The Structure and Properties of Sepiolite with Partial Lattice Ions Substituted by Aluminum Ions

Sepiolite was modified with Al³⁺ via hydrothermal reaction. The substitution amount of Al³⁺ for Mg²⁺ and Si⁴⁺ located at sepiolite lattice and the influence of substitution amount on the structure, specific surface area, and surface acidity of Al-modified sepiolite were investigated. On this basis, indigo–sepiolite composite pigments were prepared by Al-modified sepiolite and indigo via grinding method to evaluate the influence of Al-modified sepiolite on the structure, bonding strength, and weather resistance of composite pigment. The crystal structure of Al-modified sepiolite had no obvious change after modification. Al³⁺ mainly substituted Mg²⁺ located at the octahedron of the sepiolite lattice, and the substitution amount was positively related to the dosage of Al³⁺. The specific surface area of Al-modified sepiolite decreased and the distribution of channel size became wider after Al modification. In addition, the absolute value of zeta potential decreased as well as the solid acid sites increased with the increase of Al substitution in Al-modified sepiolite. For indigo–sepiolite composite pigments, the structure of Al-modified sepiolite had no obvious change as well. The adsorption amount of indigo in composite pigment after treating by DMSO and Al content as well as weak acid amount in Al-modified sepiolite presented linear correlation, indicating that Al modification could enhance the bonding strength between indigo and Al-modified sepiolite by increasing the amount of coordinated water with Al. For indigo, Al-modified sepiolite could brighten the color and reduce the weather resistance of the prepared composite pigment. The results of this study provide a new idea and basis for regulating the structure and properties of clay and for studying the preparation of composite pigment and clay functional materials.

Introduction

Maya Blue (MB) pigment is an organic–inorganic composite pigment that widely exists in the murals and codes of ancient Maya ruins (Gettens, 1962; Giustetto et al., 2006; Arnold et al., 2012; Doménech-Carbó et al., 2014; Buti et al., 2018). It has attracted considerable attention because of its characteristic brightness after centuries of vicissitudes (José-Yacamán et al., 1996; Vandenabeele et al., 2005; Chiari et al., 2008; Grazia et al., 2020). MB was confirmed as a complex fabricated by precipitating indigo into palygorskite. Plenty of research studies on MB mainly concerned the type of attachment between indigo and palygorskite and the location of indigo in palygorskite to reveal the mystery of its unique stability (Giustetto et al., 2005; Chiari et al., 2008).

Sepiolite is widely used to prepare composite pigment with indigo and in turn compared with MB because it has a similar structure to palygorskite (Van Olphen, 1966; Giustetto et al., 2011). The result shows that the indigo–sepiolite composite pigment is less stable than MB (Sánchez Del Río et al., 2006; Giustetto et al., 2011). Both sepiolite and palygorskite are fibrous phyllosilicate formed by two continuous [SiO₄] tetrahedrons and an intermittent [MgO₆] octahedron, and the periodic inversion in [SiO₄] tetrahedron forms the channels of sepiolite and palygorskite. The difference between these two minerals is that the inverse period of [SiO₄] tetrahedron in sepiolite is 4, while that in palygorskite is 6, resulting in larger size of channels in sepiolite. In addition, the isomorphic substitution of Al³⁺ usually occurs in [SiO₄] tetrahedron and [MgO₆] octahedron in the two minerals, leading to different Al contents of palygorskite and sepiolite (Giulieri et al., 2012). Therefore, the difference in stability between the indigo–sepiolite composite pigment and MB is extremely possible due to the different channel sizes and Al content of the mineral substrate.

Silicate minerals possess acid–base conjugation formed by negative charge generated by isomorphic substitution, neutralized protons, and countercations in minerals (Ramírez et al., 2011; Tazi et al., 2012). The surface acidity is essentially determined by the electronegativity of the element bonding with oxygen (Busca, 1999), and thus, the Al content will directly affect the surface acidity and basicity of sepiolite and palygorskite. The acid and base in silicate minerals show catalytic activity in organic reactions, e.g., the pyrolysis behaviors of organic matters, the methylbutynol conversion, the Biginelli type reaction of aldehydes, and the synthesis of malononitrile prepolymers (Corma and Martín-Aranda, 1993; Hu et al., 2003; Niwa et al., 2010; Pushpaletha and Lalithambika, 2011; Liu et al., 2013a; Jha et al., 2013; Novikova et al., 2013; Bu et al., 2017; Phukan et al., 2017). The acid–base conjugation in minerals plays a role to fix organic molecules during the reaction, for example, in the polymerization reaction of D, L-Lactid catalyzed by acid-modified montmorillonite, the D, L-Lactid molecules were fixed on the accessible tetrahedral Al sites (act as acid sites) through oxygen atoms (Aslya et al., 2016). The amino group in aminobenzodifurandione dye was protonated by the acid bound to the oxygen atom of silanol (Lewis base) when probing the basicity of solid acids (Spange et al., 2005). In composite materials, the combination of organic molecules and inorganic substrates is usually affected by the solid surface acid. The flavylium dye was stabilized by the solid acid that is derived from an Al impurity in silicate (Kohno et al., 2008). The azobenzene molecule was protonated by Brönsted acid in AlPO₄-5 zeolite and then interacted with the framework oxygen atoms (Polisi et al., 2018). The acidic site montmorillonite framework played an important role to form a strong bond with thioindigo (Ramírez et al., 2011). Indigo possesses a similar structure to thioindigo, and sepiolite and palygorskite have similar acid–base conjugation to silicate minerals as well. Therefore, the acidity and basicity in sepiolite and palygorskite will also affect the bonding strength with indigo and the stability of the composite pigment, while it has not been discussed in the previous research.

