Aether destructive theory of gravity: Calculation of the aether pressure at the surface of the earth
Bibliographic record
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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How this classification was reachedexpand
Full frame machine prediction
Teacher imitationNot calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.
Distilled classifier scores by category (both heads)
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.000 | 0.002 |
| Meta-epidemiology (narrow) | 0.001 | 0.000 |
| Meta-epidemiology (broad) | 0.001 | 0.001 |
| Bibliometrics | 0.002 | 0.001 |
| Science and technology studies | 0.001 | 0.001 |
| Scholarly communication | 0.001 | 0.002 |
| Open science | 0.002 | 0.001 |
| Research integrity | 0.001 | 0.001 |
| Insufficient payload (model declined to judge) | 0.003 | 0.001 |
Machine scores (provisional)
The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.
Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from itClassification
machine, unvalidatedMachine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.
How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".