Supplementary Information Leaf-architectured 3D Hierarchical Artificial Photosynthetic System of Perovskite Titanates Towards CO2 Photoreduction Into Hydrocarbon Fuels Han Zhou 1, 5, Jianjun Guo1, 3, Peng Li 1, 3, Tongxiang Fan 5, Di Zhang 5, and Jinhua Ye *1, 2 ,3, 4 1 International Center for Materials Nanoarchitectonics (WPI-MANA), National Institute for Materials Science (NIMS), 1-1, Namiki, Tsukuba, Ibaraki 305-0044, Japan *Email: [email protected] 2 Environmental Remediation Materials Unit, Catalytic Materials Group, National Institute for Materials Science (NIMS), 1-2-1 Sengen, Tsukuba, Ibaraki, 305-0047, Japan 3 Department of Chemistry, Graduate School of Science, Hokkaido University, Sapporo, Japan 4 TU−NIMS Joint Research Center, School of Materials Science and Engineering, Tianjin University, 92 Weijin Road, Nankai District, Tianjin 300072, P. R. China 5 State Key lab of Composites, Shanghai Jiaotong University, Shanghai, 200240, China 1 Figure S1. FESEM images of (a) the upper epidermis of Cherry Blossom Leaf, with the inset of the illustration of epidermal focusing by a lens mechanism and light distribution within the leaf (b) the cross-section of the vein architecture, indicating the highly porous feature. (c) the cross-section of Cherry Blossom leaf, indicating the differentiation of leaf mesophyll into palisade and spongy layers. Right part: Possible pathway of light through the leaf. The whole architecture of natural leaves strongly favors light harvesting: For example, many kinds of leaves are evolved lens-like epidermal cells, which act as lenses that focus the incident light via refraction 1 (Fig. S1a). As a result, refraction of light through the epidermis of leaves can create significantly higher local irradiances within the leaf than that present in the ambient light environment. Theoretically maximal focal intensification can approach 20 times the irradiance of incident light 2 when that light is collimated. Furthermore, internal light-scattering can trap light so that internal fluence rates can exceed that of incident light. Furthermore, the FESEM image (Fig. S1b) of the cross-section of the veins reveal the hierarchical porous network. Light that enters leaf venation architectures becomes highly 2 scattered and increases light absorption. Another important factor is the differentiation of leaf mesophyll into palisade and spongy layers (Fig. S1c). The columnar cells in palisade layer are elongated and parallel to the direction of light, facilitating light channeling into the deeper layers. 3 These cells act as light guides, propagating light through vacuoles and intercellular air spaces. 3 The spongy mesophyll cells are less regularly arranged, leading to greater effective light path length and light scattering 4. Such complex architectures bring about multiple scattering and enhance light absorption within the leaves. Figure S2 TGA curves of (a) pretreated original leaves Cherry Blossom (b) Sr(CH3COO)2 (c) as– synthesized precursor for SrTiO3. For the as-synthesized precursor for SrTiO3, below 120 °C, the weight loss is owing to volatile species (including water, CH3COOH, and EtOH). Between 120 °C and 280 °C, a mass loss arised from the oxidation of P123 template. At the temperatures between 280 to 550 °C, the Sr(CH3COO)2 decomposed, some residual organic matter, such as amorphous carbon or carboxylate species and possibly hydroxyl groups, was removed. Between 550 to 610 °C, a rapid weight loss appeared. It may be explained by that the SrCO3, a decomposition product of 3 Sr(CH3COO)2, reacted with TiO2 for formation of crystalline SrTiO3, which is an exothermic reaction. 5 Figure S3 TEM images of leaf-architectured (a) SrTiO3 (b) CaTiO3 (c) PbTiO3, indicating the mesoporous features. Table S1 Characterization of the Porosity of the synthesized samples Sample name SBET [m2 g-1] Mesopore size [nm] Vmeso [cm3 g-1] APS STO 72.6 7.2 0.13 Referenced STO 26.4 7.6 0.05 APS CTO 45.9 7.4 0.09 Referenced CTO 27.9 7.1 0.05 APS PTO 11.8 7.7 0.023 Referenced PTO 1.7 7.9 0.003 4 Figure S4 Comparative hierarchical pore size distributions of CaTiO3 series derived from the N2 (BJH model, red triangles) adsorption (the inset of (1), and mercury intrusion porosimetry, respectively. The plots are offset for clarity. (1)leaf-architectured APSCTO, with the inset of sample’s optical image. (2) the corresponding powder constituents of APSCTO, with the inset of sample’s optical image. (3) referenced CTO synthesized without templates. 