Can You Throw Something Away For Good?

Throw a stone up and it comes back. Throw it harder and it comes back from higher up. A cannon does better, a rocket better still. So a natural question: is there a speed at which it simply never returns?

There is, and the answer takes about four lines. It is not a dynamics problem at all — the force keeps changing all the way up, so chasing it with F=maF = ma is hopeless. It is an energy problem, and Section 5 has just given us the tool.

Setting up the accounts

Launch a body of mass mm from the Earth's surface with speed vv. With the zero of potential energy at infinity, its total mechanical energy at the moment of launch is

E=K+U=12mv2GMEmREE = K + U = \frac{1}{2}mv^{2} - \frac{GM_Em}{R_E}

Kinetic energy is positive, potential energy is negative, and gravity is conservative, so this total EE does not change for the rest of the flight (ignore the atmosphere for now).

Three radial launches from Earth and the kinetic, potential and total energy bars

Now ask what has to be true for the body to get infinitely far away. Out there U0U \to 0, and its kinetic energy 12mvf2\frac{1}{2}mv_f^{2} cannot be negative. So the energy it arrives with is

E()=12mvf2+0  0E(\infty) = \frac{1}{2}mv_f^{2} + 0 \ \geq\ 0

Energy is conserved, so the energy it left with must have been 0\geq 0 too. That single inequality is the whole of this section.

Key Point — the escape condition: 12mv2GMEmRE  0\frac{1}{2}mv^{2} - \frac{GM_Em}{R_E} \ \geq\ 0 A body escapes if and only if its total mechanical energy is zero or positive, with the zero of potential energy taken at infinity. Negative total energy means it is bound and must come back; zero is the borderline; positive means it escapes and still has speed left over.

The escape speed

The slowest launch that satisfies the condition is the one that turns it into an equality:

12mve2=GMEmREve=2GMERE\frac{1}{2}mv_e^{2} = \frac{GM_Em}{R_E} \qquad \Longrightarrow \qquad v_e = \sqrt{\frac{2GM_E}{R_E}}

The mass mm has cancelled. We shall come back to that in a moment, because it is the most quoted feature of the result.

Since g=GMERE2g = \frac{GM_E}{R_E^{2}}, we can trade GMEGM_E for gRE2gR_E^{2} and get a second form that needs no knowledge of GG or MEM_E at all:

Key Point — escape speed: ve=2GMERE=2gREv_e = \sqrt{\frac{2GM_E}{R_E}} = \sqrt{2gR_E} Both forms are examinable. Use the first when you are given GG and the planet's mass, and the second when you are given the planet's surface gravity.

The number

With 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 and RE=6.37×106R_E = 6.37 \times 10^{6} m:

ve=2×3.982×10146.37×106=1.250×108=1.118×104 m/sv_e = \sqrt{\frac{2 \times 3.982 \times 10^{14}}{6.37 \times 10^{6}}} = \sqrt{1.250 \times 10^{8}} = 1.118 \times 10^{4} \text{ m/s}

and by the other route, with g=9.8g = 9.8 m/s2^2:

ve=2×9.8×6.37×106=1.249×108=1.117×104 m/sv_e = \sqrt{2 \times 9.8 \times 6.37 \times 10^{6}} = \sqrt{1.249 \times 10^{8}} = 1.117 \times 10^{4} \text{ m/s}

Key Point: The escape speed at the Earth's surface is about 11.2 km/s, or roughly 40 000 km/h. Memorise it. It is the single most quoted number in the chapter.

What "just escaping" looks like

A body launched at exactly vev_e has E=0E = 0. Its speed at a distance rr from the centre is v=veRErv = v_e\sqrt{\frac{R_E}{r}}, which keeps falling but never reaches zero at any finite distance. It arrives at infinity with precisely zero speed, after an infinite time. Launch it a whisker slower and it turns round — very far out, but it turns round. Launch it a whisker faster and it sails away with speed to spare.

[Board Important] The derivation is a standard three-mark question. Write down the total energy at launch, argue that the energy at infinity cannot be negative, set E0E \geq 0, state the zero-of-potential convention, and solve. Skipping the convention costs a mark.

What It Depends On, and What It Emphatically Does Not

Look at the answer again:

ve=2GMEREv_e = \sqrt{\frac{2GM_E}{R_E}}

Three things are in it: GG, the mass of the planet, and the radius of the planet. Three things are conspicuously not in it, and each absence is a favourite exam question.

It does not depend on the mass of the projectile

The mm cancelled in the very first step, because kinetic energy and gravitational potential energy are both proportional to mm. A grain of sand, a cricket ball and a fully fuelled rocket all need the same 11.2 km/s.

Key Point: vev_e is independent of the mass of the escaping body. A heavier body needs more energy to escape — the energy needed is GMEmRE\frac{GM_Em}{R_E}, which does scale with mm — but it needs the same speed.

Keep those two sentences apart in your head. "Does a heavier rocket need a bigger escape speed?" No. "Does it need more fuel?" Yes, proportionally.

It does not depend on the direction of launch

This one surprises people. Fire the projectile straight up, at 45°45°, or almost horizontally — as long as it clears the ground and the atmosphere, 11.2 km/s is enough.

