Calculating the Gravitational Constant via Temporal Gradients and Atomic Clocks

Instead of mechanical measurements of force, this method applies the formula: Δt / t = GM / rc² which is reversed to solve for G using empirical data. Calculations are performed for three separate systems – Earth, the Sun, and Sagittarius A* – yielding values within 0.01–0.3% of the officially accepted gravitational constant.

This is the first evidence that the gravitational constant (and possibly other constants) may be derived from a temporal gradient, rather than being a postulated universal constant — a result that is part of a broader theory about the influence of time on reality, which is to be published separately.