Xiulei Ji‡
a,
Guang Hea,
Carmen Andreib and
L. F. Nazar*a
aUniversity of Waterloo, Department of Chemistry, Waterloo, Ontario, N2L 3G1, Canada. E-mail: lfnazar@uwaterloo.ca
bMcMaster University, Department of Chemistry and Canadian Facility for Electron Microscopy, Hamilton, Ontario L8S 4L8, Canada
First published on 17th April 2014
We report the transformation of mesoporous silica to its silicon replica with maintenance of structural regularity. The method employs mild displacement reactions with Mg intermetallics as the source of Mg vapor at low partial pressure. The mild conditions aid in high fidelity replication of the nanoporous framework of the starting silica.
The challenge still remains to find an effective porous silica → porous silicon conversion methodology which maintains nanostructural regularity for a wide variety of porous silica structures as bulk materials irrespective of morphology. Herein, we introduce a route described in Scheme 1 below, which employs MgxMy intermetallics as the reductants to gently convert silica nanostructures such as SBA-15 into their silicon replicas. The morphological and nanostructural features of the mesoporous silica are retained in their silicon replica without triggering over-reduction.
To realize the reaction in Scheme 1, the electronegativity of M in the intermetallic needs to be comparable or higher than that of silicon. In order to maintain the structure of the starting silica material, the enthalpy of the reaction needs to be weakly negative to prevent the highly exothermic reaction which gives rise to internally generated local heating that collapses the porous structure. Eqn. (1)–(5) show the reactions when Mg, Mg vapour, Mg2Sn, Mg3Sb2 and Mg2Si are used, respectively. The reactants and products are in their solid state unless otherwise specified.
| 2Mg + SiO2 → Si + 2MgO, ΔH = −292 kJ mol−1 | (1) |
| 2Mg(g) + SiO2 → Si + 2MgO, ΔH = −219 kJ mol−1 | (2) |
| Mg2Sn + SiO2 → Si + Sn + 2MgO, ΔH = −227 kJ mol−1 | (3) |
| 2Mg3Sb2 + 3SiO2 → 3Si + 4Sb + 6MgO, ΔH = −102 kJ mol−1 | (4) |
| Mg2Si + SiO2 → Si + Si* + 2MgO, ΔH = −221 kJ mol−1 | (5) |
The enthalpy changes per mole of silicon extracted from silica in the reactions (1)–(5) are calculated based on basic thermodynamic data.15 Note that Si* represents the silicon phase that originates from Mg2Si, which can be separated on the basis of density. The intermetallics, MgxMy (M = Si, Sn, Sb) exhibit more positive enthalpy changes than pure Mg due to their increased lattice energy arising from the polarized Mg–M bond. Heat capacities of different reaction mixtures can be estimated with the Dulong–Petit equation (c = 3R/M, where R is the gas constant, and M is the molar mass). The maximum temperature rises can therefore be calculated. They are 2131 °C for the SiO2/Mg (1
:
1 in mass) mixture, 603 °C for the SiO2/Mg3Sb2 (1
:
4 in mass) mixture and 1147 °C for the SiO2/Mg2Si (1
:
2 in mass) mixture under adiabatic conditions. The practical values will be less since the flowing argon gas carries away some heat and heat is also lost to the reaction container. The values shed light on the large difference in local reaction temperatures between different reduction reactions.
These reactions are effective because at elevated temperatures, Mg intermetallics sustain a measurable Mg vapour pressure which is naturally lower than that of Mg metal owing to the contribution of Mg-M bonding. Mg infusion into GaAs has been achieved using Mg3Sb2,16 and Mg vapour pressures have been measured for Mg2M (M = Ge, Si, Sn, Pb) between 600 and 900 °C, showing they increase in that order.17 The lower concentration of Mg in the gas phase (vis a vis the metal) results in a slower reaction rate, which consequently allows more effective dissipation of local heating.18 Differential scanning calorimetry (DSC) measurements were conducted to investigate reactions (1), (4), and (5) for a qualitative comparison, as depicted in Fig. 1. Silica and the reductants were ground together and loaded into a Pt cup. The variance in the elemental Mg loading between the three measurements was kept within 2%. A large and early exothermic peak at 590 °C is observed for reaction (1) in accord with the enthalpy estimate above. The exothermic signatures observed for (4) and (5) are weaker and appear at higher temperatures of 660 °C and 700 °C, respectively. The shift in temperature is likely due to the lower Mg vapor pressures, coupled with mass transport effects. The results thus inspired us to use reactions (4) and (5) to deoxygenate silica under mild conditions that preserve the nanostructural integrity. We demonstrate here that Mg2Si gives rise to better nanostructure retention at the temperature where magnesiothermic reduction occurs.
