Thermal Migration Behavior of Na⁺, Cu²⁺ and Li⁺ in Montmorillonite

Abstract

The main aim of this paper is to study the cation fixation sites in montmorillonite after heating at different temperatures. Montmorillonite was used to adsorb cations (Na⁺, Cu²⁺ and Li⁺) in the solution, and the montmorillonite-adsorbed cations were heated at different temperatures (unheated, 100 °C, 200 °C and 300 °C) for 25 h. Subsequently, the basal spacing of montmorillonite treated at different temperatures was monitored by X-ray diffraction (XRD). The exchangeable cationic content (Na⁺, Cu²⁺ and Li⁺) in montmorillonite was determined based on an inductively coupled plasma emission spectrometer (ICP-OES). In addition, the stretching and bending vibration changes in the OH group and the Si-O bond in montmorillonite were detected by Fourier transform infrared spectroscopy (FTIR). The vibration changes were related to the cation fixation sites. The XRD data showed that when the heating temperature reached 200 °C, the structure of montmorillonite adsorbing Li⁺ and Cu²⁺ ions completely collapsed, but the layer spacing of montmorillonite adsorbing Na⁺ decreased slightly, which indicated that Li⁺ and Cu²⁺ were more easily able to enter the crystal structure. The ICP-OES results showed that the contents of exchangeable Na⁺, Cu²⁺ and Li⁺ in montmorillonite decreased with the increase in heating temperature, and Li⁺ was more easily fixed by montmorillonite than Na⁺ and Cu²⁺. The FTIR data showed that when montmorillonite adsorbed with Li⁺ was heated at more than 200 °C, a new OH stretching vibration band appeared at 3971 cm⁻¹, which may be caused by the migration of Li⁺ into the octahedral vacancy to form a local trioctahedral structure. Na⁺ has a large radius; it can only be fixed near the OH group and may not enter the tetrahedron/octahedron of montmorillonite. The number of charges carried by Cu²⁺ is high and the dehydration enthalpy of hydrated Cu²⁺ is high. When the heating temperature was greater than 200 °C, Cu²⁺ mainly entered the hexagonal cavity of the tetrahedron and caused slight changes in the OH bending vibration. The vibration of the Si-O bond hardly changed after montmorillonite adsorbed Na⁺, but the stretching vibration peak of the Si-O bond moved to the high value region after adsorbing Cu²⁺ and Li⁺, which was speculated to be related to the migration of Cu²⁺ and Li⁺ into the crystal structure.

1. Introduction

Montmorillonite is a typical layered silicate mineral, which is composed of two layers of silicon-oxygen tetrahedron and one layer of aluminium-oxygen octahedron. The octahedron of montmorillonite has the following two types: one is dioctahedral and only two-thirds of the cation coordination positions of the octahedron are filled with trivalent central atoms; the other is trioctahedral and the cation coordination positions of the octahedron are occupied by divalent cations [1,2,3]. The tetrahedral and octahedral layers of montmorillonite have a considerable degree of ion substitution. Si⁴⁺ in the tetrahedral layer can be replaced by Al³⁺ and Al³⁺ in the octahedral layer can be replaced by Fe³⁺, Fe²⁺, Mg²⁺, etc., so that the structural unit layer has negative charges, which are balanced by exchangeable cations between structural unit layers and at the edge of unit layer [4,5,6]. Heating montmorillonite at 200–300 °C would lead to the fixation of the exchangeable cations, the reduction in interlayer charge and the irreversible collapse of the mineral structure layer, behavior which is called the Hofmann-Klemen effect [7,8,9]. The final fixation sites of cations in minerals in the Hofmann-Klemen effect have been studied for more than 70 years, with no definitive answers [10,11]. There are three explanations for the Hofmann-Klemen effect, as follows: (i) cations migrate into the hexagonal cavity of the tetrahedral sheet [12,13]; (ii) the cation enters the vacancy in the octahedral sheet through the hexagonal channel of the tetrahedral sheet [14]; (iii) cation migration at both sites [15]. The exchangeable cations would remove the bound water on the surface during heating, and cations with small radii could be fixed in the mineral structure, resulting in the reduction in negative charge in the mineral layer [4].

