4.8 Article

CO2, water, and sunlight to hydrocarbon fuels: a sustained sunlight to fuel (Joule-to-Joule) photoconversion efficiency of 1%

Journal

ENERGY & ENVIRONMENTAL SCIENCE
Volume 12, Issue 9, Pages 2685-2696

Publisher

ROYAL SOC CHEMISTRY
DOI: 10.1039/c9ee00734b

Keywords

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Funding

  1. Ministry of Science and ICT [2017R1E1A1A01074890, 2017M2A2A6A01070912]
  2. Technology Development Program to Solve Climate Changes of the National Research Foundation (NRF) - Ministry of Science and ICT [2015M1A2A2074670]
  3. Basic Science Research Program through the National Research Foundation of Korea - Ministry of Science and ICT of the Korean Government [2016R1A2B4014448]
  4. National Research Foundation of Korea [2016R1A2B4014448, 2017M2A2A6A01070912] Funding Source: Korea Institute of Science & Technology Information (KISTI), National Science & Technology Information Service (NTIS)

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If we wish to sustain our terrestrial ecosphere as we know it, then reducing the concentration of atmospheric CO2 is of critical importance. An ideal pathway for achieving this would be the use of sunlight to recycle CO2, in combination with water, into hydrocarbon fuels compatible with our current energy infrastructure. However, while the concept is intriguing such a technology has not been viable due to the vanishingly small CO2-to-fuel photoconversion efficiencies achieved. Herein we report a photocatalyst, reduced blue-titania sensitized with bimetallic Cu-Pt nanoparticles that generates a substantial amount of both methane and ethane by CO2 photoreduction under artificial sunlight (AM1.5): over a 6 h period 3.0 mmol g(-1) methane and 0.15 mmol g(-1) ethane are obtained (on an area normalized basis 0.244 mol m(-2) methane and 0.012 mol m(-2) ethane), while no H2 nor CO is detected. This activity (6 h) translates into a sustained Joule (sunlight) to Joule (fuel) photoconversion efficiency of 1%, with an apparent quantum efficiency of j = 86%. The timedependent photoconversion efficiency over 0.5 h intervals yields a maximum value of 3.3% (j = 92%). Isotopic tracer experiments confirm the hydrocarbon products originate from CO2 and water.

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