Sol–gel derived mesoporous GaAlPO4 glass for heavy metal ion sequestration

Jin Heabc, Pengfei Maa, Ge Zhanga, Rihong Li*a and Long Zhang*a
aKey Laboratory of Materials for High Power Laser, Shanghai Institute of Optics and Fine Mechanics, Chinese Academy of Sciences, Shanghai 201800, China. E-mail: lzhang@siom.ac.cn; lirihong@siom.ac.cn; Fax: +86 21 69918675; Tel: +86 21 69918196 Tel: +86 21 69918841
bSchool of Materials, University of Manchester, Manchester M13 9PL, UK
cInstitute of Chemistry, The Center for Nanoscience and Nanotechnology, The Hebrew University of Jerusalem, Jerusalem 91904, Israel

Received 12th July 2016 , Accepted 29th September 2016

First published on 5th October 2016


Abstract

Mesoporous phosphate materials with chemical diversity and a high surface area are essential for their practical applications as heavy metal ion adsorbent materials. Herein, novel gallium aluminum phosphate mesoporous glasses are prepared through a simple aqueous sol–gel route free of any surfactant or template. The glass structure and its evolution from the gel to the final glass were monitored using solid-state NMR techniques, providing detailed insight into the reaction mechanism. During the formation of the mesoporous GaAlPO4 glass, the gallium entered into the PO4 tetrahedron via Ga–O–P bonds. The resulting mesoporous glass samples were tested as adsorbents to remove Pb(II) anions from solution and the ternary oxide glasses show high adsorption capacities (>36.63 mg g−1, that is 0.18 mmol g−1). Owing to their integrated features (including their variable compositions, high specific surface area, tunable pore size and shape flexibility) as well as specific acid–base surface properties, such mesoporous gallium aluminum phosphate materials are also expected to have potential either as catalysts or catalyst supports for industrial applications.


1. Introduction

The increase of heavy metal pollution in water resources is a major environmental health risk to human beings.1 Heavy metal ions in water, such as Pb(II), Cd(II), Hg(II) and so on, can seriously threaten local residents’ health.2 One of the most efficient routes for the removal of heavy metals is adsorption-based processes, the fundamental challenge of which is developing highly efficient adsorbents.3,4 Mesoporous materials have attracted tremendous research interest in the exploration of ideal adsorbent materials.5,6 They possess an intrinsic ability for accommodating capacious guest species as a result of high specific surface areas, tunable pore sizes, large pore volumes, as well as stable and interconnected frameworks. Since their discovery, mesoporous materials have shown great potential as adsorbents for heavy metal ion sequestration.7 To date, the most developed mesoporous materials employed for heavy metal ion sequestration are based on silica and carbon-based systems, the neutral SiO4 and C skeleton of which lack binding properties for heavy metal ions.6,8 The generation of specific active sites on the pore surfaces is based on post modification through attaching functional groups. However, the incorporation of organic groups would lead to an inhomogeneous distribution of active sites on the pore surface, which would limit its high adsorption efficiency and the organic active sites hinder application in harsh water environments (high temperature, strong acidic or basic). Therefore, the aim of the present task is synthesis of mesoporous materials that can be directly used as adsorbents without any further surface modification, through careful selection of the active component for binding heavy metal ions.

Phosphates have been shown to be high performance adsorbents in the field of water treatment to remove heavy metal ions.9,10 The phosphate group is an active component in the adsorption of heavy metal ions due to its strong binding capacity for heavy metal ions.11 Sol–gel synthesis has become a predominant approach for the preparation of mesoporous materials, because of the flexibility in shaping that allows these materials to be made into films, monoliths or coatings, which could be applied as separation membranes, sensors, and low-dielectric-constant (low-k) insulators.12 Although great efforts have been made during the past two decades, progress has been limited in the development of sol–gel derived mesoporous phosphate materials with chemical diversity and high surface areas,13–15 which are considered to be critical to the adsorption properties.

