The Trouble with mghmgh

You have been writing U=mghU = mgh since Class 9. It works. Drop a ball, catch it, do the sum, and the numbers come out right.

Here is the thing, though. That formula has a constant gg buried inside it — and Section 4 has just spent a whole section proving that gg is not constant. It falls off as 1r2\frac{1}{r^2} once you leave the surface. So mghmgh cannot possibly be the whole truth. It is a local rule, valid in the thin shell of air near the ground where gg genuinely does not change much, and it quietly stops being right the moment you go anywhere interesting.

This section builds the honest version.

Gravity is conservative, so a potential energy exists

Before we can define a potential energy at all, we need one guarantee: the work done by gravity in moving a body from point A to point B must not depend on the path taken. A force with that property is called conservative, and only for such a force can we bottle up the work as a stored energy that depends on position alone.

Gravity passes the test. It is a central force — it always points along the line joining the two bodies, and its size depends only on the separation rr. Move along a circular arc centred on the source and gravity does zero work, because the force is perpendicular to the motion. Move radially and the work depends only on the starting and finishing values of rr. Any path whatsoever can be chopped into arcs and radial steps, so the total work depends only on where you started and where you ended.

Key Point: Gravity is a conservative force. That is what licenses us to define a gravitational potential energy UU such that the work done by gravity going from A to B is Wgrav=UAUB=ΔUW_{grav} = U_A - U_B = -\Delta U.

Doing the integral

Take a body of mass mm at a distance rr from the centre of a body of mass MM, with rr outside MM so that the shell theorem lets us treat MM as a point at its centre. The gravitational force on mm points inwards, towards MM:

F=GMmr2r^\vec{F} = -\frac{GMm}{r^{2}}\,\hat{r}

where r^\hat{r} points radially outwards. Now carry mm from very far away in to the distance rr, and add up the work gravity does. Over a small outward step drdr the work is dW=Fdr=GMmr2drdW = \vec{F}\cdot d\vec{r} = -\frac{GMm}{r^{2}}\,dr, so

Mass carried in from infinity, work strip, and the resulting negative potential energy

U(r)U()=Wgrav=rGMmr2dr=[GMmr]r=GMmr0U(r) - U(\infty) = -W_{grav} = \int_{\infty}^{r}\frac{GMm}{r^{2}}\,dr = \left[-\frac{GMm}{r}\right]_{\infty}^{r} = -\frac{GMm}{r} - 0

Fixing the zero, and why we put it at infinity

Notice what actually came out of that integral: a difference, U(r)U()U(r) - U(\infty). Only differences in potential energy have physical meaning, because only differences show up as work. The absolute value of UU at any one place is ours to choose.

So we choose. And the natural choice is the place where the two bodies stop interacting at all — infinite separation.

Key Point — the zero-of-potential-energy convention: We set U=0U = 0 when the two bodies are infinitely far apart. With that convention, U(r)=GMmrU(r) = -\frac{G M m}{r} and U(r)U(r) is then, by construction, the work done by gravity in bringing mm from infinity to rr — or equivalently, minus the work an external agent must do to bring it in slowly. State this convention whenever you write down a value of UU. Every negative sign in this chapter descends from it.

If somebody instead chose U=0U = 0 at the Earth's surface, they would write U(r)=GMEmr+GMEmREU(r) = -\frac{GM_Em}{r} + \frac{GM_Em}{R_E}, and every energy difference they computed would come out exactly the same. Their numbers for UU itself would be different, and mostly positive. Nothing physical changes. But the infinity convention is universal, so use it, and say you are using it.

Where the formula is valid

U=GMmrU = -\frac{GMm}{r} holds for rRr \geq R, that is, from the surface outwards. Inside a solid sphere the enclosed mass changes with rr and the expression is different — that is a JEE-level extension and it is developed in the JEE Corner section rather than here.

[Board Important] Two marks are routinely lost by writing U=GMmrU = \frac{GMm}{r} without the minus sign, and one more by not saying where the zero is. Write both, every time.

What That Minus Sign Actually Means

A negative energy sounds alarming the first time you meet it. It is not. It is a bookkeeping statement, and once you read it correctly it tells you something real.

Reading the sign

U(r)=GMmrU(r) = -\frac{GMm}{r} is negative for every finite rr. Since we agreed that U=0U = 0 at infinity, that means:

Key Point: A body sitting a finite distance from a mass has less energy than the same body infinitely far away. The deficit, GMmr\frac{GMm}{r}, is exactly the energy you would have to supply to drag it out to infinity and leave it there at rest. That is the physical content of the minus sign: the body is in an energy pit, and U\lvert U \rvert is how deep the pit is.

Three consequences follow immediately, and all three are examined:

  1. UU increases as rr increases. Going from 6.25×107-6.25 \times 10^7 J to 3.13×107-3.13 \times 10^7 J is going up. Less negative means larger. Students lose marks here constantly.
  2. UU is largest at infinity, where it equals zero. There is nowhere with a larger value.
  3. UU approaches -\infty as r0r \to 0. The pit has no bottom for idealised point masses. For real bodies you stop at the surface, and the shell theorem takes over inside.

Recovering mghmgh — and watching it fail

Now let us prove that mghmgh really is the near-surface limit of the real thing, and find out precisely where it stops working.

