Seongseop
Kim‡
a,
Ji Yeon
Park
bc,
Yang Mo
Gu
bc,
Il-Seop
Jang
de,
Hayoung
Park
de,
Kyeong Keun
Oh
f,
Jin Hyung
Lee
*b and
Jinyoung
Chun
*d
aMax-Planck-Institut für Kohlenforschung, Kaiser-Wilhelm-Platz 1, Mülheim an der Ruhr, 45470, Germany
bConvergence R&D Division, Korea Institute of Ceramic Engineering and Technology (KICET), Cheongju, Chungbuk 28160, Republic of Korea. E-mail: leejinh1@kicet.re.kr
cDivision of Chemical Engineering & Bio Engineering, Hanyang University, Seoul, 04763, Republic of Korea
dEnergy and Environment Division, Korea Institute of Ceramic Engineering and Technology (KICET), Jinju, Gyeongnam 52851, Republic of Korea. E-mail: jchun@kicet.re.kr
eDepartment of Materials Science and Engineering, Korea University, Seoul 02841, Republic of Korea
fDepartment of Chemical Engineering, Dankook University, Yongin, Gyeonggi 16890, Republic of Korea
First published on 8th October 2021
The valorization of inorganic silica components from rice husk has been considered an important research topic over the last few decades. However, owing to various problems, such as the difficulty in controlling precise morphological properties, complex extraction and manufacturing processes, and the use of hazardous acids, the technology for producing high value-added silica for industrial applications is still insufficient. In this study, we developed a method for obtaining size-controlled spherical silica from rice husk using an eco-friendly and simplified process that overcomes the above-mentioned limitations. Silica particles were obtained by extraction from rice husk in alkaline media under mild conditions (80 °C) followed by pH adjustment with acetic acid. Therefore, the use of strong acids was excluded, no special equipment was required for the process, and the overall synthetic process was significantly simplified. The silica particles obtained through this method were uniformly spherical in shape, with a surface area of more than 200 m2 g−1. Our results indicate that the preparation of silicate solution under appropriate conditions and the use of polyethylene glycol (PEG) additives during the precipitation step are important for obtaining spherical silica. Moreover, by adjusting the temperature in the precipitation step, the size of the spherical silica particles can be controlled in the range of ∼250 nm to ∼1.4 μm. Our study contributes to the development of rice husk-derived silica that can be applied to practical industrial applications.
The widely adopted approach for obtaining inorganic silica from rice husk is through direct combustion. This is a simple and cost-effective process, which can control the surface area, purity, and crystallinity of silica by adjusting the combustion conditions.5,6 Chemical treatments, such as acid leaching, have also been investigated to obtain high-purity silica with a large surface area from rice husk.7–10 For example, it was reported that silica particles with a purity of more than 99.5% could be successfully obtained through acid leaching followed by pyrolysis, with a surface area of 85 m2 g−1.9 Vayghan et al. reported that silica particles with a purity of 98% were obtained from pre-combustion acid-treated rice husk; the particles had a surface area of more than 280 m2 g−1.8 However, these methods not only result in the release of greenhouse gases or rely on the use of strong acids but also have clear limitations in terms of the shape and porous structure of the silica products.11,12 Although research on producing silica with a high purity and surface area through an eco-friendly process in which strong acids are replaced with an ionic liquid has been published, some limitations still exist in terms of precise morphology control of silica and the need for very expensive reagents.9
To obtain the high value-added silica required for various applications in modern industries, including the cosmetics, catalyst, biomaterial, and energy device industries,13–19 it is essential that the silica particles derived from rice husk have precise and specific morphological properties. Accordingly, synthetic methods based on bottom-up processes, which obtain nano- or micro-particles through chemical reactions of precursors at the atomic or molecular level, have received increasing research interest over recent years.12 In particular, various studies have investigated the production of nanostructured silica with well-defined mesopores through bottom-up processes using a rice husk-derived silicate solution.4,20–28
However, some critical problems are yet to be solved, including the following: (i) synthetic methods are complex; the steps include the acid leaching of rice husk, pyrolysis, silicate extraction in alkaline media, and reprecipitation with hazardous reagents (e.g., ammonia, sulfuric acid, and hydrochloric acid) (Fig. 1). The acid leaching of rice husk usually relies on the use of strong acids. Alkali extraction sometimes progresses at temperatures above the boiling point of the solution,4,21,25,28 in which case the evaporation of the solvent has to be safely prevented. This results in large energy consumption, and an increase in the process cost due to multiple steps and special equipment. This makes it difficult to apply the developed methods to real industries; (ii) although most studies have focused on controlling the pore structure and surface area of produced silica, there is a lack of research centered on the shape of silica particles; (iii) although several studies have reported on the production of spherical silica particles from rice husk, results included an uneven size distribution or aggregation of particles, and high-risk acids were still required during the acid leaching or precipitation steps.29–33 Therefore, to obtain high value-added silica from rice husk through precise morphological control for use in real industries, the above-mentioned problems must be solved comprehensively.