In recent years, our group has contributed research on exploiting novel aqueous sol–gel routes based on an unusual chelation of the metal precursors to prepare a series of phosphate multi-component mesoporous glasses with attractive high surface areas (>500 m2 g−1).16–19 Both aluminum phosphate and gallium phosphate materials with open frameworks have attracted continued interest in the area of porous materials.16,20 However, studies concerned with the incorporation of gallium into aluminum-based mesoporous materials have so far been poorly developed and not well understood. Here, we report the preparation of mesoporous GaAlPO4 glasses using a facile aqueous sol–gel technique, free of any surfactant or template, for the first time. The compositions of the ternary oxide glasses varied from 0 to 25% Ga, resulting in high surface areas up to 515 m2 g−1. In contrast, Ga-rich samples tend to phase-separate (>30% Ga) and crystallize (>50% Ga) during the calcination process. The resultant GaAlPO4 (GAP) mesoporous glasses were employed as adsorbents for the adsorption of the heavy metal ion Pb(II) from solution. The ternary oxide glasses show a fast adsorption process and high adsorption capacities, with a maximum adsorption capacity of 36.63 mg g−1 (0.18 mmol g−1) achieved using the mesoporous Ga0.1Al0.9PO4 glasses, indicating their potential for application in water treatment. This facile and reproducible sol–gel approach is an important step toward the synthesis of multi-component mesoporous phosphates for environmental protection and industrial catalysis applications.

2. Experimental

2.1 Materials and methods

Gallium aluminum phosphate samples were prepared via an aqueous sol–gel route, using aluminum lactate, gallium nitrate and H3PO4 (1 M) as the precursors. A H3PO4 (1 M) solution was prepared by dissolving solid H3PO4 (98%, Fluka) in distilled water. The pH of the precursor solutions was adjusted with ammonia solution (1 M) and controlled to within 0.01 U using a pH meter (Mettler Toledo S20, Switzerland). Gel annealing was performed in a Nabertherm muffle furnace. A more detailed synthesis procedure can be found in the ESI.

A stock solution containing 1000 mg L−1 of Pb(II) was prepared by dissolving 0.8041 g of Pb(NO3)2 in 500 mL of deionized water. Simulated wastewater samples with different Pb(II) concentrations (50.0, 100.0, 200.0 mg L−1) were prepared through dilution of the stock Pb(NO3)2 standard solution with deionized water. Typically, the Pb(II) adsorption experiments were carried out in a 20 mL glass bottle containing 10 mL of simulated wastewater at room temperature (25 °C) and without further pH adjustment. After the adsorption process, the samples were filtered through a 0.45 μm membrane, and the filtrates were analyzed using ICP-AES (iCAP 6300, Thermo Scientific). All the adsorption experiments were carried out in duplicate. The relative standard deviations were in the range of ±5%. The amount of Pb(II) adsorbed per unit mass of the adsorbent was evaluated using a mass balance equation (eqn (1))

 
qt = (C0Ct)V/W (1)
where qt (mg g−1) is the amount adsorbed per gram of adsorbent at time t (min), C0 is the initial concentration of Pb(II) in the solution (mg L−1), Ct is the concentration of Pb(II) at time t of the adsorption process (mg L−1), W is the mass of the adsorbent used (g), and V (L) is the initial volume of the Pb(II) solution.

2.2 Characterization

The crystallinity of the prepared samples was checked via X-ray powder diffraction using the Guinier method, with CuKα1 radiation and using α-quartz (a: 5491.30 pm, c: 5540.46 pm) as an internal standard. Differential thermal analysis (DTA) and thermogravimetric analysis (TGA) were carried out with an EXSTER instrument (EXSTAR, TG/DTA 7300 Japan) using a heating rate of 10 K min−1. Measurements for the BET surface area were obtained using a Micro-meritics ASAP 2010 volumetric adsorption analyzer with N2 as the adsorbate at 77 K. Prior to the analysis, samples weighing between 0.1 and 0.3 g were outgassed at 200 °C for at least 6 h under vacuum until a residual pressure of ≤6 μm Hg was reached. The BET specific surface area was calculated according to the BET equation, using nitrogen adsorption data in the relative adsorption range from 0.06 to 0.2. The total pore volume, Vp, was obtained from the amount adsorbed at a P/P0 of about 0.99. Mesopore size distributions were obtained using the Barrett–Joyner–Halenda (BJH) method and a cylindrical pore model.