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| Fig. 1 Differential scanning calorimetry (DSC) under dynamic argon flow, of Mg and SiO2 (black curve, eqn (1)); Mg3Sb2 and SiO2 (blue curve, eqn (4)); Mg2Si and SiO2 (red curve, eqn (5)). | ||
Syntheses of Mg3Sb2 and Mg2Si were conducted by solid state reaction (see ESI†), and their purity was confirmed by comparison of their X-ray diffraction (XRD) patterns to the JPDS database ([01-071-0404] and [01-075-0445] respectively). These intermetallic phases are active in the magnesiothermic displacement reactions described below. We chose SBA-15,19 a well-established mesoporous silica, as the target nanostructure for reduction to its silicon replica analogue. The SBA-15 samples and an excess of reductant (by ∼25% in a molar ratio) were ground together intimately under an Ar atmosphere and pressed into a pellet under a pressure of 104 N cm−2, prior to reaction at 700 °C for 5 h (see ESI† for details). At this pressure, the pores in SBA-15 remain intact. Based on the measured densities of the pellets and the densities of solid components, these pellets have about 30% porosity. Within the pellets, magnesium vapor released from the decomposition of the intermetallic will react with the nearest neighbour silica particles. Mass transfer is of critical importance in this system, which is optimized to minimize Mg diffusion length while maintaining pathways for transport. We estimate that an Mg atom would have to travel a length scale of microns at most, given that the particle size of the SBA-15 is on this order, and that the particles are relatively well packed. This gives rise to good reaction homogeneity. Three different reactions were explored for comparison. Micron-sized particles of SBA-15 shown in Fig. 2a were reacted with Mg3Sb2 to form a silicon material referred to as Si–Mg3Sb2. Nano-sized SBA-15 was prepared as previously reported,20 and reacted with Mg2Si to form Si–Mg2Si. First, however, to provide a reference point, micron-sized SBA-15 particles were also reacted with Mg powder in a pellet (Mg/SiO2 mass ratio: 1 to 1) at 650 °C for 5 h under Ar to form Si–Mg. The SEM images in Fig. 2a and b show the difference in morphology between SBA-15 before and after conversion. Significant residual SBA-15 crystallites are evident due to incomplete reduction. These are easily identified because of their characteristic hexagonal morphology, (examples are highlighted in the red boxes). This is similar to that previously reported for other porous silicas.12 More importantly, reduction with Mg causes the discrete SBA-15 crystals to merge into large macroporous silicon agglomerates. The extensive morphology change is akin to a “welding process”, which indicates a local temperature above the melting point of the silicon micron-rods (∼1400 °C) was achieved despite the set temperature of 650 °C. This confirms the results of the above calculation on the temperature rise of the reaction mixture. This was so high that the reaction mixture pellet burst into powder after heating. The reaction is comparable to the well-known solid state metathesis processes21,22 that are also highly exothermic. The reaction of micron-sized SBA-15 with the intermetallic reducing agent Mg3Sb2 produced different results. The reaction mixture pellet remains intact after the reaction, and the excess Mg3Sb2 and residual MgO (indicated by the XRD pattern, Fig. S1†) were easily leached out from the crushed pellet with a mixture of HCl–HNO3. The particle morphology of SBA-15 is much better maintained under these conditions and forms the silicon product whose representative morphology is shown in the SEM image (Fig. 2c). These Si particles exhibit a characteristic surface morphology which appears very roughened, in contrast to the smooth solid surface of the SBA-15 particles shown in Fig. 2a. A thorough inspection of the sample confirmed that no SBA-15 particles remain. The crystalline nature of the Si–Mg3Sb2 is confirmed by the well resolved peaks in its wide angle XRD pattern (Fig. S2†). The coherence length is calculated to be approximately 25 nm, much less than that of Si–Mg (>40 nm). The non-Gaussian lineshape of the pattern indicates that there are in fact, two contributions to the line width, which were deconvoluted into a sharper more crystalline component with a coherence length of 25 nm, and a broader component with a coherence length of ∼6 nm. This indicates that Si–Mg3Sb2 was formed at a local reaction temperature high enough to melt silicon domains less than 20 nm, but low enough not to melt ones larger than 20 nm. The local temperature is lower than that of the Mg vapour reduction, as judged by the silicon domain sizes. Thus, given sufficient reaction time, the complete conversion of SiO2 to Si is readily achieved without over-reduction using the intermetallic. This is a significant advantage, since an excess of Mg3Sb2 ensures that complete reduction of silica stops at the formation of silicon. However, the highly ordered porous structure of the silica precursor is not maintained on the nanoscale. As in the case of Si–Mg, this is indicated by the absence of a well resolved peak in the low angle XRD pattern, (Fig. 3a and b) showing there is no long range order. TEM analysis confirmed this finding. The overall loosely connected structure of the SBA-15 derived silicon particles is shown in the TEM image in Fig. 2d, which is representative of the overall sample based on extensive mapping. Expansion of the region outlined by the white box is shown in Fig. 2e, with higher magnification and the accompanying HRTEM image is shown in Fig. 2f. Evident are silicon domains about 20 nm in dimension that exhibit clear (111) crystalline fringes (d: 0.32 nm), crystallized within larger particles (Fig. 2f) indicative of partial melting as suggested by the XRD.
