Discussion Overview
The discussion revolves around the calculation of gravity for different particles and celestial bodies, including protons and neutron stars. Participants explore the formulas applicable to these scenarios and the implications of adding masses together in gravitational contexts.
Discussion Character
- Exploratory
- Technical explanation
- Debate/contested
Main Points Raised
- Mike questions how to calculate the gravity of a single proton and a neutron star, seeking examples and formulas.
- One participant provides the formula for gravitational acceleration, \(\vec{g}=\frac{GM}{r^{2}}\hat{r}\), and asserts that adding particles together does result in a total gravity that can be summed.
- Another participant challenges the validity of discussing the "gravity of a single proton," suggesting that it is more appropriate to talk about the gravitational field or force of a system of particles.
- There is mention of the equivalence principle, which posits that the active gravitational mass of a particle should equal its inertial mass, but this is described as a postulate rather than an established fact.
- Concerns are raised about the lack of experimental tests regarding the active gravitational mass of particles, with references to the Kreuzer experiment of 1966 as a notable but limited study.
- Further clarification is provided regarding the distinction between active and passive gravitational mass, emphasizing that the Kreuzer experiment specifically relates to active gravitational mass and its correlation to composition.
Areas of Agreement / Disagreement
Participants express differing views on the concept of gravity as it applies to individual particles versus macro objects. There is no consensus on how to approach the calculation of gravity for particles, and the discussion remains unresolved regarding the implications of the equivalence principle and the validity of existing experimental evidence.
Contextual Notes
The discussion highlights limitations in experimental validation of the equivalence principle for different compositions and the challenges in applying classical gravitational formulas to individual particles.