[Space, Spaceships] Total ΔV for Interplanetary Travel
When calculating the total ΔV for an interplanetary trip, do we have to add the ΔV for breaking planetary orbit (both from the origin and braking to the destination) to that of the interplanetary transfer orbit?
Dalton “who is working on a One-Tangent Burn Orbit spreadsheet” Spence |
Re: [Space, Spaceships] Total ΔV for Interplanetary Travel
You want the sum of the ΔV required to break orbit from the origin, the ΔV used in the transfer itself, and then, yes, the ΔV expended to attain orbit at the destination.
In theory. In practice, good piloting can reduce the ΔV needed on arrival, and if the destination has an appropriate atmosphere and you have a ship that can handle hypersonic atmospheric burns, you can use areobreaking to achieve orbit at the destination for a fraction of the ΔV cost. All of this assumes a Hoffman transfer, which is generally both simple and low-ΔV-cost. The downsides are that it requires specific windows to work well, and it's fairly slow. If one has very large reserves of ΔV, it's possible to fly from the origin to the destination directly, and I think there's notes on that in GURPS Space. Or Spaceships. Can't remember. Best of luck! |
Re: [Space, Spaceships] Total ΔV for Interplanetary Travel
On consideration, I think that's probably necessary.
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How much difference is there if launching from Earth's surface as opposed to being launched from a facility already in orbit?
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The limit case for infinite thrust is ΔV = sqrt( escape velocity ^ 2 + transfer velocity ^ 2 ) - orbital velocity, to either enter or leave orbit. For example, from low earth orbit (escape velocity = 11.2 km/sec, velocity = 7.92 km/s) to a Mars transfer orbit (2.9 km/s) requires sqrt( 11.2^2 + 2.9^2) - 7.92 = 3.65 km/s, which is barely more than the 3.28 km/s required to break orbit. Launch direct from ground saves the fuel required to circularize your orbit. |
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Dalton “still working on his Mars Semi-Cycler” Spence |
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It's usually a glossed over effect and I know of no easy databases but the planets of our solar system mostly do have different orbital planes.. |
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Dalton “what sort of ΔV can we get from Pinot Grand Fenwick?” Spence |
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Dalton “just when I think I'm getting it, what I get is confused” Spence |
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Dalton “did I get this right?” Spence |
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After next spring, I may reprise the article with something more detailed, but I won't attempt this before I do more in depth study of the material. I probably won't present it through Pyramid unless Steven asks for it or there appears to be enough demand for something more math-heavy than the original. |
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Dalton “who missed the limit number somewhere” Spence |
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10 Gs: 3.6 km/s ΔV for a transfer orbit (less than 3.65 because I assumed an initial 200 altitude) 1 G: 3.65 km/s ΔV for a transfer orbit. 0.1G: 4.6 km/s ΔV for a transfer orbit. 0.01G: 6.9 km/s ΔV for a transfer orbit. 0.001G: 8.4 km/s ΔV for a transfer orbit. 0.0001G: 9.4 km/s ΔV for a transfer orbit. |
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