Fig. 1 Schematic representation of the procedure used to obtain morphology-controlled silica particles from rice husk. |
In this study, we developed and investigated an eco-friendly and facile method for obtaining size-controlled spherical silica particles from rice husk. Specifically, we obtained silica particles by alkali extraction under mild conditions, followed by precipitation with acetic acid (Fig. 1). Therefore, the use of strong acids was excluded, no special equipment was required, and the overall synthetic process was simplified. The silica particles obtained through this method were uniformly spherical in shape with a large surface area. Our results indicate that the preparation of silicate solution under appropriate conditions and the use of polyethylene glycol (PEG) additives during the precipitation step are important for obtaining spherical silica particles. As PEG has a sufficient number of ethylene oxide (EO) chains to stabilize the silicate species, it is presumed that even a small amount of PEG additive can control the morphology of the silica particles. PEG also has the advantageous of low toxicity and low cost, meaning that the manufacturing process can be made cheaper and safer. Furthermore, by adjusting the reaction temperature during precipitation, the size of the silica particles could be controlled in the range of ∼250 nm to ∼1.4 μm. Thus, we expect the developed method to have a great impact on the production of rice husk-derived silica for use in the practical industrial applications.
Fig. 2 Silica extraction yield depending on (a) the NaOH concentration at 80 °C and (b) the temperature using 0.2 M NaOH. |
The rice husk used in this study was composed of 52 wt% carbohydrates, 29 wt% lignin, and 14 wt% ash (Table 1). After treating with 0.2 M NaOH solution at 80 °C, the composition of the extracted solution was 46 wt% ash, 23 wt% lignin, and 19 wt% carbohydrates (Table 1). This result shows that some carbohydrates and lignin in rice husk were also leached into the solution, 9% and 19%, respectively. However, we found that if the ratio of leached carbohydrates and lignin is not relatively high, it does not interfere with the morphology control of silica particles, which are synthesized using the extracted solution in the next process. This will be further discussed in the next section.
Carbohydrates (wt%) | Lignin (wt%) | Ashb (wt%) | Others (wt%) | |
---|---|---|---|---|
a Ash means inorganic solid components. b See Tables 2 and S1 for the silica content in the ash. | ||||
Raw rice husk | 52 | 29 | 14 | 5 |
Extracted silicate solution (80 °C) | 19 | 23 | 46 | 12 |
Residual solid (80 °C) | 62 | 31 | 3 | 4 |
Extracted silicate Solution (150 °C) | 24 | 36 | 31 | 9 |
Residual solid (150 °C) | 88 | 12 | — | — |
On the other hand, when silica in rice husk was extracted under harsh conditions (150 °C), a large amount of carbohydrates and lignin was also leached into the solution. The composition of the extracted solution under harsh conditions was 31 wt% ash, 36 wt% lignin, and 24 wt% carbohydrates (Table 1). This indicates that almost 21% of carbohydrates and 56% of lignin in rice husk were leached into the solution. Accordingly, although the silica extraction yields under harsh conditions slightly increased due to high temperature and pressure (Fig. S1†), morphology-controlled silica particles could not be obtained in the next process due to the large amounts of organic components in the extracted solution. The effect of the extraction conditions on the production of silica particles will be covered in the next section.