The NMR measurements were carried out at ambient temperature with a Bruker AVANCE-400 spectrometer, using 4.0 mm MAS NMR probes operated at spinning speeds between 9 and 12 kHz. At a field strength of 9.4 T, the resonance frequencies were 104.3 MHz for 27Al, and 162.4 MHz for 31P, respectively. The typical acquisition parameters were a pulse length of 5.0 μs (90°) for 31P and 1.0 μs (30°) for 27Al, and a recycle delay of 60 s (31P) and 1 s (27Al), respectively. The 27Al and 31P NMR chemical shifts were referenced to a 1 M aluminium nitrate aqueous solution and 85% H3PO4. XPS measurements were performed using a Thermo Fisher Scientific K-Alpha spectrometer using non-monochromatic Al K radiation with a constant pass energy of 20.0 eV. All the binding energies (BE ± 0.2 eV) were referenced to the C-1s signal (284.6 eV). The morphology of the sample surface was determined using a Zeiss scanning electron microscope (SEM, JSM-6360LA).

3. Results and discussion

3.1 Composition and porous properties

Ga2O3–Al2O3–P2O5 system glasses have not been reported previously, while a wide compositional range of amorphous materials can be achieved using our sol–gel route (see Fig. S1). Grey colored Ga2O3–Al2O3–P2O5 glasses were obtained when P/(Al + Ga) = 1.5 and 2. The grey color suggests the entrapment of small amounts of residual free carbon in the gel-derived samples as a result of the low specific surface area for the samples of this composition line. In particular, homogeneous transparent colorless glasses with a high surface area were obtained from the composition line of GaxAl1−xPO4. These glasses remained transparent and colorless until the amount of Ga was increased up to 25%. Increase of the amount of Ga results in phase separations (separated amorphous phases) and crystallization. The XRD results of Ga0.3Al0.7PO4 confirm its amorphous structure after phase separation (Fig. S2). The positions of the XRD peaks of Ga0.5Al0.5PO4 match well with those of the AlPO4 and Ga2O3 crystallization phases (Fig. S2). Fig. S3 summarizes the thermal analysis data. The TGA trace of the xerogel with Ga[thin space (1/6-em)]:[thin space (1/6-em)]Al = 1[thin space (1/6-em)]:[thin space (1/6-em)]9 indicates that the volatile components (e.g. organics and water) are not completely removed below 400 °C, and a final weight loss near 700 °C was found. Xerogels with different Ga[thin space (1/6-em)]:[thin space (1/6-em)]Al ratios show similar curves. Fig. S3b illustrates the TGA and DTA curves for the Ga0.1Al0.9PO4 glass, and the minor weight loss observed below 200 °C is most likely due to an endothermic event arising from desorption and removal of physically adsorbed water in the porous material. The real compositions, and the glass transition temperatures (Tg) and crystallization temperatures (Tx) determined from the DTA traces are summarized in Table S1. The ICP results of the samples from the GaxAl1−xPO4 composition line prove that the real compositions are quite consistent with the ratio of precursors that was used for the sol–gel route.

The specific surface area and porosity of selected GAPs were investigated using N2 adsorption and desorption isotherms as shown in Fig. 1. A material is generally classified as mesoporous if it has a pore size between 2 and 50 nm, according to the International Union of Pure and Applied Chemistry (IUPAC). All the isotherms of the samples reveal stepwise adsorption and desorption branches of type IV curves, showing the typical pattern of a mesoporous material that has a three dimensional (3D) intersection according to the IUPAC classification.21 The hysteresis loop with stepwise adsorption and desorption branches was observed over a wide pressure range (P/P0), and the surface area values for the Ga0.05Al0.95PO4 and Ga0.1Al0.9PO4 obtained at 600 °C are 388 m2 g−1 and 328 m2 g−1, respectively. Fig. 1b and d illustrate the pore size distributions of the two representative samples. After calcination at 600 °C, the average pore diameter of Ga0.05Al0.95PO4 is 8.2 ± 0.1 nm. Table 1 further summarizes the main pore texture characteristics, BET surface area (SBET), pore volume (Vp) and average pore diameter (dp) of some representative glasses with different compositions. As indicated in Table 1, when 1% gallium was incorporated into the AlPO4 network, the pore texture characteristics were similar to those for gallium-free AlPO4 glasses prepared via a similar sol–gel route. As the amount of gallium increases, the average pore diameter (dp) increases to 8–12 nm, which suggests that the incorporation of gallium into AlPO4 glasses serves to tune the pore size of the mesoporous structure. With continuous increase of the gallium, the surface area decreases significantly. This behavior was attributed to the fact that the SiO2-like three-dimensional network was destroyed through the incorporation of gallium, as indicated by the NMR results. To the best of our knowledge, the present contribution is the first successful preparation of Ga2O3–Al2O3–P2O5 glassy materials, exhibiting a high surface area and mesoporous structure.


