Akira Kuwahara‡
*a,
Yuki Mizushima‡*b,
Makoto Matsuibc,
Tomoki Kozukad and
Nobuyuki Masecd
aDepartment of Applied Energy, Nagoya University, Aichi 464-8603, Japan. E-mail: akuwahara@energy.nagoya-u.ac.jp
bDepartment of Mechanical Engineering, Shizuoka University, Shizuoka 432-8561, Japan. E-mail: mizushima.yuhki@shizuoka.ac.jp
cGreen Energy Research Division, Research Institute of Green Science and Technology, Shizuoka University, Shizuoka 432-8561, Japan
dDepartment of Engineering, Shizuoka University, Shizuoka 432-8561, Japan
First published on 24th March 2022
This study presents the first experimental evidence of direct H2 production from seawater without harmful gas emissions (e.g., CO2, Cl2), which uses multiphoton ionization water splitting with a femtosecond pulse laser. According to H2 analysis using a gas chromatograph, the H2 production rate in seawater was 70 μmol h−1, which was approximately 3.3 times more than the ultrapure water case reported in the literature. This positive effect derives from focusing through the cuvette wall and the more significant Kerr effect in seawater. Such ion enhancement was observed in the case of seawater and diluted seawater compared with the ultrapure water case, but excessive salt can lead to ion suppression and adverse effects. These differences in salinity suggest appearances of nonlinear optical effects near the focal point and ionization of metallic elements with low ionization potential and are discussed in relation to results of bubble visualization, gas composition analysis, and pressure measurement in gaseous products.
While the cost of H2 production by water splitting will decline with renewable energy becoming more prevalent, the economic desalination technique of seawater is still under development due to the high costs of the cation exchange membrane and catalyst layer. Electrochemically active anions interfere and compete with the catalysis in seawater.13 In addition, toxic Cl2 gas forms at anode, which requires regular gaseous waste management system. The corrosion of tank and pipes by Cl2 also increases maintenance costs. Thus, a direct and selective water splitting of seawater into H2 and O2, in which chlorine ions are not involved in the process, is a potentially attractive breakthrough.14
Herein we present a game-changing solution for direct H2 production from seawater using multiphoton ionization water splitting (MPI-WS) with a femtosecond pulse laser. The ionization reaction triggered by multiphoton absorption of H2O molecules (the ionization potential of 6.5 eV) produces H2 and O2 gas.15,16 This approach not only provides optical breakdown and rapid process without desalination but also does not emit CO2 and Cl2 gases selectively. The demonstration of the developed MPI-WS system was conducted using artificial seawater as water sample. We analyzed the amount of H2 production by a gas chromatograph (GC) with a dielectric-barrier discharge ionization detector (BID). The analyses highlight that the femtosecond laser radiation produces more H2 gas than the ultrapure water case.16 The difference in the cell shape between a rectangular and cylindrical cell and curvature particularly affected gas production. Next, bubble generation from ultrapure water, seawater, and concentrated seawater were visualized by a high-speed camera to make comparison among the processes. Such results support the gas analysis results based on the sizes of the regions and bubble growth due to the nonlinear optical effect. Additionally, the differences in salinity are discussed with gas composition analysis and pressure measurement in gaseous products. The compact yet simple equipment configuration requiring only a water tank allows easy on-site installation that overcomes transportation difficulties.17,18
Fig. 2(a) shows the comparison of H2 production from ultrapure water between a rectangular and cylindrical cell at the radiation times of 5 minutes and Fig. 2(b) shows the linear dependence between the amount of hydrogen gas, and the time of femtosecond laser irradiation. First, the comparison of the experimental configurations between this study and the previous study is listed in Table S3.† Here there is a slight difference in the NA value of an objective lens, but H2 production used a rectangular cell is in good agreement with that in the previous work within the error bar, and the difference in the NA value does not affect H2 production (Fig. 2(a)).16 Then, the H2 productions from both ultrapure water and seawater linearly increase with the radiation time (Fig. 2(b)). The high significance of our work is demonstrated through two important findings: (i) H2 production using ultrapure water in this study was approximately 2.5 times higher than that in the previous work where a rectangular cell was used.16 The use of cylindrical cell caused the enhancement of the H2 production due to the effect of curvature;20 and (ii) laser irradiation to seawater produced approximately 1.3 times more H2 gas than ultrapure water, where the production rate in seawater was 70 μmol h−1. This finding indicates that a decrease in H2 production by the salt component did not occur in seawater.
Fig. 3 shows the salinity dependence on the amount of hydrogen gas at the radiation times of 5 minutes, and here in addition to ultrapure water and seawater, we prepared 1/10 and 1/5 diluted seawater, and 2.5 times concentrated seawater. While H2 production from seawater was more than those from diluted seawater samples, H2 production decreased considerably in the presence of excess salt. The findings prove that salinity has a positive effect on H2 production to some extent.
