Acessibilidade / Reportar erro

Micro-mechanism of Shear Strength and Water Stability Enhancement of Montmorillonite by Microwave Heating

Abstract

Microwave heating potentially reinforces the muddy intercalation to eliminate slope failure. Montmorillonite has the worst water resistance among the muddy intercalation components, which is a primary facet of inducing muddy intercalation failure. This study investigates the mechanism of shear strength and water stability enhancement of montmorillonite heated by the microwave oven and muffle furnace from room temperature to 800 °C. Results show that montmorillonite mineralogical evolution can be divided into three stages: room temperature-300 °C, 300-600 °C, and 600-800 °C. Microwave heating is more efficient in montmorillonite heat treatment than muffle furnace heating and makes the montmorillonite dehydroxylated earlier. It is worth noting that hot spots formed inside the montmorillonite specimens during the microwave heat treatment. Microwave significantly promotes the shear resistance of montmorillonite, where the maximum increases are 39.94% of cohesion at 600 °C and 20.54% of internal friction angle at 700 °C. This enhancement is due to the rough surfaces and large particles produced by dehydroxylation and Mg-Al spinel synthesis, and the significant degree of disorder state of MMT after dehydroxylation also plays a vital role. The microwave-heated montmorillonite over 500 °C presents good integrity in the water immersion test over 24 h. Considering the shear behavior and water stability, we believe the most reasonable heating interval for microwaves is 500-600°C.

Keywords:
Montmorillonite; Microwave heating; Muffle furnace heating; Shear behavior; Water stability; Microstructure


1. Introduction

The muddy intercalation is a weak material between the upper and lower rock layers in the argillaceous slope, consisting of quartz, clay minerals, calcite, and feldspar11 Haruo S. Process of slip-surface development and formation of slip-surface clay in landslides in Tertiary volcanic rocks, Japan. Eng Geol. 2001;61(4):199-220.

2 Liu J, Xu Q, Wang S, Subramanian SS, Wang L, Qi X. Formation and chemo-mechanical characteristics of weak clay interlayers between alternative mudstone and sandstone sequence of gently inclined landslides in Nanjiang, SW China. Environ Earth Sci. 2020;79:4701-15.
-33 Chai B, Yin K, Du J, Xiao L. Correlation between incompetent beds and slope deformation at Badong town in the Three Gorges reservoir, China. Environ Earth Sci. 2013;69(1):209-23.. And the slopes containing muddy intercalations are prone to slide driven by heavy rainfall or earthquake, resulting in catastrophic economic losses and casualties44 Yang YC, Xing HG, Yang XG, Chen M. Experimental study on the dynamic response and stability of bedding rock slopes with weak interlayers under heavy rainfall. Environ Earth Sci. 2018;77:12:433.. The shear failure of muddy intercalation under the water function is mainly due to the clay minerals swelling and softening55 Skempton AW. Long-term stability of clay slopes. Geotechnique. 1964;14(2):77-102.

6 Ali Y. The effects of clay on landslides: a case study. Appl Clay Sci. 2007;37:77-85.
-77 Regmi AD, Yoshida K, Cui P, Hatano N. Development of Taprang landslide, West Nepal. Landslides. 2016;14:1-18.. The clay minerals take account for 60% of muddy intercalation22 Liu J, Xu Q, Wang S, Subramanian SS, Wang L, Qi X. Formation and chemo-mechanical characteristics of weak clay interlayers between alternative mudstone and sandstone sequence of gently inclined landslides in Nanjiang, SW China. Environ Earth Sci. 2020;79:4701-15.,33 Chai B, Yin K, Du J, Xiao L. Correlation between incompetent beds and slope deformation at Badong town in the Three Gorges reservoir, China. Environ Earth Sci. 2013;69(1):209-23.,88 Zhang S, Xu Q, Hu Z. Effects of rainwater softening on red mudstone of deep-seated landslide, Southwest China. Eng Geol. 2016;204:1-13., and among which the montmorillonite (MMT) presents the worst water resistance99 Ohlmacher GC. The relationship between geology and landslide Hazards of Atchison, Kansas, and Vicinity. Curr Res Earth Sci, 2001;244(1):1-16.,1010 Li G, Jiang Z, Feng X, Zhang N, Xu X. Relation between molecular structure of smectite and liquefaction of mudstone. RSC Advances. 2015;5(30):23481-8.. Therefore, ameliorating MMT properties probably reinforces muddy intercalation to prevent structural failure from heavy rainfall or high groundwater content.

The MMT crystal has a unique 2:1 layered structure that two inward-pointing tetrahedral sheets sandwich one octahedral sheet1111 Bergaya F, Lagaly G. Developments in clay science. USA: Elsevier; 2006. Chapter 1, General Introduction: Clays, Clay Minerals, and Clay Science; p. 1-18.. This structure easily absorbs the environmental water and then swells1212 Ferrage E, Lanson B, Sakharov BA, Drits VA. Investigation of smectite hydration properties by modeling experimental X-ray diffraction patterns. Part I. Montmorillonite hydration properties. Am Mineral. 2005;90(8-9):1358-74.,1313 Ferrage E, Kirk CA, Cressey G, Cuadros J. Dehydration of Ca-montmorillonite at the crystal scale. Part I: structure evolution. Am Mineral. 2007;92(7):994-1006.. Besides, the MMT crystal presents the highest cation exchange capacity compared to other clay minerals1010 Li G, Jiang Z, Feng X, Zhang N, Xu X. Relation between molecular structure of smectite and liquefaction of mudstone. RSC Advances. 2015;5(30):23481-8.,1414 Greeshma G, Zhang F, Andrew JA. Towards understanding the microstructural and structural changes in natural hierarchical materials for energy recovery: in-operando multi-scale X-ray scattering characterization of Na- and Ca-montmorillonite on heating to 1150 degrees C. Fuel. 2017;196:195-209.. High-temperature treatment is a popular approach to modify MMT by increasing adsorption1515 Attar LA, Safia B, Ghani BA. Uptake of 137Cs and 85Sr onto thermally treated forms of bentonite. J Environ Radioact. 2018;193-194:36-43.. The pure MMT undertakes dehydration, dehydroxylation, layered structure collapsing, and decomposition/melting-recrystallization with a temperature ranging from room temperature to 1000 °C1414 Greeshma G, Zhang F, Andrew JA. Towards understanding the microstructural and structural changes in natural hierarchical materials for energy recovery: in-operando multi-scale X-ray scattering characterization of Na- and Ca-montmorillonite on heating to 1150 degrees C. Fuel. 2017;196:195-209.,1616 Wu P, Wu H, Li R. The microstructural study of thermal treatment montmorillonite from Heping, China. Spectrochim Acta A Mol Biomol Spectrosc. 2005;61(13-14):3020-5.