The surface acidity and basicity of the minerals are affected by the modified cations since the electronegativity of cations changes. The basicity of sepiolite increased after being modified by Fe³⁺; therefore, Lewis acid CH₃Cl had a greater affinity towards the modified sepiolite result from stronger acid–base interaction (Lazarevic et al., 2011). Two ways were used in cation modification to regulate the surface acidity and basicity of clay minerals. One is that the cations are simply adsorbed in the clay minerals. The polarization of these cations to adsorbed water molecules affects the acidity and basicity of the clay minerals. Montmorillonite, modified with Zn²⁺, Fe³⁺, and Al³⁺ through interlayer cation exchange, had increasing acidity in turn (Jha et al., 2013). Another is the substitution between free cations and lattice cations in clay minerals to change the acidity and basicity according to the electronegativity of cations. Al³⁺, Cr³⁺, H⁺, Na⁺, and La³⁺ were used to modify sepiolite, and only Al-modified sepiolite has super strength acid sites (Corma et al., 1991) since Al³⁺ was introduced in the octahedron of sepiolite, and then the catalytic activity of Al-modified sepiolite for dehydration of ethanol and gasoil cracking was improved (Corma and Perez-Pariente, 1987; Zheng et al., 2010). Therefore, the Al content in the sepiolite can be regulated by the substitution of Al for the lattice cations in sepiolite, thereby changing the surface acidity of the sepiolite and the interaction between organic and inorganic substances.

In this study, sepiolite with low content of Al was modified by hydrothermal reaction with different dosages of AlCl₃ to regulate its solid acidity. The obtained Al-modified sepiolite was used to prepare composite pigment with indigo via the grinding method. The bonding strength between indigo and Al-modified sepiolite and the weather resistance of the composite pigment were evaluated to explore the interaction between reactants.

Experimental

Materials

Sepiolite (Sep) was obtained from Sigma-Aldrich (Shanghai) Trading Co., Ltd. The pattern of XRD and the chemical composition are given in Figure 1 and Table 1, respectively. AlCl₃ 6H₂O (analytically pure) was purchased from Beijing Chemical Plant. Indigo (Id, purity of 98%) was purchased from Shanghai Macklin Biochemical Technology Co., Ltd.

FIGURE 1

FIGURE 1. XRD pattern of Sep.

TABLE 1

TABLE 1. Chemical composition of Sep used in the study.

Preparation of Al-Modified Sep

The suspensions were prepared by mixing 7.00 g of Sep, 70 ml of the solution containing different dosages of AlCl₃ 6H₂O (0.00, 3.50, 7.00, and 70.0 mmol). The suspensions were kept in a 100 ml tetrafluoroethylene-lined autoclave at 120°C for 10 h. The precipitate was centrifuged and washed with deionized water until Cl⁻-ion-free and then dried at 60°C for 24 h in an oven. Finally, the dry precipitate was ground and passed through a 200-mesh sieve for further use. The resultant Al-modified Sep (Al-Sep) was marked as Al-x-Sep (x represents the amount of substance of AlCl₃ 6H₂O, and the unit is mmol). In addition, the supernatant after centrifugation was collected and volumed to 2 L, marked as “S”.

Preparation of Id-Al-Sep Composite Pigments

Id was dispersed in deionized water, sonicated for 30 min in an ultrasonic cleaner (SN-4200 DTDN, Scientz, Zhejiang, China), and then shaken until the Id was evenly dispersed. 1 g of Al-x-Sep was mixed with 10 ml of Id dispersion (Id/Sep is 0.125 mmol/g) and milled in a planetary ball mill (XGB2, BYT, Jiangsu, China) at 560 rpm for 2 h. The obtained solid was dried, milled, and sieved (200-mesh sieve). The resultant composite pigment was labeled as Id-Al-x-Sep.