Raise a mass mm from the surface, r=REr = R_E, to a height hh, r=RE+hr = R_E + h. The rise in potential energy is

ΔU=GMEmRE+h(GMEmRE)=GMEm(1RE1RE+h)=GMEmhRE(RE+h)\Delta U = -\frac{GM_Em}{R_E+h} - \left(-\frac{GM_Em}{R_E}\right) = GM_Em\left(\frac{1}{R_E} - \frac{1}{R_E+h}\right) = \frac{GM_Em\,h}{R_E(R_E+h)}

Use g=GMERE2g = \frac{GM_E}{R_E^2} to trade GMEGM_E for gRE2gR_E^2:

Flat field near the surface, and exact energy rise against the mgh straight line

Key Point — the exact rise in UU, and its limit: ΔU=mgh1+hRE hRE ΔUmgh\Delta U = \frac{mgh}{1 + \frac{h}{R_E}} \qquad \xrightarrow{\ h \,\ll\, R_E\ } \qquad \Delta U \approx mgh So mghmgh is not wrong — it is the first term of the exact result, and it is always an overestimate. The fractional error is exactly hRE\frac{h}{R_E}.

That last sentence is worth more than the formula. You do not have to guess whether mghmgh is safe; you can compute the error in your head.

The error, with numbers attached

Using RE=6.37×106R_E = 6.37 \times 10^6 m and g=GMERE2g = \frac{GM_E}{R_E^2}, which comes to 9.819.81 m/s2^2 with G=6.67×1011G = 6.67 \times 10^{-11} N m2^2/kg2^2 and ME=5.97×1024M_E = 5.97 \times 10^{24} kg:

Height hh h/REh/R_E Exact ΔU\Delta U per kg (J/kg) ghgh (J/kg) mghmgh is too high by
1 km 0.00016 9.812×1039.812 \times 10^{3} 9.813×1039.813 \times 10^{3} 0.016%
10 km 0.00157 9.798×1049.798 \times 10^{4} 9.813×1049.813 \times 10^{4} 0.16%
63.7 km 0.0100 6.189×1056.189 \times 10^{5} 6.251×1056.251 \times 10^{5} 1.0%
100 km 0.0157 9.662×1059.662 \times 10^{5} 9.813×1059.813 \times 10^{5} 1.6%
300 km 0.0471 2.812×1062.812 \times 10^{6} 2.944×1062.944 \times 10^{6} 4.7%
1000 km 0.157 8.482×1068.482 \times 10^{6} 9.813×1069.813 \times 10^{6} 15.7%
RER_E = 6370 km 1.000 3.126×1073.126 \times 10^{7} 6.251×1076.251 \times 10^{7} 100%

Read the last row carefully. At h=REh = R_E, mghmgh gives exactly twice the true answer. Not slightly off — double.

Key Point: mghmgh is trustworthy to about 1% up to 64 km and to about 5% up to 300 km. Beyond that, use ΔU=GMEm(1r11r2)\Delta U = GM_Em\left(\frac{1}{r_1} - \frac{1}{r_2}\right).

Compare this with the altitude rule for gg itself from Section 4: gg loses 1% in 32 km, while mghmgh goes 1% wrong in 64 km. Different quantities, different tolerances — do not mix the two numbers up.

[JEE Tip] Any problem phrased with h=REh = R_E, h=2REh = 2R_E, "half the radius of the Earth" or "the height at which gg halves" is telling you plainly that mghmgh is banned. Reach for GMmr-\frac{GMm}{r} at both ends and subtract.

A System of Masses: Count Every Pair Exactly Once

So far there have been two bodies. Real problems put three, four or six masses in a row, in a triangle, at the corners of a square. The rule for handling them is short, and the mistake people make with it is always the same.

The rule

Potential energy belongs to a pair, not to a single body. You cannot ask "what is the potential energy of that particle" in isolation — you can only ask what the energy of the configuration is. So:

Key Point — potential energy of a system: Usystem=GpairsmimjrijU_{system} = -G\sum_{\text{pairs}}\frac{m_im_j}{r_{ij}} Take every distinct pair once, write Gmimjrij-\frac{Gm_im_j}{r_{ij}} for it, and add. With nn particles there are n(n1)2\frac{n(n-1)}{2} pairs: 1 for two particles, 3 for three, 6 for four, 10 for five. Zero of potential energy at infinite separation, as always.

The mistake is double counting — treating the pair (1,2)(1,2) and the pair (2,1)(2,1) as two different terms and getting an answer twice too big. Count pairs, not ordered pairs. Listing them explicitly before you start (ABAB, ACAC, ADAD, BCBC, BDBD, CDCD for four particles) costs ten seconds and removes the error entirely.

What the number means

UsystemU_{system} is the work done by gravity while the particles are brought in from infinite separation and assembled. Equivalently, Usystem-U_{system} is the work an external agent must supply to pull them all apart again and leave them at rest infinitely far from one another.

Key Point: Work to assemble the system =Usystem= U_{system} (negative — gravity helps you). Work to dismantle it completely =Usystem=+Usystem= -U_{system} = +\lvert U_{system} \rvert (positive — you have to pay).

The square, worked in general

Four equal masses mm at the corners of a square of side ll. There are six pairs: four sides, each of length ll, and two diagonals, each of length l2l\sqrt{2}.

Usystem=4(Gm2l)+2(Gm2l2)=Gm2l(4+22)=(4+2)Gm2lU_{system} = 4\left(-\frac{Gm^{2}}{l}\right) + 2\left(-\frac{Gm^{2}}{l\sqrt{2}}\right) = -\frac{Gm^{2}}{l}\left(4 + \frac{2}{\sqrt{2}}\right) = -\left(4 + \sqrt{2}\right)\frac{Gm^{2}}{l}

Usystem=5.41Gm2lU_{system} = -5.41\,\frac{Gm^{2}}{l}

Notice how the diagonals contribute less per pair, because they are longer. Notice too that the answer does not care which corner is which — the configuration has an energy, the individual particles do not.

