681: Gravity Wells

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Gravity Wells
This doesn't take into account the energy imparted by orbital motion (or gravity assists or the Oberth effect), all of which can make it easier to reach outer planets.
Title text: This doesn't take into account the energy imparted by orbital motion (or gravity assists or the Oberth effect), all of which can make it easier to reach outer planets.

The xkcd page links to a much larger version.

Explanation

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If you can address this issue, please edit the page! Thanks.

The comic shows the gravitational potential (energy transferred per unit mass due to gravity) for the positions of each planet in the solar system, including some moons and Saturn's rings. An object traveling along an upward slope would be giving up energy, while an object traveling along a downward one would be gaining energy. The graph is scaled to kilometers via the gravitational potential an object has at the given height assuming at a constant acceleration due to earths surface gravity.

To rise out of each well on the diagram, and therefore escape the planets gravity, it would require the same energy required to rise out of a physical well of that depth at Earth's surface gravity. Each planet is shown cut in half at the bottom of its well, with the depth of the well measured down to the planet's flat surface. In reality, the strength of gravity decreases the further you get from the planet. However, a comparison of energy expended to escape the gravitational pull allows for a simpler comparison between the objects.

The moons shown in the chart are at the appropriate distance from their respective planets' gravity wells for their orbits. The Sun's gravity well is not shown in its entirety, but is just indicated on the far left as "Very very far down". Had it been shown in its full extent it would have made the rest of the drawing so small in comparison that it would have been unreadable.

The Earth's gravity well's depth in the inset and in the main part of the comic don't match. This is most likely a mistake by Randall.

Inner Planets

  • Venus — no facts listed
  • Earth & Moon — listed with the depth of the gravity well of 5,478 km for Earth and 288 km for the Moon. Calculations of depth is explained in the Saturn insert.
  • Mars — listed with the depth of gravity well of 1286 km

Cut outs

  • The Mars cutout shows how small Mars' moons really are, specifically in terms of gravity. Deimos is so small that a bike jump would be sufficient to escape its gravity well and on Phobos you could launch a baseball into space simply by throwing it.
  • The drawing next to Jupiter is playing on the classic "Yo Mama" joke, combining the aspects of your mom being very fat (having a huge gravitational pull) and very slutty (having sex with the entire football team), represented by the football team being attracted to, and falling into, her gravity well. A "Yo Mama" joke also appears in comic 89: Gravitational Mass.

Outer Planets

  • Jupiter — is so massive and dense that it is comparable in mass to a Brown dwarf which is the smallest kind of star. Saturn, while similar in size, is composed of much lighter gas material. Hence Saturn's mass and therefore its gravitational pull are much smaller. Strong gravitational pull is a significant factor in igniting fusion. As gravity pulls matter together the pressure and temperature increase. With sufficient increase in pressure and temperature nuclear fusion begins. Had that happen during creation of our solar system, i.e. had a few dozen times the mass of gasses contained in Jupiter condensed in that location, then we would had two Suns and our solar system would have been a Binary system.
    • Ganymede -- (Moon of jupiter) -- no facts given.
    • Io -- (Moon of jupiter) -- no facts given.
    • Europa -- (Moon of jupiter) -- no facts given.
  • Saturn & its rings — The "Rings" in Saturn's gravity well are Saturn's rings. The farther you get from a planet, the weaker the effect of its gravity on you, so, at some point, when climbing out of Saturn's gravity well, you've reached the point equivalent to starting your climb from the rings of Saturn, or, in fact, from specific rings of Saturn. Saturn's rings start fairly near the planet and extend out quite far, therefore multiple stripes are shown in the figure. The rings are also shown in multiple colors and roughly match the observed colors from photos take by the Cassini spacecraft expedition as it passed Saturn. All of the colors of the planets and moons represent the predominant color of that object as observed from earth.
  • Uranus — notably absent is any "your-anus" jokes.
  • Neptune — Megan's quote is a paraphrase of Carl Sagan's quote, "...but from a planet orbiting a star in a distant globular cluster, a still more glorious dawn awaits, not a sun-rise, but a galaxy rise." Video here

How to interpret gravity wells

To escape a planet's or moon's orbit, you need merely climb to the highest of the two peaks to either the left or right of the object. So, for example, to escape Venus, you need merely reach the peak left of it, the slope right of it is part of the Sun's gravity well, and shows how much further you'd need to climb out of the Sun's gravity well to get from Venus to Earth. Likewise, the peak left of Jupiter is slightly lower than the one to the right; this is because the rightmost peak includes the difficulty of moving away from the Sun to get to Saturn, the next planet along.

