Why gravity stores energy
Potential energy is the energy stored in a body on account of its position, measured by the work done in bringing the body from a chosen standard position to its present one. For this idea to be well-defined the force must be conservative — the work it does between two points must be independent of the path taken. NCERT §7.7 states plainly that the force of gravity is a conservative force, so a gravitational potential energy function exists.
The consequence is the central rule of this topic: when a body moves in a gravitational field, the change in its potential energy equals the work done on it by the gravitational force. Two positions, one number — and that number does not care which route the body took between them.
The near-surface result: U = mgh
Start close to the Earth's surface, at heights much smaller than the Earth's radius. Here the gravitational force is practically constant, equal to \(mg\) and directed towards the centre. Lifting a mass \(m\) from a height \(h_1\) to a height \(h_2\) costs work
$$W_{12} = mg\,(h_2 - h_1).$$
Associate with each height a potential energy \(W(h) = mgh + W_0\), where \(W_0\) is a constant. Then \(W_{12} = W(h_2) - W(h_1)\), and the constant \(W_0\) cancels — confirming that only the difference matters. Setting \(h=0\) shows \(W_0\) is simply the potential energy at the surface. Dropping that constant gives the schoolbook form \(U = mgh\).
This is clean, but it rests on one assumption: that \(g\) does not change over the height involved. The moment \(h\) becomes comparable to the Earth's radius, that assumption collapses and \(mgh\) is no longer valid. For that regime we need the exact expression.
The exact two-body form: U = −GMm/r
For points at arbitrary distance from the Earth, the force is no longer constant; it follows the inverse-square law \(F = \dfrac{GM_E m}{r^2}\) directed towards the centre. Integrating this force to find the work done in moving the particle from \(r_1\) to \(r_2\) gives
$$W_{12} = \int_{r_1}^{r_2}\frac{GM_E m}{r^2}\,dr = -\,GM_E m\left(\frac{1}{r_2}-\frac{1}{r_1}\right).$$
So we may associate a potential energy \(W(r) = -\dfrac{GM_E m}{r} + W_1\), valid for \(r > R\), such that once again \(W_{12} = W(r_2) - W(r_1)\). Setting \(r \to \infty\) makes the first term vanish, so \(W_1\) is the potential energy at infinity. Conventionally one sets \(W_1 = 0\): the potential energy at a point becomes exactly the work done in bringing the particle from infinity to that point. With that choice, for a two-body system of masses \(M\) and \(m\) separated by \(r\),
$$\boxed{\,U = -\dfrac{GMm}{r}\,}\qquad (U \to 0 \text{ as } r \to \infty).$$
Why U is negative
The negative sign is not a quirk of algebra; it carries physical meaning. Because the zero of potential energy sits at infinity and gravity is attractive, bringing two masses together from infinity lets gravity do positive work, draining the system's energy below zero. Every finite separation therefore gives a negative \(U\).
The deeper (more negative) the value, the more tightly bound the system: more external work is needed to separate the masses back to infinity. This is exactly why the total mechanical energy of an orbiting satellite is negative — the system is gravitationally bound.
Gravitational potential V and the relation U = mV
The gravitational potential at a point is defined as the potential energy of a particle of unit mass placed there. Dividing the two-body energy by the test mass gives
$$V = \frac{U}{m} = -\frac{GM}{r}.$$
Potential \(V\) describes the field itself, independent of any test mass; potential energy \(U\) describes a particular mass \(m\) sitting in that field. They are linked by \(U = mV\). Crucially, \(V\) is a scalar — its SI unit is J/kg, while \(U\) is measured in joules.
| Quantity | Symbol & formula | Depends on | SI unit |
|---|---|---|---|
| Gravitational potential | \(V = -\dfrac{GM}{r}\) | Source mass and position only | J kg\(^{-1}\) |
| Gravitational potential energy | \(U = -\dfrac{GMm}{r}\) | Both masses and separation | J |
| Link between them | \(U = mV\) | Test mass \(m\) | — |
Because \(V\) is a scalar, the potential due to several masses is the simple arithmetic sum of their individual contributions — the superposition principle. For masses \(M_1, M_2, M_3,\dots\) at distances \(r_1, r_2, r_3,\dots\) from a point,
$$V = -G\left(\frac{M_1}{r_1}+\frac{M_2}{r_2}+\frac{M_3}{r_3}+\cdots\right).$$
No angles, no vector components — that is the chief advantage of working with potential rather than field. The total potential energy of an isolated system of particles is likewise the sum over all distinct pairs.