Adding a mass to an existing system

A common exam move: three masses already sit at fixed positions, and you are asked for the work needed to bring a fourth in from infinity. You do not recompute the whole system. The three existing pairs are unchanged; only the three new pairs appear. So

Wext=UfinalUinitial=Gm4(m1r14+m2r24+m3r34)W_{ext} = U_{final} - U_{initial} = -Gm_4\left(\frac{m_1}{r_{14}} + \frac{m_2}{r_{24}} + \frac{m_3}{r_{34}}\right)

which, as the next block will show, is just m4m_4 times the potential the other three had already created at that spot. That is exactly the shortcut potential was invented for.

[NEET Important] For two particles, the numerical value of UU changes if either mass changes or if the separation changes — nothing else. Rotating the pair, or moving both of them together across the room, changes nothing.

Gravitational Potential: the Field's Own Property

Look again at U=GMmrU = -\frac{GMm}{r}. The source mass MM and the distance rr describe the field. The mass mm is just whatever you happened to put there. Divide it out, and what is left belongs to the field alone.

Key Point — gravitational potential: V=Um=GMrV = \frac{U}{m} = -\frac{GM}{r} VV at a point is the potential energy per unit mass of a body placed at that point, or equivalently the work done by gravity per unit mass in bringing a body from infinity to that point. Zero of potential at infinity, as before, so VV is negative everywhere around a mass. SI unit: joule per kilogram (J/kg), equivalently m2^2/s2^2. Dimensions [M0L2T2][M^0L^2T^{-2}].

VV exists at a point whether or not any mass is sitting there — exactly like gg. In fact VV and g\vec{g} are two descriptions of the same field, one a scalar and one a vector, and the rest of this block is about the relationship between them.

Why potential is so much easier than field

Because VV is a scalar, potentials from several sources add by ordinary arithmetic:

Key Point — superposition of potential: VP=V1+V2+V3+=G(m1r1+m2r2+m3r3+)V_P = V_1 + V_2 + V_3 + \cdots = -G\left(\frac{m_1}{r_1} + \frac{m_2}{r_2} + \frac{m_3}{r_3} + \cdots\right) where each rir_i is the distance from that source to the point PP. No components, no angles, no resolving. Compare that with gP=g1+g2+\vec{g}_P = \vec{g}_1 + \vec{g}_2 + \cdots, which needs full vector addition.

This is why potential is worth learning even though the field already tells you everything. A problem that takes half a page with vectors takes one line with potentials.

Potential at the centre of a square

Square of four masses, ring seen edge-on, and potential versus field curves

Four masses mm at the corners of a square of side ll. The centre is a distance l22=l2\frac{l\sqrt{2}}{2} = \frac{l}{\sqrt{2}} from every corner, so

Vcentre=4×(Gml/2)=42Gml=5.66GmlV_{centre} = 4 \times \left(-\frac{Gm}{l/\sqrt{2}}\right) = -\frac{4\sqrt{2}\,Gm}{l} = -5.66\,\frac{Gm}{l}

And the field there? By symmetry each corner's pull is cancelled by the diagonally opposite corner, so

gcentre=0\vec{g}_{centre} = 0

Stop and look at that pair of results. At the centre of the square the potential is at its most negative anywhere in the square, and the field is exactly zero. A large potential does not mean a large field. Hold on to that; it is the single most productive source of exam questions in this section.

Potential and field on the axis of a ring

Take a ring of mass MM and radius aa, and a point PP on its axis a distance xx from the centre. Every mass element dmdm of the ring is the same distance a2+x2\sqrt{a^{2}+x^{2}} from PP — that is the whole trick. So the scalar sum is trivial:

V=Ga2+x2dm=GMa2+x2V = -\frac{G}{\sqrt{a^{2}+x^{2}}}\int dm = -\frac{GM}{\sqrt{a^{2}+x^{2}}}

At the centre, x=0x = 0, this gives V=GMaV = -\frac{GM}{a}.

The field is harder, because the pulls from opposite elements point in different directions. Their components perpendicular to the axis cancel in pairs, and only the axial components survive, each scaled by cosθ=xa2+x2\cos\theta = \frac{x}{\sqrt{a^{2}+x^{2}}}:

gx=GMx(a2+x2)3/2g_x = -\frac{GMx}{\left(a^{2}+x^{2}\right)^{3/2}}

the minus sign saying it points back towards the ring. At the centre, x=0x = 0 makes gx=0g_x = 0: the deepest potential on the axis, and no field at all. The field is largest at x=a2x = \frac{a}{\sqrt{2}}, where it reaches 2GM33a2\frac{2GM}{3\sqrt{3}\,a^{2}}.

The bridge: field is minus the slope of potential

Those two ring results are not independent. Differentiate the potential and you get the field:

dVdx=ddx[GM(a2+x2)1/2]=GMx(a2+x2)3/2=gx-\frac{dV}{dx} = -\frac{d}{dx}\left[-GM\left(a^{2}+x^{2}\right)^{-1/2}\right] = -\frac{GMx}{\left(a^{2}+x^{2}\right)^{3/2}} = g_x

That is completely general.