The reason is that energy is a scalar. The condition 12mv2GMEmRE0\frac{1}{2}mv^{2} - \frac{GM_Em}{R_E} \geq 0 contains v2v^{2}, the square of the speed, and nothing about direction at all. Gravity is a central force, so no matter which way the body sets off, the same energy sum governs whether it can reach infinity.

Key Point: vev_e is independent of the direction of projection. This is why it is properly called escape speed, not escape velocity, even though you will hear the second name constantly.

Two honest footnotes. First, a horizontal launch from the ground would plough through the atmosphere and hit a mountain, so in practice rockets go up first and turn later — that is aerodynamics, not gravitation. Second, launching eastward from the equator does help a little, because the surface is already moving east at ωRE=464\omega R_E = 464 m/s, about 4.2% of vev_e. That is a gift from the Earth's rotation, not a change in the escape speed itself, and it is why launch sites cluster near the equator.

It does not depend on where the body ends up going

The condition is only about reaching infinity. Whether the body ends up drifting to Mars, to another star, or nowhere in particular is a separate question.

It does depend on the planet: on MM and on RR

veMRv_e \propto \sqrt{\frac{M}{R}}

so a more massive planet is harder to leave and a larger one is easier, and the two effects fight each other. For bodies of the same mean density ρ\rho, substituting M=43πR3ρM = \frac{4}{3}\pi R^{3}\rho gives a neat alternative:

ve=R8πGρ3veRρv_e = R\sqrt{\frac{8\pi G\rho}{3}} \qquad \Longrightarrow \qquad v_e \propto R\sqrt{\rho}

Two planets made of the same stuff, one twice as wide, and the bigger one has twice the escape speed. This is the cleanest way to handle any question phrased in terms of density.

The relation to orbital speed

There is one more relation worth carrying, even though its other half belongs to the next section. A satellite skimming just above the Earth's surface moves at the orbital speed vo=GMEREv_o = \sqrt{\frac{GM_E}{R_E}}, which works out to 7.917.91 km/s. Compare:

Key Point: ve=2GMERE=2GMERE=2vov_e = \sqrt{\frac{2GM_E}{R_E}} = \sqrt{2}\,\sqrt{\frac{GM_E}{R_E}} = \sqrt{2}\,v_o The escape speed from a planet's surface is 21.414\sqrt{2} \approx 1.414 times the speed of a satellite in a surface-skimming orbit. Numerically, 2×7.91=11.18\sqrt{2} \times 7.91 = 11.18 km/s.

Section 7 derives vov_o properly from the circular-orbit condition; here it is quoted only so that you can see the factor of 2\sqrt{2}, which examiners adore. Note carefully that this relation holds for an orbit at the surface. For a satellite at height hh the comparison has to be made at the same radius, which Section 8 handles when it does the full energy accounting.

[NEET Important] Three one-line facts to have ready: escape speed does not depend on the mass of the body; does not depend on the direction of projection; and equals 2\sqrt{2} times the surface orbital speed.

Other Worlds, and Why the Moon Has No Air

Nothing in the derivation was specific to the Earth. For any spherical body of mass MM and radius RR,

ve=2GMR=2gRv_e = \sqrt{\frac{2GM}{R}} = \sqrt{2gR}

where gg now means the surface gravity of that body. Feed in the numbers and the solar system spreads out over three orders of magnitude.

Escape speeds across the solar system, and Earth beside the Moon to scale

Body Mass (kg) Radius (m) Surface gg (m/s2^2) vev_e (km/s)
Ceres 9.4×10209.4 \times 10^{20} 4.70×1054.70 \times 10^{5} 0.28 0.52
Pluto 1.31×10221.31 \times 10^{22} 1.19×1061.19 \times 10^{6} 0.62 1.21
Moon 7.34×10227.34 \times 10^{22} 1.74×1061.74 \times 10^{6} 1.62 2.37
Titan 1.35×10231.35 \times 10^{23} 2.58×1062.58 \times 10^{6} 1.36 2.64
Mercury 3.30×10233.30 \times 10^{23} 2.44×1062.44 \times 10^{6} 3.70 4.25
Mars 6.42×10236.42 \times 10^{23} 3.39×1063.39 \times 10^{6} 3.73 5.03
Venus 4.87×10244.87 \times 10^{24} 6.05×1066.05 \times 10^{6} 8.87 10.36
Earth 5.97×10245.97 \times 10^{24} 6.37×1066.37 \times 10^{6} 9.81 11.18
Uranus 8.68×10258.68 \times 10^{25} 2.54×1072.54 \times 10^{7} 8.97 21.35
Neptune 1.02×10261.02 \times 10^{26} 2.46×1072.46 \times 10^{7} 11.24 23.52
Saturn 5.68×10265.68 \times 10^{26} 6.03×1076.03 \times 10^{7} 10.42 35.45
Jupiter 1.90×10271.90 \times 10^{27} 7.15×1077.15 \times 10^{7} 24.79 59.54
Sun 1.99×10301.99 \times 10^{30} 6.96×1086.96 \times 10^{8} 274 617.6

Read a few rows against each other and the M/R\sqrt{M/R} competition shows up plainly. Mercury and Mars have nearly the same surface gravity, yet Mars has the higher escape speed, because it is the bigger ball. Uranus has a lower surface gravity than the Earth and an escape speed nearly twice as large, for the same reason. Surface gravity and escape speed do not rank worlds in the same order.