5 Figure S5 CO and CH4 evolution activities on bare CTO series. Table S2 One-, two-, six-, and eight-electron reduction potentials (vs NHE) of some reactions involved in CO2 photoreduction at pH 7 and unit activity. Adapted from 6 6 Figure S6 UV-vis absorption spectra of the as-synthesized APSATO series. Figure S7 (a) SEM image of leaf-framed STO after grounding and sonication (b, c) TEM images of leaf-framed STO after grounding and sonication, indicating the existence of a part of macropores after a series of treatment. 7 Detailed calculations and explanations of gas diffusion in the samples Mean free path of a molecule is the average distance that the molecule travels between collisions. L= Where K equals to 1.38 ×10 -23 KT 2 2D0 P (1) , T is assumed to be 323K in our experiment, D0 refers to the diameters of gas molecules (nm). Table S3 listed the values of D0 and L of six gas molecules. Table S3 Values of D0 and mean free path (L) of six typical gas molecules. Gases CO2 CH4 CO O2 H2 H2O D0 (nm) 0.39 0.38 0.38 0.35 0.29 0.27 L (nm) 73.7 70.2 71.7 63.7 121.4 139.0 K d L (2) d is mean diameters of pores, L is the mean free path of a molecule. There are three main gas diffusion types (Knudsen diffusion, molecular diffusion and surface diffusion) according to different values of K as shown in Figure S8. Figure S8. Schematic illustration of three main gas diffusion types according to different sizes of pores. 8 (1) K<0.1, Knudsen Diffusion In many applications involving gases in mesoporous materials, which are materials with most pore sizes between 2 and 50 nm, Knudsen diffusion is the predominant transport mechanism. Knudsen diffusion is a result of collisions of gas molecules with the pore walls, rather than intramolecular collisions (Brownian motion). According to gas diffusion theories, diffusion of gas molecules in mesopores smaller than a mean free path is described with Knudsen equation7 D 2 8RT 1 / 2 rp ( ) 3 M (3) Where D, rp, R, T, and M are diffusion coefficient in pores, pore radius, gas constant, temperature, and molecular weight of gas molecules, respectively. The smaller the mesopore size is, the smaller the diffusion coefficient becomes. A time, t, necessary to diffuse particular length, l, is roughly estimated by the relation t l 2 / 2D (4) Therefore, long time is required for reactants (CO2 and H2O vapor) to move into the deeper layer of photocatalysts with small mesopores in which diffusion coefficient is also small. Then, the deeper layer of photocatalysts does not effectively work in reaction. Similarly, long time is also needed for products (e.g. CO, CH4, etc) to move from the deeper layer into the atmosphere. An excellent catalyst is expected to suffer a minimum effect of diffusion. (2) K>10, Molecular (Fick) diffusion The transport diffusivity relates the macroscopic flux of molecules in a system to a driving force in the concentration. This diffusion mode is applicable to Brownian motion, where the movement of each particle is random and not dependent on its previous motion. It is clear that 9 the size of macropores in is much larger than average free path of gas molecules, typically in the order of μm. Therefore, the diffusion coefficient is evaluated assuming the molecular diffusion. For the estimation of diffusion coefficient in macroporous samples, we used the following equation for molecular diffusion. The binary diffusion coefficient is calculated using the Chapman-Enskog equation 7: Dm 0.0018583 T 3 / 2 (1 / M A 1 / M B )1 / 2 P 2 AB AB (5) Where P, σ, Ω are respectively total pressure, lennard-Jones potential parameter, and collision integral. AB ( A B ) / 2 (6) AB is the collision diameter, M is the molecular weight of species. D pore = D ideal (7) ε is the porosity, ζ is the tortuosity which is 3-6 for usual porous materials 7. For this example, the following temperature and pressure conditions have been chosen: T=323K, P=0.85 atm. For ease of representation, the components are numbered as 1:CO2, 2:H2O, 3: CH4, 4: CO. The molecular weights are: M1=44 g/mol M2=18 g/mol M3=16 g/mol M4=28 g/mol. The values of σ of the components are 8: σ1=3.941, σ2=2.641, σ3=3.758, σ4=3.69. So