Lithium ion (Li⁺) is one of the most common elements in the interlayer of montmorillonite and its ionic radius is small enough [4]. Relevant studies showed that the Hofmann-Klemen effect is likely caused by the interlayer Li⁺ migration into the lattice structure [4,9]. It is common to study the migration behavior of Li⁺ in heated montmorillonite. Luca et al. [13] used the ⁵⁷Fe nucleus probe to detect the electronic disturbance of montmorillonite during heating. The results showed that Li⁺ would not enter the octahedral site. Gournis et al. [14] studied the lattice structure of lithium-saturated montmorillonite before and after heat treatment at 300 °C with neutron diffraction. The diffraction pattern showed that some Li were fixed in the octahedral sheet, and the rest remained in the interlayer space. Ebina et al. [15] calculated based on density functional theory (DFT) that Li⁺ in montmorillonite could migrate from the interlayer to the hexagonal cavity and the octahedral site when heated at 250–350 °C; the mobility is 60% and 40%, respectively. In addition, other scholars have studied the thermal migration behavior of other cations (Ni²⁺, Zn²⁺, Mg²⁺, Cd²⁺) [4,13,16,17,18], but there is still great controversy about whether the cations are fixed in the hexagonal cavity of the tetrahedral sheet or the previously vacant octahedral vacancy. Therefore, in this paper, three cations (Li⁺ with controversial fixed sites, Cu²⁺ with a similar radius to Li⁺ and Na⁺ with the same valence as Li⁺) are selected to explore the thermal migration behavior of interlayer cations in montmorillonite.

A large number of studies have used infrared spectroscopy to detect the fixed position of cations in clay [12,13,19]. When the molecule is irradiated with infrared light, the chemical bonds or functional groups in the molecule undergo vibration absorption. The absorption frequencies of different kinds of chemical bonds or functional groups are different; they would be in different positions in the infrared spectra, so as to obtain the information of internal chemical bonds or functional groups of clay minerals [20,21,22]. Fourier transform infrared spectroscopy (FTIR) has been widely used in the study of clay minerals.

Previous studies on the thermal migration behavior of single cations in clay have made some progress, but there are few studies on the fixed sites of different kinds of cations in montmorillonite [16,23,24]. Comparing the research results of different authors, it can be observed that the mineral structure, radius and charge of cations affect the cationic migration sites in clay minerals [7,23,25]. Therefore, based on infrared spectroscopy, the thermal migration behavior of different cations in montmorillonite was investigated in this study. The aim is to provide further reference information for the possible thermosetting sites of exchangeable cations in montmorillonite and to explore the influence of the types of cations on their thermosetting sites in clay minerals.

2. Experimental Section

2.1. Sample Preparation

The montmorillonite used in this study was purchased from Xianding Biotechnology Co., Ltd. (Shanghai, China). The Li⁺ solution, Na⁺ solution and Cu²⁺ solution used in the experiment were prepared from Li₂SO₄ (AR), Na₂SO₄ (AR) and CuSO₄ (AR), respectively.

In order to remove the soluble impurities in montmorillonite, it was repeatedly washed with deionized water three times, then dried in an oven at 60 °C for 12 h and grinded into powder in a mortar for standby. In order to prepare Li⁺, Na⁺ and Cu²⁺ montmorillonite (Li-MT, Na-MT and Cu-MT), 2.00 g of montmorillonite was immersed in 50 mL of Li⁺ (1 M), Na⁺ (1 M) and Cu²⁺ (1 M) solution, respectively, placed in an oscillator for about 2 h (50 r/min), and then the solid and liquid were separated by a filter. The separated solid was naturally dried at 20–25 °C. Through the above operations, a total of 4 groups of samples (Mt0, Mt100, Mt200 and Mt300) were prepared. Referring to the relevant literature, each group of samples was heated at a given temperature for 25 h (e.g., Mt0 for unheated samples and Mt100 for heating at 100 °C) [8,12,20].

2.2. Characterization

X-ray diffraction (XRD) was used to characterize the mineral composition in the sample, using an XRD-6100 (Shimadzu, Japan) with Cu-Kα radiation (λ = 0.412 nm) operating at 60 kV and 40 mA, with a 2θ scan range of 2° to 90° and scan rate of 4°/min.

The content of the exchangeable cations (Cu²⁺, Na⁺ and Li⁺) in the sample was determined by extraction with ammonium acetate solution (1 M) at pH 7. In step 1, 25 mg sample was dispersed in 5 mL of ethanol, then 5 mL of ammonium acetate solution was added, and the extract was collected after standing for 24 h. In step 2, 5 mL of deionized water was added to the remaining solid and the extract was collected after 24 h. In step 3, Step 1 and Step 2 were repeated three times. In step 4, the extracts of the same sample were mixed and the cation concentration in the solution was determined by the inductively coupled plasma emission spectrometer (ICP-OES, Agilent 5110, Santa Clara, CA, USA) [19].