The Moon's missing atmosphere

Here is where escape speed stops being an exam number and starts explaining something you can see.

Gas molecules are not all moving at the same speed, but the kinetic theory you will meet in a later chapter gives their typical speed as the root-mean-square speed

vrms=3RTMmolarv_{rms} = \sqrt{\frac{3RT}{M_{molar}}}

with R=8.314R = 8.314 J/mol/K the gas constant, TT the absolute temperature and MmolarM_{molar} the molar mass in kilograms per mole. Light molecules move faster; hot gas moves faster.

Molecular speeds of five gases against Earth and Moon retention thresholds

At 300 K:

Gas Molar mass (g/mol) vrmsv_{rms} at 300 K (m/s)
Hydrogen, H2H_2 2 1934
Helium, He 4 1368
Nitrogen, N2N_2 28 517
Oxygen, O2O_2 32 484
Carbon dioxide, CO2CO_2 44 412

Now compare. The Moon's escape speed is 2372 m/s, so hydrogen molecules at 300 K are already moving at 82% of it — and that is only the average; the fastest molecules in the distribution are well past it. Every one of the five gases above is a substantial fraction of the Moon's escape speed, so over geological time the fast tail of every distribution leaks away, and the leak never stops.

The Earth's escape speed is 11 181 m/s. Nitrogen at 517 m/s is under 5% of it. Nitrogen is going nowhere.

Key Point — the retention rule of thumb: A body holds on to a gas indefinitely only if vrmsv_{rms} is well below the escape speed — the usual working criterion is vrms<ve6v_{rms} < \frac{v_e}{6}, because it is the fast tail of the distribution that escapes, not the average molecule.

  • Earth: ve6=1864\frac{v_e}{6} = 1864 m/s. Nitrogen, oxygen and carbon dioxide are far below it and are kept. Hydrogen at 1934 m/s is above it, which is exactly why the Earth has almost no free hydrogen left in its atmosphere, and why helium leaks away too.
  • Moon: ve6=395\frac{v_e}{6} = 395 m/s. Every common gas exceeds it. The Moon keeps nothing.

That is the answer to a question every syllabus asks: the Moon has no atmosphere because its escape speed, 2.4 km/s, is too small compared with the speeds of gas molecules at its surface temperature. Jupiter, at the other end, has an escape speed of 59.5 km/s and has held on even to hydrogen and helium — which is why it is made mostly of them.

[JEE Tip] If a question asks for the temperature at which a gas would escape from a given body, set vrms=vev_{rms} = v_e and solve for TT: T=Mmolarve23RT = \frac{M_{molar}v_e^{2}}{3R}. For nitrogen on the Moon that gives about 6300 K, which sounds comfortably far off — until you remember that the criterion is really ve6\frac{v_e}{6}, not vev_e, and the corresponding temperature drops by a factor of 36.

Leaving From a Height, and Falling In From Far Away

Two variations account for most of the harder questions in this section, and they turn out to be the same calculation read in two directions.

Escaping from a height hh

Nothing in the derivation demanded that the launch happen at the surface. Start instead at a distance r=RE+hr = R_E + h from the centre. The energy condition reads

12mv2GMEmRE+h  0\frac{1}{2}mv^{2} - \frac{GM_Em}{R_E+h} \ \geq\ 0

Key Point — escape speed from a height hh: ve(h)=2GMERE+h=ve1+hREv_e(h) = \sqrt{\frac{2GM_E}{R_E+h}} = \frac{v_e}{\sqrt{1 + \frac{h}{R_E}}} Higher up, the potential energy pit is shallower, so less speed is needed. At h=REh = R_E the requirement is ve2=7.91\frac{v_e}{\sqrt{2}} = 7.91 km/s; at 1000 km it is 10.40 km/s; at 300 km, a typical low orbit, it is still 10.93 km/s.

Escape speed falling with launch height beside impact speed rising with drop distance

Notice how gently the requirement falls off. Climbing 300 km — higher than most satellites — buys you barely 2%. Gravity's grip weakens slowly because the potential goes as 1r\frac{1}{r}, not 1r2\frac{1}{r^{2}}.

How high does a sub-escape launch go?

If v<vev < v_e the body must come back, and energy conservation says exactly where it turns round. At the highest point the speed is zero, so

12mv2GMEmRE=0GMEmrmax\frac{1}{2}mv^{2} - \frac{GM_Em}{R_E} = 0 - \frac{GM_Em}{r_{max}}

Solving, and writing v=fvev = f v_e for the launch speed as a fraction of the escape speed:

Key Point — the turning point: rmax=RE1v2ve2=RE1f2sohmax=RE(f21f2)r_{max} = \frac{R_E}{1 - \frac{v^{2}}{v_e^{2}}} = \frac{R_E}{1-f^{2}} \qquad\text{so}\qquad h_{max} = R_E\left(\frac{f^{2}}{1-f^{2}}\right) Half the escape speed gets you only to r=4RE3r = \frac{4R_E}{3}, a height of RE3=2123\frac{R_E}{3} = 2123 km. Seventy per cent of it reaches 1.96RE1.96R_E. The formula blows up as f1f \to 1, which is the mathematics telling you the body no longer turns round at all.

