Sodium Silicate from Rice Husk Ash and Their Effects as Geopolymer Cement

Sodium silicate is a commonly used activator in geopolymer that is produced commercially. In this study, rice husk ash (RHA) from agricultural waste was used to synthesize sodium silicate as an activator for geopolymer cement. This white ash was applied for producing sodium silicate with different molarities (8, 10, and 12) and then used to synthesize fly ash-based geopolymer cement. Scanning Electron Microscopy (SEM), X-ray Diffraction (XRD), and Fourier Transform Infrared Spectroscopy (FTIR) were applied to investigate the micro-characteristics of the geopolymerization products. Bulk density, water absorption, compressive strength, flexural strength, and fracture toughness were carried out to measure and evaluate the geopolymers with sodium silicate. The combination of 10 M NaOH with sodium silicate increased the compressive strength by 16.21% and the flexural strength and fracture toughness by 81.6%. However, sodium silicate combined with 12 M NaOH decreased compressive strengths by 13.23% and flexural strength and fracture toughness by 61.94%. The lowest water absorption value of 12.3% was obtained in a geopolymer paste using sodium silicate combined with 10 M NaOH, and the largest was 13.3% for sodium silicate combined with 8 M NaOH. The microstructure analysis showed the hydrated calcium alumina silicate gel (C–A–S–H) and the SEM image also revealed a compact geopolymer matrix. Thus, it can be concluded that sodium silicate from rice husk ash can be utilized as an activator or reactive material to produce geopolymer cement with a good geopolymer network.


Introduction
Ordinary Portland Cement (OPC) is a construction material that is widely used due to its availability, ease of application, cost-effectiveness, superior mechanical properties, and durability. Currently, cement production is 2.8 billion tonnes yearly and will rise by 4 billion tonnes yearly [1]. This trend shows that global cement demand will grow to 5.5 Gt yearly by 2050 [2]. Its production leads to carbon dioxide (CO 2 ) emissions, causing global warming. Cement is an energy-dense material that depletes available natural resources and releases 0.8 tonnes of CO 2 for every tonne of cement production [3,4].
Several studies have been conducted to find a substitute for cement that is more environmentally friendly and possesses good durability. Many researchers have suggested geopolymers because they are stronger than cement, are more environmentally friendly, and can be produced at lower temperatures [5][6][7]. Geopolymers are a class of "inorganic polymers processed by polycondensation of aluminum and silicon monomeric or oligomeric species in metal alkali-activated solutions" [8]. The geopolymer precursors can be generated from silica and aluminosilicate sources, such as fly ash, metakaolin, clays, etc.
In producing geopolymers, commercial sodium silicate is applied, and they are produced from sand containing high silica and use a high temperature of approximately 1400 • C [9]. An alternative is needed in producing sodium silicate so that it can be more environmentally friendly. Sodium silicate is required by a geopolymer as an activator along with a solution of sodium hydroxide to become an alkaline solution. One alternative material that can be used to produce sodium silicate is rice husk ash (RHA). This material is a reasonably available agricultural waste containing up to 90% SiO 2 , and its application to geopolymers has been reported [10,11]. RHA has been widely examined recently as a promising additive to cement and geopolymer and is also used to produce sodium silicate [12]. However, the mechanical testing of geopolymers on flexural strength and fracture toughness using sodium silicate from RHA has never been carried out.
Using agricultural waste, geopolymer preparation for new applications can be more complicated than using pure materials, because of the impurities in rice husk ash and fly ash. Studies investigating the use of RHA activators in geopolymer applications are limited. Therefore, the chemical explanation of geopolymer formation from industrial byproducts is a challenge. The primary objective of this study was to investigate RHA as a material for making sodium silicate and using it as an activator in geopolymer cement. The monitoring of geopolymer cement formation was characterized by water absorption, bulk density, and compressive strength after 28 days at room temperature. The microstructural properties of at least 28 days of geopolymer cement was determined using X-ray Diffraction (XRD) and Scanning Electron Microscopy Coupled with Energy-Dispersive X-ray (SEM-EDX).

