First-principles study on the mechanism of water-gas shift reaction on the Fe3O4 (111)-Fetet1

2021 ◽  
Vol 516 ◽  
pp. 111998
Author(s):  
Xiaoyan Liu ◽  
Zeyu Ma ◽  
Yu Meng ◽  
Ya-jun Ma ◽  
Xiao-dong Wen
2017 ◽  
Vol 7 (19) ◽  
pp. 4294-4301 ◽  
Author(s):  
Xiang-Kui Gu ◽  
Chuan-Qi Huang ◽  
Wei-Xue Li

A single Ni atom substituted on a ZnO surface is a promising catalyst for the water gas shift reaction.


2017 ◽  
Vol 7 (19) ◽  
pp. 4534-4534
Author(s):  
Xiang-Kui Gu ◽  
Chuan-Qi Huang ◽  
Wei-Xue Li

Correction for ‘First-principles study of single transition metal atoms on ZnO for the water gas shift reaction’ by Xiang-Kui Gu et al., Catal. Sci. Technol., 2017, DOI: 10.1039/c7cy00704c.


ACS Catalysis ◽  
2018 ◽  
Vol 8 (12) ◽  
pp. 11633-11647 ◽  
Author(s):  
Minttu M. Kauppinen ◽  
Marko M. Melander ◽  
Andrey S. Bazhenov ◽  
Karoliina Honkala

2008 ◽  
Vol 112 (12) ◽  
pp. 4608-4617 ◽  
Author(s):  
Lars C. Grabow ◽  
Amit A. Gokhale ◽  
Steven T. Evans ◽  
James A. Dumesic ◽  
Manos Mavrikakis

2020 ◽  
Author(s):  
Nore Stolte ◽  
Junting Yu ◽  
Zixin Chen ◽  
Dimitri A. Sverjensky ◽  
Ding Pan

The water-gas shift reaction is a key reaction in Fischer-Tropsch-type synthesis, which is widely believed to generate hydrocarbons in the deep carbon cycle, but is little known at extreme pressure-temperature conditions found in Earth’s upper mantle. Here, we performed extensive ab initio molecular dynamics simulations and free energy calculations to study the water-gas shift reaction. We found the direct formation of formic acid out of CO and supercritical water at 10∼13 GPa and 1400 K without any catalyst. Contrary to the common assumption that formic acid or formate is an intermediate product, we found that HCOOH is thermodynamically more stable than the products of the water-gas shift reaction above 3 GPa and at 1000∼1400 K. Our study suggests that the water-gas shift reaction may not happen in Earth’s upper mantle, and formic acid or formate may be an important carbon carrier, participating in many geochemical processes in deep Earth.<br>


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