image file: c6ra17766b-f1.tif
Fig. 1 (a) Adsorption–desorption isotherms and (b) pore size (diameter) distribution (calculated using a BJH method) of the Ga0.05Al0.95PO4 glass obtained after calcination at 600 °C for 6 h. (c) Adsorption–desorption isotherms and (d) pore size (diameter) distribution of the Ga0.1Al0.9PO4 glass obtained after calcination at 600 °C for 6 h.
Table 1 The BET surface area, SBET, total pore volume, Vp, and average pore diameter, dp, of the samples with different compositions annealed at 600 °C for 6 h
Sample SBET ± 5/m2 g−1 dp ± 0.1/nm Vp ± 0.05/cm3 g−1
Ga0.01Al0.99PO4 415 4.1 0.42
Ga0.02Al0.98PO4 515 8.6 1.11
Ga0.05Al0.95PO4 388 8.2 0.71
Ga0.1Al0.9PO4 328 8.2 0.71
Ga0.2Al0.8PO4 132 12.1 0.40
Ga0.25Al0.75PO4 152 8.2 0.31


3.2 Gel to glass transition

To monitor the structural evolution during the gel → glass transition and reveal the local structure and site distribution of various atoms in the sol–gel samples, 31P and 27Al NMR spectra were recorded for some representative samples after various processing steps. Fig. 2 (left) shows the 27Al MAS-NMR spectra of samples with a composition of Ga0.2Al0.8PO4 annealed at different temperatures. First of all, Fig. 2a and b illustrate the 27Al MAS-NMR spectra of the Ga0.2Al0.8PO4 xerogels annealed at 50 °C and 100 °C, respectively. Peak assignments can be made in relation to corresponding gallium-free aluminum phosphate xerogels.22 The two 27Al peaks can be assigned to [Al(lact)2(PO3)2] (∼5 ppm), and [Al(lact)1(PO3)4] (∼−4 ppm). The 27Al spectra indicate that lactate ligands (bound to aluminum) tend to be increasingly replaced by phosphorous ligands as the processing temperature increases. Dramatic structural changes occurred when the gels were heated from 100 °C to 200 °C. The signal attributed to [Al(lact)2(PO3)2] was completely suppressed, whereas three new lactate-free Al sites were predominant, for which the peaks were attributed to Al(OP)4 (near 38 ppm), Al(OP)5 (near 4 ppm) and Al(OP)6 (near −12 ppm). After calcination at 300 °C or above, no lactate-linked species can be observed and the aluminum was completely converted into three lactate-free units, which can be assigned as four-, five- and six-coordinated (Al(OP)4, Al(OP)5 and Al(OP)6) aluminum sites. Subsequent heating at higher temperatures results in more subtle spectral changes for the aluminum sites. The Al(OP)4 sites were the major Al-species, the proportion of which was increased somewhat at the expense of the Al(OP)6 units. The final gallium aluminum phosphate glass structure is established after heating above 600 °C. Further evidence for the truly amorphous rather than nanocrystalline nature of the prepared materials is the five-coordinate aluminum species in the final structure.23
image file: c6ra17766b-f2.tif
Fig. 2 104.3 MHz 27Al (left) and 162.4 MHz 31P (right) MAS-NMR spectra of Ga0.2Al0.8PO4 samples at various processing stages during the gel to glass conversion.

Fig. 2 (right) shows 31P MAS-NMR spectra during the gel to glass conversion. The Qn(mAl) notation was used to assign these peaks to specific phosphorus species. Here n is the number of P next-nearest-neighbors (NNN) per P tetrahedron and m is the number of Al NNN per P. The center of gravity shifts monotonically towards a lower frequency with increase of the annealing temperature, reflecting an increase in the average degree of P/Al connectivity. Q0(3Al), at −17.2 ppm, is already an overwhelmingly dominant species, while no Q0(0Al) sites can be detected, for the xerogel heated at 100 °C (Fig. 2i). For the gel heated at 200 °C (Fig. 2j), the Q0(3Al) species is significantly diminished again (only present as a shoulder), and the main 31P spectral component occurs at −22.7 ppm. This peak can be assigned to polymerized phosphate species of type Q0(4Al), based on the same trend of these chemical shift with that of gallium-free Al2O3–P2O5 glass.22 Fig. 2k and l indicate that this Al environment dominates in the samples calcined at 400 °C or higher temperatures, which is consistent with the conclusions drawn from the 27Al MAS NMR spectra (Fig. 2 left). Compared with gallium-free Al2O3–P2O5 glass, we have noted that all the Q0(mAl) peaks in the 31P MAS-NMR spectra are slightly shifted (∼2–4 ppm) towards a lower frequency, the structural evolution induced by the introduction of gallium is discussed in detail in the ESI.