Calculation of Substitution Amount of Al³⁺ for Mg²⁺ and Si⁴⁺ in Sep

The consumption of Al³⁺ and the amount of Mg²⁺ and Si⁴⁺ substituted by Al³⁺ in Sep were tested and calculated by an inductively coupled plasma emission spectroscopy (ICP, ICAP7600, Thermo, United States). 3.5 ml of AlCl₃ solution for modification was diluted to 100 ml, marked as “Al”. The supernatant “S” and diluted AlCl₃ solution “Al” were then diluted by the same multiple $a$. The obtained solution was characterized by ICP to determine the concentration of Al³⁺, Mg²⁺, and Si⁴⁺. The substitution amount $R$ (mmol/g) (including the consumption of Al³⁺ and the amount of Mg²⁺ and Si⁴⁺ substituted by Al³⁺ in Sep) was calculated according to the following equation:

$R=\frac{2\times \left|C_I^S-C_I^{Al}\right|}{M\times 7a},(1)$

where $C_I^S$ (ppm) and$C_I^{Al}$ (ppm) are the concentrations of ion $I$ in diluted solution “S” and “Al,” respectively, $M$ (g/mol) is the molar mass of ion $I$, $a$ is the dilution multiple of solution “S” and “Al,” $7$ (g) refers to the mass of Sep during the Al modification, $2$ stands for the volume of solution “S” 2L, and $I$ represents Al³⁺, Mg²⁺, and Si⁴⁺.

Evaluation of Bonding Strength Between Id and Al-Sep

0.01 g of composite pigments was dispersed in 8 ml DMSO and shaken in a water bath shaker (SHA-B, Guohua, Jiangsu) at 30°C and 170 rpm for 24 h. The supernatants were separated by centrifugation and analyzed by a UV–Vis spectrophotometer (UV7600, Lengguang, Shanghai). The concentration of the supernatants was calculated by the Lambert–Beer law, and then, the adsorption amount of Id in Al-Sep was calculated to evaluate the bonding strength between Id and Al-Sep.

Weather Resistance of Id-Al-Sep Composite Pigments

0.2 g of composite pigment was pressed into a glass groove with a diameter of 2 cm, covered by a quartz glass, and irradiated by a UV lamp (AC/90–240 V, Zigu, Guangzhou) with a wavelength of 395 nm and radiation intensity of 650 mW/cm². The CIE of composite pigment irradiated by a UV lamp at different times was measured by a colorimeter (NR60CP, 3 nh, Guangzhou). The following formula was used to calculate the color difference $\left(\Delta E\right)$:

$\Delta E=\sqrt{{\left(L_1-L_0\right)}^2+{\left(a_1-a_0\right)}^2+{\left(b_1-b_0\right)}^2},(2)$

where ($L,a,b$) reflects the lightness, red-green, and yellow-blue of the pigment, respectively, determining the color of the pigment. ($L_1,a_1,b_1$) and ($L_0,a_0,b_0$) are the average of three measurements collected on the pigments after and before UV irradiation, respectively. $\Delta E$ reflects the weather resistance of the composite pigments; the smaller $\Delta E$, the better the weather resistance (Ouellet-Plamondon et al., 2015).

Characterization

The chemical composition of Al-Sep was analyzed by an X-ray fluorescence spectrometer (XRF, XRF-1800, Shimadzu, Japan). 0.1 g of Al-Sep powder was pressed with boric acid into a tablet for analysis. The morphology of samples was characterized by a transmission electron microscopy (TEM, JEM-2100Plus, JEOL). The Fourier Transform infrared (FTIR) spectra were carried out by a FTIR spectrometer (Spectrum 100, PerkinElmer, United States) range from 1,200 to 2000 cm⁻¹ with KBr background. X-ray diffraction (XRD) pattern used X-ray diffractometer (B8 Advance, Bruker, Germany) operating at Cu Kα, 40 mA, and 20 kV, scanning from 3° to 80° with a rate of 8°/min. The zeta potential (ζ) was tested by a zeta potential analyzer (Zetasizer Nano ZS90, Malvern, United Kingdom), and 0.01 g of sample was dispersed in 10 ml deionized water with sonication for 30 min. The specific surface area (BET method) of the sample was obtained from the adsorption–desorption isotherm of N₂ measuring by a specific surface area and pore size analyzer (Autosorb IQ, Quantachrome, United States of America) at 77 K. The sample was firstly degassed at 120°C for 2 h. The pore size distribution of the sample was calculated by the density functional theory (DFT) model. The ²⁷Al NMR one-pulse signal was obtained by a nuclear magnetic resonance instrument (Bruker AVANCE III 600 M, Bruker, Germany) at the frequency of 156.38 MHz and the tube diameter of 3.2 mm. The chemical shift of ²⁷Al resonance line was referred to Al (NO₃)₃ aqueous solution. The ²⁷Al experiment was recorded with a spinning rate of 15 kHz, relaxation delay of 1 s, and number of scans of 1,024. The TPD analysis was carried out by a chemical adsorption analyzer (AutoChem II 2,920, Micromeritics, United States). 0.1 g of sample was pretreated with Ar gas at 160°C, and NH₃ was then introduced until the adsorption of the sample was saturated. Following NH₃ adsorption, Ar gas was used to remove residual NH₃ on the surface of the sample. Finally, the sample was degassed at a rate of 10°C/min from 50 to 600°C, and the desorbed NH₃ at different temperatures was collected.

