Role of Bicarbonate Ions in Aqueous Solution as a Carbon Source for Photocatalytic Conversion of CO2 into CO
Source abstract
Abstract
Ag/SrNb2O6 nanorods exhibited a high CO formation rate and high selectivity toward CO evolution in aqueous solutions containing bicarbonate ions even without CO2 bubbling. Notably, the formation rate of CO reached as high as 287 μmol h–1 with selectivity toward CO evolution of higher than 94.1% when NH4HCO3 was used as an additive. Both the formation rate of CO and selectivity toward CO evolution increased with the concentration of HCO3–. According to the experimental results and analytical chemistry calculations, it was concluded that CO2(aq) obtained by the dissociation of HCO3– is the actual reactant in the photocatalytic conversion of CO2. In contrast, the HCO3– species in the aqueous solution is beneficial for improving the photocatalytic activity and selectivity toward CO evolution by increasing the adsorption of carbon-related species on the photocatalyst surface and/or suppressing the backward reaction for the photocatalytic conversion of CO2.
Source: openalex_inverted_index · Quality: baseline
Research context
OpenAlex topics: Advanced Photocatalysis Techniques · CO2 Reduction Techniques and Catalysts · Carbon dioxide utilization in catalysis
SciVX discovery tags are terminology-based. OpenAlex topics are source-provided classifications.
Affiliations
Department of Molecular Engineering, Graduate School of Engineering, Kyoto University, Kyotodaigaku Katsura, Nishikyo-ku, Kyoto 615-8510, Japan
Elements Strategy Initiative for Catalysts and Batteries, Kyoto University, 1-30 Goryo-Ohara, Nishikyo-ku, Kyoto 615-8245, Japan
Funding
Ministry of Education, Culture, Sports, Science and Technology · China Scholarship Council
References (40)
Show source-provided references
1. Pachauri, R. K.; Allen, M. R.; Barros, V. R.; Broome, J.; Cramer, W.; Christ, R.; Church, J. A.; Clarke, L.; Dahe, Q.; Dasgupta, P. Climate Change 2014: Synthesis Report. Contribution of Working Groups I, II and III to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change; IPCC: 2014.
2. 10.1039/C7CP07783A10.1039/C7CP07783A ↗
3. 10.1002/anie.20110201010.1002/anie.201102010 ↗
4. 10.1038/275115a010.1038/275115a0 ↗
5. 10.1038/277637a010.1038/277637a0 ↗
6. 10.1021/acs.chemrev.8b0040010.1021/acs.chemrev.8b00400 ↗
7. Anderson R. B. · 1984 · 16
8. 10.1002/anie.19760136110.1002/anie.197601361 ↗
9. 10.1039/c3ee00056g10.1039/c3ee00056g ↗
10. 10.1021/acs.chemrev.5b0037010.1021/acs.chemrev.5b00370 ↗
11. 10.1021/ja207586e10.1021/ja207586e ↗
12. 10.1246/bcsj.2014035010.1246/bcsj.20140350 ↗
13. 10.1002/cssc.20160136010.1002/cssc.201601360 ↗
14. 10.1016/j.catcom.2017.06.04610.1016/j.catcom.2017.06.046 ↗
15. 10.1016/j.apsusc.2016.06.14810.1016/j.apsusc.2016.06.148 ↗
16. 10.1039/C5CY01280E10.1039/C5CY01280E ↗
17. 10.1002/chem.20140224210.1002/chem.201402242 ↗
18. 10.1039/C5TA01697E10.1039/C5TA01697E ↗
19. 10.1016/j.apcatb.2016.06.03910.1016/j.apcatb.2016.06.039 ↗
20. 10.1021/acs.langmuir.7b0319110.1021/acs.langmuir.7b03191 ↗
21. 10.1016/j.cattod.2017.03.04310.1016/j.cattod.2017.03.043 ↗
22. 10.1039/C7CC07800E10.1039/C7CC07800E ↗
23. 10.1021/acs.jpcc.6b1280910.1021/acs.jpcc.6b12809 ↗
24. 10.1246/bcsj.2014038510.1246/bcsj.20140385 ↗
25. 10.1016/j.apcatb.2014.07.05210.1016/j.apcatb.2014.07.052 ↗
26. 10.1021/cr00058a00410.1021/cr00058a004 ↗
27. 10.1149/1.204418210.1149/1.2044182 ↗
28. 10.1016/j.apcatb.2017.06.05210.1016/j.apcatb.2017.06.052 ↗
29. 10.1021/cm803471410.1021/cm8034714 ↗
30. 10.1016/j.apcatb.2011.10.01110.1016/j.apcatb.2011.10.011 ↗
31. 10.1039/C7SC01851G10.1039/C7SC01851G ↗
32. 10.1021/jp509043h10.1021/jp509043h ↗
33. 10.1016/0016-7037(82)90056-410.1016/0016-7037(82)90056-4 ↗
34. 10.1016/0009-2614(87)80070-210.1016/0009-2614(87)80070-2 ↗
35. 10.1007/s11244-005-3837-x10.1007/s11244-005-3837-x ↗
36. 10.1246/cl.1992.25310.1246/cl.1992.253 ↗
37. 10.1016/j.catcom.2005.09.00810.1016/j.catcom.2005.09.008 ↗
38. 10.1039/a607662i10.1039/a607662i ↗
39. 10.1016/1010-6030(95)04204-010.1016/1010-6030(95)04204-0 ↗
40. 10.1023/A:101909632369410.1023/A:1019096323694 ↗