according to equation 2, σ12=3.291, σ13=3.849, σ14=3.816, σ23=3.199, σ24=3.166, σ34=3.724. According to the porosity values of these samples measured by N2 adsorption and mercury intrusion porosimetry, we calculated the Dk (diffusion coefficient in mesopores) and Dm (diffusion coefficient in macropores) of some typical samples. The diffusion coefficients of the four typical gases calculated for mesopores in leaf-architectured STO are as follows: 10 D1k =0.0189 cm2/s, D2k =0.0296 cm2/s D3k =0.0314 cm2/s D4k =0.0237 cm2/s Table S4 summarizes diffusion coefficients calculated for macropores. Ideally, coefficient of molecular diffusion is about 20 times larger than that of Knudsen diffusion. In addition, we have to take into account the contribution of structural factors such as porosity, ε, and tortuosity, ζ, to diffusion in a real porous materials 7. The real diffusion coefficients in macropores are at least 5 times larger than that of Knudsen diffusion in mesopores. Table S4 Diffusion coefficients in macropores (Dm) Dpore (cm2/s) Dm values Dideal (cm2/s) Leaf-architectured STO Powdered form D12 0.33 0.097 0.077 D13 0.25 0.074 0.058 D14 0.21 0.062 0.049 D23 0.42 0.124 0.098 D24 0.38 0.112 0.089 D34 0.29 0.085 0.067 11 Figure S9 Schematic illustration of the comparison between (a) 3D APS and (b) corresponding powder constituents and referenced ATO. Figure S10 UV-vis absorption spectra of the as-synthesized noble metal loaded SrTiO3. 12 Figure S11. TEM images of 1 wt % noble metal loaded leaf-framed STO (a) Pt (b) Au, (c) Ag, (d) Cu. The loading method is photodeposition method. Table S5 CO2 photoreduction over APS STO photocatalyst with various cocatalysts Activity /nmol h-1g-1 Cocatalyst (1wt %) Loading method None CO CH4 84.8 9.5 Pt Photodeposition 0 7.7 Au Precipitation 349 231 Au Photodeposition 154.1 82.2 Ag Photodeposition 131.8 44.7 Cu Photodeposition 56.1 36.1 RuO2 Impregnation 18.2 9.6 NiOx Impregnation+H2 reduction+O2 oxidation 87.1 12.4 13 Figure S12. CO2 photoreduction activities on (a) APSCTO with and without Au cocatalyst under full arc Xe lamp. (b) Au (1wt%)-APSPTO under full arc Xe lamp and under λ>420nm, respectively. The edge of the valence band (EVB) of PTO was determined to be 2.6 V (vs normal hydrogen electrode, NHE), more positive than that of E°(H2O/H+) (H2O→1/2O2 + 2H+ + 2e-, E° redox = 0.82 V vs NHE), and the edge of the conduction band was estimated to be -0.3 V, more negative than that of E° (CO2/CH4) (CO2 + 8e- + 8H+ → CH4 + 2H2O, E° redox = -0.24 V vs NHE), but positive than that of E° (CO2/CO) (CO2 + 2e- + 2H+ → CO+H2O, E° redox = 0.53 V vs NHE). This indicates that the photogenerated electrons and holes on the irradiated PTO can react with adsorbed CO2 and H2O to produce CH4, but no CO. 14 Figure S13 Reaction setup for evaluation of conversion rate of CO 2. References 1. M. E. Poulson, T. C. Vogelmann, Epidermal focusing and effects upon photosynthetic lightharvesting in leaves of Oxalis, Plant Cell Environ. 1990, 13, 803-811. 2. R. A. Bone, D. W. Lee, J. M. Norman, Epidermal cells functioning as lenses in leaves of tropical rain-forest shade plants, Appl. Opt. 1985, 24, 1408-1412. 3. T. C. Vogelmann, G. Martin, The functional significance of palisade tissue: penetration of directional versus diffuse light, Plant Cell Environ. 1993, 16, 65-72. 4. E. H. Delucia, K. Nelson, T. C. Vogelmann, W. K. Smith, Contribution of intercellular reflectance to photosynthesis in shade leaves, Plant Cell Environ. 1996, 19, 159-170. 15 5. X. Fan, Y. Wang, X. Chen, L. Gao, W. Luo, Y. Yuan, Z. Li, T. Yu, J. Zhu, Z. Zou, Facile method to synthesize mesoporous multimetal oxides (ATiO3, A=Sr, Ba) with large specific surface areas and crystalline pore walls, Chem. Mater. 2010, 22, 1276-1278. 6. V. P. Indrakanti, J. D. Kubicki, H. H. Schobert, Photoinduced activation of CO2 on Ti-based heterogeneous catalysts: current state, chemical physics-based insights and outlook, Energy Environ. Sci. 2009, 2, 745-758. 7. J. M Smith, in Chemical Engineering kinetics, third ed., McGraw-Hill Book Co, New York, 1981, Ch. 11. 8. P. Chinda, S. Chanchaona, P. Brault, W. Wechsatol, Mathematical modeling of a solid oxide fuel cell with nearly spherical-shaped electrode particles, Journal of sustainable energy and environment, 2010, 1, 185-196. 16
© Copyright 2026 Paperzz