Key Point — the field-potential relation: g=dVdrr^\vec{g} = -\frac{dV}{dr}\,\hat{r} The gravitational field is minus the rate of change of potential with distance. Check it on the point mass: V=GMrV = -\frac{GM}{r} gives dVdr=+GMr2\frac{dV}{dr} = +\frac{GM}{r^{2}}, so g=GMr2r^\vec{g} = -\frac{GM}{r^{2}}\hat{r} — the familiar inward field. The minus sign says the field points downhill in potential, from less negative towards more negative.

Read the relation both ways and you have the whole story of this block:

  • Where VV is changing fastest, the field is strongest.
  • Where VV has a maximum or a minimum along a line, the field along that line is zero. That is the centre of the square, and the centre of the ring.
  • VV can be large and negative with g=0\vec{g} = 0; g\vec{g} can be large where VV happens to be unremarkable. They are the value and the slope of the same curve.

The reverse trip works too: knowing the field everywhere, you recover the potential by integrating, V(r)=rgdrV(r) = -\int_{\infty}^{r} \vec{g}\cdot d\vec{r}, with the same zero at infinity.

[JEE Tip] If a question hands you VV as a function of position and asks for the field, differentiate — do not go back to masses and distances. If it hands you VV in two dimensions, such as V=(5x+3y)V = -(5x+3y), differentiate with respect to each coordinate in turn: gx=Vxg_x = -\frac{\partial V}{\partial x}, gy=Vyg_y = -\frac{\partial V}{\partial y}.

UU versus VV: the Distinction Examiners Live On

If you take one thing from this section, take this. More marks are lost to confusing gravitational potential energy with gravitational potential than to anything else in the chapter, because the two symbols look alike, the two formulas differ by a single letter, and both are negative.

Potential energy curves for three test masses beside a single potential curve

Key Point — the one-line version: VV is a property of the field. UU is a property of the field and the body you put in it. VV exists at a point in empty space. UU only exists once you have placed a mass mm there, and then U=mVU = mV. Change mm and UU changes in proportion; VV does not budge.

Look at the two graphs above. On the left, three different test masses give three different UU curves through the same region of space. On the right there is one VV curve, and it would be the same curve if nothing were there at all. Both are negative, both climb towards zero as rr grows, and neither ever reaches it.

Side by side

Potential energy UU Potential VV
Belongs to the pair: source and the placed body the field alone, i.e. the point in space
Exists without a test mass? No Yes
Point mass MM, distance rr U=GMmrU = -\frac{GMm}{r} V=GMrV = -\frac{GM}{r}
Depends on the placed mass mm? Yes, directly proportional Never
Scalar or vector scalar scalar
SI unit joule, J joule per kilogram, J/kg
Dimensions [ML2T2][ML^{2}T^{-2}] [M0L2T2][M^{0}L^{2}T^{-2}]
Zero taken at infinite separation infinite distance
Sign around a mass negative negative
Converting between them U=mVU = mV V=UmV = \frac{U}{m}
Adding several sources sum over pairs, once each sum the source potentials at that point
What you get by differentiating force, F=dUdrF = -\frac{dU}{dr} field, g=dVdrg = -\frac{dV}{dr}
Typical exam use work done, energy conservation quick superposition, then multiply by mm

The four traps

Trap 1 — writing VV for a system of particles. There is no such thing as "the potential of a system". Potential is defined at a point. If a question says "find the gravitational potential due to four masses at the centre of the square", it wants a scalar sum of four terms giving J/kg. If it says "find the gravitational potential energy of the four masses", it wants a sum over the six pairs, in joules. Same figure, completely different sums, different units.

Trap 2 — thinking zero potential means zero field. These are independent. At the centre of a square of equal masses, V0V \neq 0 and g=0\vec{g} = 0. At the neutral point between the Earth and the Moon, g=0\vec{g} = 0 but VV is a large negative number. And a point exactly halfway between two equal masses has neither zero.

Trap 3 — treating "more negative" as "more". 1×107-1 \times 10^{7} J/kg is a larger potential than 6×107-6 \times 10^{7} J/kg. Potential increases outwards. If a question asks where the potential is maximum, the answer for an isolated mass is "at infinity, where it is zero".

Trap 4 — dropping the mass, or adding it twice. U=mVU = mV. If you have already used VV to do the superposition, multiply by mm once at the end. A dimensional check catches this instantly: joules or joules per kilogram?

A checking habit worth building

Before you write a final answer in this section, ask three questions.

  1. Units? J means UU, J/kg means VV.
  2. Sign? Both must be negative for ordinary masses with the zero at infinity. A positive answer means a lost minus sign — unless you were asked for work done against gravity, which is positive.
  3. Pairs or points? Energy of a configuration counts pairs. Potential at a place counts sources.

[Board Important] The definitions are themselves worth marks, and they must include the convention. Write: "The gravitational potential at a point is the work done by an external agent, per unit mass, in bringing a small test mass from infinity to that point without acceleration; the potential at infinity is taken as zero."

Everything in the next four sections is built on this block. Escape speed is a statement about UU at the surface. Orbital energetics is KK plus UU. Binding energy is E-E. Get UU and VV straight now and the rest of the chapter becomes bookkeeping.

Solved Examples

Constants used throughout this section, unless a problem states otherwise: G=6.67×1011G = 6.67 \times 10^{-11} N m2^2/kg2^2, ME=5.97×1024M_E = 5.97 \times 10^{24} kg, RE=6.37×106R_E = 6.37 \times 10^{6} m, and where a rounded surface value is needed, g=9.8g = 9.8 m/s2^2. The zero of potential energy and of potential is at infinity everywhere in this section.

Example 1: How deep is the pit?

Find the gravitational potential energy of a 1 kg stone resting on the Earth's surface, and the gravitational potential there. What do the two numbers mean?

