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The electrochemical reduction of carbon dioxide, also known as CO2RR, is the conversion of carbon dioxide (CO 2) to more reduced chemical species using electrical energy. It represents one potential step in the broad scheme of carbon capture and utilization. [1]
Thermodynamic potentials for the reduction of CO 2 to various products is given in the following table versus NHE at pH = 7. Single electron reduction of CO 2 to CO 2 − radical occurs at E° = −1.90 V versus NHE at pH = 7 in an aqueous solution at 25 °C under 1 atm gas pressure.
It is the disproportionation of carbon monoxide into carbon dioxide and graphite or its reverse: [1] 2CO ⇌ CO 2 + C Boudouard-Equilibrium at 1 bar calculated with 2 different methods Standard enthalpy of the Boudouard reaction at various temperatures. The Boudouard reaction to form carbon dioxide and carbon is exothermic at all
Photochemical reduction of carbon dioxide harnesses solar energy to convert CO 2 into higher-energy products. Environmental interest in producing artificial systems is motivated by recognition that CO 2 is a greenhouse gas. The process has not been commercialized.
Where is the standard reduction potential of the half-reaction expressed versus the standard reduction potential of hydrogen. For standard conditions in electrochemistry (T = 25 °C, P = 1 atm and all concentrations being fixed at 1 mol/L, or 1 M) the standard reduction potential of hydrogen E red H+ ⊖ {\displaystyle E_{\text{red H+ ...
The Bosch reaction is a catalytic chemical reaction between carbon dioxide (CO 2) and hydrogen (H 2) that produces elemental carbon (C,graphite), water, and a 10% return of invested heat. CO 2 is usually reduced by H 2 to carbon in presence of a catalyst (e.g. iron (Fe)) and requires a temperature level of 530–730 °C (986–1,346 °F). [1] [2]
And also, after the gasification process, CO 2 takes up to 13% - 15.3% by mass in the syngas stream for biomass sources, while it is only 1.7% - 4.4% for coal. [29] This limit the conversion of CO to CO 2 in the water gas shift, and the production rate for H 2 will decrease accordingly.
The reducing atmosphere, rich in CO and H 2, can be created from the high-temperature cracking of natural gas at around 1100-1150 °C, in the presence of oxidized gases (H 2 O and CO 2) from ore reduction reactors. CH 4 + CO 2 → 2 CO + H 2 CH 4 + H 2 O → CO + 3 H 2. The system that generates the reducing gases is called a "reformer".