Please wait a minute...
Adv search
PLATEAU METEOROLOGY  1993, Vol. 12 Issue (1): 90-94    DOI:
    
ARTIFICIALLY TRIGGERED LIGHTNING AND THE CORN VARIATION
Liu Xinzhong1, Chen Mingli2, Fang Guangseng1, Wang Huaibin2, Yuan Yi3
1. The Second Institute of second Artillery, PLA, 100085;
2. Lanzhou Institute of Plateau Atmospheric Physics, Chinese Academy of Sciences, Lanzhou, Gansu 730000;
3. Xujiaying Village, Yanqin County, Beijing 102100
Download:  PDF (1676KB) 
Export:  BibTeX | EndNote (RIS)      
Abstract  In this paper,the artificially triggered lightning in the maize field during the earing and flowering stages was discussed.The change of the electromagnetic field near the stroke points was measured.It was found that the rates of two earing and the earing of male flower of the maize near the stroke points and the thoroughfare of igniting wire of artificially triggered lightning in the crop field are much greater.They are 4 times and 2.8 times higher than in common one respectively.The phenomenon is the same as that of mutation induced by physical factors.If it can repeat and the mutation can inherit,it must be one of the evidence of the evolution of life in nature.
Key words:  Artificially triggered lightning      Electric shock      Corn variation     
Received:  12 December 1991      Published:  24 March 1993

Cite this article: 

Liu Xinzhong, Chen Mingli, Fang Guangseng, Wang Huaibin, Yuan Yi. ARTIFICIALLY TRIGGERED LIGHTNING AND THE CORN VARIATION. PLATEAU METEOROLOGY, 1993, 12(1): 90-94.

URL: 

http://www.gyqx.ac.cn/EN/     OR     http://www.gyqx.ac.cn/EN/Y1993/V12/I1/90

[1] . Characteristic Analysis of Structure and Lightning for ConvectiveSystem Produced Heavy Precipitation in Warm Sector of South China[J]. PLATEAU METEOROLOGY, 2011, 30(4): 1034 -1045 .
[2] . Revision of the Measured Value of Slow Antenna under the ComplexTerrain Condition of Qinghai-Tibetan Plateau[J]. PLATEAU METEOROLOGY, 2011, 30(4): 1046 -1051 .
[3] . Stream Structure of a Convective Line with Leading StratiformPrecipitation during Meiyu Period[J]. PLATEAU METEOROLOGY, 2011, 30(4): 1052 -1066 .
[4] . Observational Study on Vertical Microphysical Structure ofan Autumn Cold-Front Cloud in Shijiazhuang Region[J]. PLATEAU METEOROLOGY, 2011, 30(5): 1324 -1336 .
[5] . Analysis of Changes in Different-Class Precipitationover Eastern China under Global Warming[J]. PLATEAU METEOROLOGY, 2009, 28(4): 889 -896 .
[6] . Characteristic of a Couple of Vortexes on the East Sideof Tibetan Plateau from Winter to Spring and TheirImpact on the Weather and Climate in China[J]. PLATEAU METEOROLOGY, 2009, 28(5): 945 -954 .
[7] . Simulation on Impact of Water Vapor in Various SourceAreas on NWC Precipitation Summer(I): Experiment Schemes and Contrast Run Results[J]. PLATEAU METEOROLOGY, 2009, 28(6): 1211 -1219 .
[8] . [J]. PLATEAU METEOROLOGY, 2010, 29(1): 137 -145 .
[9] . Research of Spatial Distribution Characteristic of AtmosphricAerosol in Jinan and Its Surrounding Regions[J]. PLATEAU METEOROLOGY, 2011, 30(5): 1346 -1355 .
[10] . Study on Vertical Microphysical Structure of Cloud for aMulti-layer Cloud System[J]. PLATEAU METEOROLOGY, 2011, 30(5): 1368 -1375 .