scholarly journals The rate constant of the reaction NCN + H2 and its role in NCN and NO modeling in low pressure CH4/O2/N2-flames

2015 ◽  
Vol 17 (24) ◽  
pp. 15876-15886 ◽  
Author(s):  
Nancy Faßheber ◽  
Nathalie Lamoureux ◽  
Gernot Friedrichs

The high temperature rate constant of the so-far neglected reaction NCN + H2 has been measured for the first time and its influence on NOx flame modeling has been evaluated by implementation into the GDFkin3.0_NCN mechanism.

2014 ◽  
Vol 16 (23) ◽  
pp. 11647-11657 ◽  
Author(s):  
Nancy Faßheber ◽  
Johannes Dammeier ◽  
Gernot Friedrichs

The high-temperature rate constant of the reaction NCN + H, a key reaction for modelling NOx formation in flames, has been directly measured for the first time.


2012 ◽  
Vol 116 (39) ◽  
pp. 9607-9613 ◽  
Author(s):  
Genny A. Pang ◽  
Ronald K. Hanson ◽  
David M. Golden ◽  
Craig T. Bowman

Temperatures and concentrations of OH(X 2 II and A 2 ∑+), CH(X 2 II and A 2 ∆) and C 2 (X 3 II u and A 3 II g ) have been further studied in low-pressure C 2 H 2 + O 2 flames. For any given state (with the possible but unlikely exception of upper state OH), vibrational and rotational temperatures are in close agreement. The upper state temperature of a given species always exceeds the corresponding lower state temperature. The highest upper state temperatures normally recorded are 7000 K, for C 2 (A 3 II g ) and OH(A 2 ∑+), but, quite exceptionally, values up to 9000 K are found for OH(A 2 ∑+) at the very earliest stages of combustion. No lower state temperature exceeds 3000 K. The temperature of CH( 2 II) is quite normal, equalling within 100 K the measured translational flame temperatures. The temperatures of CH( 2 ∆), OH(X 2 II) and C 2 (X 3 II u ) are all similar, lying in the range 2500 to 3000 K. C 2 (A 3 II g ) and OH(A 2 ∑+) temperatures are broadly similar too, falling between 5000 and 7000 K. Firm experimental evidence in support of Gaydon’s reaction C 2 (X 2 II 0 ) + OH(X 2 II) → CH(A 2 ∆) + CO(X 1 ∑+) Is provided for the first time; its rate constant at 2200 K is estimated to be 8 ± 4 x 10 -12 ml molecules -1 s -1 . This reaction is not, however, responsible for formation of CH(X 2 H). Neither C 2 (X 3 II u ) nor C 2 (A 3 II g ) are formed in the reaction CH + CH → C 2 + H 2. At the pressures of these experiments, OH(A 2 Ʃ -) is strongly quenehed, but both CH(A 2 ∆) and C 2 (A 3 II z ) decay predominantly through radiative emission.


2012 ◽  
Vol 116 (19) ◽  
pp. 4720-4725 ◽  
Author(s):  
Genny A. Pang ◽  
Ronald K. Hanson ◽  
David M. Golden ◽  
Craig T. Bowman

2005 ◽  
Vol 30 (1) ◽  
pp. 1023-1031 ◽  
Author(s):  
Christian L. Rasmussen ◽  
Martin S. Skjøth-Rasmussen ◽  
Anker D. Jensen ◽  
Peter Glarborg

2015 ◽  
Vol 162 (6) ◽  
pp. 2348-2353 ◽  
Author(s):  
Ahmed Elwardany ◽  
Jihad Badra ◽  
Aamir Farooq

2015 ◽  
Vol 119 (33) ◽  
pp. 8799-8805 ◽  
Author(s):  
Shengkai Wang ◽  
Sijie Li ◽  
David F. Davidson ◽  
Ronald K. Hanson

2020 ◽  
Author(s):  
Ruobin Dai ◽  
Hongyi Han ◽  
Tianlin Wang ◽  
Jiayi Li ◽  
Chuyang Y. Tang ◽  
...  

Commercial polymeric membranes are generally recognized to have low sustainability as membranes need to be replaced and abandoned after reaching the end of their life. At present, only techniques for downcycling end-of-life high-pressure membranes are available. For the first time, this study paves the way for upcycling fouled/end-of-life low-pressure membranes to fabricate new high-pressure membranes for water purification, forming a closed eco-loop of membrane recycling with significantly improved sustainability.


JOM ◽  
1961 ◽  
Vol 13 (7) ◽  
pp. 490-493 ◽  
Author(s):  
R. A. Perkins ◽  
D. D. Crooks

1969 ◽  
Vol 11 (2) ◽  
pp. 189-205 ◽  
Author(s):  
E. A. Bruges ◽  
M. R. Gibson

Equations specifying the dynamic viscosity of compressed water and steam are presented. In the temperature range 0-100cC the location of the inversion locus (mu) is defined for the first time with some precision. The low pressure steam results are re-correlated and a higher inversion temperature is indicated than that previously accepted. From 100 to 600°C values of viscosity are derived up to 3·5 kilobar and between 600 and 1500°C up to 1 kilobar. All the original observations in the gaseous phase have been corrected to a consistent set of densities and deviation plots for all the new correlations are given. Although the equations give values within the tolerances of the International Skeleton Table it is clear that the range and tolerances of the latter could with some advantage be revised to give twice the existing temperature range and over 10 times the existing pressure range at low temperatures. A list of the observations used and their deviations from the correlating equations is available as a separate publication.


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