Materials
This study utilized these materials for synthesizing sodium silicate and industrial by-product-based epoxy-geopolymer pastes. Rice husk ash (RHA) is taken from a refinery in the Aceh Besar District, Aceh, Indonesia. The RHA is white. Table 1 presents the chemical composition of RHA, indicated by XRF, and Figure 1 illustrates the SEM images and XRD of RHA. Class C fly ash (SiO 2 + Al 2 O 3 + Fe 2 O 3 > 70%) (ASTM C618) was taken from the Nagan Raya Thermal Power Project (PLTU Nagan Raya), Aceh, Indonesia. The chemical composition of fly ash was indicated by XRF, as shown in Table 1. The SEM image in Figure 1 shows that the fly ash particles are not spherical and tend to be irregular. From a workability point of view, the fly ash particles with non-spherical particle shapes will increase internal friction, absorption ability, and liquid demand. The fly ash used has an average size of 30 m and an average specific gravity of 2.45. The SEM micrographs obtained for RHA and fly ash are shown in Figure 1, presenting their specific morphologies.  The alkaline solution is the combination of 10 M sodium hydroxide pellets (NaOH) and sodium silicate (Na2SiO3). The industrial-grade sodium hydroxide pellets, with 98% purity, were dissolved in distilled water. The sodium silicate used in this study is a solution made in the laboratory with the sol-gel method as purposed by some researchers [13,14]. The alkaline solutions in this study for different Na2SiO3 to NaOH volume ratios were 1:1 and were prepared in the laboratory the day before use. The role of the alkaline solution is to improve the polymerization process with fly ash.

Synthesis of Sodium Silicate
In this study, sodium silicate was prepared in three variations with 8, 10, and 12 M NaOH solutions. Beforehand, NaOH solution was prepared with a molarity of 8, 10, and 12 M. Sodium silicate from RHA was synthesized by attaching the RHA to sodium hydroxide pellets with a ratio of RHA/NaOH solution = 1:6 (w/v). One hundred grams of rice husk ash was weighed and dissolved in a 600 mL NaOH solution. The assembly was mixed for 1 h at 90 °C under reflux conditions to improve the silica dissolution from RHA, and the mixture was undertaken at 1100 rpm. It was filtered, and then 1 N HCl was added so that the pH of the solution was 7. The gel was then left for 18 h at room temperature. Next, it was washed using warm distilled water and re-filtered. The addition of HCl re- The alkaline solution is the combination of 10 M sodium hydroxide pellets (NaOH) and sodium silicate (Na 2 SiO 3 ). The industrial-grade sodium hydroxide pellets, with 98% purity, were dissolved in distilled water. The sodium silicate used in this study is a solution made in the laboratory with the sol -gel method as purposed by some researchers [13,14]. The alkaline solutions in this study for different Na 2 SiO 3 to NaOH volume ratios were 1:1 and were prepared in the laboratory the day before use. The role of the alkaline solution is to improve the polymerization process with fly ash.

Synthesis of Sodium Silicate
In this study, sodium silicate was prepared in three variations with 8, 10, and 12 M NaOH solutions. Beforehand, NaOH solution was prepared with a molarity of 8, 10, and 12 M. Sodium silicate from RHA was synthesized by attaching the RHA to sodium hydroxide pellets with a ratio of RHA/NaOH solution = 1:6 (w/v). One hundred grams of rice husk ash was weighed and dissolved in a 600 mL NaOH solution. The assembly was mixed for 1 h at 90 • C under reflux conditions to improve the silica dissolution from RHA, and the mixture was undertaken at 1100 rpm. It was filtered, and then 1 N HCl was added so that the pH of the solution was 7. The gel was then left for 18 h at room temperature. Next, it was washed using warm distilled water and re-filtered. The addition of HCl resulted in a pH of 7 for the solution, and the initial pH of the solution was 12. The addition of HCl, up to pH 7, causes polymerization and the formation of Si-O-Si bonds. This bond will contribute to the geopolymer. The obtained products were nanosilica-based sodium silicates. Specimens prepared with these silicates were denoted as N-X, where X refers to the molarity of the NaOH used in the preparation of sodium silicate. The synthesis of sodium silicate is shown in Figure 2a. will contribute to the geopolymer. The obtained products were nanosilica-based sodium silicates. Specimens prepared with these silicates were denoted as N-X, where X refers to the molarity of the NaOH used in the preparation of sodium silicate. The synthesis of sodium silicate is shown in Figure 2a.