Solution:

  1. Potential energy, with the zero at infinity: U=GMEmRE=(6.67×1011)(5.97×1024)(1)6.37×106U = -\frac{GM_Em}{R_E} = -\frac{(6.67 \times 10^{-11})(5.97 \times 10^{24})(1)}{6.37 \times 10^{6}} U=3.982×10146.37×106=6.25×107 JU = -\frac{3.982 \times 10^{14}}{6.37 \times 10^{6}} = -6.25 \times 10^{7} \text{ J}

  2. Potential is the same thing per kilogram: V=Um=6.25×107 J/kgV = \frac{U}{m} = -6.25 \times 10^{7} \text{ J/kg}

  3. Meaning. To carry that stone away from the Earth entirely and leave it at rest infinitely far off, you must supply 6.25×1076.25 \times 10^{7} J. That is 62.5 megajoules for a single kilogram — roughly the energy in one and a half litres of petrol.

Final Answer: U=6.25×107U = -6.25 \times 10^{7} J and V=6.25×107V = -6.25 \times 10^{7} J/kg.

Takeaway: The two have the same magnitude here only because m=1m = 1 kg. For a 5 kg stone UU would be five times as big while VV would not change at all — check your units before you decide which one you have computed.

Example 2: Lifting 2 kg by one Earth radius

How much work must be done against gravity to raise a 2 kg mass from the Earth's surface to a height equal to the Earth's radius? Compare with what mghmgh would predict.

Solution:

  1. The exact change. The mass goes from r=REr = R_E to r=2REr = 2R_E. Wext=ΔU=GMEm2RE(GMEmRE)=GMEm2REW_{ext} = \Delta U = -\frac{GM_Em}{2R_E} - \left(-\frac{GM_Em}{R_E}\right) = \frac{GM_Em}{2R_E}

  2. Put the numbers in. Wext=(3.982×1014)(2)2×6.37×106=7.964×10141.274×107=6.25×107 JW_{ext} = \frac{(3.982 \times 10^{14})(2)}{2 \times 6.37 \times 10^{6}} = \frac{7.964 \times 10^{14}}{1.274 \times 10^{7}} = 6.25 \times 10^{7} \text{ J}

  3. What mghmgh would say, with g=9.8g = 9.8 m/s2^2 and h=REh = R_E: mgh=2×9.8×6.37×106=1.25×108 Jmgh = 2 \times 9.8 \times 6.37 \times 10^{6} = 1.25 \times 10^{8} \text{ J}

  4. The comparison. The shortcut is almost exactly twice the truth. That is no accident: at h=REh = R_E the exact result is mgh1+h/RE=mgh2\frac{mgh}{1+h/R_E} = \frac{mgh}{2}.

Final Answer: 6.25×1076.25 \times 10^{7} J. The mghmgh estimate, 1.25×1081.25 \times 10^{8} J, is 100% too large.

Takeaway: mghmgh always overestimates, and by the factor 1+hRE1 + \frac{h}{R_E}. Once hh is comparable with RER_E the shortcut is not approximate, it is simply wrong.

Example 3: How high can you trust mghmgh?

At what height does mghmgh become 1% too large? What is its error at 1000 km?

Solution:

  1. Write the exact ratio. mghΔUexact=1+hRE\frac{mgh}{\Delta U_{exact}} = 1 + \frac{h}{R_E} so the fractional error of the shortcut is exactly hRE\frac{h}{R_E}.

  2. Set that to 0.01. h=0.01×RE=0.01×6.37×106=6.37×104 m=63.7 kmh = 0.01 \times R_E = 0.01 \times 6.37 \times 10^{6} = 6.37 \times 10^{4} \text{ m} = 63.7 \text{ km}

  3. At h=1000h = 1000 km. hRE=1.00×1066.37×106=0.157error=15.7%\frac{h}{R_E} = \frac{1.00 \times 10^{6}}{6.37 \times 10^{6}} = 0.157 \qquad \Longrightarrow \qquad \text{error} = 15.7\%

  4. Sanity check with real energies per kilogram. Exact: 8.482×1068.482 \times 10^{6} J/kg. Shortcut: 9.813×1069.813 \times 10^{6} J/kg. Ratio 1.1571.157. It agrees.

Final Answer: 1% error at 63.7 km; 15.7% error at 1000 km.

Takeaway: You never have to guess whether mghmgh is allowed. Divide hh by RER_E and you have the percentage error directly.

Example 4: Four masses on a square

Four particles, each of mass 1000 kg, sit at the corners of a square of side 1 m. Find (a) the potential energy of the system, (b) the gravitational potential at the centre, and (c) the gravitational field at the centre.

Solution:

  1. (a) List the pairs. Four particles give 4×32=6\frac{4 \times 3}{2} = 6 pairs: four sides of length ll and two diagonals of length l2l\sqrt{2}. U=4Gm2l2Gm2l2=(4+2)Gm2l=5.41Gm2lU = -\frac{4Gm^{2}}{l} - \frac{2Gm^{2}}{l\sqrt{2}} = -\left(4+\sqrt{2}\right)\frac{Gm^{2}}{l} = -5.41\,\frac{Gm^{2}}{l}

  2. Substitute. With m=1000m = 1000 kg and l=1l = 1 m, Gm2l=6.67×1011×106=6.67×105\frac{Gm^2}{l} = 6.67 \times 10^{-11} \times 10^{6} = 6.67 \times 10^{-5} J. U=5.414×6.67×105=3.61×104 JU = -5.414 \times 6.67 \times 10^{-5} = -3.61 \times 10^{-4} \text{ J}

