Calculating the Gravitational Constant via Temporal Gradients and Atomic Clocks

We present a novel analytical approach for determining the gravitational constant G, based on the measurement of gravitational time dilation using 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.本研究提出一种基于原子钟(atomic clocks)引力时间膨胀(gravitational time dilation)测量的引力常数G(gravitational constant)测定新分析方法。相较于传统的力学测力手段，本方法采用公式Δt/t = GM/rc²，并通过经验数据反推求解引力常数G。研究针对地球、太阳及人马座A*(Sagittarius A*)三个独立天体系统开展计算，所得结果与官方公认引力常数的偏差处于0.01%至0.3%的区间内。本研究首次证实，引力常数（或其他部分基础常数）可通过时间梯度(temporal gradient)推导得到，而非作为预设的普适常数(universal constant)；该成果属于一项探讨时间对物理实在之影响的广义理论的组成部分，相关完整内容将另行发表。