Components | SS-1 | S-1 | S-2 | |
---|---|---|---|---|
ICP-OES | SiO2 | 97.76 | 98.15 | 97.85 |
Na2O | 2.000 | 1.763 | 2.030 | |
Al2O3 | 0.017 | 0.011 | 0.018 | |
Fe2O3 | 0.017 | 0.003 | 0.002 | |
CaO | 0.039 | 0.018 | — | |
MgO | 0.057 | 0.007 | — | |
K2O | 0.067 | 0.046 | 0.097 | |
MnO | 0.032 | 0.004 | — | |
Elemental analysis | Carbon (after drying) | 6.64 | 1.80 | 8.09 |
Carbon (after calcination) | 0.03 | 0.02 | 0.13 |
PEG plays an important role in the control of the particle morphology of silica during the precipitation. For comparison, bulk silica particles (S-1) were prepared with an identical procedure to SS-1 in the absence of the PEG additive. Fig. 4a and b show the overall morphology of S-1; only large-sized particles with irregular shapes were observed in the microscope images of S-1, indicating that PEG is an essential additive for controlling the spherical shape of silica particles. Similar phenomena were observed in previous studies that produced spherical silica using polymer additives.34,35 The silicate species were hydrolyzed and condensed for the silica growth, and therefore they have a number of hydroxyl groups, allowing interaction with EO chains in PEG by hydrogen bonding. When EO chains are long enough, the silicate species can be stabilized by interaction with EO chains during the precipitation process, leading to the formation of spherically shaped particles. As shown in Fig. S4,† absorption peaks related to the stretching and bending mode of the functional groups in PEG were also observed in the IR spectrum of SS-1 (before calcination). Referring to the results of previous studies,34,35 we assumed that the molecular weight of the PEG polymer (Mr: 2700–3300) used in this study was sufficient to produce uniform spherical particles.
Fig. 4 (a and b) SEM images (inset: TEM image), (c) XRD pattern, and (d) N2 physisorption isotherms of silica particles (S-1), synthesized without the polyethylene glycol (PEG) additive. |
The pore properties (e.g., pore size and pore volume) of S-1 were also changed in the absence of the PEG additive. The silicate species were precipitated with bulky organic components (e.g., lignin) to form irregular particles. Mesopores of S-1 were generated by removing lignin molecules after calcination, which is different from the formation of mesopores of SS-1. Lignin is composed of phenolic macromolecules which are larger molecules than PEG, resulting in an increased pore size (∼9 nm) and pore volume (0.659 cm3 g−1) of S-1 compared to those of SS-1 (Fig. 4d, S2b† and Table 3). For these reasons, S-1 showed a very large difference in the particle shape and pore properties from those of SS-1, while the other physicochemical properties of S-1 are similar to those of SS-1: purity (98.15%, Table 1), surface area (294 m2 g−1), and amorphous crystallinity (Fig. 4c). The concentration of PEG used when producing the silica particles also affects the uniformity of their shape. When less than 0.4 g of PEG per 200 mL of silicate solution was used, only irregular particles were obtained (data not shown). Therefore, we assumed that a certain concentration of PEG or higher is required to interact with the hydroxyl group of silica sufficiently for uniform spherical silica to form.
