl
−27.452
−3.802
21.141
0.999

Elastic modulus (GPa)
pH = 1 H₂SO₄
97.182
−11.001
3.201
0.998
pH = 1 HCl
99.241
−9.709
1.801
0.998

pH = 3 H₂SO₄
80.707
−14.706
5.463
0.999
pH = 3 HCl
160.863
−15.873
4.792
0.994

pH = 5 H₂SO₄
251.895
−22.727
6.616
0.994
pH = 5 HCl
101.375
−15.151
5.652
0.999

(a)

(b)

(c)

Figure 12: Relationship between the damage variables of the sandstone samples and (a) peak stress, (b) peak strain, and (c) elastic modulus.

It can be seen from Figure 11 that the damage variable of the sandstone samples increases with the increase of soaking time in the acidic environment. When the soaking solution is the same, the damage variable of the rock samples increases with the decrease of the pH value of the solution. The damage variable of the rock samples in the hydrochloric acid solution is larger than that in the sulfuric acid solution with the same pH value, and the difference between the two decreases with the extension of soaking time. It can be seen from Figures 12(a) and 12(c) that the peak strength and elastic modulus of the acid-corroded sandstone decrease with the increase of damage variable, and the decreasing rate gradually decreases with the increase of damage variable. It can be seen from Figure 12(b) that the peak strain of acid-corroded rock samples increases as damage variable increases. The above analysis shows that as the chemical damage of sandstone samples becomes more and more serious, the mechanical properties of the sandstone samples gradually deteriorate. However, the plastic deformation of the rock samples gradually increases. The damage variable of the acid-corroded sandstone samples has a power function relationship with the corrosion time and an exponential function relationship with the peak strength, peak strain, and elastic modulus.

5. Conclusions

Based on the results of this study, the following conclusions can be drawn:

(1)In the acidic environment, the pH value of the soaking solution and the mass change of the sandstone sample have visible phased characteristics. The smaller the pH value of the soaking solution is, the more violent the reaction between the soaking solution and the rock is, and the higher the change rate and amplitude of the mass loss rate are. The pH value of the solution increased rapidly at the initial of each soaking stage (30 days) and stabilized gradually with the prolongation of the corrosion time. The mass change rate shows an increasing trend in the whole corrosion stage, and its growth rate gradually decreased and tended to be stable. Under the same soaking conditions, the corrosion of hydrochloric acid solution to sandstone was more durable than that of sulfuric acid solution.(2)With the extension of soaking time and the increase of acidity, the compaction stage of the rock samples became longer, and the elastic stage became shorter. The damage of the sandstone samples showed ductile characteristics gradually. The smaller the pH value of the soaking solution was, the greater the deterioration degree of mechanical parameters of rock samples was. Under the same conditions, the deterioration degree of the hydrochloric acid solution was similar to that of sulfuric acid solution at the initial stage of soaking. With the extension of corrosion time, the deterioration degree of the hydrochloric acid solution was greater than that of sulfuric acid solution.(3)With the same soaking solution, the smaller the pH value was, the greater the dissolution rate of Ca²⁺ and Na⁺ was. With the extension of corrosion penetration path, the dissolution rate fluctuated with soaking time, indicating that the process of acid corrosion of rocks had a phased characteristic. Under the same pH value, the dissolution rate of Ca²⁺ in the sulfuric acid solution was less than that in the hydrochloric acid solution, and the dissolution rate of Na⁺ is the same approximately. The cation dissolution rate under the action of the weak acid with higher pH value was not significantly different from that under the action of distilled water with pH = 7.(4)The damage variable of acid-corroded sandstone based on CT number was calculated, and the macroscopic mechanical effect of corroded rocks was expressed by mesoscopic damage variables quantificationally. The regression analysis shows that the damage variable has a power function relationship with the corrosion time and an exponential function relationship with the peak strength, peak point strain, and elastic modulus of acid-corroded sandstone.

Data Availability

The data included in this study are available from the corresponding author upon request.

Conflicts of Interest

The authors declare that they have no conflicts of interest.

Acknowledgments

The authors would like to thank the National Natural Science Foundation of China (41172237), China Railway 20th Bureau Group Co. Ltd. (YF2000SD01A) and China Postdoctoral Science Foundation (2020M673525) for supporting this research project.

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