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Physics · Ch 6 — Gravitation

Gravitational Potential Energy Near the Surface of the Earth

6.2.4

Gravitational Potential Energy Near the Surface of the Earth

The formula U=mghU=mgh, used constantly for objects near the Earth's surface, is not an independent rule -- it is simply the general result U(r)=−GMem/rU(r)=-GM_em/r approximated for the special case where the height hh above the surface is tiny compared with the Earth's radius ReR_e.

Derivation. With r=Re+hr=R_e+h, the general potential energy is

U=−GMemRe+h=−GMemRe(1+hRe)−1.(6.30-6.32)U=-\frac{GM_em}{R_e+h}=-\frac{GM_em}{R_e}\left(1+\frac{h}{R_e}\right)^{-1}. \qquad (6.30\text{-}6.32)

Since h≪Reh\ll R_e, a first-order binomial expansion (1+x)−1≈1−x(1+x)^{-1}\approx 1-x gives

U≈−GMemRe(1−hRe)=−GMemRe+GMemRe2h.(6.33)U\approx -\frac{GM_em}{R_e}\left(1-\frac{h}{R_e}\right)=-\frac{GM_em}{R_e}+\frac{GM_em}{R_e^2}h. \qquad (6.33)

Using GMem/Re2=mgRe/Re=mgGM_em/R_e^2 = mgR_e/R_e = mg (from GMe/Re2=gGM_e/R_e^2=g), this becomes

U≈−mgRe+mgh.(6.35)U\approx -mgR_e+mgh. \qquad (6.35)

The first term, −mgRe-mgR_e, does not depend on hh at all -- it is a fixed constant offset for the chosen reference (infinity). Since only differences in potential energy have physical meaning, this constant term can simply be dropped, or equivalently, we can choose the surface of the Earth (h=0h=0) as our new zero reference. What remains is exactly the familiar

U=mgh,U=mgh, …

Figure 6.14A mass raised to height h above the Earth

What this figure shows. The Earth is drawn as a circle of radius R_e with its centre marked O; a small mass m sits at height h above the surface, so its distance from Earth's centre is r = R_e + h. The diagram visually sets up why, once h is much smaller than R_e, the general formula U(r) = -GM_em/r can be simplified into the familiar near-surface form U = …