Water vapor effect on photochemical ozone formation in a propylene-NOx-air system

1980 ◽  
Vol 14 (8) ◽  
pp. 985-989 ◽  
Author(s):  
F. Sakamaki ◽  
H. Akimoto ◽  
M. Okuda



1979 ◽  
Vol 13 (1) ◽  
pp. 53-58 ◽  
Author(s):  
Hajime Akimoto ◽  
Fumio Sakamaki ◽  
Mikio Hoshino ◽  
Gen Inoue ◽  
Michio Okuda


2013 ◽  
Vol 108 ◽  
pp. 121-127 ◽  
Author(s):  
Lunbo Duan ◽  
Zhongxiao Jiang ◽  
Xiaoping Chen ◽  
Changsui Zhao


2009 ◽  
Vol 10 (4) ◽  
pp. 045006 ◽  
Author(s):  
Sebastian Chevalier ◽  
Pitor Juzon ◽  
Kazimierz Przybylski ◽  
Jean-Pierre Larpin


1996 ◽  
pp. 57-67
Author(s):  
Montserrat Martín-Reviejo ◽  
Klaus Wirtz ◽  
Karl H. Becker


2004 ◽  
Vol 15 (5) ◽  
pp. 646-651 ◽  
Author(s):  
Pedro Afonso de P. Pereira ◽  
Leilane Maria B. Santos ◽  
Eliane Teixeira Sousa ◽  
Jailson B. de Andrade


2010 ◽  
Vol 28 (6) ◽  
pp. 1199-1205 ◽  
Author(s):  
S. K. Sharma ◽  
T. K. Mandal ◽  
B. C. Arya ◽  
M. Saxena ◽  
D. K. Shukla ◽  
...  

Abstract. In this paper, we present the effect of total solar eclipse on surface O3, NO, NO2, NH3, CO mixing ratio and the meteorological parameters on 15 January 2010 at Thiruvanathapuram, India. On the day of total solar eclipse (i.e., 15 January 2010), the decrease in mixing ratio of surface O3 and NO2 is observed after the beginning of the solar eclipse events (11:15 to 15:30). Decrease in surface O3 may be due to decreased efficiency of the photochemical ozone formation, whereas, mixing ratio of NO and NH3 have been changed following the night time chemistry. Surface O3 reduced to 20.3 ppb after 22 min of full phase of the eclipse. During the solar eclipse period, the ambient temperature and wind speed have decreased, whereas, relative humidity has increased as expected.



2004 ◽  
Vol 1 (2) ◽  
pp. 65 ◽  
Author(s):  
Donald H. Stedman


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