Preparation of Geopolymer Paste
Geopolymer cement pastes were made by placing fly ash into an alkaline solution and mixing for 20 min. Afterwards, the specimens were cast in 5 × 5 × 5 cm 3 cubes. Specimens were released from the mold after three days. The geopolymer cement specimens, after casting, were placed at ambient temperature (28-30 °C) until the test age of 28 days. Samples are denoted as Geo N-X, where X refers to the molarity of the NaOH used in the preparation of sodium silicate. Table 2 illustrates the mix proportion of geopolymer pastes. The preparation of geopolymer paste is shown in Figure 2b.

Microstructure Characterization
The XRD scans were performed at 10 to 50 °2theta with a scan speed of 0.5 s/step. XRD samples were prepared by pressing raw materials between two glass slides into flattening sheets and were analyzed using Shimadzu XRD-7000, Kyoto, Japan. FTIR spectra were measured using Shimadzu-IRPrestige-21, Japan. The spectra were collected in the transmittance mode from a 4 cm −1 resolution over a 4000-500 cm −1 range. Spectra were recorded at a spectral resolution of 4 cm −1 , a scan speed of 0.2 cm/s, and were analyzed with Spectrum software.
The microstructures and surface morphologies were tested by the scanning electron microscope (SEM, EVOMA 15, ZEISS, Oberkochen, Germany). The specimens were observed and imaged at an 8 mm working distance and 5 kV accelerating voltage. Sulfur mapping was conducted using EDS adjunct to SEM at a spot size of 5 and magnification of 5000 with a 5 kV accelerating voltage. Synthesized nanosilica-based sodium silicate was measured and analyzed by TEM (JEOL JEM 1400 Peabody, MA, USA). TEM was used to obtain microstructural observations of sodium silicate-based nanosilica with high resolution with a voltage commonly used of 100 kV. The particle size of sodium silicate-based nanosilica was measured using a Particle Size Analyzer (PSA, Horiba SZ-100V2, Kyoto, Japan).

Preparation of Geopolymer Paste
Geopolymer cement pastes were made by placing fly ash into an alkaline solution and mixing for 20 min. Afterwards, the specimens were cast in 5 × 5 × 5 cm 3 cubes. Specimens were released from the mold after three days. The geopolymer cement specimens, after casting, were placed at ambient temperature (28-30 • C) until the test age of 28 days. Samples are denoted as Geo N-X, where X refers to the molarity of the NaOH used in the preparation of sodium silicate. Table 2 illustrates the mix proportion of geopolymer pastes. The preparation of geopolymer paste is shown in Figure 2b.

Microstructure Characterization
The XRD scans were performed at 10 to 50 • 2 Theta with a scan speed of 0.5 s/step. XRD samples were prepared by pressing raw materials between two glass slides into flattening sheets and were analyzed using Shimadzu XRD-7000, Kyoto, Japan. FTIR spectra were measured using Shimadzu-IRPrestige-21, Japan. The spectra were collected in the transmittance mode from a 4 cm −1 resolution over a 4000-500 cm −1 range. Spectra were recorded at a spectral resolution of 4 cm −1 , a scan speed of 0.2 cm/s, and were analyzed with Spectrum software.
The microstructures and surface morphologies were tested by the scanning electron microscope (SEM, EVOMA 15, ZEISS, Oberkochen, Germany). The specimens were observed and imaged at an 8 mm working distance and 5 kV accelerating voltage. Sulfur mapping was conducted using EDS adjunct to SEM at a spot size of 5 and magnification of 5000 with a 5 kV accelerating voltage. Synthesized nanosilica-based sodium silicate was measured and analyzed by TEM (JEOL JEM 1400, Peabody, MA, USA). TEM was used to obtain microstructural observations of sodium silicate-based nanosilica with high resolution with a voltage commonly used of 100 kV. The particle size of sodium silicate-based nanosilica was measured using a Particle Size Analyzer (PSA, Horiba SZ-100V2, Kyoto, Japan).

Water Absorption, Bulk Density, and Compressive Strength
The water absorption test was conducted following the ASTM C67-07 method. The three specimens were calculated at the average value and were set at 28 days. The bulk density was determined following the ASTM C8300-00 method. The compressive strength test was performed using a testing machine in accordance with ASTM C109. The geopolymer's compressive strength was calculated after 28 days under the ambient temperature. Three specimens of each synthesized geopolymer cement were examined and reported the average compressive strength values. The testing machine of compressive strength and the test setup are displayed in Figure 3. After the compressive strength test had been carried out, some of the geopolymer fragments were crushed. The powder obtained was used to identify the microstructure such as SEM, XRD, and infrared spectroscopy. The water absorption test was conducted following the ASTM C67-07 method. The three specimens were calculated at the average value and were set at 28 days. The bulk density was determined following the ASTM C8300-00 method. The compressive strength test was performed using a testing machine in accordance with ASTM C109. The geopol ymer's compressive strength was calculated after 28 days under the ambient temperature Three specimens of each synthesized geopolymer cement were examined and reported the average compressive strength values. The testing machine of compressive strength and the test setup are displayed in Figure 3. After the compressive strength test had been carried out, some of the geopolymer fragments were crushed. The powder obtained was used to identify the microstructure such as SEM, XRD, and infrared spectroscopy.