  3. (b) Potential at the centre. Every corner is l2=0.707\frac{l}{\sqrt{2}} = 0.707 m away, and potentials are scalars, so just add four equal terms. V=4Gml/2=42Gml=5.657×6.67×1011×1000=3.77×107 J/kgV = -\frac{4Gm}{l/\sqrt{2}} = -\frac{4\sqrt{2}\,Gm}{l} = -5.657 \times 6.67 \times 10^{-11} \times 1000 = -3.77 \times 10^{-7} \text{ J/kg}

  4. (c) Field at the centre. Each corner pulls with the same magnitude, and the diagonally opposite corner pulls equally in the opposite direction. gcentre=0\vec{g}_{centre} = 0

Final Answer: (a) 3.61×104-3.61 \times 10^{-4} J; (b) 3.77×107-3.77 \times 10^{-7} J/kg; (c) zero.

Takeaway: Six pairs for the energy, four terms for the potential, and a symmetry argument for the field. Three different questions about one picture, and only the first one involves pairs.

Example 5: An unequal triangle, assembled and dismantled

Masses of 100 kg, 200 kg and 300 kg sit at the corners of an equilateral triangle of side 1 m. Find the potential energy of the system, and the work an external agent must do to separate the three masses to infinity.

Solution:

  1. Three particles, three pairs. All three separations are the same, 1 m, so U=Ga(m1m2+m2m3+m3m1)U = -\frac{G}{a}\left(m_1m_2 + m_2m_3 + m_3m_1\right)

  2. The products. m1m2=2×104,m2m3=6×104,m3m1=3×104m_1m_2 = 2 \times 10^{4}, \qquad m_2m_3 = 6 \times 10^{4}, \qquad m_3m_1 = 3 \times 10^{4} sum=1.1×105 kg2\text{sum} = 1.1 \times 10^{5} \text{ kg}^2

  3. Evaluate. U=6.67×1011×1.1×1051=7.34×106 JU = -\frac{6.67 \times 10^{-11} \times 1.1 \times 10^{5}}{1} = -7.34 \times 10^{-6} \text{ J}

  4. Work to dismantle. The final state is complete separation, where U=0U = 0 by our convention. Wext=UfinalUinitial=0(7.34×106)=+7.34×106 JW_{ext} = U_{final} - U_{initial} = 0 - \left(-7.34 \times 10^{-6}\right) = +7.34 \times 10^{-6} \text{ J}

Final Answer: U=7.34×106U = -7.34 \times 10^{-6} J; the work needed to pull them apart is +7.34×106+7.34 \times 10^{-6} J, about 7.3 microjoules.

Takeaway: Work to dismantle is always +U+\lvert U \rvert, and work to assemble is UU itself. The zero at infinity is what makes the two numbers mirror images.

Example 6: A square with unequal masses — potential and field

Masses mm, 2m2m, 3m3m and 4m4m are placed in that order around the corners of a square of side ll. Find the gravitational potential and the gravitational field at the centre.

Solution:

  1. Set up. Label the corners A(m)A(m), B(2m)B(2m), C(3m)C(3m), D(4m)D(4m) going round, and let PP be the centre. Every corner is a distance d=l2d = \frac{l}{\sqrt{2}} from PP.

  2. Potential — a scalar sum, so the geometry does not matter at all. VP=Gd(m+2m+3m+4m)=10Gml/2=102GmlV_P = -\frac{G}{d}\left(m + 2m + 3m + 4m\right) = -\frac{10Gm}{l/\sqrt{2}} = -\frac{10\sqrt{2}\,Gm}{l} VP=14.14GmlV_P = -14.14\,\frac{Gm}{l}

  3. Field — now the geometry matters. Take the diagonals in turn. Along ACAC the pulls from mm and 3m3m oppose, leaving a net effect equal to a mass 2m2m sitting at CC: gAC=G(2m)d2=G(2m)l2/2=4Gml2directed from P towards Cg_{AC} = \frac{G(2m)}{d^{2}} = \frac{G(2m)}{l^{2}/2} = \frac{4Gm}{l^{2}} \quad \text{directed from } P \text{ towards } C

  4. Along BDBD, the pulls from 2m2m and 4m4m leave a net equal to 2m2m at DD, so the same magnitude 4Gml2\frac{4Gm}{l^{2}}, directed from PP towards DD.

  5. Add the two. PCPC and PDPD are perpendicular, so gP=(4Gml2)2+(4Gml2)2=42Gml2=5.66Gml2g_P = \sqrt{\left(\frac{4Gm}{l^{2}}\right)^{2} + \left(\frac{4Gm}{l^{2}}\right)^{2}} = \frac{4\sqrt{2}\,Gm}{l^{2}} = 5.66\,\frac{Gm}{l^{2}} and it points along the bisector of PCPC and PDPD, that is, towards the midpoint of the side CDCD that carries the two heaviest masses.

Final Answer: VP=102GmlV_P = -\frac{10\sqrt{2}\,Gm}{l} and gP=42Gml2g_P = \frac{4\sqrt{2}\,Gm}{l^{2}}, pointing towards the midpoint of the side joining 3m3m and 4m4m.

Takeaway: The potential needed one line and no diagram; the field needed a diagram and two vector steps. That difference is the entire practical argument for learning potential.

Example 7: On the axis of a ring

A thin ring of mass 200 kg and radius 3 m lies in a plane. Find the gravitational potential and the gravitational field at a point on the axis 4 m from the centre. Where on the axis is the field strongest?