Results and Discussion

Preparation of Al-Modified Sep

The Influence of Al Dosage on the Composition of Al-Modified Sep

The consumption of Al³⁺ and the substitution amount of Mg²⁺ and Si⁴⁺ in Sep were calculated by Eq. (1), shown in Table 2. For Al-0.00-Sep, traces of Mg²⁺ and Si⁴⁺ exist in the solution “S,” indicating that traces of Mg²⁺ and Si⁴⁺ elute from the Sep during the hydrothermal reaction even without AlCl₃. After introducing AlCl₃, the substitution amount of Mg²⁺ and Si⁴⁺ (i.e., the amounts of Mg and Si dissolved from Sep) increases, demonstrating that Al³⁺ can promote the substitution of Mg²⁺ and Si⁴⁺ in Sep. The consumption of Al³⁺ and the substitution amount of Mg²⁺ increase, while the substitution amount of Si has no obvious change with the increase in dosage of AlCl₃. As the dosage of AlCl₃ reaches 70.0 mmol, the substitution amounts of Al³⁺, Mg²⁺, and Si⁴⁺ are 1.5831 mmol/g, 1.6756 mmol/g, and 0.1017 mmol/g, revealing that the substitution of Al³⁺ mainly occurs with Mg²⁺.

TABLE 2

TABLE 2. The substitution amount (mmol/g) of Al³⁺, Mg²⁺, and Si⁴⁺.

Table 3 shows the element content of Al-Sep modified by different dosages of AlCl₃ characterized by XRF. As the dosage of AlCl₃ increases, the content of Al in Sep increases, the content of Mg gradually decreases, while the content of Si has no significant change, which is consistent with the substitution amount result exhibited in Table 2. The content of Cl in Al-Sep is less than 0.10%, which is significantly lower than the content of Al in the samples, indicating that Cl⁻ adsorbed on the surface of Al-Sep during the modification process is effectively removed.

TABLE 3

TABLE 3. Element content of Al-Sep modified by AlCl₃ with different dosages.

According to the calculation of the ion substitution amount and characterization of XRF, the composition of Al-Sep is mainly changed via the substitution of Al³⁺ for Mg²⁺ in Sep during the Al modification process. Since the radius of Al³⁺ is smaller than that of Mg²⁺ and the charge of Al ³⁺ is larger than that of Mg²⁺, the substitution of Al³⁺ for Mg²⁺ can reduce the energy and stabilize the system (Liao and Xia, 2013).

The Structure of Al-Modified Sep

Figure 2 presents the XRD patterns of Sep and Al-Sep. The typical reflection peaks of Sep are located at 2θ = 7.45°, 20.53°, and 34.92°corresponding to (110), (131), and (371) planes, according to JCPDS card no. 13-0595 (Figure 1), without other impurity peaks. The peaks of Al-Sep are identical with that of Sep (Figure 2A), suggesting that the fiber structure of sepiolite has no significant change, and no impurity crystal is formed during the modification. The reflection peaks at a small angle of Al-Sep shift to a low angle slightly compared with that of Sep, and as the dosage of AlCl₃ increases, the shift angle increases (Figure 2B). The diffraction angles at (110) plane in Sep, Al-3.50-Sep, and Al-70.0-Sep are 7.45°, 7.43°, and 7.34°, respectively, corresponding to the interplanar spacing of 11.85 Å, 11.89 Å, and 12.03 Å, revealing that the interplanar space of (110) plane increases as the dosage of Al increases. The change in the interplanar space and the difference between the radii of Al³⁺ and Mg²⁺are in the same order of magnitude; therefore, the shift of diffraction angle at (110) plane is attributed to a slight distortion of the sepiolite during the modification process.

FIGURE 2

FIGURE 2. (A) XRD patterns of Sep, Al-3.50-Sep, and Al-70.0-Sep. (B) Partially enlarged view of Figure 2A.

