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Physics · Ch 7 — Gravitation

Acceleration Due to Gravity of the Earth

7.5

Acceleration Due to Gravity of the Earth

Consider an object of mass mm resting at the Earth's surface, a distance RR (the Earth's own radius) from the Earth's centre, and treat the Earth, for this purpose, as though its entire mass MM were concentrated at a single point at its centre (a valid simplification for a body that is very nearly spherically symmetric, which Newton himself proved rigorously using integral calculus). By Newton's law of gravitation, the Earth pulls this object toward its centre with a force

F=GMmR2F = \frac{GMm}{R^2}

By Newton's second law, this same force also equals mgmg, where gg is exactly the familiar acceleration due to gravity used throughout ordinary mechanics problems. Equating the two expressions for FF and cancelling the one factor of mm common to both sides,

mg=GMmR2⟹g=GMR2mg = \frac{GMm}{R^2} \quad \Longrightarrow \quad g = \frac{GM}{R^2}

This single equation is the real origin of the number g≈9.8 m/s2g \approx 9.8\ \text{m/s}^2 used throughout mechanics: gg is not some separate, independently defined constant of nature at all, but simply what Newton's inverse-square law of gravitation works out to, for an object sitting specifically at the Earth's own surface, a fixed distance RR from the Earth's centre. Two consequences follow immediately from this: first, gg must depend only on the Earth's own mass MM and radius RR, and not at all on the mass mm of the falling object itself -- exactly why, famously, a heavy stone and a light feather fall with the very same acceleration in a vacuum. Second, since g=GM/R2g = GM/R^2 holds only for an object exactly at distance RR from the Earth's centre, any object at a genuinely different distance -- higher up, or lower down -- experiences a correspondingly different value of gg, which is exactly the subject of the next two sections. …