Flexural Strength and Fracture Toughness
Three-point bending tests were undertaken to obtain the flexural strength and frac ture toughness using Testometric material testing machines with a loading rate of 10 mm/min with a specimen size of 40 mm × 40 mm × 160 mm. At the bottom of the speci mens, a crack length (a) of 20 mm was created. A saw was used to trim the specimens This method was conducted following the ASTM D5045-14 standard. The test setup sche matic is shown in Figure 4. The flexural strength ( F) was analyzed using the following formula:

Flexural Strength and Fracture Toughness
Three-point bending tests were undertaken to obtain the flexural strength and fracture toughness using Testometric material testing machines with a loading rate of 10 mm/min with a specimen size of 40 mm × 40 mm × 160 mm. At the bottom of the specimens, a crack length (a) of 20 mm was created. A saw was used to trim the specimens. This method was conducted following the ASTM D5045-14 standard. The test setup schematic is shown in Figure 4. The water absorption test was conducted following the ASTM C67-07 method. The three specimens were calculated at the average value and were set at 28 days. The bulk density was determined following the ASTM C8300-00 method. The compressive strength test was performed using a testing machine in accordance with ASTM C109. The geopolymer's compressive strength was calculated after 28 days under the ambient temperature. Three specimens of each synthesized geopolymer cement were examined and reported the average compressive strength values. The testing machine of compressive strength and the test setup are displayed in Figure 3. After the compressive strength test had been carried out, some of the geopolymer fragments were crushed. The powder obtained was used to identify the microstructure such as SEM, XRD, and infrared spectroscopy.

Flexural Strength and Fracture Toughness
Three-point bending tests were undertaken to obtain the flexural strength and fracture toughness using Testometric material testing machines with a loading rate of 10 mm/min with a specimen size of 40 mm × 40 mm × 160 mm. At the bottom of the specimens, a crack length (a) of 20 mm was created. A saw was used to trim the specimens. This method was conducted following the ASTM D5045-14 standard. The test setup schematic is shown in Figure 4. The flexural strength ( F) was analyzed using the following formula: The flexural strength (σ F ) was analyzed using the following formula: where P m is the maximum load read on the tool, S is the span of the specimen, B is the specimen width, and W is the specimen thickness. Fracture toughness (K IC ) was analyzed using the following formula: where a W is the ratio of the crack length and the thickness of 0.4, and (a/W), is the polynomial correction factor.

Bulk Density
The quality of geopolymer cement can be analyzed by its bulk densities. Geopolymer cement's bulk density range is from 1.2 to 1.7 g/cm 3 [16,17]. The bulk density values of specimens containing different sodium silicates are shown in Figure 5. The results indicate that increasing the molarity of NaOH during the sodium silicate synthesis, from 8 M to 10 M, increased the overall bulk density of geopolymer cement. Figure 5 shows that bulk density increased at 10 M NaOH concentration but decreased at 12 M concentration. This may be related to the fact that Geo N-12 paste looked more viscous, which may have made the formation of polymer gels more difficult. The lower bulk density of Geo N-12 geopolymer may also indicate a worse compaction of the specimens with respect to Geo N-10, which may be explained by a higher viscosity of the paste at a fresh state.
Polymers 2022, 14, x where Pm is the maximum load read on the tool, S is the span of the specimen, B specimen width, and W is the specimen thickness.
Fracture toughness (KIC) was analyzed using the following formula: where (a/W) is the ratio of the crack length and the thickness of 0.4, and (a/W), is t ynomial correction factor.