The Morphology of Al-Modified Sep

Figure 3 provides the TEM images of Sep, Al-3.50-Sep, and Al-70.0-Sep. The length of Sep is about 0.5–6 μm, the width is about 20 nm, and Sep mainly exists as single nanofibers (Figure 3A, D). As illustrated in Figure 3B, C, the fibrous structure of sepiolite has not been destroyed after being modified by AlCl₃ while the single fibers obviously decrease, indicating that Al modification will reduce the dispersibility of sepiolite. From the results of EDS-point (Table 4) on the sepiolite fibers marked in Figure 3D–F, the main elements on the fiber in Sep are O, Si, and Mg, and the elements Al and Cl appear on the fiber of Al-3.50-Sep after introducing AlCl₃. The content of Al in Al-70.0-Sep is significantly increased, demonstrating that the element Al exists on the fibers of sepiolite during the hydrothermal reaction with AlCl₃, and the content increases with the increase of the dosage of AlCl₃.

FIGURE 3

FIGURE 3. TEM images of (A, D) Sep, (B, E) Al-3.50-Sep, and (C, F) Al-70.0-Sep.

TABLE 4

TABLE 4. The corresponding EDS results marked in Figures 3D–F.

The Substitution Position of Al³⁺

The substitution position of Al³⁺ was distinguished by solid-state ²⁷Al NMR spectra, shown in Figure 4. The signals are observed at ∼7 and ∼70 ppm, attributed to octahedral [AlO₆] (Al_T) and tetrahedral [AlO₄] (Al_O) in the structure of sepiolite, respectively (Caillerie and Fripiat, 1992; Komarneni et al., 1986). The Al_T and Al_O in Sep occur due to amorphous impurity and the substitution of Al³⁺ for Mg²⁺ located at [MgO₆] and Si⁴⁺ located at [SiO₄] in sepiolite lattice. The intensity of ²⁷Al NMR signal reflects the content of Al, and the peak area of the signal can be integrated to calculate the content of Al at different positions, shown in Figure 4C, D. The width of the signal reflects the symmetry of Al complex, and the narrower spectrum reflexes the higher symmetry of the complex (Wang et al., 2000).

FIGURE 4

FIGURE 4. (A)²⁷ Al NMR spectra of Sep, Al-3.50-Sep, and Al-70.0-Sep. (B) Schematic diagram of the position of Al_T and Al_O in sepiolite. The simulated results of (A) (C) at 20∼-30 ppm and (D) at 150∼50 ppm.

For Sep, two bands of Al_O at 7.5 ± 0.5 ppm and −2 ± 1 ppm, deriving from the Al at the edge (Al_O2) and the section (Al_O1) of the octahedron in sepiolite, and two signals of Al_T at 65 ± 1 ppm and 74 ± 1 ppm, corresponding to the Al at the center (Al_T2) and edge (Al_T1) of tetrahedron in sepiolite, are very close to the previous literature, marked in Figure 4B (Caillerie and Fripiat, 1992; Wang et al., 2000; Aslya et al., 2016). The signals at 86 ± 5 ppm are broad, revealing poor symmetry, which might be from the Al in the tetrahedron in the amorphous impurity (Wang et al., 2000). The ²⁷Al signals in Sep come from the impurity and the substitution of Mg²⁺ in the octahedron and Si⁴⁺ in tetrahedron by Al³⁺ during the mineralization process (Zhuang et al., 2019).

The intensity of ²⁷Al signals of Al-3.50-Sep and Al-70.0-Sep is higher than that of Sep, illustrating the content of Al increases after modification, which is consistent with the result of ICP and XRF. Al-3.50-Sep and Al-70.0-Sep have similar chemical shifts to Sep, revealing that Al³⁺ can enter the tetrahedron and octahedron in sepiolite, rather than just forming oxides or adsorbing on the surface of sepiolite. Al-Sep has a signal at 2 ± 1 ppm that is absent in Sep, which belongs to the chemical shift for amorphous aluminum silicate formed during the hydrothermal reaction. The signal of Al-0.05-Sep at 86 ± 5 ppm is divided into two signals, which are attributed to the change of the impurity in sepiolite and then the formation of two kinds of Al_T with different chemical environments.

The content of Al at different positions in sepiolite of samples is calculated and shown in Table 5. The Al content at −2 ± 1 ppm and 7.5 ± 0.5 ppm increased significantly as the dosage of AlCl₃ increases, indicating that Al³⁺ mainly substitutes the Mg²⁺ at the edge and section of the octahedron in sepiolite. Al³⁺ can substitute Si⁴⁺ in tetrahedron as well, but the substitution amount is obviously lower than that occurs in the octahedron. In addition, the signals at 108 and 127 ppm are the chemical shift produced by the tetrahedral coordination formed by Al³⁺, Cl⁻, and F⁻ adsorbed on the surface of sepiolite (Wang et al., 2000).