Read that first number again. Half the escape speed does not get you half way to escaping — it gets you a third of an Earth radius up. The energy scales as v2v^{2}, and the last few per cent of speed buys almost all of the distance.

Falling in from far away

Now run the film backwards. A body starts at rest a distance rr from the Earth's centre and falls. What speed does it have when it reaches the surface? Same equation, opposite direction:

0GMEmr=12mv2GMEmRE0 - \frac{GM_Em}{r} = \frac{1}{2}mv^{2} - \frac{GM_Em}{R_E}

Key Point — impact speed after a drop from rest at distance rr: vhit=2GME(1RE1r)=ve1RErv_{hit} = \sqrt{2GM_E\left(\frac{1}{R_E} - \frac{1}{r}\right)} = v_e\sqrt{1 - \frac{R_E}{r}} Dropped from 5RE5R_E it arrives at 10.00 km/s; from 10RE10R_E, at 10.61 km/s; and in the limit rr \to \infty, at exactly ve=11.2v_e = 11.2 km/s.

That limit is worth pausing over.

Key Point: A body released from rest at a very great distance strikes the Earth at the escape speed, 11.2 km/s. It could not be otherwise: escaping and falling in are the same journey run in opposite directions, and energy conservation does not care which way time is running.

So 11.2 km/s is not just the speed you need to leave — it is also the speed at which anything arrives if it fell in from far away with no initial speed. Meteoroids that merely drift into the Earth's grip hit the atmosphere at roughly this speed; ones that were already moving relative to the Earth hit harder.

The two curves in the figure above are reflections of each other, and they are locked together by

ve(r)2+vhit(r)2=2GMERE=ve2v_e(r)^{2} + v_{hit}(r)^{2} = \frac{2GM_E}{R_E} = v_e^{2}

a constant. Where one is large the other is small, and both meet at r=2REr = 2R_E, where each equals ve2=7.91\frac{v_e}{\sqrt{2}} = 7.91 km/s.

[JEE Tip] Every problem in this block is the same three-line sum: write Ki+Ui=Kf+UfK_i + U_i = K_f + U_f with U=GMmrU = -\frac{GMm}{r}, put a zero wherever the problem gives you "at rest" or "just escapes", and solve. Do not memorise four formulas; memorise one method.

The Shortlist, and the Traps

Everything worth memorising

Quantity Formula Earth's value
Escape speed at the surface ve=2GMR=2gRv_e = \sqrt{\frac{2GM}{R}} = \sqrt{2gR} 11.2 km/s
Escape condition total energy E=K+U0E = K + U \geq 0, zero of UU at infinity
In terms of density ve=R8πGρ3v_e = R\sqrt{\frac{8\pi G\rho}{3}}, so veRρv_e \propto R\sqrt{\rho}
Escape speed from height hh ve(h)=2GMR+hv_e(h) = \sqrt{\frac{2GM}{R+h}} 7.91 km/s at h=REh = R_E
Relation to surface orbital speed ve=2vov_e = \sqrt{2}\,v_o 2×7.91\sqrt{2} \times 7.91 km/s
Height reached if v=fvev = fv_e, f<1f<1 rmax=R1f2r_{max} = \frac{R}{1-f^{2}} 4RE3\frac{4R_E}{3} for f=12f = \frac{1}{2}
Speed left far away if v>vev > v_e v=v2ve2v_\infty = \sqrt{v^{2} - v_e^{2}} 12.5 km/s if v=1.5vev = 1.5v_e
Impact speed dropped from rest at rr vhit=ve1Rrv_{hit} = v_e\sqrt{1 - \frac{R}{r}} 11.2 km/s from very far away
Energy needed to escape, for mass mm GMmR=12mve2\frac{GMm}{R} = \frac{1}{2}mv_e^{2} 6.25×1076.25 \times 10^{7} J per kg
Gas retention criterion vrms<ve6v_{rms} < \frac{v_e}{6} ve6=1864\frac{v_e}{6} = 1864 m/s

Six traps

Trap 1 — thinking a heavier body needs a bigger escape speed. It does not. It needs more energy, and therefore more fuel, but the same speed. The clean statement: speed independent of mm, energy proportional to mm.

Trap 2 — thinking the direction matters. It does not, because the energy condition contains v2v^{2} and no angle. A body flung at 45°45° at 11.2 km/s escapes just as surely as one fired straight up.

Trap 3 — using 2gh\sqrt{2gh} or mghmgh anywhere in this section. Every distance here is comparable with RER_E, so constant-gg formulas are worthless. Section 5 measured the damage: at h=REh = R_E, mghmgh is 100% too large.

Trap 4 — confusing vev_e with vov_o, or applying ve=2vov_e = \sqrt{2}v_o at the wrong radius. The relation compares two speeds at the same distance from the centre. Compare the escape speed from a height with the orbital speed at that same height, never with the surface orbital speed.

Trap 5 — forgetting that escape speed changes with the planet. 2gR\sqrt{2gR} needs the surface gravity of that body. Putting 9.8 m/s2^2 into a Moon problem is the commonest single error in this section.

Trap 6 — reading "escape velocity" as a vector. It is a speed. The name is historical and everybody uses it, but a question asking for its "direction" is a trick.

