不同环境中引力子的聚集分析——宇宙中氢元素形成的一种可能过程

Aggregation Analysis of Gravitons in Different Environments—A Possible Process for the Formation of Hydrogen in the Universe

摘要: 本文首先回顾了偏转引力理论和物质粒子的微子云理论，分析了太阳光球层、地球大气层、地球水圈层、地壳岩石层、土星大气层、木星大气层和氦、锂、铍、硼、碳元素为主的物质中引力子的聚集情况，说明由氢氦元素为主的太阳光球层、土星大气层、木星大气层中，引力子聚集可以产生氢元素，同样可以推测在由氢氦元素为主的宇宙星云中，也可以产生氢元素，此结论与天文观测事实相符。最后通过对宇宙中普通物质的占比计算，说明宇宙中绝大多数引力子都转化为氢元素，只有极少数引力子在传播引力。本文的分析提出了一种宇宙中氢元素丰度形成的新过程。

Abstract: This article first reviews the theory of deflected gravity and the micron cloud theory of matter par-ticles, and analyzes the aggregation of gravitons in the solar photosphere, earth’s atmosphere, earth’s hydrosphere, crustal rock layer, atmosphere of Saturn, atmosphere of Jupiter, and materials mainly composed of helium, lithium, beryllium, boron, and carbon elements. This situation shows that in the solar photosphere, the atmosphere of Saturn, and the atmosphere of Jupiter, which are dominated by hydrogen and helium elements, the aggregation of gravitons can produce hydrogen elements. It can also be speculated that in cosmic nebulae dominated by hydrogen and helium ele-ments, hydrogen elements can also be produced. This conclusion is consistent with the astronomical observation facts. Finally, by calculating the proportion of ordinary matter in the universe, it is shown that the vast majority of gravitons in the universe are converted into hydrogen elements, and only a very small number of gravitons are spreading gravity. The analysis in this paper propos-es a new process for the formation of hydrogen abundance in the universe.