17 Bayram H, Önal M, Yılmaz H, Sarıkaya Y. Thermal analysis of a white calcium bentonite. J Therm Anal Calorim. 2010;101(3):873-9.
-1818 Emmerich K, Steudel A, Merz D. Dehydroxylation of dioctahedral smectites in water vapor atmosphere. Appl Clay Sci. 2017;137:1-5.. Besides, the thermal stability, the structural transformation process, and the high-temperature products of MMT were significantly influenced by the interlayer species1919 Chen Q, Zhu R, Ma L, Zhou Q, Zhu J, He H. Influence of interlayer species on the thermal characteristics of montmorillonite. Appl Clay Sci. 2017;135:129-35.. Furthermore, some investigations involve the MMT structural evolution in bentonite via high-temperature treatment1717 Bayram H, Önal M, Yılmaz H, Sarıkaya Y. Thermal analysis of a white calcium bentonite. J Therm Anal Calorim. 2010;101(3):873-9.,2020 Zhang Y, Liu Q, Wu Z, Zhang Y. Thermal behavior analysis of two bentonite samples selected from China. J Therm Anal Calorim. 2015;121(3):1-9.. These bentonites generally contain inclusions, e.g., clay minerals (kaolinite, illite, and chlorite) and nonclay minerals (silica polymorphs, zeolites, feldspar, and carbonates)1717 Bayram H, Önal M, Yılmaz H, Sarıkaya Y. Thermal analysis of a white calcium bentonite. J Therm Anal Calorim. 2010;101(3):873-9.. However, these inclusions fail to affect the start-stop temperature of the crystal structure changes of MMT.

Microwave-assisted heating is an efficient thermal treatment that fastens the reaction time2121 Arpia AA, Chen WH, Lam SS, Rousset P, de Luna MDG. Sustainable biofuel and bioenergy production from biomass waste residues using microwave-assisted heating: a comprehensive review. Chem Eng J. 2021;403:126233.,2222 Perez-Martinez BT, Aboudzadeh MA, Schubert US, Leiza JR, Tomovska R. Microwave irradiation versus conventional heating assisted free-radical copolymerization in solution. Chem Eng J. 2020;399:125761.; e.g., microwave-assisted acid treatment modifies MMT2323 Korichi S, Elias A, Mefti A, Bensmaili A. The effect of microwave irradiation and conventional acid activation on the textural properties of smectite: comparative study. Appl Clay Sci. 2012;59-60:76-83.

24 Franco F, Pozo M, Antonio Cecilia J, et al. Effectiveness of microwave assisted acid treatment on dioctahedral and trioctahedral smectites. The influence of octahedral composition. Appl Clay Sci. 2016;120:70-80.
-2525 Pardo L, Cecilia J, López-Moreno C, Hernández V, Pozo M, Bentabol M, et al. Influence of the structure and experimental surfaces modifications of 2:1 clay minerals on the adsorption properties of methylene blue. Minerals (Basel). 2018;8(8):359.. However, the treatment temperatures in these investigations are lower than 100 °C. Regarding the microwave-assisted high-temperature treatment, Santana et al. considered the structural evolution of clay at microwave and conventional heat functions; still, they lacked investigating the pure MMT under microwave-assisted heat treatment2626 Santana LNL, Gomes J, Menezes RR, Neves GA, Lira HL, Segadães AM. Microstructure development in clays upon heat treatment: kinetics and equilibrium. Appl Clay Sci. 2017;135:325-32.. In our previous study, microwave heating has been proven to enforce muddy intercalation effectively2727 Hu Q, Gu Y, Zeng J, He L, Tang H, Wei G, et al. Microwave irradiation reinforcement of weak muddy intercalation in slope. Appl Clay Sci. 2019;183:105324.. However, the role of MMT played in the reinforcement was not identified. Although MMT probably presents a similar process exposed to microwaves and conventional resistance heating, its shear behavior and water stability after microwave treatment have not been investigated, which is vital to further the microwave reinforcement mechanism for muddy intercalation.

This study conducted microwave heating and muffle furnace heating of MMT specimens and compared the test results. The crystal phases were characterized by X-ray powder diffraction. The micromorphology was observed by scanning electronic microscopy. The shear behavior was measured by the direct shear test. The water immersion test estimated the water stability.

2. Materials and Methodology

2.1. Material properties and specimen preparation

The MMT sample was provided by Chengyu Mineral Products CO. Ltd and ground to 200 mesh. In order to obtain the oxide composition and mineral composition of the MMT samples, a small amount of received MMT powder samples were dried at 105°C for 4 hours. Then the XRF and XRD tests were performed, respectively. Furthermore, the XRF result is shown in Table 1. A 150 g powder sample was mixed with deionized water at a mass ratio of 1:0.2. The well-mixed sample was compacted to a cylindrical-shaped specimen with a diameter of 50 mm and a height of 50 mm. Subsequently, the cylindrical specimens were dried at 105 °C for four hours to remove the moisture. Eventually, the specimen was wrapped in plastic film to prevent environmental contamination.

Table 1
XRF results of MMT sample.

2.2. Heating apparatus and experimental conditions

The used microwave apparatus was custom-made by CHANGEMW Co. Ltd, as shown in Figure 1. The apparatus comprises a single microwave source, water coolant, metal cavity (length, width, and height are 25cm, 30cm, and 26cm, respectively), BJ-26 waveguide, operating system, and power supply, touch panel, infrared thermometer, and alumina fiber. The microwave with 2.45 GHz in frequency is generated by the microwave source and propagates from the source to the cavity through the waveguide. The microwave heating experiment used the temperature control mode, where the output power is adjusted from 0.5 kW to 1.4 kW based on the preset temperature curve. Before microwave heating, the MMT specimens were held up with an alumina ceramic plate, avoiding direct contact between the specimen and the insulation material in the cavity, which might cause the high-temperature specimen to stick to the insulation material. And then each specimen was individually heated.