Bulk Density
The quality of geopolymer cement can be analyzed by its bulk densities. Geop cement's bulk density range is from 1.2 to 1.7 g/cm 3 [16,17]. The bulk density va specimens containing different sodium silicates are shown in Figure 5. The results in that increasing the molarity of NaOH during the sodium silicate synthesis, from 8 M M, increased the overall bulk density of geopolymer cement. Figure 5 shows th density increased at 10 M NaOH concentration but decreased at 12 M concentratio may be related to the fact that Geo N-12 paste looked more viscous, which may hav the formation of polymer gels more difficult. The lower bulk density of Geo N-12 g ymer may also indicate a worse compaction of the specimens with respect to Geo which may be explained by a higher viscosity of the paste at a fresh state.

Water Absorption
The degree of geopolymerization can lead to a less permeable matrix structure a that is more dense (less porous). The specimens of Geo N-10 paste presented a min water absorption of 12.3% m while the maximum value was obtained at 13.3% at sodium silicate concentration. Furthermore, for a given sodium silicate (N-8) val geopolymer exhibited a higher water absorption as compared to N-12. This is due

Water Absorption
The degree of geopolymerization can lead to a less permeable matrix structure and one that is more dense (less porous). The specimens of Geo N-10 paste presented a minimum water absorption of 12.3% m while the maximum value was obtained at 13.3% at an N-8 sodium silicate concentration. Furthermore, for a given sodium silicate (N-8) value, the Polymers 2022, 14, 2920 7 of 14 geopolymer exhibited a higher water absorption as compared to N-12. This is due to the higher porosity in the specimens and the lower bonding between the fly ash and the geopolymer gel.
Referring to Figure 5, in general, water absorption is reduced with an increase in the density of geopolymer paste. The water absorption value was from 12.3 to 13.3%, under the maximum value of the ASTM-C216 standard (15%). Based on this standard, this material could be used in construction and buildings.

Compressive Strength
The critical parameter in the material is the compressive strength that is used to meet engineering quality. Thus, the impact of sodium silicate on the compressive strength of geopolymer cement was decided, and the means are illustrated in Figure 6.
Polymers 2022, 14, x the maximum value of the ASTM-C216 standard (15%). Based on this standard, th terial could be used in construction and buildings.

