Aether destructive theory of gravity: Calculation of the aether pressure at the surface of the earth

IF 0.6 Q4 PHYSICS, MULTIDISCIPLINARY Physics Essays Pub Date : 2022-09-06 DOI:10.4006/0836-1398-35.3.252
Peter M. Atkinson, Samuel Nlend
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Abstract

The aether theory of gravity basically states that the gravity produced by a large object such as the earth is that aether is destroyed or modified within the earth. This results in a fall in aether pressure within the earth. Aether then accelerates into the earth from outer space in order to keep the aether pressure within the earth constant. The aether accelerating into the earth exerts a force on all objects caught in the accelerating aether flow. We have modified the existing theories of what aether is, and using these modifications and existing published figures on the structure of atomic nuclei, we have been able to calculate the aether pressure at the surface of the earth, as well as calculating the gravitational force per nucleon at the surface of the earth. We calculated the aether pressure at the surface of the earth as being 3311 N/m2 or 337.66 kg/m2. The gravitational force per nucleon is 1.627 × 10−26 N/nucleon. We present an entirely new way to calculate the gravitational force acting on an object at the surface of the earth based on the aether theory of gravity and aether dynamics. The force of gravity acting on an object (F) is the product of the aether pressure (P), the mass of object in grams (m), the effective surface area of a nucleon (Seff), and Avogadro’s number. The effective surface area is proportional to half of the surface area of a nucleon (S) multiplied by a factor (). The factor necessary to modify the effective surface area was calculated using calculus. The fact that this equation, based on aether dynamics, actually works demonstrates that the aether theory of gravity may well be correct.
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重力的以太破坏理论:地球表面以太压力的计算
以太引力理论基本上是说,像地球这样的大物体产生的引力是以太在地球内部被破坏或改变的。这导致地球内部的以太压力下降。然后以太从外太空加速进入地球,以保持地球内部的以太压力恒定。加速进入地球的以太对所有被加速的以太流捕获的物体都施加了一个力。我们修改了现有的以太理论,并利用这些修改和现有的原子核结构的已发表的数字,我们已经能够计算出地球表面的以太压力,以及计算地球表面每核子的引力。我们计算出地球表面的以太压力为3311 N/m2或337.66 kg/m2。每核子的引力为1.627 × 10−26 N/核子。我们提出了一种基于以太引力理论和以太动力学的计算地球表面物体引力的全新方法。作用在物体上的重力(F)是以太压力(P)、物体质量(m)、核子的有效表面积(Seff)和阿伏伽德罗数的乘积。有效表面积与核子表面积的一半(S)乘以一个因子()成正比。用微积分法计算了改变有效表面积所需的因子。这个基于以太动力学的方程确实有效,这一事实证明了以太引力理论很可能是正确的。
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来源期刊
Physics Essays
Physics Essays PHYSICS, MULTIDISCIPLINARY-
自引率
83.30%
发文量
50
审稿时长
6-12 weeks
期刊介绍: Physics Essays has been established as an international journal dedicated to theoretical and experimental aspects of fundamental problems in Physics and, generally, to the advancement of basic knowledge of Physics. The Journal’s mandate is to publish rigorous and methodological examinations of past, current, and advanced concepts, methods and results in physics research. Physics Essays dedicates itself to the publication of stimulating exploratory, and original papers in a variety of physics disciplines, such as spectroscopy, quantum mechanics, particle physics, electromagnetic theory, astrophysics, space physics, mathematical methods in physics, plasma physics, philosophical aspects of physics, chemical physics, and relativity.
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