Fig. 3 Bar chart displaying the salinity dependence on the amount of hydrogen gas. Error bars represent three standard deviations. |
The effect of the salinity on bubble generation was then visualized through a high-speed camera. The typical digital images of generated bubbles in ultrapure water, 1/10 diluted seawater, 1/5 diluted seawater, seawater, 2.5 times concentrated seawater are shown in Fig. 4 (see videos for bubble generation in ESI†). The bubbles generated in ultrapure water dispersed. Conversely, the bubbles generated in the seawater were densely populated, indicating the enhanced bubble growth. The single bubble collapsed and dissolved into liquid in the sparse regime; however, when the bubbles were close to each other, they coalesced into a larger bubble. The bubble nuclei distribution at the foci of the femtosecond pulse is lengthened/shortened along its optic axis21 by the Kerr effect,22 which depends on the liquid's nonlinear refractive index (n2).23 Through observation, the salinity seems to have an advantage over the bubble growth.
The time evolutions of the inner pressure in cells, which filled with ultrapure water, seawater, 2.5 times concentrated seawater are shown in Fig. 5, in which Δp on the vertical axis presents the increase from the initial pressure of the atmospheric pressure. The details of the pressure measurements are described in ESI.† While the inner pressure for all samples increased almost linearly until 30 minutes, the absolute pressure values showed the exact magnitude correlation as H2 production shown in Fig. 3, not the growth of bubbles shown in Fig. 4. These results suggest plasma products in bubbles generated in 2.5 times concentrated seawater include chemical species that are not gaseous in a stable state and are re-dissolved in water within the lifetimes of microseconds to a few seconds. Indeed, bubble growth does not necessarily indicate an increase in gaseous products in a stable state. Therefore, although seawater has a positive effect on bubble growth, excessive salt (∼7%) does not necessarily enhance H2 production due to surface ion suppression, that is, the interference of Na, Mg, Ca, and other metals with low ionization potential.24
Fig. 5 Graph showing time evolutions of the inner pressure during femtosecond laser irradiation of ultrapure water, seawater, and 2.5 times concentrated seawater. |
Here we discuss hydrogen evolution reaction (HER) triggered by multiphoton absorption. The photolysis reactions by femtosecond laser pulses have been studied by Reuther et al.15 and Meader et al.,25 and include
H2O + nhν → H2O* → H* + OH* | (1) |
H2O + nhν → H+ + e− + OH | (2) |
e− → eaq− | (3) |
H* + OH* → H2O | (4) |
2H* → H2 | (5) |
2OH* → H2O2 | (6) |
Kierzkowska-Pawlak et al. revealed that the initial multiphoton absorption and sequent H2 production depend on the pulse energy, and the threshold pulse energy of hydrogen production was estimated to be approximately 0.0017–0.0028 mJ.16 Our experiments were performed with a moderate pulse energy of approximately 0.5 mJ to increase the overall H2 production while decreasing the H2 production per pulse. For high values of the pulse energy (>0.3 mJ), H2O2 decreases with the decomposition of H2O2, resulting in generating O2. This is due to H2O2 accumulations in the plasma volume generated by successive laser pulses. The overall reaction taking into account the decomposition of H2O2 has been proposed as:
(X + 1)H2O → XH2 + H2O2 + ((X − 1)/2)O2 | (7) |
The results of the chemical composition analysis using a mass spectrometer indicate the formation of O2, as shown in Table S2 and Fig. S2.† Furthermore, the partial pressure of O2 generated from seawater increased compared with that generated from ultrapure water, suggesting accelerated decomposition of H2O2. According to the reaction (7), as the pulse energy was the same value for both samples, H2O2 decomposition enhancement implies that the energy density in seawater is enhanced compared with that in ultrapure water. As shown in Fig. 2(a) and (b), the curvature of the cylindrical cell affects H2 production strongly, and a larger n2 of the aqueous solution also provides H2 enhancement. In the literature, the n2 values of ultrapure water and physiological saline (included 0.9% NaCl) have been reported to be (1.3 ± 0.6) × 10−13 and (1.8 ± 1.3) × 10−13 esu, respectively,26 and that of seawater would be greater. These understandings are consistent with the result of H2O2 decomposition enhancement.
The H2 production capability of the MPI-WS system using femtosecond laser pulses is estimated to be 0.3 g kW h−1, considering the experimental conditions of the pulse energy (0.5 mJ per pulse) and repetition of femtosecond laser pulses (1 kHz). Our preliminary results are even comparable with leading plasma methods, e.g., corona (2 g H2 kW h−1),27 cost reduction of ion exchange membranes, and catalysts owing to direct H2 production from seawater can have a critical advantage. Furthermore, the light efficiency was evaluated by measuring the transmittance of laser beams with a power meter. The experimental apparatus and light efficiency for 30 minutes are shown in Fig. S3 and Table S4,† respectively. The light efficiency in seawater was evaluated to be 49% from the transmittance of the incident laser beam, and this value was higher than that reported by Reuther et al.15 The efficiency decreases with an increase of pulse energy, as the probability of multiphoton absorption increases exponentially with an increase of pulse energy. Note that H2 production per pulse saturates and the total H2 production would not show a significant increase.
Footnotes |
† Electronic supplementary information (ESI) available. See DOI: 10.1039/d2ra01337a |
‡ These authors contributed equally. |
This journal is © The Royal Society of Chemistry 2022 |