TABLE 5

TABLE 5. The calculated results of ²⁷Al NMR spectra of Sep, Al-3.50-Sep, and Al-70.0-Sep.

The Specific Surface Area and Micropores of Al-Modified Sep

The N₂ adsorption-desorption isotherms and the pore size distribution plots of Sep, Al-3.50-Sep, and Al-70.0-Sep are shown in Figure 5. As illustrated in Figure 6A, the N₂ amounts adsorbed on Al-3.50-Sep and Al-70.0-Sep are smaller than that adsorbed on Sep, indicating they have a smaller specific surface area, as the dispersibility of sepiolite rapidly reduces after Al modification (exhibited in Figure 3). The micropores ranging from 1 to 2 nm represent the channels of sepiolite formed by the periodic reversal of [SiO₄] (Chen et al., 2019). As the dosage of AlCl₃ increases, the distribution of channel size becomes wide, since the substitution of Al³⁺ for Mg²⁺ at the edge and section of the octahedron, i.e., the edge of sepiolite channel, makes the distribution of sepiolite channel size becoming uneven.

FIGURE 5

FIGURE 5. (A) N₂ adsorption–desorption isotherms and (B) the pore size distribution plots of Sep, Al-3.50-Sep, and Al-70.0-Sep.

FIGURE 6

FIGURE 6. The NH₃-TPD curves after heating from 50 to 600°C of (A) Sep, (B) Al-0.00-Sep, (C) Al-3.50-Sep, (D) Al-7.00-Sep, and (E) Al-70.0-Sep. (F) The acid amounts of samples.

The Zeta Potential of Al-Modified Sep

Table 6 gives the zeta potential of Al-Sep. The following possibilities will occur during the Al modification: 1) the substitution of Al³⁺ for Mg²⁺ in the octahedron will reduce the negative surface charges; 2) the substitution of Al³⁺ for Si⁴⁺ in tetrahedron will increase the negative surface charges; 3) the formation of vacancy defects in the octahedron and tetrahedron will increase the negative surface charges; and 4) the adsorption of Al³⁺ on sepiolite surface will reduce the negative charges. These actions conduct at the same time and affect the final zeta potential of the sepiolite. The result shows that the absolute value of the zeta potential decreases with the increase of dosage of AlCl₃, since the substitution of Al³⁺ mainly occurs on the octahedron in sepiolite and reduces the negative charge on the sepiolite surface.

TABLE 6

TABLE 6. The zeta potential of Al-Sep modified with different dosages of AlCl₃.

The Solid Acidity of Al-Modified Sep

NH₃-TPD has been verified to characterize the solid acidity of clay mineral quantitatively by calculating relative areas of resolved bands. The acid strength is positively correlated with the desorption temperature of NH₃ (Liu et al., 2013b). The acidity of montmorillonite is formed by the water polarized by cations, Si-OH and H₃O⁺ adsorbed on the negative charges, unsaturated Al³⁺ in the octahedron, and adsorbed water on unsaturated Al³⁺ (marked as Al-OH₂) (Heller-Kallai, 2006; Liu et al., 2013b; Liu et al., 2011). Si-OH, H₃O⁺, and Al-OH₂ behave as weak-strength acid sites (Hair and Hertl, 1970). The polarized water and unsaturated Al³⁺ behave as medium-strength acid site. The water polarized by adsorbed cations, e.g., Al³⁺, Ca²⁺, and Fe³⁺, will be transformed into exposed hydroxy and then behaves as strong-strength acid site after heating at 160°C (Liu et al., 2013b; Kaufhold et al., 2011). The acid sites of sepiolite are similar to montmorillonite; therefore, the bands of NH₃-TPD curves of samples (shown in Figure 6A–E) at 100–200°C, 200–400°C, and 400–600°C correspond to weak-strength, medium-strength, and strong-strength acid sites, respectively. In addition, the desorption temperature occurs at ∼100°C attributed to physical adsorbed and hydrogen-bound NH₃ (Liu et al., 2011; Liu et al., 2013b). The total acid amounts of Sep, Al-0.00-Sep, Al-3.50-Sep, Al-7.00-Sep, and Al-70.0-Sep are 1.137, 1.273, 1.177, 1.440, and 2.220 mmol/g. The amounts of weak-strength and strong-strength acid sites increase while the amount of medium-strength acid sites firstly decreases and then increases with the increase of the dosage of AlCl₃ (Figure 6F).