Figure 1
Schematic diagram of microwave heating apparatus.

The muffle furnace used is an SX2-5-12A box resistance furnace. The output power is 5 kW, the length, width, and height of the cavity are 300mm, 200mm, 120mm, individually. 2-3 specimens were put into the cavity for heat treatment in each batch.

All specimens were heated to preset maximum temperature (300-800 °C at 100 °C increments) and held for 30 min, and after that, the power was shut down, and the specimens were allowed to cool to room temperature in the cavity. It is worth noting that five specimens were included for comparison at each temperature, and a total of 60 high-temperature treated MMT specimens were produced; among them, the microwave heated specimens and muffle furnace heated specimens are half each.

2.3. Characterization methods

2.3.1. Thermogravimetric analysis

The thermogravimetric analysis was performed on the received MMT powder samples. The analyzer used is the Netzsch STA 449C synchronous thermal analyzer, heated in the air atmosphere from room temperature to 900 °C at a heating rate of 5 °C/min.

2.3.2. Mass loss of heat-treated specimens

Five specimens heated at the same temperature are conducted to determine the average mass loss produced by the two heat treatment methods.

2.3.3. Direct shear test

A total of 55 cylindrical specimens with a diameter and height of about 5 cm were conducted to the direct shear test by a YZW-30 shear instrument, including 5 specimens dried in the oven at 105 °C, 25 microwave heat-treated specimens (300-700 °C, 5 specimens at the same temperature), and 25 muffle furnace heat-treated specimens (300-700 °C, 5 specimens at the same temperature). The preset normal stress adopted is 0-2 MPa at 0.5 MPa increments. As shown in Figure 2, after applying the preset normal stress, the shear force was applied continuously until damage to the specimen, and the maximum shear force was recorded. Then, calculate the actual normal stress and shear stress (due to the sample shrinkage, the diameter is not the standard 5cm, so the actual stress needs to be calculated) of the same set of specimens (5 specimens at the same temperature). Then draw the same set of data in the analysis software with normal stress as the x-axis and shear stress as the y-axis. Finally, according to the linear fitting results of 5 points, the y-axis intercept is the cohesion, and the slope of the straight line is the internal friction angle. That is the method to obtain the shear strength parameters of the specimens. Of course, it is worth noting that if data deviate too much in the same set, it can be deleted to obtain the best linear fitting result.

Figure 2
Schematic diagram of direct shear test.

2.3.4. XRPD test

The fragments of each specimen after the direct shear test were collected separately. In order to explore whether the microwave heating caused hot spots inside the specimens, the internal and external fragments of specimens (one specimen at the same temperature) were selected separately and ground into 200 mesh with an agate mortar. Then the powder samples were prepared for the XRPD test. For comparison, the specimens heated by the muffle furnace are subjected to the same operation. The mineralogical compositions of the specimens heat-treated by microwave and muffle furnace were determined over the range of 3-65° (2θ) at a scanning rate of 5°/min on an Ultima IV multipurpose X-ray powder diffractometer (XRPD). The measurements were conducted at 40kV and 40mA with Cu-Kα radiation (λ=1.54056 Å). The chemical formula of MMT, the interlayer space of MMT crystals, and the crystalline phase quantification were carried out in Jade 6.5. The mass percentage of MMT is calculated by the K value method.

2.3.5. SEM test

In order to clarify the microstructure of MMT under microwave heating, especially the development of micro-cracks and micro-pores, we carried out scanning electron microscopy tests on MMT samples before and after microwave treatment. The samples were selected from the surface of the fragments after the direct shear test and polished by sandpaper. We used a ZEISS EVO MA 15 SEM instrument, the secondary electron imaging mode was used in the test, the accelerated voltage, emission current, and working distance are 20kV, 50 mA, and 9.5-11.5mm, respectively.

2.3.6. Water immersion test

We conducted the water immersion test for the MMT samples after heat treatment. After the direct shear test, we selected the appropriate size fragments of the MMT specimens and smoothed the surface with sandpaper. Then weigh the mass of each fragment, put the fragments into the 800 mL beaker individually, and put 20 times the mass of deionized water of the fragments in the beaker, then the immersion test began. It is worth noting that the pH of the deionized water we used is 6.32. After 24 h of immersion, we observed the fragments in the beaker and estimated the water stability based on the integrity of the MMT fragments. Finally, we explored the effect of long-term immersion in water on the mineralogical composition of MMT specimens. After 20 days of soaking, the specimens were taken out and dried at 105 °C for 4 hours, then ground to 200 mesh and characterized by XRPD.

3. Results and Discussion

3.1. Thermogravimetric analysis

The thermogravimetric curve of received MMT samples is shown in Figure 3. Combined with the DTG curve, the thermogravimetric change of MMT can be divided into four stages. The first stage is from room temperature to 196 °C. At this stage, the mass loss reaches 11.3%, and MMT loses adsorbed water and interlayer water on a large scale. Stage II is from 196 °C to 508.3 °C, with a low mass loss, mainly continuing to lose the small amount of incompletely removed interlayer water. But when the temperature exceeds 508.3 °C, before 719.2 °C, the mass loss of MMT speeds up again. The mass loss at this stage reaches 4.25%, which is mainly caused by the dehydroxylation of MMT. When the temperature exceeds 719.2 °C, the mass of MMT decreases at a low rate, caused by the evaporation of hydroxyl groups that were incompletely removed in the previous stage.

Figure 3
Thermogravimetric curve of received MMT samples.