What comes next

The escape condition, E0E \geq 0, is one half of a bigger picture. Section 7 works out what a body does when its energy is negative and it is moving sideways rather than radially — it goes into orbit — and Section 8 puts KK, UU and EE together for that orbit and shows that escape is simply the case where the total energy has been raised to zero. The energy needed to do that raising has a name, binding energy, and it belongs to Section 8.

[Board Important] The three-mark version of this section is: state the energy condition, derive ve=2GME/RE=2gREv_e = \sqrt{2GM_E/R_E} = \sqrt{2gR_E}, evaluate it as 11.2 km/s, and state that it is independent of the mass and the direction of projection. Everything else is variation on that.

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, g=9.8g = 9.8 m/s2^2 and the gas constant R=8.314R = 8.314 J/mol/K. The zero of potential energy is at infinity throughout.

Example 1: The escape speed from the Earth, two ways

Calculate the escape speed at the Earth's surface (a) from GG, MEM_E and RER_E, and (b) from gg and RER_E. Comment on the agreement.

Solution:

  1. (a) From the masses. ve=2GMERE=2×6.67×1011×5.97×10246.37×106v_e = \sqrt{\frac{2GM_E}{R_E}} = \sqrt{\frac{2 \times 6.67 \times 10^{-11} \times 5.97 \times 10^{24}}{6.37 \times 10^{6}}} =7.964×10146.37×106=1.250×108=1.118×104 m/s= \sqrt{\frac{7.964 \times 10^{14}}{6.37 \times 10^{6}}} = \sqrt{1.250 \times 10^{8}} = 1.118 \times 10^{4} \text{ m/s}

  2. (b) From the surface gravity. ve=2gRE=2×9.8×6.37×106=1.249×108=1.117×104 m/sv_e = \sqrt{2gR_E} = \sqrt{2 \times 9.8 \times 6.37 \times 10^{6}} = \sqrt{1.249 \times 10^{8}} = 1.117 \times 10^{4} \text{ m/s}

  3. Why they differ in the fourth figure. The two routes are algebraically identical, since g=GMERE2g = \frac{GM_E}{R_E^2}. The rounded value 9.8 m/s2^2 is slightly below the 9.819.81 m/s2^2 that these particular constants produce, and the 0.1% gap in gg becomes a 0.05% gap in vev_e, because of the square root.

Final Answer: ve11.2v_e \approx 11.2 km/s by both routes.

Takeaway: Pick whichever form matches the data you are given, and say which value of gg you used. Never mix 9.8 and 10 inside one problem.

Example 2: Leaving the Moon

The Moon has mass 7.34×10227.34 \times 10^{22} kg and radius 1.74×1061.74 \times 10^{6} m. Find its escape speed, and check it against 2gR\sqrt{2gR} using the Moon's surface gravity.

Solution:

  1. From the mass and radius. ve=2×6.67×1011×7.34×10221.74×106=9.792×10121.74×106v_e = \sqrt{\frac{2 \times 6.67 \times 10^{-11} \times 7.34 \times 10^{22}}{1.74 \times 10^{6}}} = \sqrt{\frac{9.792 \times 10^{12}}{1.74 \times 10^{6}}} =5.627×106=2.37×103 m/s= \sqrt{5.627 \times 10^{6}} = 2.37 \times 10^{3} \text{ m/s}

  2. Cross-check with the surface gravity. The Moon's surface gravity is gm=GMmRm2=4.896×10123.028×1012=1.62 m/s2g_m = \frac{GM_m}{R_m^{2}} = \frac{4.896 \times 10^{12}}{3.028 \times 10^{12}} = 1.62 \text{ m/s}^2 ve=2×1.62×1.74×106=5.638×106=2.37×103 m/sv_e = \sqrt{2 \times 1.62 \times 1.74 \times 10^{6}} = \sqrt{5.638 \times 10^{6}} = 2.37 \times 10^{3} \text{ m/s}

  3. Compare with the Earth. 11.182.37=4.7\frac{11.18}{2.37} = 4.7, so it is nearly five times easier to leave the Moon.

Final Answer: about 2.42.4 km/s, roughly one fifth of the Earth's value.

Takeaway: The Moon has 181\frac{1}{81} of the Earth's mass but only 13.7\frac{1}{3.7} of its radius, and veM/Rv_e \propto \sqrt{M/R} turns that into a factor of about 4.7 — not 81, and not 9.

Example 3: Leaving Jupiter

Jupiter has mass 1.90×10271.90 \times 10^{27} kg and radius 7.15×1077.15 \times 10^{7} m. Find its escape speed and express it as a multiple of the Earth's.

Solution:

  1. Substitute. ve=2×6.67×1011×1.90×10277.15×107=2.535×10177.15×107v_e = \sqrt{\frac{2 \times 6.67 \times 10^{-11} \times 1.90 \times 10^{27}}{7.15 \times 10^{7}}} = \sqrt{\frac{2.535 \times 10^{17}}{7.15 \times 10^{7}}} =3.545×109=5.95×104 m/s= \sqrt{3.545 \times 10^{9}} = 5.95 \times 10^{4} \text{ m/s}

  2. As a multiple of the Earth's. 59.511.18=5.32\frac{59.5}{11.18} = 5.32

  3. Where that factor comes from. Jupiter is 318 times as massive but 11.2 times as wide, so 31811.2=28.4=5.33\sqrt{\frac{318}{11.2}} = \sqrt{28.4} = 5.33. The two effects genuinely do fight, and mass wins.