The text explains that the depth of the well is mass-of-planet over radius-of-planet with newtons constant and 9.81 m/s² as constants, where 9.81 m/s² is the acceleration of a free falling body at Earth's gravity.

The calculation for a gravity well is:

depth = (G * Planet-mass ) / (9.81 m/s2 * Planet-radius)
where G is Newton's gravitational constant, and
9.81 m/s2 is the acceleration rate of a free falling body on earth at sea level (g).


The Title Text refers to that the planet motions can affect the actual amount of energy for escape velocity to gain (or loose) speed by using the planets orbital speed to gravity assist the speed of vehicle -- this is know as doing sling-shoot around planets to gain speed (or to break when needed, breaking is just doing the same in reverse) -- on earth the same principle is used slightly differently when launching rockets -- rockets are always launched in a eastward direction to make maximum use of the rotational energy -- launching rockets in a westward direction would require a significant additional energy, and hence most satellites are flying from west to east as turning them in a different orbit would be requiring more fuel. At the same time the use of rocket engines are more effective when used at a high speed which is know as the Oberth effect. The use of engines are therefore more effective when used as part of a slingshot maneuver.

The size of the gravity-well as described in this comic is not accounting for this factor, and hence leaving the solar system (or any of the gravity wells of the planets) would require less energy than described by the size of each well if the launch and slingshots are carefully planned and executed.

Escape Velocities

The following table was adapted from the table in Escape velocity, using h = V_e^2 / 2g:

Location with respect to Ve (km/s) Well depth (km) Location with respect to Ve (km/s) Solar well (Mm) Total depth (Mm)
on the Sun, the Sun's gravity: 617.5 19,435,000 19,435
on Mercury, Mercury's gravity: 4.3 942 at Mercury, the Sun's gravity: 67.7 233.6 235
on Venus, Venus' gravity: 10.3 5,407 at Venus, the Sun's gravity: 49.5 124.9 130
on Earth, the Earth's gravity: 11.2 6,393 at the Earth/Moon, the Sun's gravity: 42.1 90.3 97
on the Moon, the Moon's gravity: 2.4 294 at the Moon, the Earth's gravity: 1.4 91
on Mars, Mars' gravity: 5 1,274 at Mars, the Sun's gravity: 34.1 59.3 61
on Jupiter, Jupiter's gravity: 59.5 180,400 at Jupiter, the Sun's gravity: 18.5 17.4 198
on Ganymede, Ganymede's gravity: 2.7 372
on Saturn, Saturn's gravity: 35.6 64,600 at Saturn, the Sun's gravity: 13.6 9.43 74
on Uranus, Uranus' gravity: 21.2 22,907 at Uranus, the Sun's gravity: 9.6 4.7 28
on Neptune, Neptune's gravity: 23.6 28,400 at Neptune, the Sun's gravity: 7.7 3.02 31
on Pluto, Pluto's gravity: 1.2 73
at Solar System
galactic radius,
the Milky Way's gravity: 525 14,000

Transcript

Main Text
Gravity Wells scaled to Earth surface gravity
This chart shows the "depth" of various solar system gravity wells.
Each well is scaled such that rising out of a physical well of that depth — in constant Earth surface gravity — would take the same energy as escaping from that planet's gravity in reality.
Each planet is shown cut in half at the bottom of its well, with the depth of the well measured down to the planet's flat surface.
The planet sizes are to the same scale as the wells. Interplanetary distances are not to scale.
Depth = (G × PlanetMass) / (g × PlanetRadius)
G = Newton's constant
g = 9.81 m/s2


Planetary Descriptions
To Sun, very very far down
Mercury
Venus
Earth - 5,478 km
Moon - 288 km
Mars - 1,286 km
Ganymede
Io
Jupiter
[A drawing of a "very deep" gravity well, "Your mom" at the bottom, several member of "local football team" falling down towards her.]
Jupiter is not much larger than Saturn, but much more massive. At its size, adding more mass just makes it denser due to the extra squeezing of gravity.
If you dropped a few dozen more Jupiters into it, the pressure would ignite fusion and make it a star.
Europa
Titan
Two figures: Weeoooeeoooeeooo
Saturn
Rings
Uranus
Neptune
Megan: An even more glorious dawn awaits!