Compared with Sep, the acid amount in Al-0.00-Sep increases, since Mg²⁺ and Si⁴⁺ in sepiolite lattice are dissolved out during the hydrothermal reaction, resulting in the increase of negative charge and the adsorbed H₃O⁺. The grinding process during the preparation of Al-0.00-Sep can also increase acid sites by increasing the unsaturated cations and then enhancing the polarization of adsorbed water.

The weak-strength and strong-strength acid sites increase while the medium-strength acid sites reduce in Al-3.50-Sep, since the Al-OH₂ at the edge of the octahedron and exposed octahedral Al-OH increase and the unsaturated Al³⁺ decreases (Figure 4C) after being modified by 3.50 mmol AlCl₃. With the increase in dosage, the Al-OH₂, unsaturated Al³⁺, and exposed Al-OH increase, and thus, the weak-, medium-, and strong-strength acid amounts are improved. TPD results illustrate that Al modification will increase the acid sites of sepiolite.

The Id-Al-Sep Composite Pigments

The Structure of Id-Al-Sep Composite Pigments

X-Ray Diffraction

Id was employed as the color giving agent and ground with sepiolite modified with different dosages of AlCl₃ to prepare composite pigments. The structure of composite pigments was characterized by XRD, shown in Figure 7A. The typical reflection peaks of Id-Al-3.50-Sep are identical with that of Sep, and no obvious reflection belonging to Id is observed in Id-Al-3.50-Sep, revealing that the Id molecule is uniformly distributed on Al-Sep after grinding.

FIGURE 7

FIGURE 7. (A) XRD pattern and (B) FTIR spectra of Sep, Id, and composite pigment prepared by Id and Al-Sep.

Fourier Transform Infrared

Figure 7B shows the FTIR spectra of Id, Sep, and composite pigments, and the stretching vibration of C=O and N-H at 1,626 cm⁻¹ redshifts to 1,624 cm⁻¹, corresponding to the shift caused by the formation of hydrogen bond between indigo and two water molecules which were calculated by the literature (Giustetto et al., 2005), demonstrating that C=O and N-H in Id can bond with the coordinated water, silanol, and zeolite water in Al-Sep through hydrogen bond. The vanishment of the vibration of 1,391 cm⁻¹ attributed to crystalline indigo indicates the absence of crystalline indigo in composite pigments (Giulieri et al., 2012).

As illustrated by the results of XRD and FTIR, the presence of crystalline indigo is not detected in the composite pigment, indicating Id molecules reorganize on the Al-Sep during ball milling. Id molecules bond through hydrogen bond with coordinated water, silanol, and zeolite water in Al-Sep.

The Bonding Strength Between Id and Al-Sep

The composite pigments were desorbed by DMSO to evaluate the effect of Al modification on bonding strength between Id and Al-Sep. The removal of Id by DMSO can be an indication of available Id in Al-Sep with different bonding strengths, and the UV–Vis spectra of supernatant after desorption are shown in Figure 8A. As the dosage of modified AlCl₃ increases, the Al content in sepiolite increases, and the desorption number of composite pigments in DMSO decreases, indicating that the bonding strength between Id and Al-Sep increases. Compared with the results of specific surface area, the possibility that the channels in Al-Sep bound the Id molecule to enhance the bonding has been eliminated. By comparison, a linear correlation is found between the Al content of Al-Sep and the adsorption amount of Id in composite pigment desorbed by DMSO. Furthermore, weak acid amount and adsorption amount of Id displayed a similar correlation (Figure 8B). The general trend is similar to the result of previous studies (Ramírez et al., 2011).

FIGURE 8

FIGURE 8. (A) The UV-Vis spectra of supernatant of composite pigments desorbed in DMSO. (B) Linear correlation between the amount of weak acid, Al content in Al-Sep, and the adsorption amount of Id in composite pigment desorbed by DMSO.

Weak acid sites consist of Si-OH, H₃O⁺, and Al-OH₂. Al modification can enhance the bonding strength between Id and Al-Sep, as the substitution of Al³⁺ mainly occurs with Mg²⁺ in the octahedron, causing the increase of Al-OH₂ at the edge of the octahedron, and Al³⁺ has a higher electronegativity than Mg²⁺ and has a higher polarization of coordinated water, resulting in a stronger combination between C=O and N-H in Id and Al-OH₂ in Al-Sep, and the mechanism is shown in Figure 9.

FIGURE 9

FIGURE 9. The mechanism of the substitution of Al³⁺ for Mg²⁺ located at the octahedron in sepiolite and the bonding of Sep, Al-Sep with Id (executed in (200) plane).

Combining the results of FTIR and adsorption amount of Id in composite pigment treated by DMSO, Id bonds with sepiolite through hydrogen bonds between C=O and N-H in Id and Si-OH, H₃O⁺, Mg-OH₂, and Al-OH₂ in Al-Sep, which is consistent with the result of the previous literature (Zhuang et al., 2019). Among them, the bond energy formed by Al-OH₂ and Id is higher than that of Mg-OH₂. Al modification can increase the bonding strength of Id and Al-Sep by the substitution of Al³⁺ for Mg²⁺ in the octahedron.