Compressive Strength
The critical parameter in the material is the compressive strength that is used t engineering quality. Thus, the impact of sodium silicate on the compressive stren geopolymer cement was decided, and the means are illustrated in Figure 6. The geopolymer cement's compressive strength depends on the strength of th polymer gel and the interfacial bonding [18]. The results revealed that the comp strength increased due to the increase in C-S-H and N-A-S-H gels in geopolym formed from sodium silicate in Geo N-10 specimens. Sodium silicate plays a role formation of this geopolymer gel. The compressive strength of geopolymers con sodium silicate with NaOH concentrations of 8 and 10 M reached around 23.69 M 27.53 MPa, respectively. Using the sodium silicate produced with 12 M NaOH con tion, the compressive strength decreased to 23.89 MPa. These results are consisten studies conducted by previous researchers [13,19,20]. The increase in comp strength is related to a high amount of silicon dioxide (SiO2) in the Geo N-10 spe This silica plays a role in the interfacial bonding reaction between the fly ash m thereby increasing its strength [21]. The lower strength was observed for the geop specimens prepared at 12 M NaOH. This can be attributed to the reduced quantit Al-O bonds.  The geopolymer cement's compressive strength depends on the strength of the geopolymer gel and the interfacial bonding [18]. The results revealed that the compressive strength increased due to the increase in C-S-H and N-A-S-H gels in geopolymer gels formed from sodium silicate in Geo N-10 specimens. Sodium silicate plays a role in the formation of this geopolymer gel. The compressive strength of geopolymers containing sodium silicate with NaOH concentrations of 8 and 10 M reached around 23.69 MPa and 27.53 MPa, respectively. Using the sodium silicate produced with 12 M NaOH concentration, the compressive strength decreased to 23.89 MPa. These results are consistent with studies conducted by previous researchers [13,19,20]. The increase in compressive strength is related to a high amount of silicon dioxide (SiO 2 ) in the Geo N-10 specimen. This silica plays a role in the interfacial bonding reaction between the fly ash matrices, thereby increasing its strength [21]. The lower strength was observed for the geopolymer specimens prepared at 12 M NaOH. This can be attributed to the reduced quantity of Si-Al-O bonds.       Increasing the molarity of sodium silicate can increase the amount of reaction production of the geopolymer matrix significantly so that the compressive and flexural strength of the geopolymer paste also increases. High alkali and calcium from the fly ash react to form C-H-S, or C-A-S-H and N-A-S-H gels and contribute to the increased mechanical strength of the geopolymer paste [22,23]   12 M molarity on geopolymer paste resulted in a fracture toughness of 0.47, 0.86, and 0.32 MPa·m 1/2 , respectively. The increase in the fracture toughness of the geopolymer with 10 M sodium silicate is related to the good dispersion and reaction of the silica in the sodium silicate throughout the matrixso as to increase the geopolymer gel and fracture toughness [24]. Table 3 compares the mechanical strength results of this study with several other studies using commercial sodium silicate.  [29] NaOH + Na 2 SiO 3 50.1-56.7 7.0-9. Polymers 2022, 14, x M sodium silicate is related to the good dispersion and reaction of the silica in the silicate throughout the matrixso as to increase the geopolymer gel and fracture tou [24]. Table 3 compares the mechanical strength results of this study with sever studies using commercial sodium silicate.  [29] NaOH + Na2SiO3 50.1-56.7 7.0-9.3 10 3.1.6. XRD Patterns of Geopolymers Figure 9 presents the XRD patterns of selected geopolymer paste showing a broad hump pattern between 2θ = 25 and 30° centered around 26.64-26.78 °2 Theta corresponds to the quartz phase that is well-identified in FA. All XRD patterns show similar behavior. The presence of mineral quartz is ob with the peaks at 26.64°, 26.78°, and 26.72° (2θ, CuKα) in geopolymers with sodi cate Geo N-8, Geo N-10, and Geo N-12, respectively. The intensity of the X-ray dif patterns of the geopolymer with sodium silicate shows nearly similar bands to (Figure 9a), which is related to the formation of geopolymer networks in all spe The intensity of this broad hump is higher on the XRD patterns of sodium silica 10 M NaOH (Figure 9c). Mineral phases, mullite, and quartz were visible in the g mer XRD patterns, indicating that these minerals remain present during the geop ization process. This implies that the higher the SiO2/Na2O molar ratio, the more All XRD patterns show similar behavior. The presence of mineral quartz is observed with the peaks at 26.64 • , 26.78 • , and 26.72 • (2θ, CuKα) in geopolymers with sodium silicate Geo N-8, Geo N-10, and Geo N-12, respectively. The intensity of the X-ray diffraction patterns of the geopolymer with sodium silicate shows nearly similar bands to fly ash (Figure 9a), which is related to the formation of geopolymer networks in all specimens. The intensity of this broad hump is higher on the XRD patterns of sodium silicate with 10 M NaOH (Figure 9c). Mineral phases, mullite, and quartz were visible in the geopolymer XRD patterns, indicating that these minerals remain present during the geopolymerization pro-cess. This implies that the higher the SiO 2 /Na 2 O molar ratio, the more sialate (Si-O-Al-O) bonds tend to increase, enhancing the geopolymer network [30]. Figure 10 represents the FTIR spectrum of geopolymer paste measured after 28 days. The FTIR spectrum of the geopolymer pastes showed a band around 464 cm cribed to the Si-O vibration. A very weak band discerned at 459-572 cm −1 related formation of sialate bonds (Si-O-Al-O) related to the sodium silicate's polycondens This band is characteristic of crystalline cristobalites [31]. The band at 978-991 cm − cated that the main geopolymer structure from RHA was Si-O-Al [32,33]. This sh that RHA's sodium silicate could be used as an activator to produce good geopo cement. This band is recognized as the primary band of geopolymer cement and signed to Si-O-M (M = Si, Al, Na) [34]. The bands that appeared at 1387-1392 cm −1 sh the C-O bond of the carbonate groups. This indicated the emergence of sodium bonate due to atmospheric carbonation. The bending of H-O-H and stretching of appeared to have formed in the bands at 1664 and 3182 cm −1 . This signified the pre of bound water molecules in the polymeric framework.

FTIR Spectra of Geopolymers
On the specimens of Geo N-8, Geo N-10, and Geo N-12, the value of the wavenu showed that the asymmetric Si-O-M (M Si, Al, Na, H) almost changed at 1387 cm reduction in this wavenumber that appeared at about 991 and 3182 cm −1 in the IR spe indicates the depolymerization of the silica network [35].