3.2. Mineralogical and microstructure evolution

Figure 4a illustrates the XRPD patterns of MMT before and after microwave heating. Owing to the un-uniform heating of the microwave, the powders samples used for XRPD tests were sampled from the surface of the MMT specimens to prevent the test results from interfering caused by hot spots. The XRPD results showed that the MMT belongs to the calcium-based MMT (Ca0.2(Al, Mg)2Si4O10(OH)2·4H2O), which mainly consists of 57% MMT, 30.7% cristobalite, 5.3% albite, and 4% quartz. The interlayer space is calculated as 15.0937 Å in the received MMT samples, and it reduces to 9.7212 Å at 300 °C. Besides, the value of 2θ of MMT diffraction peak offsets from 5.6 ° of 105 °C to 9.1 ° of 300 °C, which also proves the interlayer spacing reduction. Subsequently, the intensity of the MMT diffraction peak keeps constant at 300-600 °C. However, it sharply decreases at 600-700 °C, and a small amount of magnesia-alumina spinel peaks are detected at 700 °C. Eventually, when the temperature reaches 800 °C, the MMT diffraction peak intensity was further reduced, and an apparent increase is observed in magnesia-alumina spinel and cristobalite. The mass percentage of these minerals can be seen in Figure 3b.

Figure 4
XRPD patterns and quantitative of MMT before and after microwave heating.

The mineralogical changes of microwave heat-treated specimens reveal three stages in the MMT microstructure evolution, which are 105-300 °C, 300-600 °C, and 600-800 °C, respectively. The MMT crystal advantages in the absorption and cation exchange capacity, numerous adsorbed water exists among the MMT particles, and numerous interlayer water exists in the interlayer space2828 Osipov VI. Nanofilms of adsorbed water in clay: mechanism of formation and properties. Water Resour. 2012;39(7):709-21.. The MMT exposed to microwaves dehydrates the adsorbed water and interlayer water at 105-300 °C1717 Bayram H, Önal M, Yılmaz H, Sarıkaya Y. Thermal analysis of a white calcium bentonite. J Therm Anal Calorim. 2010;101(3):873-9.. Since the adsorbed water and interlayer water are non-combined water, the MMT crystal avoids structural failure, but the interlayer space reduces among particles and crystal layers2929 Hong W, Meng J, Li C, Yan S, He X, Fu G. Effects of temperature on structural properties of hydrated montmorillonite: experimental study and molecular dynamics simulation. Adv Civ Eng. 2020. Consequently, MMT can still be detected from the XRPD patterns, exhibiting the diffraction peaks to offset and the interlayer space to reduce. The MMT continues to dehydrate at 300-600 °C and initiates to dehydroxylate at an uncertain temperature between 300-600 °C, and this is evidenced by the MMT’s diffraction peaks offset and intensity reduction in XRPD patterns. The OH- loss in Al-O octahedron destroys the crystal structure to induce the diffraction peaks intensity to decrease1616 Wu P, Wu H, Li R. The microstructural study of thermal treatment montmorillonite from Heping, China. Spectrochim Acta A Mol Biomol Spectrosc. 2005;61(13-14):3020-5., as shown in Figure 4. During this stage, the dehydroxylated MMT gradually decomposes and recrystallizes to form the Mg-Al spinel. However, Wu et al. and Chen et al. declared that the MMT formed cordierite at 900 °C1616 Wu P, Wu H, Li R. The microstructural study of thermal treatment montmorillonite from Heping, China. Spectrochim Acta A Mol Biomol Spectrosc. 2005;61(13-14):3020-5.,1919 Chen Q, Zhu R, Ma L, Zhou Q, Zhu J, He H. Influence of interlayer species on the thermal characteristics of montmorillonite. Appl Clay Sci. 2017;135:129-35.. This difference is due to the relatively high alumina content (16.941%) in the received samples. Schreyer et al. explained that alumina’s high content in the MgO-Al2O3-SiO2 system would lead to spinel formation3030 Schreyer W, Schairer JF. Compositions and structural states of anhydrous mg-cordierites: a re-investigation of the central part of the system MgO–Al2O3–SiO2. J Petrol. 1961;2(3):324-406.. Besides, Wu et al. indicated that the presence of cristobalite could increase the required temperature to form cordierite due to the low activation of cristobalite at high temperatures3131 Wu J, Lu C, Xu X, Wang D, Sang Y, Zhang C. Influence of silica phase transformation on synthesis of cordierite ceramic. J Aust Ceram Soc. 2017;53(2):499-510.. Therefore, the high content cristobalite suppresses the cordierite to form and promote the synthesis of Mg-Al spinel.

Figure 5 illustrates the comparison between the inside and outside of the microwave heat-treated specimens (marked with MW) and muffle furnace heat-treated specimens (marked with MF) at 300 °C, 500 °C, 700 °C. First, the XRPD patterns of specimens produced by different heat treatment methods are significantly different at 300 and 700 °C. At 300 °C, the specimens heat-treated in the muffle furnace have almost no diffraction peaks shift than the samples dried at 105 °C. This phenomenon means that the interlayer water of muffle furnace heat-treated specimens did not remove on a large scale. And the microwave heat treatment seems to make the MMT diffraction peak disappear faster, whether internal (marked with INT) or external (marked with EXT). The XRPD patterns at 500 °C are relatively similar. In addition, we first pay attention to the microwave heat-treated specimens for the inside and outside of the same specimen. We can find that the XRPD patterns of the internal and external specimens heat-treated by microwave at 300,500 °C are the same, but at 700 °C, the Mg-Al spinel diffraction peaks are more prominent inside the specimen. And more Mg-Al spinel diffraction peaks were also detected in the microwave heat-treated MMT specimen at 800 °C, as shown in Figure 3. As we know, microwave heating poses a characteristic of provisioning high microwave energy into dielectric materials with deeper penetration for internal heat generation2121 Arpia AA, Chen WH, Lam SS, Rousset P, de Luna MDG. Sustainable biofuel and bioenergy production from biomass waste residues using microwave-assisted heating: a comprehensive review. Chem Eng J. 2021;403:126233.. The phenomenon we observed confirms that during the microwave heat treatment of the MMT specimen, hot spots with a higher temperature than the actual external monitoring temperature were formed inside the specimen. In addition, for comparing the internal and external heat-treated specimens in the muffle furnace, the internal and external XRPD results after heat treatment at the same temperature are the same, which means that we can regrade the muffle furnace heat treatment as uniform heating.

Figure 5
Internal and external comparison of the heat-treated specimens.

