Resolving Local Reaction Environment toward an Optimized CO2-to-CO Conversion Performance

Author(s):  
Ke Ye ◽  
Guiru Zhang ◽  
Xian-Yin Ma ◽  
Chengwei Deng ◽  
Xin Huang ◽  
...  

The local reaction environment, especially the electrode-electrolyte interface and the relevant hydrodynamic boundary layer in the vicinity of cathode, plays a vital role in defining the activity and selectivity of...

1984 ◽  
Vol 19 (3) ◽  
pp. 289-308 ◽  
Author(s):  
G.L. Flynn ◽  
A.B. French ◽  
N.F.H. Ho ◽  
W.I. Higuchi ◽  
E.A. Ostafin ◽  
...  

Author(s):  
Wekesa Waswa Simon ◽  
Winifred Nduku Mutuku

Heat transfer fluids play a vital role in many engineering and industrial sectors such as power generation, chemical production, air-conditioning, transportation and microelectronics. Aim: To numerically investigate the effect of double stratification on magneto-hydrodynamic boundary layer flow and heat transfer of an Eyring-Powell fluid. Study Design: Eyring-Powell fluid is one of the non-Newtonian fluid that possess different characteristics thus different mathematical models have been formulated to describe such fluids by appropriate substitution into Navier-Stoke’s equations. The challenging complexity and the nature of the resultant equations are of great interest hence attract many investigations. Place and Duration of Study: Department of Mathematics and Actuarial Science, Kenyatta University, Nairobi, Kenya between December 2019 and October 2020. Methodology: The resultant nonlinear equations are transformed to linear differential equations by introducing appropriate similarity transformations. The resulting equations are solved numerically by simulating the predictor-corrector (P-C) method in matlab ode113. The results are graphically depicted and analysed to illustrate the effects of magnetic field, thermophoresis, thermal stratification, solutal stratification, material fluid parameters and Grashoff number on the fluid velocity, temperature, concentration, local Sherwood number and local Nusselt number. Results: The results show that increasing the magnetic field strength, thermophoresis, thermal stratification and solutal stratification lead to a decrease in the fluid velocity, temperature, Sherwood number, Nusselt number and skin friction while an increase in the magnetic field strength, thermal stratification, solutal stratification, and thermophoresis increases the fluid concentration. Conclusion: The parameters in this study can be varied to enhance heat ejection of Eyring-Powell fluid and applied in industries as a coolant or heat transfer fluid.


2019 ◽  
Vol 22 (8) ◽  
pp. 1015-1025
Author(s):  
P. N. Vinay Kumar ◽  
U. S. Mahabaleshwar ◽  
K. R. Nagaraju ◽  
Mohaddeseh Mousavi Nezhad ◽  
A. Daneshkhah

1971 ◽  
Vol 3 (6) ◽  
pp. 649-652
Author(s):  
G. A. Danilin ◽  
A. V. Ryabushkin ◽  
A. T. Serkov

2021 ◽  
Vol 21 (15) ◽  
pp. 11829-11842
Author(s):  
Anoop S. Mahajan ◽  
Mriganka S. Biswas ◽  
Steffen Beirle ◽  
Thomas Wagner ◽  
Anja Schönhardt ◽  
...  

Abstract. Iodine plays a vital role in oxidation chemistry over Antarctica, with past observations showing highly elevated levels of iodine oxide (IO) leading to severe depletion of boundary layer ozone in West Antarctica. Here, we present MAX-DOAS-based (multi-axis differential absorption spectroscopy) observations of IO over three summers (2015–2017) at the Indian Antarctic bases of Bharati and Maitri. IO was observed during all the campaigns with mixing ratios below 2 pptv (parts per trillion by volume) for the three summers, which are lower than the peak levels observed in West Antarctica. This suggests that sources in West Antarctica are different or stronger than sources of iodine compounds in East Antarctica, the nature of which is still uncertain. Vertical profiles estimated using a profile retrieval algorithm showed decreasing gradients with a peak in the lower boundary layer. The ground-based instrument retrieved vertical column densities (VCDs) were approximately a factor of 3 to 5 higher than the VCDs reported using satellite-based instruments, which is most likely related to the sensitivities of the measurement techniques. Air mass back-trajectory analysis failed to highlight a source region, with most of the air masses coming from coastal or continental regions. This study highlights the variation in iodine chemistry in different regions in Antarctica and the importance of a long-term dataset to validate models estimating the impacts of iodine chemistry.


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