The infrared spectra were obtained on a Fourier transform infrared spectra analyzer (PerkinElmer FTIR, Spectrum Two, Waltham, MA, USA) equipped with a DTGS detector. The samples to be tested (2 mg sample and 200 mg KBr) were prepared by KBr tablet pressing technology [8,19]. The samples were tested in the range of 4000–450 cm⁻¹. The scanning times of each sample were 128 cm⁻¹ and the resolution was 4 cm⁻¹.

The infrared spectra were usually divided into the following three regions: near infrared (NIR), medium infrared (MIR) and far infrared (FIR). The spectral vibrations of clay minerals in NIR (12,000–4000 cm⁻¹) include combination and overtone modes of the fundamental vibrations. The combined mode refers to the addition of two or more basic modes, and the overtone mode appears when a basic mode is excited by two or more quantum simultaneously [20]. The combination and overtone modes of water molecules appear at 5500–4500 cm⁻¹ and 7100–6000 cm⁻¹, respectively. In clay minerals, the combination mode (v_OH + σ_OH) and overtone mode (2v_OH) of structural hydroxyl groups appear near 5000–4000 cm⁻¹ and 7000 cm⁻¹, respectively [20]. There are few studies on montmorillonite FIR (400–10 cm⁻¹), mainly because it has no significant absorption bands in the region of 120–50 cm⁻¹ [20]. The thermal migration of cations in montmorillonite is mainly studied based on the vibration changes of OH groups, Si-O and Al-O in the mid-infrared region (4000–400 cm⁻¹) [20]. The vibration forms of OH groups include stretching vibration (v_OH) and bending vibration (σ_OH); the spectral regions are 3750–3000 and 950–600 cm⁻¹, respectively. The stretching vibration of Si-O and Al-O is located at 1200–700 cm⁻¹, and the bending vibration of Si-O and Al-O occurs in the spectral region of 600–400 cm⁻¹ [20].

Compared with NIR and FIR, MIR spectroscopy is more commonly used to study the mineral structure [26,27,28]. In addition, FTIR spectrometers collected in the MIR region are relatively cheap and available in most laboratories [20]. Therefore, in this experiment, the MIR spectroscopy was analyzed in detail to identify the fixed sites of exchangeable cations.

3. Results and Discussion

3.1. XRD Analysis

The montmorillonite used in this study has high purity and contains only a small amount of quartz and other impurities, and the XRD diffraction is shown in Figure 1. All the diffractions include both the basal reflections and the general hk diffractions of the montmorillonite. The characteristic of the basal reflection varies with the hydration state of minerals. The general hk diffractions (marked with asterisks) are the structural characteristics of the montmorillonite layers themselves, which do not depend on interlayer hydration [11,25]. Moreover, the XRD patterns of montmorillonite after heating at different temperatures were studied. The hk-bank positions are the same in any sample and no new peaks that may be related to the new crystal structure were observed; whereas the basal reflection changes in the peak position.

The basal spacing of montmorillonite corresponds to its hydrated structure where hydrated cations are located in the interlayer space. Furthermore, the basal reflection peaks of montmorillonite are related to its chemical composition and the type of exchangeable cations [29]. The d₀₀₁ spacing of unheated samples (Cu-Mt0, Na-Mt0 and Li-Mt0) were all in the range 13.1–14.4 Å (

Table 1. The d₀₀₁ diffraction values of samples at different temperatures.

	d001 (Å)
Heating Temperature (°C)	Cu-Mt	Na-Mt	Li-Mt
unheated	14.1	14.4	13.1
100 °C	12.5	12.6	12.5
200 °C	9.7	12.6	9.9
300 °C	9.6	12.6	9.5

). The value of Li-Mt0 (13.1 Å) was slightly smaller than that of Na-Mt0 (14.4 Å) and Cu-Mt0 (14.1 Å), which was because the hydration degree of Cu²⁺ and Na⁺ was higher than that of Li⁺ [30]. Therefore, the interlayer spacing of Cu²⁺ and Na⁺ in the mineral interlayer was larger than that of Na⁺ in the interlayers.

