IRRADIATION OF CARBON DIOXIDE WITH A VACUUM UV SOURCE AND OBTAINING OF STRATOSPHERIC OZONE

Marat Huseynov Elshan Aliyev, Hilal Tahirli Tarana Aghadiyeva
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Abstract

It has been known for more than 100 years that carbon dioxide absorbs photons in the ultraviolet and infrared ranges of radiation, creating a greenhouse effect. However, so far no one has answered the question: what is a photon? It is known that a photon has corpuscular and wave properties, has a certain pressure. An interesting experiment was carried out when a photon was dissected using Wilson chamber and it left traces of the opposite sign. The correct conclusion was made that one trace in the Wilson chamber was left by an electron, and the other - by a positron. There were other experiments, for example: birefringence of light in quartz crystals, Icelandic spar, etc., but there were no correct conclusions made about what a photon is. A photon is an electric dipole, consisting of an electron and a positron charges, without a spin charge-conjugate formation, which has a dipole magnetic field. Carbon dioxide, absorbing photons with a mass of 18.210-31 kg, being structured in the core, turns into triatomic oxygen, that is, into stratospheric ozone. A photon absorbs only a carbon atom that has an excess of spins. Photons absorbed by carbon dioxide (electric dipoles) having a magnetic field interact with the magnetic force lines of the dipole magnetic field of the Earth, and as a result of such interaction, triatomic oxygen-ozone moves into the stratosphere. Stratospheric ozone is not explosive in all aggregate states and at high pressures. In the atmosphere, it enters into a nuclear interaction with neutrons emanating from the sources of future earthquakes, forming water. So, naturally, the ozone layer of the Earth is depleted, replenishing the hydrosphere. Irradiation of CO2 and production of stratospheric ozone is a solution to the problem of climate warming. Stratospheric ozone can be widely used in the defense industry. An airship filled with stratospheric ozone will be much more efficient than airships filled with hydrogen or helium. The production of stratospheric ozone from carbon dioxide is a fundamental discovery in the field of photonuclear physics. Key words: electric dipole, photon, carbon dioxide, stratospheric ozone, photonuclear reaction.
用真空紫外源照射二氧化碳和获得平流层臭氧
100多年前,人们就已经知道二氧化碳会吸收紫外线和红外线辐射范围内的光子,从而产生温室效应。然而,到目前为止,还没有人回答这个问题:光子是什么?众所周知,光子具有微粒和波的性质,具有一定的压强。一个有趣的实验是,当一个光子被威尔逊室解剖时,它留下了相反符号的痕迹。正确的结论是,威尔逊室中的一个痕迹是电子留下的,另一个是正电子留下的。还有其他的实验,例如:石英晶体、冰岛晶石等中的光的双折射,但是对于光子是什么并没有得出正确的结论。光子是电偶极子,由一个电子和一个正电子电荷组成,没有自旋电荷共轭形成,具有偶极子磁场。二氧化碳吸收了质量为18.2公斤的光子,在核心处形成三原子氧,即平流层臭氧。光子只吸收有过多自旋的碳原子。光子被具有磁场的二氧化碳(电偶极子)吸收,与地球偶极子磁场的磁力线相互作用,作为这种相互作用的结果,三原子氧臭氧进入平流层。平流层臭氧在所有聚集状态和高压下都不是爆炸性的。在大气中,它与未来地震源发出的中子发生核相互作用,形成水。所以,自然地,地球上的臭氧层被耗尽,补充了水圈。二氧化碳的辐照和平流层臭氧的产生是解决气候变暖问题的一种方法。平流层臭氧可广泛用于国防工业。充满平流层臭氧的飞艇将比充满氢或氦的飞艇效率高得多。从二氧化碳中产生平流层臭氧是光核物理学领域的一项基本发现。关键词:电偶极子,光子,二氧化碳,平流层臭氧,光核反应。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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