Work done in a gravitational field
Since gravity is conservative, the work done depends only on the endpoints. Two equivalent statements are worth keeping straight. The work done by gravity as a mass moves from point 1 to point 2 equals the drop in potential energy, \(W_{\text{grav}} = U_1 - U_2\). The work an external agent must do, moving the mass slowly so its speed does not change, equals the rise in potential energy:
$$W_{\text{ext}} = U_2 - U_1 = m\,(V_2 - V_1).$$
If the mass is carried between two points at the same potential, the net work is zero regardless of path — the defining mark of a conservative field. These relations turn every "work to move a mass" problem into a difference of two potential energies, no integration required once \(U=-GMm/r\) is in hand.
The conservative-force machinery here is the same as in mechanics — revisit potential energy and conservation for the general work–energy framework.
Worked example 1 — energy to lift a mass to height h
A body of mass \(m\) is lifted from the Earth's surface (radius \(R\), mass \(M\)) to a height \(h\) above the surface. Find the exact increase in its gravitational potential energy, and the work an external agent must supply.
Set up the two endpoints. Initial separation from the centre is \(r_1 = R\); final separation is \(r_2 = R+h\). Use the exact form \(U=-GMm/r\) with the zero at infinity.
Take the difference. $$\Delta U = U_2 - U_1 = -\frac{GMm}{R+h} - \left(-\frac{GMm}{R}\right) = GMm\left(\frac{1}{R}-\frac{1}{R+h}\right).$$
Simplify. $$\Delta U = GMm\cdot\frac{(R+h)-R}{R(R+h)} = \frac{GMm\,h}{R(R+h)}.$$ This is positive, as it must be: lifting against gravity raises the potential energy. The external agent, moving the mass slowly, supplies exactly \(W_{\text{ext}} = \Delta U = \dfrac{GMm\,h}{R(R+h)}\).
Sanity check. For \(h \ll R\) the denominator \(R(R+h)\to R^2\), so \(\Delta U \to \dfrac{GMm}{R^2}\,h = mgh\), since \(g = GM/R^2\) at the surface. The exact result collapses to \(mgh\) precisely in the near-surface limit.
Worked example 2 — mgh versus the exact difference
Compare the potential-energy increase given by \(mgh\) with the exact value for a mass raised to (a) \(h = R/100\) and (b) \(h = R\) above the surface. Express the exact value as a fraction of \(mgh\).
Form the ratio. From Example 1, the exact increase is \(\Delta U = \dfrac{GMm\,h}{R(R+h)}\). Using \(mgh = \dfrac{GMm}{R^2}h\), $$\frac{\Delta U_{\text{exact}}}{mgh} = \frac{R^2}{R(R+h)} = \frac{R}{R+h} = \frac{1}{1 + h/R}.$$
(a) \(h = R/100\). Ratio \(= \dfrac{1}{1+0.01} \approx 0.9901\). The \(mgh\) estimate overstates the true value by only about \(1\%\) — perfectly acceptable for near-surface problems.
(b) \(h = R\). Ratio \(= \dfrac{1}{1+1} = 0.5\). Now \(mgh\) gives twice the true potential-energy increase. At heights comparable to \(R\), the \(mgh\) formula is grossly wrong, and only \(U=-GMm/r\) is reliable.
Reading. The error in \(mgh\) is governed entirely by the ratio \(h/R\). This is the quantitative face of NCERT's statement that \(mgh\) is merely an approximation to the difference in gravitational potential energy.
Worked example 3 — potential due to several masses
Four particles, each of mass \(m\), sit at the corners of a square of side \(l\). Find the gravitational potential at the centre of the square.
Find the distance from centre to each corner. The half-diagonal of a square of side \(l\) is \(\dfrac{l\sqrt{2}}{2} = \dfrac{l}{\sqrt{2}}\). All four corners are equidistant from the centre at \(r = \dfrac{l}{\sqrt{2}}\).
Add the scalar potentials. Potential is a scalar, so the four contributions add directly: $$V_{\text{centre}} = 4\times\left(-\frac{Gm}{r}\right) = -\frac{4Gm}{\,l/\sqrt{2}\,} = -\frac{4\sqrt{2}\,Gm}{l}.$$
Reading. No vector resolution was needed — that is the whole point of working with potential. By symmetry the gravitational field at the centre is zero, yet the potential there is decidedly non-zero. Field and potential are different objects, and a zero field never implies a zero potential.
Gravitational PE in one breath
- Gravity is conservative, so a position-dependent potential energy exists; only differences in \(U\) are physical.
- Exact two-body PE: \(U = -GMm/r\), with the zero set at infinite separation.
- \(U\) is negative because gravity is attractive and the zero is at infinity — the system is bound; more negative means more tightly bound.
- \(mgh\) is only the near-surface approximation, valid when \(h \ll R\); the exact difference is \(-GMm\left(\tfrac{1}{r_2}-\tfrac{1}{r_1}\right)\).
- Gravitational potential \(V = -GM/r\) is PE per unit mass (J/kg, a scalar); \(U = mV\).
- Potentials of several masses add arithmetically; work to move a mass \(= m(V_2 - V_1)\), path-independent.