The d₀₀₁ values of samples treated at 100 °C decreased slightly compared with unheated samples (Table 1). When the heating temperature was 200 °C, the layer spacings of Cu-Mt and Li-Mt were reduced to <10 Å, which was consistent with the thickness of the completely collapsed montmorillonite layer [11,25]. However, the layer spacing of Na-Mt was 12.6 Å, which indicated that the heat treatment would not lead to the complete collapse of the Na-Mt structure. There is an interaction between interlayer cations and the aluminosilicate surface. The interlayer cation is positively charged and the aluminosilicate surface is negatively charged, which can produce electrostatic interactions [30,31]. When the cations were heated into the mineral crystal structure, it could reduce the negative charge carried by the aluminosilicate layers and reduce the spacing of mineral layers. It was inferred from the d₀₀₁ values that Li⁺ and Cu²⁺ were more easily able to enter the mineral crystal structure than Na⁺.

3.2. Exchangeable Cation Content

The contents of exchangeable Cu²⁺, Na⁺ and Li⁺ in the extract of montmorillonite heated at different temperatures were showed in

Table 2. Concentration of Cu²⁺, Na⁺ and Li⁺ in the extract.

	Concentration (mg/L)
Heating Temperature (°C)	Cu-Mt	Na-Mt	Li-Mt
unheated	374.0	162.5	66.9
100 °C	324.5	151.4	59.2
200 °C	307.4	142.9	50.4
300 °C	296.4	139.5	39.4

. Compared with the exchangeable Cu²⁺ content in Cu-Mt0, Cu-Mt100, Cu-Mt200 and Cu-Mt300 decreased to 86.7%, 82.2% and 79.3%, respectively. The exchangeable Na⁺ in Na-Mt100, Na-Mt200 and Na-Mt300 decreased to 93.2%, 87.9% and 85.8% of Na-Mt0, respectively. The exchangeable Li⁺ in Li-Mt100, Li-Mt200 and Li-Mt300 decreased to 88.5%, 75.3% and 58.9% of Li-Mt0, respectively. The results showed that the content of exchangeable Cu²⁺, Na⁺ and Li⁺ in montmorillonite decreased with the increase in temperature. When heated to 100 °C, the content of exchangeable Na⁺ in montmorillonite changed little, while the content of exchangeable Cu²⁺ and Li⁺ decreased greatly. Further, when heated to 200 °C and 300 °C, the decrease rate of exchangeable Li⁺ in montmorillonite was significantly higher than that of Na⁺ and Cu²⁺. In conclusion, Li⁺ was able to be fixed easier by montmorillonite than Cu²⁺ and Na⁺ during heating.

3.3. FTIR Analysis

3.3.1. OH Stretching Vibrations

The FTIR spectra of unheated samples (Na-Mt0, Cu-Mt0 and Li-Mt0) showed an obvious absorption band near 3627 cm⁻¹, which was the OH group stretching vibration band coordinated with the central atom in the octahedron (Figure 2A–C). The stretching vibration of the OH group in montmorillonite is mainly affected by the following two factors: one is the nature of the central atom coordinated with hydroxyl in the octahedron; the other is isomorphism in the crystal. The top oxygen (O_ap) of the tetrahedron can produce local negative charges. When the cations move into the crystal structure, which will neutralize the negative charges, it affects the stretching vibration of hydroxyl [19,32]. During the heating of Na-Mt, the stretching vibration band of OH remained near 3627 cm⁻¹ (Figure 2A). No displacement was detected in Cu-Mt100, and minimal displacement was observed in Cu-Mt200 and Cu-Mt300, ranging from 3627 to 3631 cm⁻¹, respectively (Figure 2B). The stretching vibration change in OH in Li-Mt during heating was obviously different from that of Na-Mt and Cu-Mt. When heated to 100 °C, Li-MT did not change; when the temperature continued to rise, the OH stretching vibration bands of Li-Mt200 and Li-Mt300 moved to 3635 cm⁻¹ and 3640 cm⁻¹, respectively, and a new absorption band appeared at 3671 cm⁻¹ (Figure 2C). According to reports in the relevant literature, during the heating process of Li-Mt, hydrated Li⁺ can dehydrate into the empty octahedral site of montmorillonite to form a local trioctahedral structure (AlMgLiOH), resulting in a new OH stretching vibration band at 3671 cm⁻¹ [19,20]. The experimental results showed that Li⁺ could enter the octahedral structure of montmorillonite, while Cu²⁺ and Na⁺ did not enter the octahedral structure of montmorillonite during heating.