Final Answer: ve=59.5v_e = 59.5 km/s, about 5.3 times the Earth's escape speed.

Takeaway: This is why Jupiter still has its hydrogen. At 59.5 km/s nothing in its atmosphere is going anywhere, which is a large part of why the giant planets look so different from the rocky ones.

Example 4: A heavier, wider planet

A planet has ten times the mass of the Earth and twice its radius. What is the escape speed at its surface?

Solution:

  1. Work with the ratio rather than the raw numbers. veplanetveEarth=Mp/RpME/RE=102=5=2.236\frac{v_e^{planet}}{v_e^{Earth}} = \sqrt{\frac{M_p/R_p}{M_E/R_E}} = \sqrt{\frac{10}{2}} = \sqrt{5} = 2.236

  2. Multiply. veplanet=2.236×11.18=25.0 km/sv_e^{planet} = 2.236 \times 11.18 = 25.0 \text{ km/s}

  3. Direct check. ve=2×6.67×1011×5.97×10251.274×107=6.251×108=2.50×104 m/sv_e = \sqrt{\frac{2 \times 6.67 \times 10^{-11} \times 5.97 \times 10^{25}}{1.274 \times 10^{7}}} = \sqrt{6.251 \times 10^{8}} = 2.50 \times 10^{4} \text{ m/s}

Final Answer: 25.025.0 km/s.

Takeaway: Ratios are faster and safer than substituting nine-digit constants. Whenever a problem gives you multiples of Earth values, work in multiples all the way to the last line.

Example 5: Same rock, bigger ball

A planet is made of the same material as the Earth, with the same mean density, but has twice the radius. Find its escape speed. Also find the escape speed of a body with the Earth's mass compressed to half the Earth's radius.

Solution:

  1. Rewrite vev_e in terms of density. Put M=43πR3ρM = \frac{4}{3}\pi R^{3}\rho into ve=2GMRv_e = \sqrt{\frac{2GM}{R}}: ve=2GR43πR3ρ=R8πGρ3v_e = \sqrt{\frac{2G}{R}\cdot\frac{4}{3}\pi R^{3}\rho} = R\sqrt{\frac{8\pi G\rho}{3}}

  2. So at fixed density, veRv_e \propto R. Doubling the radius doubles the escape speed. ve=2×11.18=22.4 km/sv_e = 2 \times 11.18 = 22.4 \text{ km/s}

  3. Sanity check on the Earth's mean density. ρE=ME43πRE3=5.97×10241.083×1021=5.51×103 kg/m3\rho_E = \frac{M_E}{\frac{4}{3}\pi R_E^{3}} = \frac{5.97 \times 10^{24}}{1.083 \times 10^{21}} = 5.51 \times 10^{3} \text{ kg/m}^3 and RE8πGρE3R_E\sqrt{\frac{8\pi G\rho_E}{3}} does return 1.118×1041.118 \times 10^{4} m/s, as it must.

  4. The compressed Earth. Same mass, half the radius, so ve1Rv_e \propto \frac{1}{\sqrt{R}}: ve=2×11.18=15.8 km/sv_e = \sqrt{2} \times 11.18 = 15.8 \text{ km/s}

Final Answer: 22.422.4 km/s for the twice-as-wide planet of the same density; 15.815.8 km/s for the Earth squeezed to half its radius.

Takeaway: veRρv_e \propto R\sqrt{\rho} at fixed density, but ve1Rv_e \propto \frac{1}{\sqrt{R}} at fixed mass. Read carefully which of the two a question is holding constant — they push in opposite directions.

Example 6: A pebble, a rocket, and a sideways launch

A 2 kg pebble and a 2000 kg rocket are both to escape from the Earth. (a) Compare the speeds they need. (b) Compare the energies. (c) Does firing at 45°45° to the vertical change either answer?

Solution:

  1. (a) Speeds. The escape condition, 12mv2GMEmRE\frac{1}{2}mv^{2} \geq \frac{GM_Em}{R_E}, has mm on both sides. Cancel it: ve=2GMERE=11.2 km/s for bothv_e = \sqrt{\frac{2GM_E}{R_E}} = 11.2 \text{ km/s for both}

  2. (b) Energies. The minimum energy is 12mve2=GMEmRE\frac{1}{2}mv_e^{2} = \frac{GM_Em}{R_E}, which is 6.25×1076.25 \times 10^{7} J per kilogram. Epebble=2×6.25×107=1.25×108 JE_{pebble} = 2 \times 6.25 \times 10^{7} = 1.25 \times 10^{8} \text{ J} Erocket=2000×6.25×107=1.25×1011 JE_{rocket} = 2000 \times 6.25 \times 10^{7} = 1.25 \times 10^{11} \text{ J} a factor of 1000 apart, exactly the mass ratio.

  3. (c) Direction. The condition contains v2v^{2}, the square of the speed, with no reference to direction, so 45°45° needs the same 11.2 km/s. (In practice a shallow launch would have to cross far more atmosphere, but that is drag, not gravity.)

Final Answer: same speed, 11.2 km/s, for both; energies of 1.25×1081.25 \times 10^{8} J and 1.25×10111.25 \times 10^{11} J; direction irrelevant.