Microstructure
Specimens were analyzed to identify geopolymer paste's morphological pas tained with sodium silicate from RHA as an activator. The scanning electron micro images of geopolymer pastes at 28 days on Geo N-8, Geo N-10, and Geo N-12 spec are shown in Figure 11. This band is characteristic of crystalline cristobalites [31]. The band at 978-991 cm −1 indicated that the main geopolymer structure from RHA was Si-O-Al [32,33]. This showed that RHA's sodium silicate could be used as an activator to produce good geopolymer cement. This band is recognized as the primary band of geopolymer cement and is assigned to Si-O-M (M = Si, Al, Na) [34]. The bands that appeared at 1387-1392 cm −1 showed the C-O bond of the carbonate groups. This indicated the emergence of sodium bicarbonate due to atmospheric carbonation. The bending of H-O-H and stretching of (OH) appeared to have formed in the bands at 1664 and 3182 cm −1 . This signified the presence of bound water molecules in the polymeric framework.
On the specimens of Geo N-8, Geo N-10, and Geo N-12, the value of the wavenumber showed that the asymmetric Si-O-M (M Si, Al, Na, H) almost changed at 1387 cm −1 . The reduction in this wavenumber that appeared at about 991 and 3182 cm −1 in the IR spectrum indicates the depolymerization of the silica network [35].

Microstructure
Specimens were analyzed to identify geopolymer paste's morphological paste obtained with sodium silicate from RHA as an activator. The scanning electron microscope images of geopolymer pastes at 28 days on Geo N-8, Geo N-10, and Geo N-12 specimens are shown in Figure 11. All images show the presence of micro-fissures related to the previously tested geopolymer paste. The images with higher magnification showed that geopolymer paste has a homogeneous microstructure. Figure 11a,c show the presence of a bright, sponge-like powder indicating that the NaOH present in the alkaline solution did not react to form Na2CO3. This Na2CO3-like sponge is commonly found in a NaOH solution-activated geopolymer when excess Na + ions are not bound to the Al 3+ sites of the geopolymer matrix All images show the presence of micro-fissures related to the previously tested geopolymer paste. The images with higher magnification showed that geopolymer paste has a homogeneous microstructure. Figure 11a,c show the presence of a bright, sponge-like powder indicating that the NaOH present in the alkaline solution did not react to form Na 2 CO 3 . This Na 2 CO 3 -like sponge is commonly found in a NaOH solution-activated geopolymer when excess Na + ions are not bound to the Al 3+ sites of the geopolymer matrix [20]. This finding is the same as the result of the FTIR analysis in the band 1387-1392 cm −1 , indicating that the vibration of sodium bicarbonate's C-O bond is due to atmospheric carbonation.
Micrographs (Figure 11b) did not show much white powder, and the paste appeared to be denser. Thus, Na + ions can bind to Al 3+ and play a role in improving the mechanical strength of the geopolymer and produce good connectivity between fly ash and sodium silicate solution from rice husk ash. From micrograph investigations, it was observed that sodium silicate made from rice husk ash could be used as an alternative to commercial sodium silicate. Micro-cracks and visible pores appeared in all specimens. RHA dissolved in 10 M NaOH solution showed that the soluble silica formed could play the same role as standard sodium silicate.

Conclusions
This study showed that silica obtained from an agricultural byproduct can be used to produce sodium silicate and can be applied as an activator for geopolymer cement based on fly ash. The test results demonstrated that the sodium silicate from RHA with NaOH concentrations of 8 and 10 M increased the geopolymers' density and increased the compressive strength; however, at 12 M, the NaOH concentration in sodium silicate decreases. The best compressive strength and water absorption were at 27.53 MPa and 12.3%. The compressive strength of the geopolymer pastes with NaOH concentrations in sodium silicate 8, 10, and 12 M were 23.69, 27.53, and 23.89 MPa, respectively. The bulk density of the geopolymer based on sodium silicate from NaOH also showed a similar trend. In this study, the best value was found for sodium silicate with 10 M NaOH, namely 1.59 g/cm 3 . In sodium silicate with a 12 M NaOH concentration, there was an increase in the chemical compound Na 2 CO 3 . On specimen Geo N-12, the mechanical strength of the geopolymer paste decreased because the excess Na + was not bounded to Al 3+ from the geopolymer matrix. The same trend was confirmed in compressive strength, flexural strength, and fracture toughness which each increased by 16.2, 81.6, and 81.6%. The method in this study can be used as an alternative for communities in rice-producing areas to use RHA waste to produce this valuable chemical reagent. The utilization of agricultural waste materials is not only economical but also can lead to environmental pollution control.