The Chromaticity and Weather Resistance of Composite Pigments

Chromaticity

The chromaticity of Id-Al-Sep composite pigments is presented in Figure 10A. The absolute value of L, a, and b increases as the dosage of AlCl₃ rises, indicating a more vivid color of composite pigments as the bonding strength between Id and sepiolite increases. Increasing the bonding strength between Id and sepiolite is an effective way to improve the chromaticity of composite pigments.

FIGURE 10

FIGURE 10. (A) The chromaticity of the composite pigments. (B) The ΔE curves of composite pigments at different irradiation times.

Weather Resistance

ΔE results of composite pigments were measured and calculated after UV irradiation at different times during 24 h (Figure 10B). A smaller ΔE performs better weather resistance. Obviously, the weather resistance of composite pigments is as follows: Id-Al-3.50-Sep > Id-Al-0.00-Sep > Id-7.00-Sep > Id-70.0-Sep shows a positive correlation with the acid amounts in Al-Sep. Intramolecular proton transfer between C=O and N-H in the Id molecule is the main pathway for Id to decolor under UV irradiation (Rondão et al., 2010). The acid in Al-Sep will promote this proton transfer in Id under UV irradiation and promotes the fading rate of Id and reduces the weather resistance of composite pigments.

In summary, Al modification can increase the amount of weak acid Al-OH₂ in sepiolite. The Al-OH₂ enhances the combination of sepiolite and indigo. For indigo, the acid in Al-Sep can brighten the color and accelerate the fading of composite pigments. This phenomenon originates from the special structure of indigo, and there may be different results in composite pigments prepared by other dyes.

Conclusion

In this study, AlCl₃ was used to modify sepiolite. The substitution of Al³⁺ mainly occurs with Mg²⁺ located at the edge and section of the octahedron in sepiolite lattice and the substitution amount increases with the increase in the dosage of AlCl₃, since the substitution can reduce the energy of the system. The absolute value of zeta potential and specific surface area of sepiolite decreases, while the solid acidity of sepiolite increases as the dosage of AlCl₃ rises. Al modification can enhance the bonding between indigo and sepiolite by increasing the amount of weak acid Al-OH₂ through the substitution of Al³⁺ for Mg²⁺ located at the octahedron of sepiolite lattice. The electronegativity of Al³⁺ is greater than that of Mg²⁺, and thus, indigo can form a stronger bonding with Al-OH₂ than that with Mg-OH₂. Enhancing the bonding strength between indigo and sepiolite can brighten the composite pigment. The acid in sepiolite will provide a pathway to decolor by promoting the intramolecular proton transfer in the Id molecule, resulting in worse weather resistance. This conclusion is for indigo, and the protective effect of Al modification on other dyes needs further discussion.

The solid acidity and basicity of sepiolite can be regulated by changing the content and position of Al, and the catalytic activity and adsorption performance of sepiolite will be adjusted, accordingly widening the application of sepiolite in the fields of catalysis and adsorption.

Data Availability Statement

The original contributions presented in the study are included in the article/supplementary material; further inquiries can be directed to the corresponding author.

Author Contributions

HC designed experimental plans, performed main experimental work, analyzed and discussed results, and wrote the manuscript. JG assisted in the design of the scheme, performed the main experimental work, analyzed and discussed the results, and participated in the manuscript writing. ZZ proposed the themes, ideas, and content of the manuscript research work, guided the design of the research plan, the analysis, and discussion of problems, and guided the writing and revision of the manuscript. RJ assisted in literature review and manuscript sorting. JYZ participated in some experimental work. JCZ guided experimental work and manuscript revision.

Funding

The research and publication fees are supported by the National Natural Science Foundation of China with the project name of Key Parameter Test and Intelligent Evaluation System of Gas-bearing Shale (award number: 41927801). The research fees are supported by Fundamental Research Funds for Central Universities from the Ministry of Education with the project name of Exploration on the preparation process of Maya-like blue pigment (award number: 2652018319)

Conflict of Interest

The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.

Publisher’s Note

All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors, and the reviewers. Any product that may be evaluated in this article, or claim that may be made by its manufacturer, is not guaranteed or endorsed by the publisher.

Acknowledgments

This work was financially supported by the Key Parameter Test and Intelligent Evaluation System of Gas-bearing Shale from the National Natural Science Foundation (no. 41927801) and Exploration on the preparation process of Maya-like blue pigment from the Fundamental Research Funds for Central Universities (China) (no. 2652018319).

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