Takeaway: "Same speed, different energy" is the sentence to write in an exam. Saying only "escape speed is independent of mass" without adding what does scale with mass usually loses the second mark.

Example 7: Only half as fast

A body is projected vertically upward from the Earth's surface with half the escape speed. How high does it rise?

Solution:

  1. Energy conservation, with zero speed at the top. 12mv2GMEmRE=GMEmrmax\frac{1}{2}mv^{2} - \frac{GM_Em}{R_E} = -\frac{GM_Em}{r_{max}}

  2. Put v=ve2v = \frac{v_e}{2}, so v2=ve24=142GMERE=GME2REv^{2} = \frac{v_e^{2}}{4} = \frac{1}{4}\cdot\frac{2GM_E}{R_E} = \frac{GM_E}{2R_E}. GME4REGMERE=GMErmax\frac{GM_E}{4R_E} - \frac{GM_E}{R_E} = -\frac{GM_E}{r_{max}}

  3. Tidy up. GMErmax=GMEREGME4RE=3GME4RErmax=4RE3\frac{GM_E}{r_{max}} = \frac{GM_E}{R_E} - \frac{GM_E}{4R_E} = \frac{3GM_E}{4R_E} \qquad \Longrightarrow \qquad r_{max} = \frac{4R_E}{3}

  4. Height above the surface. h=rmaxRE=RE3=6.37×1063=2.12×106 m=2123 kmh = r_{max} - R_E = \frac{R_E}{3} = \frac{6.37 \times 10^{6}}{3} = 2.12 \times 10^{6} \text{ m} = 2123 \text{ km}

Final Answer: it rises RE3\frac{R_E}{3}, about 2123 km.

Takeaway: Half the escape speed does not take you anywhere near half way. Energy goes as v2v^{2}, so half the speed is a quarter of the energy, and a quarter of the way out of a 1r\frac{1}{r} pit is barely off the ground.

Example 8: Fifty per cent over

A projectile leaves the Earth's surface at 1.51.5 times the escape speed. With what speed is it travelling when it is very far away?

Solution:

  1. Energy conservation between the surface and infinity, where U=0U = 0. 12mv2GMEmRE=12mv2\frac{1}{2}mv^{2} - \frac{GM_Em}{R_E} = \frac{1}{2}mv_\infty^{2}

  2. Recognise GMERE=ve22\frac{GM_E}{R_E} = \frac{v_e^{2}}{2} and cancel m2\frac{m}{2}. v2=v2ve2v_\infty^{2} = v^{2} - v_e^{2}

  3. Substitute v=1.5vev = 1.5v_e. v=(1.5)21 ve=1.25 ve=1.118vev_\infty = \sqrt{(1.5)^{2} - 1}\ v_e = \sqrt{1.25}\ v_e = 1.118\,v_e

  4. Evaluate. v=1.118×11.18=12.5 km/sv_\infty = 1.118 \times 11.18 = 12.5 \text{ km/s}

Final Answer: about 12.512.5 km/s, which is 1.1181.118 times the escape speed.

Takeaway: v2=v2ve2v_\infty^{2} = v^{2} - v_e^{2} is the whole of this family of problems. Half the launch speed's worth of energy was spent climbing out; only the surplus survives.

Example 9: Escaping from orbit height

What speed would a body need in order to escape from a point one Earth radius above the surface? Compare with the surface value.

Solution:

  1. The launch radius. At h=REh = R_E the distance from the centre is r=2REr = 2R_E.

  2. Apply the condition at that radius. ve(h)=2GMERE+h=2GME2RE=GMEREv_e(h) = \sqrt{\frac{2GM_E}{R_E+h}} = \sqrt{\frac{2GM_E}{2R_E}} = \sqrt{\frac{GM_E}{R_E}}

  3. Evaluate. ve(h)=3.982×10146.37×106=6.251×107=7.91×103 m/sv_e(h) = \sqrt{\frac{3.982 \times 10^{14}}{6.37 \times 10^{6}}} = \sqrt{6.251 \times 10^{7}} = 7.91 \times 10^{3} \text{ m/s}

  4. Compare. That is exactly ve2=11.181.414=7.91\frac{v_e}{\sqrt{2}} = \frac{11.18}{1.414} = 7.91 km/s, a saving of 29% for a climb of 6370 km.

Final Answer: 7.917.91 km/s, which is 12\frac{1}{\sqrt{2}} of the surface escape speed.

Takeaway: Height helps, but slowly. Because the potential goes as 1r\frac{1}{r}, you have to double your distance from the centre to cut the escape speed by only 29%.

Example 10: Dropped from far away

(a) With what speed does a body released from rest at a very great distance strike the Earth's surface? (b) What if it is released from rest at 5RE5R_E from the centre? Ignore the atmosphere.