3.3 Capacity and behavior for Pb(II) adsorption

Due to the high specific surface area and the high affinity of the phosphate group for metals, the resulting mesoporous GAPs were expected to show promise in the uptake of heavy metal ions for water purification applications.

Lead was chosen to illustrate the adsorption capabilities of the resulting GAPs. In this study, the Ga0.1Al0.9PO4 glass, as a representative sample, was tested for adsorptive removal of Pb(II) from simulated wastewater. Fig. 3 shows the time profile of Pb(II) removal using 5 g L−1 of the Ga0.1Al0.9PO4 mesoporous glass with different initial Pb(II) concentrations and at neutral pH. The adsorption rates within the first 5 min were surprisingly fast for all the concentrations, and above 88% of the adsorption process occurred in the first 5 min. In a material with accessible active sites, the adsorption kinetics are determined by surface chemistry.24 However, diffusion takes precedence over surface chemistry in monomodal mesoporous materials.25 Therefore, Pb(II) adsorption occurred at a significantly fast rate with the mesoporous GAPs. The adsorption process was almost finished within 80 min, and there was no significant change from 80–240 min. The removal efficiencies were found to be 100, 96.9%, and 91.6% when the initial Pb(II) concentration was 50, 100, and 200 mg L−1, respectively. Therefore, the maximum Pb(II) adsorption capacity of the Ga0.1Al0.9PO4 mesoporous glass was found to be 36.63 mg g−1 with an initial Pb(II) concentration of 200 mg L−1. This reveals a high efficiency for the adsorption of Pb(II) onto the mesoporous GAPs in aqueous solution. It was also observed that the adsorption amount of Pb(II) increases with the initial Pb(II) concentration. This is because more Pb(II) results in a higher driving force for the ions to relocate from the solution onto the mesoporous GAPs and results in more collisions between the Pb(II) ions and active sites of the mesoporous GAPs. Similar phenomena have also been reported in the literature.26,27 The excellent heavy metal adsorption capacity of phosphates is derived mainly from the ion-exchange properties of HxPO4 groups, which can exchange with heavy metal ions.28,29 The HxPO4 ions required for ion-exchange with Pb2+ are provided from surface hydrolysis of the GAPs. It has been shown that the primary mechanism of metal ion removal by phosphates under neutral and weakly acidic environments is governed by surface hydrolysis, followed by subsequent ion-exchange.30 Thus, the conceived mechanism for heavy metal adsorption by the GAPs can be described as follows:

Ga0.1Al0.9PO4 + xH2O ↔ Ga0.1Al0.9(OH)x(HxPO4)

Ga0.1Al0.9(OH)x(HxPO4) + xM2+ ↔ Ga0.1Al0.9(OH)x(MHx−2PO4) + 2xH+
where M represents the corresponding heavy metal element. In the above hypothesis, where P in the form of HxPO4 helps to adsorb the metal ions in aqueous solutions, H+ ions within HxPO4 are released in a continuous and stepwise manner to allow for exchange with heavy metal ions.


image file: c6ra17766b-f3.tif
Fig. 3 (a) Time profile of Pb(II) removal with Ga0.1Al0.9PO4 mesoporous glass. The concentration of the GAP was 5.0 g L−1; the initial Pb(II) concentration ranged from 50 to 200 mg L−1. (b) The adsorption isotherm for Pb(II) on Ga0.1Al0.9PO4 mesoporous glass, (c) Langmuir and (d) Freundlich adsorption isotherms for Pb(II) on Ga0.1Al0.9PO4 mesoporous glass.