It was shown that the cations entering the hexagonal cavity of clay minerals cause the OH stretching vibration band to move to a higher value [19,20]. For samples Li-Mt0, Na-Mt0 and Cu-Mt0, the charge imbalance in montmorillonite tetrahedral structure is caused by O_ap. When montmorillonite has a dioctahedral structure, OH and O_ap interact in the form of a hydrogen bond to form OH···O_ap, and the interaction between O and H in OH is weakened [19]. When the cations migrate into the crystal structure, the negative charge of O_ap is balanced, the interaction between OH and O_ap is weakened, and the interaction between O and H in OH is enhanced, resulting in the movement of v_OH to a higher wavelength [19].

The movement of the OH stretching band is related to the properties (radius and charge) of interlayer cations. The radii of Cu²⁺, Na⁺ and Li⁺ are 0.72 Å, 0.95 Å and 0.68 Å, respectively [19,33]. Compared with Li⁺ and Cu²⁺, Na⁺ has a larger radius, which makes it unable to enter the hexagonal cavity/vacancy octahedron of montmorillonite. The radius difference between Li⁺ and Cu²⁺ is small, but the dehydration enthalpy of hydrated Cu²⁺ (−502 kcal mol⁻¹) is higher than that of hydrated Li⁺ (−124 kcal mol⁻¹); that is, hydrated Cu²⁺ ions are more difficult to dehydrate into the tetrahedral/octahedral structure of the crystal [20,23].

3.3.2. OH Bending Vibrations

The bending vibration of OH can further provide supplementary data for the migration behavior of cations during montmorillonite heating. The FTIR spectra of unheated samples (Li-Mt0, Na-Mt0 and Cu-Mt0) showed that there were obvious absorption bands near 797 cm⁻¹, 844 cm⁻¹ and 912 cm⁻¹ (Figure 3A–C), which presumably correspond to the OH group bending absorption bands of FeMgOH, AlMgOH and AlAlOH in minerals [34,35,36]. The absorption band at 629 cm⁻¹ may be caused by silicate impurities in the sample.

During the heating process of Na-Mt, the bending vibration of OH did not change significantly, and only the strength allocated to AlMgOH and AlAlOH in Na-Mt300 decreased slightly (Figure 3A). The radius of Na⁺ is larger and its hydrated ions cannot enter the hexagonal cavity of tetrahedron after dehydration, but the layer spacing of montmorillonite decreases when heated to 300 °C, making Na⁺ closer to the OH group, resulting in weak changes in the OH bending vibration band. Compared with Cu-Mt0, the OH bending vibration of Cu-Mt100 did not change (Figure 3B). When the heating temperature was further increased, the OH bending vibration band of Cu-Mt was weakened, the vibration peak of AlMgOH of Cu-Mt200 moved from 844 to 868 cm⁻¹ and the AlAlOH moved from 912 to 925 cm⁻¹. The vibration peak of AlMgOH of Cu-Mt300 appeared at 868 cm⁻¹ and that of AlAlOH appeared at 925 cm⁻¹ (Figure 3B). Cu²⁺ can enter the hexagonal cavity of the tetrahedron during heating. The coulombic repulsion forces of Cu²⁺ may change the direction of the dipole moment of the OH group, thus interfering with the deformation vibration of the OH group. The infrared spectra of Li-Mt showed that when heated to 200 °C and 300 °C, the spectral peaks of AlMgOH appeared near 850 cm⁻¹ and the bending vibration of OH in AlAlOH was hardly observed (Figure 3C). The results showed that Li⁺ may migrate to the hexagonal cavity of the tetrahedron. According to the stretching vibration results of OH in Figure 2C, the migration site of Li⁺ is not singular and can exist in the tetrahedron and octahedron. Skoubris et al. [35] reported that during the heating process of montmorillonite, the hydrated Li⁺ between layers first migrated to the hexagonal cavity after dehydration, and then entered the vacancy octahedral site. In conclusion, Na⁺ cannot enter the hexagonal cavity during montmorillonite heating, but Cu²⁺ and Li⁺ can enter.