Solution:

  1. (a) Energy conservation from infinity. At the start, both KK and UU are zero. 0=12mv2GMEmREv=2GMERE=ve0 = \frac{1}{2}mv^{2} - \frac{GM_Em}{R_E} \qquad \Longrightarrow \qquad v = \sqrt{\frac{2GM_E}{R_E}} = v_e v=11.2 km/sv = 11.2 \text{ km/s}

  2. (b) From a finite distance r=5REr = 5R_E. GMEm5RE=12mv2GMEmRE-\frac{GM_Em}{5R_E} = \frac{1}{2}mv^{2} - \frac{GM_Em}{R_E} 12v2=GME(1RE15RE)=4GME5RE\frac{1}{2}v^{2} = GM_E\left(\frac{1}{R_E} - \frac{1}{5R_E}\right) = \frac{4GM_E}{5R_E}

  3. Evaluate. v=8GME5RE=8×3.982×10145×6.37×106=1.000×108=1.00×104 m/sv = \sqrt{\frac{8GM_E}{5R_E}} = \sqrt{\frac{8 \times 3.982 \times 10^{14}}{5 \times 6.37 \times 10^{6}}} = \sqrt{1.000 \times 10^{8}} = 1.00 \times 10^{4} \text{ m/s}

  4. Or, more quickly, use vhit=ve1REr=11.1810.2=11.18×0.894=10.0v_{hit} = v_e\sqrt{1 - \frac{R_E}{r}} = 11.18\sqrt{1 - 0.2} = 11.18 \times 0.894 = 10.0 km/s.

Final Answer: (a) 11.211.2 km/s; (b) 10.010.0 km/s.

Takeaway: A body falling in from infinity arrives at exactly the escape speed, because escaping and falling in are one journey run in opposite directions. Note also that four fifths of that final speed is picked up between 5RE5R_E and the surface.

Example 11: Which gases can a world keep?

Take 300 K for both worlds. Using vrms=3RTMmolarv_{rms} = \sqrt{\frac{3RT}{M_{molar}}} with R=8.314R = 8.314 J/mol/K, decide whether the Earth and the Moon can retain hydrogen and nitrogen, using the criterion vrms<ve6v_{rms} < \frac{v_e}{6}.

Solution:

  1. Molecular speeds at 300 K. vrms(H2)=3×8.314×3002×103=3.741×106=1934 m/sv_{rms}(H_2) = \sqrt{\frac{3 \times 8.314 \times 300}{2 \times 10^{-3}}} = \sqrt{3.741 \times 10^{6}} = 1934 \text{ m/s} vrms(N2)=3×8.314×30028×103=2.672×105=517 m/sv_{rms}(N_2) = \sqrt{\frac{3 \times 8.314 \times 300}{28 \times 10^{-3}}} = \sqrt{2.672 \times 10^{5}} = 517 \text{ m/s}

  2. The two thresholds. veEarth6=111816=1864 m/sveMoon6=23726=395 m/s\frac{v_e^{Earth}}{6} = \frac{11181}{6} = 1864 \text{ m/s} \qquad\qquad \frac{v_e^{Moon}}{6} = \frac{2372}{6} = 395 \text{ m/s}

  3. Compare, one line at a time.

Gas vrmsv_{rms} (m/s) Earth (threshold 1864) Moon (threshold 395)
Hydrogen 1934 above it, escapes far above it, escapes
Nitrogen 517 far below it, retained above it, escapes
  1. Read the result. The Earth keeps nitrogen comfortably — 517 m/s is under 5% of its escape speed — but loses hydrogen, which is exactly what we observe: free hydrogen is essentially absent from the Earth's atmosphere. The Moon loses both, and everything else besides.

Final Answer: the Earth retains nitrogen and loses hydrogen; the Moon retains neither, which is why it has no atmosphere.

Takeaway: The Moon is airless because its escape speed of 2.4 km/s is simply too small compared with molecular speeds, not because the Moon somehow "lost" its air in an event. It is a slow, permanent leak.

Example 12: How fast at the Moon's distance?

A probe leaves the Earth's surface at 12.512.5 km/s. How fast is it moving when it crosses the Moon's orbit, 3.84×1083.84 \times 10^{8} m from the Earth's centre? Ignore the Moon's own gravity.

Solution:

  1. Energy conservation between the two radii. 12v12GMERE=12v22GMEr\frac{1}{2}v_1^{2} - \frac{GM_E}{R_E} = \frac{1}{2}v_2^{2} - \frac{GM_E}{r}

  2. Rearrange for v22v_2^{2}. v22=v122GME(1RE1r)v_2^{2} = v_1^{2} - 2GM_E\left(\frac{1}{R_E} - \frac{1}{r}\right)

  3. The two potential terms. 2GMERE=1.250×108 m2/s22GMEr=7.964×10143.84×108=2.074×106 m2/s2\frac{2GM_E}{R_E} = 1.250 \times 10^{8} \text{ m}^2\text{/s}^2 \qquad \frac{2GM_E}{r} = \frac{7.964 \times 10^{14}}{3.84 \times 10^{8}} = 2.074 \times 10^{6} \text{ m}^2\text{/s}^2

  4. Substitute. v22=1.5625×1081.250×108+2.074×106=3.330×107v_2^{2} = 1.5625 \times 10^{8} - 1.250 \times 10^{8} + 2.074 \times 10^{6} = 3.330 \times 10^{7} v2=5.77×103 m/sv_2 = 5.77 \times 10^{3} \text{ m/s}

Final Answer: about 5.775.77 km/s.

Takeaway: The probe has shed more than half its speed by the time it reaches the Moon, and almost all of that loss happened in the first few Earth radii. Since it left above escape speed, it still has 5.77 km/s at the Moon's distance and would arrive at infinity with 12.5211.182=5.59\sqrt{12.5^{2} - 11.18^{2}} = 5.59 km/s.