Solution:

  1. The distance from every element to the point. a2+x2=32+42=5 m\sqrt{a^{2}+x^{2}} = \sqrt{3^{2}+4^{2}} = 5 \text{ m}

  2. Potential. Every mass element is exactly 5 m away, so the scalar sum is immediate. V=GMa2+x2=6.67×1011×2005=2.67×109 J/kgV = -\frac{GM}{\sqrt{a^{2}+x^{2}}} = -\frac{6.67 \times 10^{-11} \times 200}{5} = -2.67 \times 10^{-9} \text{ J/kg}

  3. Field. Differentiate, or quote the axial result: gx=GMx(a2+x2)3/2=6.67×1011×200×453=5.336×108125=4.27×1010 m/s2g_x = \frac{GMx}{\left(a^{2}+x^{2}\right)^{3/2}} = \frac{6.67 \times 10^{-11} \times 200 \times 4}{5^{3}} = \frac{5.336 \times 10^{-8}}{125} = 4.27 \times 10^{-10} \text{ m/s}^2 directed along the axis, towards the centre of the ring.

  4. Where is it strongest? Set dgxdx=0\frac{dg_x}{dx} = 0; the maximum sits at x=a2=31.414=2.12 mx = \frac{a}{\sqrt{2}} = \frac{3}{1.414} = 2.12 \text{ m} gmax=2GM33a2=2×1.334×1083×1.732×9=5.71×1010 m/s2g_{max} = \frac{2GM}{3\sqrt{3}\,a^{2}} = \frac{2 \times 1.334 \times 10^{-8}}{3 \times 1.732 \times 9} = 5.71 \times 10^{-10} \text{ m/s}^2

Final Answer: V=2.67×109V = -2.67 \times 10^{-9} J/kg, g=4.27×1010g = 4.27 \times 10^{-10} m/s2^2 towards the ring; the field peaks at x=2.12x = 2.12 m with gmax=5.71×1010g_{max} = 5.71 \times 10^{-10} m/s2^2.

Takeaway: At the centre of the ring the potential is deepest and the field is exactly zero. Move outwards and the field climbs to a peak at a2\frac{a}{\sqrt{2}} before falling away — the classic shape of a curve whose slope, not whose value, is the field.

Example 8: From potential to field, in a plane

In a certain region the gravitational potential is V=(5x+3y)V = -(5x + 3y) J/kg, with xx and yy in metres. Find the gravitational field there.

Solution:

  1. Differentiate with respect to each coordinate. The field is minus the rate of change of VV along each direction. gx=Vx=x[(5x+3y)]=+5 m/s2g_x = -\frac{\partial V}{\partial x} = -\frac{\partial}{\partial x}\left[-(5x+3y)\right] = +5 \text{ m/s}^2 gy=Vy=+3 m/s2g_y = -\frac{\partial V}{\partial y} = +3 \text{ m/s}^2

  2. Assemble the vector. g=5i^+3j^\vec{g} = 5\hat{i} + 3\hat{j}

  3. Magnitude and direction. g=52+32=34=5.83 m/s2\lvert \vec{g} \rvert = \sqrt{5^{2}+3^{2}} = \sqrt{34} = 5.83 \text{ m/s}^2 at tan1(35)=31.0°\tan^{-1}\left(\frac{3}{5}\right) = 31.0° above the xx-axis.

  4. Check the sense. VV decreases as xx and yy increase, and the field points the way VV decreases — towards larger xx and yy. Consistent.

Final Answer: g=5i^+3j^\vec{g} = 5\hat{i} + 3\hat{j}, of magnitude 5.835.83 m/s2^2 at 31.0°31.0° to the xx-axis.

Takeaway: The field always points downhill in potential. When VV is given as a function of position, you never need to know what masses produced it.

Example 9: The neutral point between the Earth and the Moon

The Moon has mass 7.34×10227.34 \times 10^{22} kg and its centre is 3.84×1083.84 \times 10^{8} m from the Earth's centre. Find the point on the line joining them where the gravitational field vanishes, and the gravitational potential there.

Solution:

  1. Set up. Let the point be a distance xx from the Earth's centre, so it is dxd - x from the Moon's. Equate the two field magnitudes. GMEx2=GMM(dx)2dxx=MMME\frac{GM_E}{x^{2}} = \frac{GM_M}{(d-x)^{2}} \qquad \Longrightarrow \qquad \frac{d-x}{x} = \sqrt{\frac{M_M}{M_E}}

  2. The mass ratio. 7.34×10225.97×1024=0.01230=0.1109\sqrt{\frac{7.34 \times 10^{22}}{5.97 \times 10^{24}}} = \sqrt{0.01230} = 0.1109

  3. Solve. x=d1+0.1109=3.84×1081.1109=3.46×108 mx = \frac{d}{1 + 0.1109} = \frac{3.84 \times 10^{8}}{1.1109} = 3.46 \times 10^{8} \text{ m} That is 90% of the way to the Moon, leaving dx=3.83×107d - x = 3.83 \times 10^{7} m, about 38 300 km, still to go.

  4. Potential there — and this is the point of the question. Potentials are scalars, so they simply add; there is no cancellation. V=GMExGMMdx=3.982×10143.46×1084.896×10123.83×107V = -\frac{GM_E}{x} - \frac{GM_M}{d-x} = -\frac{3.982 \times 10^{14}}{3.46 \times 10^{8}} - \frac{4.896 \times 10^{12}}{3.83 \times 10^{7}} V=1.152×1061.278×105=1.28×106 J/kgV = -1.152 \times 10^{6} - 1.278 \times 10^{5} = -1.28 \times 10^{6} \text{ J/kg}

Final Answer: the null point is 3.46×1083.46 \times 10^{8} m from the Earth's centre; the potential there is 1.28×106-1.28 \times 10^{6} J/kg, which is emphatically not zero.