Mars Inset
[Mars gravity well, the Pathfinder probe on its surface, with its moons Deimos and Phobos as smaller gravity wells.]
[Figure of a man (to scale) in Deimos's gravity well.]
You could escape Deimos with a bike and a ramp.
[Figure of a man (to scale) in Phobos's gravity well.]
A thrown baseball could escape Phobos.


Earth Inset
[Zoomed-in view of Earth/moon gravity well, featuring the relative locations of the atmosphere, Low Earth Orbit, the International Space Station, the Space Shuttle, GPS satellites, and satellites in geosynchronous orbit.]
Cueball: This is why it took a huge rocket to get to the moon but only a small one to get back.
It takes the same amount of energy to launch something on an escape trajectory away from Earth as it would to launch it 6,000 km upward under constant 9.81 m/s2 Earth gravity.
Hence, Earth's well is 6,000 km deep.


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Discussion

Why is Earth's well's depth listed as 5478km but as 6379km in the inset? Compare with Mars which has 1286 in both places. 87.174.225.131 07:21, 12 April 2013 (UTC)

Best guess is either a goof, or that the lower number is just for Earth itself, while the greater number is for the Earth/Moon system as a whole. Proportionally speaking, we have the largest moon in the solar system, so maybe it wouldn't nicely fit in the Earth well as easily as Mars's and Jupiter's moons do.--Druid816 (talk) 08:28, 12 April 2013 (UTC)
It may be the height needed to go from one gravity well to another. You don't have to get all the way up to escape speed for that.
Randall wasn't kidding about the Sun being "very very far down"; its well is 100 times deeper than Jupiter's!
Wwoods (talk) 19:47, 12 April 2013 (UTC)
OTOH, from the table above i'm thinking that the 5.4 might be the Venus figure, and it was wrongly placed besides Earth...
Secondly, what i found interesting was that the Earth's 6.4 looks so much like its radius! I wonder if it's merely a coincidence, or there's a connection between the two... -- 141.101.99.233 21:25, 30 October 2013 (UTC)
The table is great, it must be included in the article; layout and time is just my problem right now. PRO TIP: Do not care about the x-axis.--Dgbrt (talk) 22:18, 30 October 2013 (UTC)
The fact that the density of the Earth is 5478 kilograms per cubic kilometer makes me pretty sure it is a typo. Fewmet (talk) 03:04, 4 July 2014 (UTC)
Hehe, you might be right. That's the best explanation. It would be a strange coincidence otherwise. But your units are wrong: a cubic kilometer of water, ice-cream or Natalie Portmans would be already something like a billion kilograms. Or a trillion, if you are American. Oh, you might be American. In this case: happy 4th of July! -188.114.102.35 12:39, 4 July 2014 (UTC)
Thanks for catching that (and for the July 4 wishes). It should be kilograms per cubic meter. Looking into that, though, leaves me less sure that is the origin of the problem. I thought I had multiple sources for Earth having a density of 5478 kg/m3, but can find only one (and not a very compelling one at that). I have sounder sources for 5513 kg/m3. 5514 kg/m3, 5515 kg/m3, 5520 kg/m3 and 5540 kg/m3. It may be trivial in that all round to 5500 kg/m3.
It was corrected on the poster version. Earth's well in the main graphic is marked as 6379km, just like the inset.108.162.216.86 00:19, 21 August 2014 (UTC)
I solved for the wells on Earth, Moon and Mars using the equation Randall gave and masses and equatorial radii from NASA, getting 6371 km, 287 km and 1286 km, respectively. Fewmet (talk) 23:07, 5 July 2014 (UTC)

The Oberth Effect mentioned in the title text is well-explained here (assuming you are not intimidated by the algebra in squaring a binomial). The gist of it is that using a bit of fuel in a rocket thrust will increase the rocket’s kinetic energy . The higher the kinetic energy at the time of the thrust, the greater the increase in kinetic energy. It works because the energy of the fuel goes into increasing the kinetic energy of the ship and the kinetic energy of the spent fuel. The faster you go, the greater the portion of the energy the ship gets.

