Nothing of the kind is required. Construct the Dyson sphere out of
computronium
and, after expending much of the resources of the entire solar system for the construction, upload the human civilisation on it.
I was talking about things like beaming power to interplanetary or interstellar spacecraft, industrial processes, and power for habitats on planetary surfaces or orbital habitats. Note that
anything else that you attach to the power collectors will cost mass, not only the systems I suggested. The mass figure is for the power collection system alone.
Though of course if you want to destroy everything in the solar system and replace it all with a gigantic version of Second Life, be my guest. I'm sure it'll go swimmingly.
Note that I never suggested a solid shell sphere; I was implying seperate orbiting satellites (or statites). A solid shell would be a massive, unstable, implausible structure. My figure of 0.38% the mass of the Earth, is around 6.9% of Mercury. Hardly solar system destroying, but still an utterly monumental task. One that would likely be undertaken over centuries or decades, as power requirements slowly grow.
It may make more sense to position the satellites closer to the sun, perhaps at Mercury's orbit. There are about 9116 watts per m^2 at Mercury's orbit, versus 1366 at 1 AU. A system similar to the one discussed earlier (with the same area) could harness 7.68e24 watts, or 7684788 exawatts. This is 52 times less than the 4e26 watts required to qualify as a Kardashev class II civilisation.
Using a number of 20 kilograms per kilowatt, the power collectors would mass 2.5% that of the Earth, or about 45% the mass of Mercury. Something tells me though, that the system would have much lower mass at this distance from the sun.
well, moon will stop mving in a few billion years.
somewhere the nergie for tides must come from...
The Moon will not stop moving, it is constantly moving through space.
If you mean stop spinning relative to the Earth, it has already done that. It is currently escaping the Earth at a rate of 1 cm per year due to tidal acceleration, but the timescale for this to become troublesome is so long as not to be worrisome.