To preserve the nanoporous long range order inherent in SBA-15, we reacted nano-sized SBA-15 together with the intermetallic Mg2Si which has a reported vapour pressure of Mg of 1 mm Hg at 790 °C.17 After reduction and HCl (2 M) treatment, two silicon phases remain, as described by reaction (5): one is the nano-phase from the reduction of the nano-SBA-15 silica that we term Si–Mg2Si. The other is the bulk Si phase released from reaction of the micron-sized Mg2Si reductant. Their separation was achieved by a sonication-precipitation method due to their vastly different particle sizes and density. After the mixture was sonicated for 10 h and allowed to stand for 24 h, the heavier bulk silicon phase settled and the lighter, suspended silicon nanorods were collected by simple centrifugation. The Si–Mg2Si was examined by SEM and analysed by EDX (Fig. 4b; S3†). Mapping under the microscope confirmed that the major product was nanorod Si–Mg2Si, although a few large particles from contamination of bulk Si arising from the reductant were still visible, which dominated the XRD pattern. EDX indicated the nanorods were primarily Si, with some residual oxide as expected from surface passivation. The nanorod morphology is well maintained after reduction to Si–Mg2Si; moreover, the well resolved peak in the low angle XRD pattern reveals the long range order is also preserved (Fig. 3c). The peak is assigned as the (100) plane inherited from the original hexagonal structure. The inherent porosity was confirmed by nitrogen absorption measurements of Si–Mg2Si which revealed a specific Brunauer–Emmett–Teller (BET) surface area of 300 m2 g−1 and a total Barrett–Joyner–Halenda (BJH) specific pore volume of 0.30 cm3 g−1 (see Fig. S4, ESI† for details). If the parent SBA-15 (620 m2 g−1) were topotactically converted to Si, a surface area of 530 m2 g−1 would be predicted in light of the density difference of the frameworks (2.3 cm3 g−1 for Si; 2.0 cm3 g−1 for mesoporous SiO2). Thus a sizable fraction of the silica structural porosity is retained in the transformation to silicon, although some is lost as expected. The pore size distribution shown in Fig. 3 (inset) indicates mesopores of 4 nm in dimension, in accord with the expected shrinkage of the 7 nm pores in SBA-15 silica on densification. To further confirm that it is the silicon that constitutes the nanoscopic regularity, we carried out high resolution TEM studies. Representative images (Fig. 4c, and expansions in Fig. 4d–f) show that discrete silicon nanocrystallites with characteristic d spacings of 0.32 nm or 0.196 nm ((111) and (220), respectively) form the wall structure in the well preserved nanoporous material. The size of the nanocrystallites is only ∼5 nm, substantially smaller than the silicon domains obtained by the other magnesiothermic chemistry, and also less than 13 nm as previously reported.12,14 This indicates the local reaction temperature must be much lower than the melting temperature of silicon. During reduction, magnesia particles and liberated silicon nanocrystallites are formed in concert. Nonetheless, the SBA-15 nanostructure is still maintained after magnesia removal.
Footnotes |
| † Electronic supplementary information (ESI) available: Syntheses of the intermetallics, and SBA-15,15,16 preparation of the nanoporous silicon, and BET and EDX data. See DOI: 10.1039/c3ra46557h |
| ‡ Current address: Professor Xiulei Ji, Department of Chemistry, Oregon State University, Corvallis OR, USA. |
| This journal is © The Royal Society of Chemistry 2014 |