From the XRPD results, we found two critical phenomena. The first phenomenon is that the microwave heat treatment of MMT specimens has higher efficiency, and at the same heat treatment temperature, the microwave heating reaction process is faster. The second important phenomenon is the existence of hot spots inside the microwave heat-treated MMT specimens. In fact, for the first phenomenon, the research of Whittaker3232 Whittaker AG. Diffusion in microwave-heated ceramics. Chem Mater. 2005;17(13):3426-32. shows that the electric field component of the microwave radiation could concentrate the lattice defects and enhance ion mobility at the interface. The presence of microwaves will improve the rate of mass transport at a given temperature. Therefore, the first phenomenon is supported by literature, and microwave heating has an efficiency advantage compared with muffle furnace heating. In addition, regarding the hot spots that may exist in the microwave heat-treated specimens, because of the complicated phase composition of the MMT samples, the dielectric constant of the samples is difficult to calculate, so it is difficult to predict the location of the hot spot inside the specimen, so we sampled from the surface of the specimen and the center of the specimen and conducted the XRPD tests. Fortunately, we confirmed the existence of the hot spot through the XRPD tests.

Compared with muffle furnace heat treatment, microwave heat treatment accelerates the reaction process when heating the MMT specimens. However, from the XRPD results of the specimens heat-treated at 300, 500, and 700 °C, the reaction process of the muffle furnace heat-treated specimens is still consistent with the microwave heat-treated specimens. Still, the muffle furnace must provide a higher temperature to achieve the same process as the microwave heat treatment. Therefore, we carried out the scanning electron microscope observation on the microwave heat-treated specimens to explore the influence of high-temperature heat treatment on the microstructure of MMT.

Figure 6 presents the micromorphology of specimens before and after microwave heating. Generally, the 105 °C dried specimen has a dense structure without large cracks. It presents some narrow cracks with a diameter of fewer than 1 μm which accompanies few tiny pores. These cracks” width propagates to 2-3 μm at 300 °C, so do the pores. Figure 6c still clearly identifies the layer structure of MMT. When the temperature exceeds 600-700 °C, the structure became more porous. Some of the mineral particles that occluded together mechanically are chemically combined under the effect of a high temperature, and some cracks are observed on the aggregate’s edge. The temperature of 800 °C creates some layered particles with sharper edges than those at lower temperatures in the MMT. By comparing the SEM images of Mg-Al spinel in the research of Li et al3333 Li D, Lu M, Cai Y, Cao Y, Zhan Y, Jiang L. Synthesis of high surface area MgAl2O4 spinel as catalyst support via layered double hydroxides-containing precursor. Appl Clay Sci. 2016;132-133:243-50., we think this substance is Mg-Al spinel.

Figure 6
SEM images of MMT specimens before and after microwave heating.

3.3. Macro-morphology and physical properties

Figure 7 shows the specimen macro-morphology before and after heat treatment. The color of specimens changed from the light olive of the virgin specimen to white at 105 °C, then became pale-yellow with the temperature increasing. Besides, numerous cracks occur after microwave heat treatment, and the number increases as temperature rise. When the temperature reaches 700 °C, the cracks of microwave-heated specimens expand obviously, and the specimens lose their integrity at 800 ° C. In comparison, the crack development of the muffle furnace heat-treated specimens is more stable. From 300 °C to 800 °C, the number of cracks on the specimens’ surfaces gradually increases, but the size does not increase significantly, especially for the specimens heated at 700 and 800 °C. The muffle furnace heat-treated specimens still kept good integrity, unlike the specimens after microwave treatment.

Figure 7
Specimen macro-morphology before and after heat treatment.

In fact, we can clearly see from Figure 7 that at 300-600 °C, the crack development of the specimens produced by the two different heating methods is similar. But when the temperature reaches 700 and 800 °C, the crack development shows a significant difference, reflecting the different effects of microwave and traditional heating on MMT specimens. We guess that the formation of this phenomenon is related to the hot spots inside the microwave-heated MMT specimens, and the existence of hot spots has been confirmed in section 3.2. We believe that the hot spot will lead to the rapid increase of cracks and destroy the integrity of the specimens.

The comparison of specimens’ mass loss heated by two methods is shown in Figure 8. The green line in the figure illustrates the mass change curve of the specimens after heat treatment in the muffle furnace. Compared with the thermogravimetric curve of the received sample shown in Figure 2, the trends of the two curves are the same. However, the mass change curve of the specimens after microwave heat treatment shown by the red line is obviously different from the two curves mentioned above. We can learn from the thermogravimetric curve that MMT will remove a large amount of absorbed water and interlayer water at room temperature - 196 °C, and dehydroxylate at 508.3 °C - 719.2 °C, this process can obviously correspond to the specimens heat-treated in the muffle furnace. However, the mass of the specimens heat-treated in the microwave oven began to drop significantly before 500. This phenomenon corresponds to the faster microwave heating process observed in Section 3.2. The mass of the microwave heat-treated specimens re-started to drop sharply at about 400 °C, and it started to level off around 700 °C. However, the mass of the muffle furnace heat-treated specimens re-started to drop sharply at about 500 °C, and it continues to decrease at 700-800 °C. This phenomenon proves that the microwave can effectively increase the thermal reaction rate of MMT once again.

Figure 8
Specimen mass loss before and after heat treatment.

3.4. Shear behavior

As shown in Figure 9, linear fitting was performed with the maximum shear stress and actual normal stress obtained in the direct shear test. The y-axis intercept and slope of the straight line are the specimens’ cohesion and internal friction angle, respectively. Table 2 presents the cohesion and internal friction angle of the specimens heat-treated by microwave and muffle furnace. Figure 10a and Figure 10b illustrate the cohesion and internal friction angle of specimens before and after heat treatment by the microwave oven and muffle furnace. Because the microwave heat-treated specimens lost their integrity at 800 °C, the direct shear test results did not involve the 800 °C heat-treated specimens. The cohesion and internal friction angle are calculated and fitted by the Akima spline in Origin Pro 2020.

Figure 9
Linear fitting results of MMT specimens after the direct shear test.
Table 2
Cohesion and internal friction angle of specimens.
Figure 10
Comparison of shear behavior of MMT specimens.

