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Detailed Reference Information |
Navarro-González, R., Villagrán-Muniz, M., Sobral, H., Molina, L.T. and Molina, M.J. (2001). The physical mechanism of nitric oxide formation in simulated lightning. Geophysical Research Letters 28: doi: 10.1029/2001GL013170. issn: 0094-8276. |
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We report an experimental assessment of the contributions of the shockwave and the hot channel to the production of nitric oxide by simulated lightning. Lightning in the laboratory was simulated by a hot plasma generated with a pulsed Nd-YAG laser. The temporal evolution of electric breakdown in air at atmospheric pressure was studied from the nanosecond to the millisecond time scale by shadowgraphy and interferometry techniques. The shock-wave front velocity was determined to be about 60 km s-1 at 20 ns and the temperature behind the shock front was estimated to be about 105 K. The production yield of nitric oxide by shock heating is estimated to be: P(NO) (3¿2)¿1014 molecule J-1. In contrast it was calculated that the production yield of NO by the hot channel is as much as P(NO)=(1.5¿0.5)¿1017 molecule J-1. To the extent our simulation is an accurate representation of natural lightning, the hot channel is the dominant region for nitrogen fixation. ¿ 2001 American Geophysical Union |
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Abstract |
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Keywords
Atmospheric Composition and Structure, Chemical kinetic and photochemical properties, Electromagnetics, Plasmas, Meteorology and Atmospheric Dynamics, Atmospheric electricity, Meteorology and Atmospheric Dynamics, Lightning |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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