Adsorption isotherms were used to describe the adsorption behavior for Pb(II) of the mesoporous GAPs, among which Langmuir and Freundlich isotherms are the two most common models presenting linear equations as follows:31

Langmuir isotherm:

Ce/Qe = 1/(QmKL) + Ce/Qm

Freundlich isotherm:

log(Qe) = log(KF) + (1/n)log(Ce)

The assumption for application of the Langmuir isotherm is that there is a homogeneity of the adsorption surface with all the adsorption sites having an equal adsorption surface and equal adsorbate affinity, while the Freundlich isotherm model is often applicable for heterogeneous adsorption surfaces, where Qe (mg g−1) and Ce (mg L−1) are the amount of Pb(II) adsorbed and the Pb(II) concentration at equilibrium, respectively; Qm (mg g−1) and KL (L g−1) are Langmuir constants indicating the adsorption capacity and energy of adsorption, respectively; KF (mg g−1) and 1/n are Freundlich constants, related to the capacity and intensity of the adsorption, respectively. Here, both of the models are used to assess the adsorption data (Fig. 3c and d) and the adsorption isotherm parameters along with the correlation coefficients R2 are presented in Table 2. The values of R2 (close to unity) indicate the high suitability of these two adsorption isotherms, but the Langmuir isotherm seems to fit better according to its higher R2 value.

Table 2 Adsorption isotherm parameters using Langmuir and Freundlich models for Pb(II) on Ga0.1Al0.9PO4 mesoporous glass
Langmuir isotherm model Freundlich isotherm model
Qm (mg g−1) KL (L g−1) R2 KF (mg g−1) 1/n R2
43.78 0.254 0.994 12.539 0.380 0.984


The kinetics of Pb(II) removal with the mesoporous GAPs were further investigated using different initial Pb(II) concentrations in the presence of 5.0 g L−1 of the GAP. Pseudo-second-order rate constants (k2) and the amount of Pb(II) adsorbed at equilibrium (qe) were calculated from the slope and intercept of the plots of t/qt versus t, according to eqn (2):26

 
t/qt = 1/k2qe2 + t/qe (2)
where k2 (g mg−1 g−1) is the pseudo-second-order rate constant, qe is the adsorption amount of Pb(II) (mg g−1) at equilibrium, and qt is the amount adsorbed (mg g−1) at any time t. The kinetics of the removal process are illustrated in Fig. 4. Table 3 summarizes the theoretical and calculated qe values, pseudo-second-order rate constants, k2, and correlation coefficient values (R2). The calculated qe value was obtained from the slope and intercept of the plots of t/qt versus t according to eqn (2). The calculated qe values matched well with the theoretical ones, showing a quite good linearity with R2 above 0.999. Therefore, a chemisorption process was revealed as the adsorption kinetics follow a pseudo-second-order model. Moreover, the leaching behavior of the GAPs manifests a high chemical durability from pH3 to pH9 in aqueous solution, which is beneficial for application in a harsh environment (Fig. S5).


image file: c6ra17766b-f4.tif
Fig. 4 Removal kinetics for 50, 100, 200 mg L−1 of Pb(II) in the presence of 5.0 g L−1 of the mesoporous GAP. The contact time was 4 h.
Table 3 Theoretical and calculated qe values, pseudo-second-order rate constants, k2, and correlations. The contact time was 4 h
Theoretical qe (mg g−1) Calculated qe (mg g−1) k2 (g mg−1 min−1) R2
10 9.3658 4.1144 0.9999
20 19.8972 2.2568 0.9998
40 39.2773 1.0121 0.9998


3.4 Mechanisms of Pb(II) adsorption

N2 adsorption isotherms for as-prepared and Pb-adsorbed Ga0.1Al0.9PO4 samples (Fig. S6a) revealed a decrease in the BET surface area from 328 m2 g−1 (as-prepared) to 75 m2 g−1 (Pb-adsorbed), and a corresponding reduction in the pore diameter from 12.1 nm to 9.1 nm (Fig. S6b). These observations are consistent with the presence of a significant amount of adsorbed heavy metal ions attached to the framework walls of the GAPs, causing constriction of the channels. The SEM images in Fig. S7 show significant morphological differences for the surfaces and sections of the as-prepared and Pb-adsorbed samples. Fig. S7 demonstrates clearly that the Ga0.1Al0.9PO4 has a mesoporous morphology with regular continuous wormlike mesopores of ca. 10.0 nm in diameter, which is consistent with the BET results. A narrow size distribution of the formed mesopores and no large pores were observed in the image, indicating the homogeneity of the GAP matrix and no phase separation during the sol–gel process of the GAP formation. The homogeneous distribution of the pores in the matrix provides a basis for uniform distribution of the active sites in the mesoporous framework, an essential prerequisite for highly efficient adsorption of heavy metal ions. The surface of the Pb-adsorbed samples turns rough and a layer of sediment was formed on the surface.