High-temperature heat treatment significantly increases the MMT resistance to shear behavior. The microwave heat-treated specimens present the highest cohesion at 600 °C, which is 1.76MPa, and the cohesion of the muffle furnace heat-treated specimens reached 1.93 MPa at 700 °C. However, the cohesion of microwave heat-treated specimens decreased slightly at 105-400 °C, and the cohesion of muffle furnace heat-treated specimens slightly reduced at 105-300 °C. Combining sections 3.2 and 3.3, we know that the MMT specimens continue to dehydrate at 105-400 °C, and the cohesion should theoretically increase as the intermolecular force increases due to the interlayer spacing reduction. However, we cannot ignore the macro-crack propagation inside the specimens also because of the interlayer spacing reduction. The cohesion of the microwave heat-treated specimens continues to decrease to 400 °C before it increases, but the cohesion of the muffle furnace heat-treated specimens continues to rise from 300 °C to 700 °C. We observed above is because microwave heat treatment has higher efficiency, which leads to faster dehydration and dehydroxylation of the specimens. Because the water in the microwave heat-treated specimens loses more and faster than that of the muffle furnace heat-treated specimens, and hot spots will be generated during the microwave heating process, which causes the better development of cracks inside the specimens. The porous structure lacks strong contact points to resist a higher shear force. Therefore, the cohesion of the muffle furnace heat-treated specimens is greater than that of microwave heat-treated specimens. The cohesion of the microwave heat-treated specimens exceeds that of the muffle furnace heat-treated specimens until the large-scale dehydroxylation of the microwave heat-treated specimens is at 500-600 °C. On the one hand, the structure of the specimens shrank due to dehydroxylation, and some larger size of particles were formed, accompanied by numerous shrinkage cracks, resulting in an increase in the internal roughness of the specimens. And at 700 °C and above, Mg-Al spinel appeared in the specimens, and it is harder than MMT particle, which will also lead to an increase in shear strength of the specimens. On the other hand, the significant degree of disorder state of MMT after dehydroxylation cannot be ignored. The appearance of more active sites will lead to the local combination of the internal structure of the specimens3434 Garg N, Skibsted J. Thermal activation of a pure montmorillonite clay and its reactivity in cementitious systems. J Phys Chem C. 2014;118(21):11464-77., thereby enhancing the shear strength of the specimens. But in the end, due to the influence of hot spots, the microwave heat-treated specimens cracked seriously at 700 °C, the crack re-control the shear resistance, and the cohesion dropped again.

For the internal friction angle of the MMT specimens after heat treatment, the internal friction angle of the specimens shows an upward trend from 105-700 °C, except for the slight decrease of the microwave heat-treated sample at 400 °C. Same as the cohesion, the internal friction angle of the specimens heat-treated in the microwave oven is lower than that of the muffle furnace at 300-500 °C. The internal friction angle of the microwave heat-treated specimens does not exceed the internal friction angle of the muffle furnace heat-treated specimens until 600 °C. In fact, the internal friction angle of the MMT specimens after heat treatment is comprehensively controlled by particle size, cracks, and phase composition. The increment of internal friction angle at low temperature (before the large sale of dehydroxylation, no phase change has been formed) is because MMT loses the adsorbed water and interlayer water to dense the particles, the MMT particles that are initially smaller than 80 μm are clustered together to form larger MMT particles, which will increase the friction between the particles. This effect is sufficient to offset the cracks caused by the shrinkage of the specimens, so the internal friction angle of the specimens increased. Microwave heat-treated specimens begin to dehydroxylate earlier and form denser crystals due to the interlayer structure collapsing, at the same time, the numerous active sites generated by dehydroxylation of MMT can not be ignored, which theoretically makes the internal friction angle rise faster. However, due to the existence of hot spots inside the MMT specimens heat-treated by microwave, more cracks were generated, especially at 700 °C, the difference in cracks was more prominent. Under the similar area of the shear surface (circular section of the specimen), the effective shear area of the specimens is reduced, and there are fewer supporting points for resisting the shear force. Therefore, the internal friction angle of the microwave heat-treated specimens and the muffle furnace heat-treated specimens is close.

3.5. Water stability

Water is proved to dominate the stability failure of the slope existing muddy intercalation. According to the study of Sun et al.3535 Sun H-Y, Pan P, Lü Q, Wei Z-L, Xie W, Zhan W. A case study of a rainfall-induced landslide involving weak interlayer and its treatment using the siphon drainage method. Bull Eng Geol Environ. 2019;78(6):4063-74., the cohesion and internal friction angle of muddy intercalation decrease about 60% and 39% from the natural to saturation state. Thus, evaluating the water resistance is necessary to muddy intercalation reinforcement.

Figure 11 exhibits the water immersion results of MMT after heat-treated by the microwave oven and muffle furnace. First, we observed the water stability of the microwave heat-treated specimens. The specimen heat-treated by microwave at 300 °C fails to keep integrity even less than five seconds. The 24 h soaking destroyed the 300 °C heat-treated specimens, where the specimen completely disintegrated into particles with a diameter of 2-3 mm. Although the specimen of 400 °C still disintegrates after slight shaking, the structure can be considered relative integrity. The specimens heated over 500 °C significantly promote MMT resistance to the water, where no secondary cracks and fragments are observed.

Figure 11
Water stability of MMT after heat treatment.

For comparison, we also conducted a water immersion test on the muffle furnace heat-treated specimens. We can easily find that the 300 °C heat-treated specimens began to disintegrate after being immersed in water for 5 seconds. The difference between the microwave heat-treated specimen is that the muffle furnace heat-treated specimen was directly disintegrated into particles of a small size. After 24 h of water immersion, it disintegrated completely. The 400 °C heat-treated specimens disintegrated into particles with a diameter of 4-5 mm, larger than the particle size after the microwave heat-treated specimen disintegrated at 300 °C. The specimen heat-treated by microwave at 500 °C was still damaged under slight disturbance after 24 h of water immersion, which is also different from the microwave heat-treated specimen. The specimens heat-treated at 600-800 °C showed good water resistance.

