Difference between revisions of "Space habitats"
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To balance these difficulties, living in space brings many advantages. One is reliable, abundant [[Energy|solar energy]], not blocked by the atmosphere or subject to weather or time of day. Another is control of gravity; a rotating space colony would have normal Earthlike gravity at the periphery and zero gravity at the center. Large-scale construction and other industrial activities could be done at the center, reducing the energy they need to almost zero. When we build space habitats, we have the opportunity to tailor-make ecosystems that are optimized for human habitation. A space colony could be kept at any desired temperature, have any desired weather conditions and any desired seasonal and diurnal cycles. Careful controls could keep infectious diseases and agricultural pests from being introduced to the ecosystem. | To balance these difficulties, living in space brings many advantages. One is reliable, abundant [[Energy|solar energy]], not blocked by the atmosphere or subject to weather or time of day. Another is control of gravity; a rotating space colony would have normal Earthlike gravity at the periphery and zero gravity at the center. Large-scale construction and other industrial activities could be done at the center, reducing the energy they need to almost zero. When we build space habitats, we have the opportunity to tailor-make ecosystems that are optimized for human habitation. A space colony could be kept at any desired temperature, have any desired weather conditions and any desired seasonal and diurnal cycles. Careful controls could keep infectious diseases and agricultural pests from being introduced to the ecosystem. | ||
− | A passion for space colonisation and a faith in its promise was evoked in thousands of people by an essay called [http://space.mike-combs.com/SCTHF.html ''Space Colonies: The High Frontier''], written by Gerard O'Neill in 1976. The essay outlines a fairly modest proposal, using only technology then existing, to build a series of space stations orbiting the Sun and Earth. Materials would be [[Resources in space#Mining the moon|mined from the moon and the asteroid belt]], launched into space and assembled into space colonies. Launching material from the moon is an easy matter, as there is far less gravity and no air resistance. The first colony would require about as much building material as the world's biggest skyscrapers, and would become self-replicating, as each colony could be used as a factory to assemble the next. The network of space habitats could then expand to form a Dyson swarm ([[#Lagrangian points and Solar orbit|see below]]) which could house tens of trillions of people to an extremely high standard of living. | + | A passion for space colonisation and a faith in its promise was evoked in thousands of people by an essay called [http://space.mike-combs.com/SCTHF.html ''Space Colonies: The High Frontier''], written by [http://ssi.org/the-life-of-gerard-k-oneill/ Gerard O'Neill] in 1976. The essay outlines a fairly modest proposal, using only technology then existing, to build a series of space stations orbiting the Sun and Earth. Materials would be [[Resources in space#Mining the moon|mined from the moon and the asteroid belt]], launched into space and assembled into space colonies. Launching material from the moon is an easy matter, as there is far less gravity and no air resistance. The first colony would require about as much building material as the world's biggest skyscrapers, and would become self-replicating, as each colony could be used as a factory to assemble the next. The network of space habitats could then expand to form a Dyson swarm ([[#Lagrangian points and Solar orbit|see below]]) which could house tens of trillions of people to an extremely high standard of living. |
O'Neill sets out to challenge a fundamental assumption underlying all our thinking about mankind's resources: the assumption that "The material and energy resources of the human race are just those of our planet." His calculations show that by building such colonies with [[Resources in space|materials]] from the asteroid belt and the moon, we could create "a land area many thousands of times that of the entire earth", with ideal climate, temperature and conditions. This would certainly impact just about every pressing social problem we now face on Earth. | O'Neill sets out to challenge a fundamental assumption underlying all our thinking about mankind's resources: the assumption that "The material and energy resources of the human race are just those of our planet." His calculations show that by building such colonies with [[Resources in space|materials]] from the asteroid belt and the moon, we could create "a land area many thousands of times that of the entire earth", with ideal climate, temperature and conditions. This would certainly impact just about every pressing social problem we now face on Earth. | ||
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====Lunar orbit==== | ====Lunar orbit==== | ||