X-ray photo-electron spectroscopy was applied to further investigate the surface states of the as-prepared and Pb(II)-adsorbed GAP samples. In addition to Ga, Al, P, and O, XPS peaks for Pb2+ ions (Fig. 5a) are evident for the Pb(II)-adsorbed sample. Furthermore, the high resolution XPS spectrum of the Pb-4f region clearly demonstrates the presence of Pb(II) (Fig. 5c). The two broad peaks were assigned to Pb-4f5/2 and Pb-4f7/2, respectively. Changes in the center of gravity and full width at half maximum (FWHM) for the O-1s, Al-2p, P-2p and Ga-3d spectra are summarized in Table 4. The O-1s peak after Pb(II) adsorption was broader and had shifted to a lower binding energy as a result of the appearance of additional types of oxygen species, which overlap with the original O-1s signals. It is shown that the O-1s peak of the Pb-adsorbed sample (Fig. 5b) can be deconvoluted into four Gaussian peaks at about 530.8, 531.5, 532.0, and 532.6 eV, which were attributed to oxygen atoms in H–O–P, Pb–O–P, Ga–O–P and Al–O–P groups, respectively.32–34 The formation of H–O–P and Pb–O–P after Pb adsorption suggests that hydroxyl groups played a vital role in the adsorption. The average P-2p binding energy shifts to lower values after Pb(II) adsorption, presumably reflecting the continuous alteration from P–O–Al and P–O–Ga toward P–O–H and P–O–Pb on the surface. Consistent with this difference, the average Al-2p and Ga-3d binding energies tend to decrease after Pb(II) adsorption. This trend is due to the higher ionicity of P–O–Pb and P–O–H compared with P–O–Al and P–O–Ga bonds. The XPS spectra give an impression of how the surface chemistry state of the GaAlPO4 glass is modified through adsorption of Pb(II) in water. The ion-exchange mechanism induced the formation of more highly polarized P–O–Pb and P–O–H bonds on the surface.


image file: c6ra17766b-f5.tif
Fig. 5 (a) Survey, (b) O-1s, (c) P-2p and Pb-4f, (d) Al-2p, and (e) Ga-2p high resolution XPS spectra of the as-prepared and Pb(II)-adsorbed Ga0.1Al0.9PO4 mesoporous glass.
Table 4 Average binding energies and FWHM values measured from the O-1s, P-2p, Al-2p and Ga-2p XPS spectra of the as-prepared and Pb-adsorbed Ga0.1Al0.9PO4 glass
Sample ID O-1s P-2p Al-2p Ga-2p
Ga0.1Al0.9PO4 532.4(2.9) 135.6(4.4) 76.1(2.5) 1119.8(4.1) 1146.6(3.5)
Pb-Adsorbed 531.8(3.2) 134.6(4.6) 75.5(2.6) 1118.9(4.0) 1146.1(3.5)


4. Conclusion

Mesoporous GaAlPO4 glasses with varying compositions (Ga content from 0 to 25%), high specific surface areas (up to 515 m2 g−1) and uniform worm-hole like mesopores (∼8–12 nm) were fabricated via a facile sol–gel route free of any surfactant or template, for the first time, based on an unusual chelation of the metal precursors in aqueous solution. The conversion from the gel to the final glass was monitored using advanced solid-state NMR techniques, elucidating the molecular mechanism and the nature of the gallium incorporation into the aluminum phosphate materials. The mesoporous ternary oxide glasses had a high adsorption ability (>36.63 mg g−1, that is 0.18 mmol g−1) for Pb(II) anions in aqueous solution, showing a high potential for heavy metal ion sequestration applications. Given that the precursors are all common and non-toxic (metal salts and acid), the present synthetic strategy can be further extended to the development of cheap phosphate mesoporous materials with chemical diversity and a high surface area for large-scale applications, such as the fabrication of sensors, separation membranes, supercapacitors, and catalysts.

Acknowledgements

We thank Prof. H. Eckert for helpful discussions on the glass structure. We are grateful to Dr M. Xu and Prof. J. Ren for NMR characterization, Mr J. Xie for the XRD analysis, Dr T. Ye for help with the BET measurements and Mr Y. Xu for the ICP analysis. This work was financially supported by the National Natural Science Foundation of China (Grant No. 61275208).

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Footnote

Electronic supplementary information (ESI) available. See DOI: 10.1039/c6ra17766b

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