| Literature DB >> 35560974 |
Daehyeon An1, Shunta Nishioka1, Shuhei Yasuda2, Tomoki Kanazawa3, Yoshinobu Kamakura1,4, Toshiyuki Yokoi2, Shunsuke Nozawa3, Kazuhiko Maeda1.
Abstract
Photocatalytic conversion of CO2 into transportable fuels such as formic acid (HCOOH) under sunlight is an attractive solution to the shortage of energy and carbon resources as well as to the increase in Earth's atmospheric CO2 concentration. The use of abundant elements as the components of a photocatalytic CO2 reduction system is important, and a solid catalyst that is active, recyclable, nontoxic, and inexpensive is strongly demanded. Here, we show that a widespread soil mineral, alpha-iron(III) oxyhydroxide (α-FeOOH; goethite), loaded onto an Al2 O3 support, functions as a recyclable catalyst for a photocatalytic CO2 reduction system under visible light (λ>400 nm) in the presence of a RuII photosensitizer and an electron donor. This system gave HCOOH as the main product with 80-90 % selectivity and an apparent quantum yield of 4.3 % at 460 nm, as confirmed by isotope tracer experiments with 13 CO2 . The present work shows that the use of a proper support material is another method of catalyst activation toward the selective reduction of CO2 .Entities:
Keywords: Artificial Photosynthesis; Earth-Abundant Metals; Iron; Photocatalysis; Solar Fuels
Year: 2022 PMID: 35560974 PMCID: PMC9325401 DOI: 10.1002/anie.202204948
Source DB: PubMed Journal: Angew Chem Int Ed Engl ISSN: 1433-7851 Impact factor: 16.823
Scheme 1A photochemical CO2 reduction system consisting of a catalyst and a photosensitizer. D indicates an electron donor. The catalyst may be in the form of a molecule or nanoparticle.
Figure 1Characterization of Fe‐loaded Al2O3: a) SEM images and b) EDS mapping images. Fe K‐edge c) XANES spectra and d) EXAFS oscillation.
Results of visible‐light CO2 reduction experiments (λ>400 nm).[a]
[a] Reaction conditions: catalyst, 4 mg (Fe loaded 10.0 wt % to catalyst); solution, 4 mL DMA containing 1.0 mM Ru and 0.1 M BNAH; reaction time, 3 h. [b] In the dark. [c] Under an Ar atmosphere. n.d.=Not detected.
Figure 2a) A typical time course of CO2 reduction using α‐FeOOH/Al2O3 under visible light (λ>400 nm). Reaction conditions: catalyst, 4 mg (Fe loaded 10.0 wt % to catalyst); solution, 4 mL DMA containing 1.0 mM Ru and 0.1 M BNAH. b) Amounts of reaction products and the HCOOH selectivity in photocatalytic CO2 reduction using α‐FeOOH/Al2O3 under visible light (λ>400 nm). Each run was conducted for 3 h, and the α‐FeOOH/Al2O3 catalyst was subsequently recovered by centrifugation. The next reaction was then started using a new reaction solution and the recovered catalyst.
Figure 3CO2 sorption isotherms of catalyst samples at 298 K.