The image at the top is out of date and should be fixed as well as the earth's comment about how it's different--172.70.178.107 10:52, 7 September 2022 (UTC)
I, for one, don t understand at all what you think is out-of-date/different. There's a new planet, or some rescaling of gravity? If serious, do elaborate. (If not serious, elaborate to add to the humour.) 141.101.99.154 12:27, 7 September 2022 (UTC)

The “gravity assist” is also known as the slingshot effect. The Wikipedia explanation is good, especially with its diagram. In it a spaceship (or other body) accelerates toward a planet (or moon, star, etc.) in the same direction that body was going. The ship picks up a little of the body’s momentum and so goes faster, although only according to an external reference frame. An observer at rest with respect to that other body would actually see the ship approach and depart with the same speed.

The title text reference to orbital speed is unclear to me. I suppose it just means that the given gravity wells assume you are at rest on the surface of the planet. Then being in orbit (and necessarily having an orbital speed) would mean you are part way out of the well already. Fewmet (talk) 02:57, 4 July 2014 (UTC)

If the first stage of a rocket is still supplying lift for a while after its fuel is used up and the stage is cut adrift, would there be any saving in waiting for the next phase to cut in when forward motion is almost ended rather than continuing the burn immediately from the second stage?

The higher the vehicle gets the more productive the fuel becomes.Or is it preferable to continue the journey as fast as possible? -- Weatherlawyer (talk) (please sign your comments with ~~~~)

My first instinct would be to say burn as continuously as possible. If you wait until your speed is almost zero, you have to use a whole load of energy (fuel) to get back to the speed you were going in the first place. --Pudder (talk) 17:12, 27 January 2015 (UTC)

Hence the need to use ultra light containers in the first stage? -- Weatherlawyer (talk) (please sign your comments with ~~~~)

Maybe the typo is based on Randall's days at NASA? It might already incorporate gravity assists and the Oberth effect. That number might even be what NASA was using as the minimum potential with known cost-effective techniques. flewk (talk) 21:22, 8 January 2016 (UTC)

Earth's Geosynchronous Orbital Altitude

In the XKCD strip, the artist states above Earth in the lower right popout that the geosynchronous altitude is well below top of Earth's gravity well. While the rest of his strip is a wonderful representation of the science behind gravity wells, this one bit is not accurate. A geosynchronous altitude for Earth is nearly 36,000 km, not under 6000 km. Kudos for the rest of the strip, though.

The strip scales the heights of the corresponding wells based on the assumption of constant Earth surface gravity; in other words, it takes the same amount of energy to climb such a well as it does to escape the real gravity well. By contrast, as one ascends from the Earth's surface, gravity decreases, so it requires less energy to climb to an orbital altitude than it does to reach the same height in the hypothetical well. The amount of energy required to put a geostationary satellite in orbit, for example, is equivalent to that used in raising it 5413 km in Earth surface gravity, and thus it is located 5413 km from the bottom of the well. Arcorann (talk) 03:42, 8 February 2019 (UTC)

I have a question relating to this topic. I've learnt how to calculate well depth, but how did Randall Munroe calculate the position of things inside the gravity well (moons of planets, for example, or Saturn's rings)?

I'm also confused by this. Anyone have the answer? 162.158.78.78 17:50, 5 May 2020 (UTC)

How much gravity can be overcome?

How much of the gravity well can be overcome by launching from a high mountain?

If we constructed a spaceport on a mountaintop that was, say, 14,505 ft (Mt. Whitney, CA), or even 20,310 ft (Denali, Alaska), or slightly less after clearing a flat surface, would it significantly reduce the amount of the gravity well a rocket had to climb, and hence the amount of fuel needed to reach LEO? Would thinner air reduce drag and increase efficiency significantly as well? This would be tough to build and maintain, but would it be worth delivering spaceships to mountaintops by truck to reduce the need for fuel to escape Earth's Gravity well?

I am not an expert, but to my knowledge, the effect of latitude on gravity is much stronger than those of a mountain. Especially one as far north as Denali. That is why Nasa uses Florida and Texas, Russia uses Baikonur_Cosmodrome in Southern Kazakhstan , Europe uses Guiana_Space_Centre in south america (French Guiana, so technically Europe...). --Lupo (talk) 08:52, 29 May 2019 (UTC)
FWIW in the early stages of planning the Space Shuttle, the Air Force was looking at launching from the top of the Rockies, maybe in Colorado or such. The reason being exactly the savings in propellant and consequent gain in payload. I was made to believe the savings was quite significant.
What killed it was the issue of what happens when one malfunctions or crashes on launch. You've got Space Shuttle & parts raining down on the Denver metro area; not good.
Source: My dad worked on the project for the Air Force back in the 70s or thereabouts. Flug (talk) 21:52, 22 September 2019 (UTC)