Takeaway: Zero field and zero potential are different conditions and they almost never coincide. Fields are vectors and can cancel; potentials from ordinary masses are all negative and can only pile up.

Example 10: Moving a mass outwards

Calculate the work required to move a 5 kg body from a point 2RE2R_E from the Earth's centre to a point 4RE4R_E from the centre.

Solution:

  1. Initial and final potential energies. Ui=GMEm2RE,Uf=GMEm4REU_i = -\frac{GM_Em}{2R_E}, \qquad U_f = -\frac{GM_Em}{4R_E}

  2. Subtract. Wext=UfUi=GMEm(12RE14RE)=GMEm4REW_{ext} = U_f - U_i = GM_Em\left(\frac{1}{2R_E} - \frac{1}{4R_E}\right) = \frac{GM_Em}{4R_E}

  3. Numbers. Wext=(3.982×1014)(5)4×6.37×106=1.991×10152.548×107=7.81×107 JW_{ext} = \frac{(3.982 \times 10^{14})(5)}{4 \times 6.37 \times 10^{6}} = \frac{1.991 \times 10^{15}}{2.548 \times 10^{7}} = 7.81 \times 10^{7} \text{ J}

  4. Sign check. The body ends up further out, so UU has increased, so an external agent has paid. Positive, as it must be. Gravity meanwhile did 7.81×107-7.81 \times 10^{7} J of work.

Final Answer: 7.81×1077.81 \times 10^{7} J of work by the external agent.

Takeaway: Doubling the distance does not halve the job. Going from 2RE2R_E to 4RE4R_E costs GMEm4RE\frac{GM_Em}{4R_E}, while going from the surface to 2RE2R_E costs twice as much — most of the price is paid in the first few thousand kilometres.

Example 11: Released from three Earth radii

A body is released from rest at a distance 3RE3R_E from the Earth's centre. With what speed does it reach the surface? Ignore the atmosphere and the Earth's rotation. Compare with the schoolbook answer 2gh\sqrt{2gh}.

Solution:

  1. Energy conservation, with the exact potential energy. No kinetic energy at the start. 0GMEm3RE=12mv2GMEmRE0 - \frac{GM_Em}{3R_E} = \frac{1}{2}mv^{2} - \frac{GM_Em}{R_E}

  2. Cancel mm and rearrange. 12v2=GME(1RE13RE)=2GME3REv=4GME3RE\frac{1}{2}v^{2} = GM_E\left(\frac{1}{R_E} - \frac{1}{3R_E}\right) = \frac{2GM_E}{3R_E} \qquad \Longrightarrow \qquad v = \sqrt{\frac{4GM_E}{3R_E}}

  3. Evaluate. v=4×3.982×10143×6.37×106=8.335×107=9.13×103 m/sv = \sqrt{\frac{4 \times 3.982 \times 10^{14}}{3 \times 6.37 \times 10^{6}}} = \sqrt{8.335 \times 10^{7}} = 9.13 \times 10^{3} \text{ m/s}

  4. The naive answer. With h=2REh = 2R_E and a constant g=9.8g = 9.8 m/s2^2, 2gh=2×9.8×1.274×107=1.58×104 m/s\sqrt{2gh} = \sqrt{2 \times 9.8 \times 1.274 \times 10^{7}} = 1.58 \times 10^{4} \text{ m/s} which is 73% too large, because gg is nothing like 9.8 m/s2^2 for most of that fall.

Final Answer: 9.139.13 km/s. The constant-gg estimate of 15.815.8 km/s is badly wrong.

Takeaway: Falls that start high need the real potential energy. Section 6 takes the same calculation to its limit and asks what happens when the body is released from infinitely far away.

Example 12: Pulling two masses apart

Two particles of masses 10 kg and 20 kg are 1 m apart. How much work must be done to increase their separation to 4 m?

Solution:

  1. One pair, so one term at each end. Ui=Gm1m2ri=6.67×1011×2001=1.334×108 JU_i = -\frac{G m_1 m_2}{r_i} = -\frac{6.67 \times 10^{-11} \times 200}{1} = -1.334 \times 10^{-8} \text{ J} Uf=6.67×1011×2004=3.335×109 JU_f = -\frac{6.67 \times 10^{-11} \times 200}{4} = -3.335 \times 10^{-9} \text{ J}

  2. The work is the change. Wext=UfUi=3.335×109+1.334×108=1.00×108 JW_{ext} = U_f - U_i = -3.335 \times 10^{-9} + 1.334 \times 10^{-8} = 1.00 \times 10^{-8} \text{ J}

  3. Note what it is not. It is not Gm1m24\frac{Gm_1m_2}{4} or Gm1m23\frac{Gm_1m_2}{3} — the separation appears as a reciprocal, so differences of reciprocals are what count. Here 1114=34\frac{1}{1} - \frac{1}{4} = \frac{3}{4}, giving 34×1.334×108\frac{3}{4} \times 1.334 \times 10^{-8}.

Final Answer: 1.00×1081.00 \times 10^{-8} J, about 10 nanojoules.

Takeaway: To go all the way to infinity would cost only 1.334×1081.334 \times 10^{-8} J — a third as much again. Three quarters of the total price of separating two masses is paid in going from rr to 4r4r.