Figure 12 demonstrates the mineralogical composition of heat-treated specimens before and after 20 days of the water immersion test. For the specimens after microwave heat treatment (marked with MW), We can easily find that after 20 days of immersion in water, the specimens treated at 300 °C and 400 showed significant changes in the diffraction peak position of MMT. Moreover, the MMT crystal interlayer space is almost the same as the received MMT specimen. However, the specimens’ diffraction patterns heat-treated at 500 °C and above barely change before and after water immersion, which means that the MMT specimens treated at 500 °C are no longer affected by water. We inferred that the microwave heat treatment at 500°C can completely remove the interlayer water, thereby improving the water-resistance of the MMT specimen. However, according to the XRPD results of the muffle furnace heat-treated specimens (marked with MF), the specimen heat-treated at 500 °C in muffle furnace is still affected by water, the MMT absorbed water again, and the interlayer space increased significantly, this means that the 500 °C heat-treatment in the muffle furnace could not remove the interlayer water among the MMT crystal interlayer area. This phenomenon also reflects the advantages of microwave heat treatment compared to muffle furnace heating.

Figure 12
Specimens mineralogical composition before and after the water immersion test.

Combining the results of Figure 11 and Figure 12, it is found that the water-resistance of the microwave heat-treated specimens is better, so it is necessary to determine the optimal temperature of the microwave heat-treated MMT specimens in terms of water resistance. After microwave heat treatment at 300, 400°C, the specimen is seriously affected by water after water immersion, whether it is macroscopic disintegration or expansion of the crystal layer spacing in the XRPD pattern, so 300,400°C can not effectively enhance the water-resistance of montmorillonite. When the temperature reaches 500°C, since the interlayer water is completely removed, and the thermogravimetric analysis and mass loss of the specimens after microwave heat treatment (Figure 8) indicated that montmorillonite has begun to dehydroxylate on a large scale at 500°C, the interlayer structure of montmorillonite is no longer affected by water. Therefore, 500°C may be the optimal temperature for enhancing the water-resistance of montmorillonite.

4. Conclusions

This study investigates the mechanism of shear strength and water stability enhancement of montmorillonite heated by the microwave oven and muffle furnace from room temperature to 800 °C by evaluating the mineralogical composition, micromorphology, shear behavior, and water stability. We verified the existence of hot spots inside the microwave heat-treated specimens by comparing the XRPD results of the internal and external samples. But the temperature monitoring has been carried out exclusively on the superficial portion of the specimens and, therefore, the exact behavior inside the specimens is unknown. In addition, the influence of the cracks produced by microwave heat treatment has not been evaluated under other types of mechanical stresses. What’s more, this study lacks considering the interaction of multiple minerals in muddy intercalation exposed to microwaves. These should be improved in future research to promote microwave heating in reinforcing the muddy intercalation. The primary conclusions can be summarized as follows:

  1. 1

    The mineralogical evolution of microwave heat-treated montmorillonite can be divided into 105-300 °C, 300-600 °C, 600-800 °C, corresponding to lose absorbed water and interlayer water, small scale of dehydroxylation at an uncertain temperature between 300-600 °C and large scale of dehydroxylation.

  2. 2

    Microwave heat treatment of montmorillonite is more efficient than that of muffle furnace, manifested as dehydroxylation at a lower temperature. In addition, there are hot spots inside the montmorillonite heat-treated specimens, and this is closely related to the massive cracking of montmorillonite at 700 °C and the loss of integrity at 800 °C.

  3. 3

    The microwave significantly promotes the shear resistance of montmorillonite, where the maximum increases are 39.94% of cohesion at 600 °C and 20.54% of internal friction angle at 700 °C. This enhancement is due to the rough surface and large particles produced by dehydroxylation and Mg-Al spinel synthesis, and the significant degree of disorder state of MMT after dehydroxylation also plays a vital role.

  4. 4

    The microwave-heated montmorillonite over 500 °C presents good integrity in the water immersion test over 24 h by completely removing the interlayer water of montmorillonite. Since water dominates the stability failure of slopes containing muddy intercalation, the most reasonable heating interval is 500-600°C, considering the shear behavior and water stability. This is of great significance for promoting the practical application of microwave reinforcement of muddy intercalation slopes.

5. Acknowledgements

This research was supported by the National Natural Science Foundation of China (52078442), Sichuan Science and Technology Program (2019JDJQ0037, 2020JDRC0091, 2021YFSY0006).