SS-1 | SS-2 | SS-3 | SS-4 | S-1 | S-2 | |
---|---|---|---|---|---|---|
Silicate extraction conditions | Mild (80 °C) | Harsh (150 °C) | ||||
Precipitation temperature | 25 °C | 5 °C | 40 °C | 60 °C | 25 °C | 25 °C |
Additive | PEG | PEG | PEG | PEG | None | PEG |
Surface area (m2 g−1) | 291 | 221 | 328 | 407 | 294 | 294 |
Pore volume (cm3 g−1) | 0.301 | 0.131 | 0.381 | 0.659 | 0.659 | 1.19 |
Average pore size (nm) | 4.13 | 2.38 | 4.64 | 6.48 | 8.98 | 16.1 |
Average particle size (nm) | 789 (±81) | 1355 (±290) | 400 (±124) | 250 (±71) | N/A | N/A |
Interestingly, the conditions under which the silicate solution is extracted from the rice husk also affected the morphology of the silica particles obtained from the silicate solution. When the silicate solution was extracted under harsh conditions (150 °C), only irregularly shaped particles (S-2) were obtained (Fig. 5a and b). Even though PEG was added in the same way as in the preparation of the SS-1 sample, the morphology of the S-2 particles differed from that of the SS-1 particles. The silicate solution extracted under harsh conditions contained a relatively large amount of dissolved organic components compared to that extracted under mild conditions (80 °C). Although there is a difference in absolute values, both PEG and organic components (e.g., lignin) are negatively charged at neutral pH. Accordingly, we suggest that the organic components hinder the interaction of PEG with silicate species, thereby reducing the effect of the addition of PEG. Therefore, S-2 particles exhibited an irregular shape similar to that of S-1, but not that of SS-1. The surface area of S-2 (294 m2 g−1) was similar to that of S-1, but its pore volume (1.19 cm3 g−1) and average pore size (∼16 nm) were larger than those of S-1 (Fig. 5d, S2c† and Table 3). This tendency may also be affected by the presence of organic components. As a large amount of organic components that had assembled with the precipitated silica was removed during the post-treatment process (washing and calcination), relatively large pores and large pore volumes could form on the surface of the S-2 particles.
Fig. 5 (a and b) SEM images (inset: TEM image), (c) XRD pattern, and (d) N2 physisorption isotherms of silica particles (S-2), synthesized using a silicate solution extracted under harsh conditions. |
The specific conditions, under which the silicate solution was extracted, affected not only the morphology of the silica particles, but also the efficiency of the particle collection process. Fig. S5† shows the filtration process of the SS-1 sample. When 100 mL of distilled water was used in each washing cycle of SS-1, the filtering time was only 8 s, and a rapid colour change of the sample was observed. Although the filtering speed of the S-1 sample was lower than that of the SS-1 (25 s/100 mL) sample, the S-1 sample could be collected by filtration. However, it proved impossible to separate the S-2 sample from the reactant solution because the filtering speed was extremely low. We assume that a large amount of organic components was filtered out along with silica particles, thereby blocking the space between particles and interfering with the penetration of the solvent. Therefore, the S-2 sample was collected and washed via centrifugation (5000 rpm for 5 min), which inevitably increased the processing time.
Fig. 6 SEM images of (a) SS-2 (5 °C), (b) SS-1 (25 °C), (c) SS-3 (40 °C), and (d) SS-4 (60 °C). Each value in parentheses represents the temperature of the precipitation process. |
The pore sizes of the silica particles also changed depending on the temperature during the precipitation and aging steps (Fig. 7). The SS-2 sample showed type I isotherms, which are observed in the microporous materials. Meanwhile SS-1, SS-3, and SS-4 samples exhibited type IV isotherms typical of mesoporous materials (Fig. 7a). An abrupt increase of adsorption volumes and hysteresis at high P/P0 indicates the presence of large-sized mesopores. This means that the mesopores of SS-4 exhibit a larger size than SS-1 and SS-3. As the temperature increased from 5 to 60 °C, the main pore size of the silica particles increased from less than 2 nm to approximately 10 nm (Fig. 7b). This tendency is thought to be related to the change in the hydrophilicity of PEG with temperature. An increase in temperature results in the dehydration of EO chains, thereby decreasing the hydrophilicity of the chains.38,39 Accordingly, more stretched PEG molecules were confined to the silicate frameworks of SS-2 during precipitation at 5 °C, leading to the formation of micropores (<2 nm). Low hydrophilicity at increased temperature induces large EO–EO aggregates. It weakens the interaction between EO chains and silicates when the PEG and silicate oligomers cooperatively assembled. As a result, the size of the pores generated by the PEG aggregates increased at high temperature (Fig. 7b).
Silica extraction yield = weight of ash precipitated/weight of ash in RH × 100 | (1) |
Footnotes |
† Electronic supplementary information (ESI) available. See DOI: 10.1039/d1na00668a |
‡ Current address: School of Chemical Engineering, Jeonbuk National University, Jeonju 54896, Republic of Korea. |
This journal is © The Royal Society of Chemistry 2021 |