Problems solved in full
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The speed at which something thrown from Earth never comes back 5 steps
Find the speed at which something thrown from Earth never comes back — then use it to explain why Earth still has nitrogen, is slowly losing its hydrogen, and why the Moon has no air at all. Earth: M = 5.972 × 10²⁴ kg, R = 6371 km.
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“Never comes back” is a statement about energy, not about height. Gravity’s pull weakens with distance but never switches off, so the condition is that kinetic energy is at least as large as the depth of the gravitational well the object is sitting in.
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Set the total to zero — the marginal case, arriving at infinity with nothing left — and solve. The projectile’s own mass cancels, which is the first surprising thing: a bullet and a boulder need exactly the same speed.
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Put Earth’s numbers in. This is the figure the comparator above prints when Earth is selected, and it is a speed, not a thrust: nothing here says how you reach it.
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Now use the fact that m cancelled. It applies to a nitrogen molecule as much as to a rocket. Gas molecules do not all move at one speed, but the root-mean-square speed follows from temperature alone.
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A gas is not lost the moment a molecule exceeds escape speed — the fast tail of the distribution leaks away over billions of years. The standard rule of thumb is that a world keeps a gas if escape speed is at least about six times the molecular speed. The Moon’s row is at its own temperature: with no air to spread the heat, its day side reaches about 390 K, which lifts nitrogen to 0.59 km/s.
Answer
11.2 km/s, and it is the same for everything. The ratios then tell the whole story of planetary atmospheres: nitrogen on Earth sits at 22 — comfortably retained. Hydrogen sits at 5.9, just under the threshold, which is exactly why Earth leaks hydrogen to space and why the atmosphere you breathe is heavy molecules. On the Moon, escape speed is only 2.38 km/s and nitrogen scores 4.0 — below the line, which is why the Moon has no atmosphere to lose any more. The one equation that dropped the projectile’s mass is what lets it be applied to a molecule.
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What leaving the Solar System costs after 11.2 km/s escapes Earth 6 steps
11.2 km/s escapes Earth. It does not escape the Sun: it leaves you in the Sun's grip at Earth's distance, orbiting alongside the planet you just left. Work out what leaving the Solar System actually costs.
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Start with the figure on the panel, from the energy balance that produced it: kinetic energy exactly cancelling the depth of the gravitational well.
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Now change the centre you are measuring from. Earth itself is falling around the Sun, at a speed fixed by the same law one astronomical unit out.
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Escaping the Sun from that distance takes √2 times the circular speed — the identical relation as before, because the arithmetic does not care which body has hold of you.
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Subtract, and notice what you are being given. You are already travelling at 29.79 and you need 42.13, so only the difference is missing — and you collect it for free by launching along the direction Earth is already moving.
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But you still have to climb out of Earth, and it is energies that add, not speeds. That is why the two figures combine as squares: the speed needed at the surface is the hypotenuse, not the sum.
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Now turn around and launch against Earth's motion. The two speeds stop cancelling and start adding.
Answer
16.65 km/s from the surface if you go with Earth, against 72.79 km/s if you go the wrong way. A factor of more than four, and the whole of it is Earth's 29.79 km/s orbital motion, which you either take as a gift or pay for twice. This is why deep-space launches wait for a window and leave along Earth's track, and why escape velocity quoted as one number is half an answer: the honest question is always escape from what.
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References (1)
- The radius named in the first block: K. Schwarzschild, "Über das Gravitationsfeld eines Massenpunktes nach der Einsteinschen Theorie." Sitzungsberichte der Königlich Preussischen Akademie der Wissenschaften, 189–196, 1916.