6. References

  • 1
    Haruo S. Process of slip-surface development and formation of slip-surface clay in landslides in Tertiary volcanic rocks, Japan. Eng Geol. 2001;61(4):199-220.
  • 2
    Liu J, Xu Q, Wang S, Subramanian SS, Wang L, Qi X. Formation and chemo-mechanical characteristics of weak clay interlayers between alternative mudstone and sandstone sequence of gently inclined landslides in Nanjiang, SW China. Environ Earth Sci. 2020;79:4701-15.
  • 3
    Chai B, Yin K, Du J, Xiao L. Correlation between incompetent beds and slope deformation at Badong town in the Three Gorges reservoir, China. Environ Earth Sci. 2013;69(1):209-23.
  • 4
    Yang YC, Xing HG, Yang XG, Chen M. Experimental study on the dynamic response and stability of bedding rock slopes with weak interlayers under heavy rainfall. Environ Earth Sci. 2018;77:12:433.
  • 5
    Skempton AW. Long-term stability of clay slopes. Geotechnique. 1964;14(2):77-102.
  • 6
    Ali Y. The effects of clay on landslides: a case study. Appl Clay Sci. 2007;37:77-85.
  • 7
    Regmi AD, Yoshida K, Cui P, Hatano N. Development of Taprang landslide, West Nepal. Landslides. 2016;14:1-18.
  • 8
    Zhang S, Xu Q, Hu Z. Effects of rainwater softening on red mudstone of deep-seated landslide, Southwest China. Eng Geol. 2016;204:1-13.
  • 9
    Ohlmacher GC. The relationship between geology and landslide Hazards of Atchison, Kansas, and Vicinity. Curr Res Earth Sci, 2001;244(1):1-16.
  • 10
    Li G, Jiang Z, Feng X, Zhang N, Xu X. Relation between molecular structure of smectite and liquefaction of mudstone. RSC Advances. 2015;5(30):23481-8.
  • 11
    Bergaya F, Lagaly G. Developments in clay science. USA: Elsevier; 2006. Chapter 1, General Introduction: Clays, Clay Minerals, and Clay Science; p. 1-18.
  • 12
    Ferrage E, Lanson B, Sakharov BA, Drits VA. Investigation of smectite hydration properties by modeling experimental X-ray diffraction patterns. Part I. Montmorillonite hydration properties. Am Mineral. 2005;90(8-9):1358-74.
  • 13
    Ferrage E, Kirk CA, Cressey G, Cuadros J. Dehydration of Ca-montmorillonite at the crystal scale. Part I: structure evolution. Am Mineral. 2007;92(7):994-1006.
  • 14
    Greeshma G, Zhang F, Andrew JA. Towards understanding the microstructural and structural changes in natural hierarchical materials for energy recovery: in-operando multi-scale X-ray scattering characterization of Na- and Ca-montmorillonite on heating to 1150 degrees C. Fuel. 2017;196:195-209.
  • 15
    Attar LA, Safia B, Ghani BA. Uptake of 137Cs and 85Sr onto thermally treated forms of bentonite. J Environ Radioact. 2018;193-194:36-43.
  • 16
    Wu P, Wu H, Li R. The microstructural study of thermal treatment montmorillonite from Heping, China. Spectrochim Acta A Mol Biomol Spectrosc. 2005;61(13-14):3020-5.
  • 17
    Bayram H, Önal M, Yılmaz H, Sarıkaya Y. Thermal analysis of a white calcium bentonite. J Therm Anal Calorim. 2010;101(3):873-9.
  • 18
    Emmerich K, Steudel A, Merz D. Dehydroxylation of dioctahedral smectites in water vapor atmosphere. Appl Clay Sci. 2017;137:1-5.
  • 19
    Chen Q, Zhu R, Ma L, Zhou Q, Zhu J, He H. Influence of interlayer species on the thermal characteristics of montmorillonite. Appl Clay Sci. 2017;135:129-35.
  • 20
    Zhang Y, Liu Q, Wu Z, Zhang Y. Thermal behavior analysis of two bentonite samples selected from China. J Therm Anal Calorim. 2015;121(3):1-9.
  • 21
    Arpia AA, Chen WH, Lam SS, Rousset P, de Luna MDG. Sustainable biofuel and bioenergy production from biomass waste residues using microwave-assisted heating: a comprehensive review. Chem Eng J. 2021;403:126233.
  • 22
    Perez-Martinez BT, Aboudzadeh MA, Schubert US, Leiza JR, Tomovska R. Microwave irradiation versus conventional heating assisted free-radical copolymerization in solution. Chem Eng J. 2020;399:125761.
  • 23
    Korichi S, Elias A, Mefti A, Bensmaili A. The effect of microwave irradiation and conventional acid activation on the textural properties of smectite: comparative study. Appl Clay Sci. 2012;59-60:76-83.
  • 24
    Franco F, Pozo M, Antonio Cecilia J, et al. Effectiveness of microwave assisted acid treatment on dioctahedral and trioctahedral smectites. The influence of octahedral composition. Appl Clay Sci. 2016;120:70-80.
  • 25
    Pardo L, Cecilia J, López-Moreno C, Hernández V, Pozo M, Bentabol M, et al. Influence of the structure and experimental surfaces modifications of 2:1 clay minerals on the adsorption properties of methylene blue. Minerals (Basel). 2018;8(8):359.
  • 26
    Santana LNL, Gomes J, Menezes RR, Neves GA, Lira HL, Segadães AM. Microstructure development in clays upon heat treatment: kinetics and equilibrium. Appl Clay Sci. 2017;135:325-32.
  • 27
    Hu Q, Gu Y, Zeng J, He L, Tang H, Wei G, et al. Microwave irradiation reinforcement of weak muddy intercalation in slope. Appl Clay Sci. 2019;183:105324.
  • 28
    Osipov VI. Nanofilms of adsorbed water in clay: mechanism of formation and properties. Water Resour. 2012;39(7):709-21.
  • 29
    Hong W, Meng J, Li C, Yan S, He X, Fu G. Effects of temperature on structural properties of hydrated montmorillonite: experimental study and molecular dynamics simulation. Adv Civ Eng. 2020
  • 30
    Schreyer W, Schairer JF. Compositions and structural states of anhydrous mg-cordierites: a re-investigation of the central part of the system MgO–Al2O3–SiO2. J Petrol. 1961;2(3):324-406.
  • 31
    Wu J, Lu C, Xu X, Wang D, Sang Y, Zhang C. Influence of silica phase transformation on synthesis of cordierite ceramic. J Aust Ceram Soc. 2017;53(2):499-510.
  • 32
    Whittaker AG. Diffusion in microwave-heated ceramics. Chem Mater. 2005;17(13):3426-32.
  • 33
    Li D, Lu M, Cai Y, Cao Y, Zhan Y, Jiang L. Synthesis of high surface area MgAl2O4 spinel as catalyst support via layered double hydroxides-containing precursor. Appl Clay Sci. 2016;132-133:243-50.
  • 34
    Garg N, Skibsted J. Thermal activation of a pure montmorillonite clay and its reactivity in cementitious systems. J Phys Chem C. 2014;118(21):11464-77.
  • 35
    Sun H-Y, Pan P, Lü Q, Wei Z-L, Xie W, Zhan W. A case study of a rainfall-induced landslide involving weak interlayer and its treatment using the siphon drainage method. Bull Eng Geol Environ. 2019;78(6):4063-74.

Publication Dates

  • Publication in this collection
    25 Feb 2022
  • Date of issue
    2022

History

  • Received
    31 May 2021
  • Reviewed
    09 Jan 2022
  • Accepted
    24 Jan 2022
ABM, ABC, ABPol UFSCar - Dep. de Engenharia de Materiais, Rod. Washington Luiz, km 235, 13565-905 - São Carlos - SP- Brasil. Tel (55 16) 3351-9487 - São Carlos - SP - Brazil
E-mail: pessan@ufscar.br