3.3.3. Si-O Vibrations

The interlayer cations in minerals migrate into the hexagonal cavities and/or the octahedral vacancies, which changes the stretching vibration and bending vibration of Si-O in the tetrahedral structure. The layer charge of minerals is balanced with the migration of cations, so that the mineral structure of montmorillonite is close to pyrophyllite (typical non-charged dioctahedral mineral) [33,37].

The Si-O stretching vibration peaks of Na-Mt0, Cu-Mt0 and Li-Mt0 were all located near 1035 cm⁻¹ (Figure 3). After heating, the Si-O stretching vibration of the Na-Mt series hardly changed (Figure 3A). Compared with Cu-Mt0, the Si-O band of Cu-Mt100 had no movement; when heated to 200 °C, the Si-O peak value moved from 1035 cm⁻¹ to 1049 cm⁻¹; when heated to 200 °C, the Si-O band widened and the peak moved to 1050 cm⁻¹ (Figure 3B). During the heating process of montmorillonite, the change trend of Li-Mt and Cu-Mt was similar. The Si-O stretching vibration band of Li-Mt100 was located near 1037 cm⁻¹ and its movement could be ignored (Figure 3C). The vibration peaks of Li-Mt200 and Li-Mt300 were 1051 cm⁻¹ and 1053 cm⁻¹, respectively. During the heating process, the structure of montmorillonite became similar to pyrophyllite due to the migration of interlayer Cu²⁺ and Li⁺ (the Si-O stretching vibration peak of pyrophyllite was near 1049 cm⁻¹) [37].

The bending vibration bands of Si-O-Al and Si-O-Si of montmorillonite were located at 520 cm⁻¹ and 467 cm⁻¹, respectively (Figure 3). During heating, the absorption bands of Na-Mt and Li-Mt did not change. Then, when heated to 200 °C, the Si-O bending vibration intensity of Cu-Mt decreased significantly. Compared with Cu-Mt, Li-Mt had no significant change, which may be due to its smaller valence state.

It was concluded that the cationic thermal migration in montmorillonite changes the bond length and Si-O_basal-Si bond angle of the Si-O bond. Cu-Mt and Li-Mt change differently during heating, mainly due to the different fixation sites of Cu²⁺ and Li⁺ [38]. Even if Cu²⁺ and Li⁺ are located at the same site (for example, in a hexagonal cavity of a tetrahedron), their disturbance to Si-O is different. Compared with the divalent cations at the same site in the mineral structure, the electric field intensity of the monovalent cations is lower, so the disturbance to the Si-O bending vibration band is smaller [25,39].

4. Conclusions

In this paper, montmorillonite samples were characterized based on XRD, ICP-OES and FTIR in order to study the thermal migration of cations in the interlayer. The XRD data showed that Li⁺ and Cu²⁺ were more easily able to enter the crystal structure. This was because when the heating temperature reached 200 °C, the layer spacings of Cu-Mt and Li-Mt were <10 Å, which was the layer spacing of completely collapsed montmorillonite, while the layer spacing of Na-Mt was only slightly reduced. Moreover, based on the study data of exchangeable cations in montmorillonite, the fixed content of cations increases as the temperature increases. In addition, Li⁺ was more easily fixed by montmorillonite than Cu²⁺ and Na⁺.

It was found that the radius and charge of exchangeable cations affect their fixed sites in montmorillonite after heating. A new OH stretching vibration band at 3971 cm⁻¹ was observed in the heated Li-Mt200 and Li-Mt300, indicating that Li⁺ migrated to the octahedral vacancy and formed a local trioctahedral structure (AlMgLiOH). The radius of Cu²⁺ is similar to that of Li⁺, but Cu²⁺ can only migrate into the hexagonal cavity of the tetrahedron because the charges carried by Cu²⁺ are higher and the dehydration enthalpy of hydrated Cu²⁺ is higher than that of hydrated Li⁺. Na⁺ has a large radius and cannot penetrate the tetrahedron/octahedron. After heating and dehydration, interlayer hydrated Na⁺ could only be fixed near the OH group, causing slight changes in the bending vibration band of the OH group. The vibration results of the Si-O bond showed that Na-Mt hardly changes with the temperature increase. When Cu-Mt and Li-Mt were heated to 200 °C, the stretching vibration peak of the Si-O bond moved to the higher wavenumber region. In addition, the Si-O bond bending vibration bands of Na-Mt and Li-Mt did not change, but the absorption band strength of Cu-Mt decreased, which may be due to the higher valence state of Cu²⁺ than that of Li⁺.