In '''lunar orbit''' the moon is within easy reach but the habitat will be subject to the Moon's two-week long day / night cycles which might not be to everyone's taste, although of course the normal light rhythms can be replicated internally with lighting. | In '''lunar orbit''' the moon is within easy reach but the habitat will be subject to the Moon's two-week long day / night cycles which might not be to everyone's taste, although of course the normal light rhythms can be replicated internally with lighting. | ||
+ | |||
+ | ====In other solar systems==== | ||
+ | Habitable planets may turn out to be rare in other solar systems. If this proves to be the case, it need not stop us from eventually settling other solar systems. The same designs of O'Neill cylinders etc. would work equally well around other stars as around our Sun. This is a much more long-term goal. | ||
===Moons and planets=== | ===Moons and planets=== | ||
====Base on Mars==== | ====Base on Mars==== | ||
− | Before we can think about terraforming Mars, we need to land some people on it and have them live there for an extended stay. The '{{wp|Mars_Direct|Mars Direct}}' plan has rigorously demonstrated that a manned mission to Mars has been possible since the 1990s for $20 billion (in other words, about 0.4% of the US military budget, over five years). | + | Before we can think about terraforming Mars, we need to land some people on it and have them live there for an extended stay. The '{{wp|Mars_Direct|Mars Direct}}' plan has rigorously demonstrated that a manned mission to Mars has been possible since the 1990s for $20 billion (in other words, about 0.4% of the US military budget, over five years). With [[Open collaborative design|open collaborative design]], it could be done at a fraction of this price. |
A team of astronauts on the surface of Mars for years would be able to fill in the blanks in our knowledge of the Red Planet. The plan to terraform Mars is based on the assumption that there is no native life there. Before terraforming begins, we would need to confirm this assumption, as it is not ethically acceptable to deliberately destroy an entire planet's biosphere. More precise measurements of the chemical composition of Mars would allow us to perfect our terraforming plan. | A team of astronauts on the surface of Mars for years would be able to fill in the blanks in our knowledge of the Red Planet. The plan to terraform Mars is based on the assumption that there is no native life there. Before terraforming begins, we would need to confirm this assumption, as it is not ethically acceptable to deliberately destroy an entire planet's biosphere. More precise measurements of the chemical composition of Mars would allow us to perfect our terraforming plan. | ||
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Mars has a lot of frozen carbon dioxide, especially at its poles. Robert Zubrin has calculated<sup>[http://www.users.globalnet.co.uk/~mfogg/zubrin.htm]</sup> that if we heat the planet just 4°C, some of this will sublimate into the atmosphere. This carbon dioxide is a greenhouse gas, which will lead to more warming, making the frozen carbon dioxide that remains at the colder parts sublimate, leading to more global warming. This will cause the frozen water below the surface to melt and some of it will vaporise. This water vapour is another greenhouse gas, leading to even more global warming. When the planet reaches higher temperatures, more carbon dioxide, trapped in minerals, will be released into the atmosphere. So an initial nudge of 4°C can set in motion a chain of events that raise the temperature of the planet 55°C and build enough atmosphere to raise the pressure from 0.006 to 0.296 atmospheres (similar to pressure at twice the altitude of Everest). | Mars has a lot of frozen carbon dioxide, especially at its poles. Robert Zubrin has calculated<sup>[http://www.users.globalnet.co.uk/~mfogg/zubrin.htm]</sup> that if we heat the planet just 4°C, some of this will sublimate into the atmosphere. This carbon dioxide is a greenhouse gas, which will lead to more warming, making the frozen carbon dioxide that remains at the colder parts sublimate, leading to more global warming. This will cause the frozen water below the surface to melt and some of it will vaporise. This water vapour is another greenhouse gas, leading to even more global warming. When the planet reaches higher temperatures, more carbon dioxide, trapped in minerals, will be released into the atmosphere. So an initial nudge of 4°C can set in motion a chain of events that raise the temperature of the planet 55°C and build enough atmosphere to raise the pressure from 0.006 to 0.296 atmospheres (similar to pressure at twice the altitude of Everest). | ||
− | This whole process may take about 25 years. By the end of it, the average temperature of the planet is 0°C (though we can locate our colonies at places much warmer than average) | + | This whole process may take about 25 years. By the end of it, the average temperature of the planet is 0°C (though we can locate our colonies at places much warmer than average), the pressure allows people to walk around without a spacesuit and oceans cover large parts of the planet. The atmosphere is still nearly all carbon dioxide, so breathing apparatus will be required when colonists venture beyond sealed habitats. The planet is not fully terraformed, but we are off to a very good start and all it took was heating the planet 4°. |
How do we create this 4°C increase? Ironically, the very scientific knowledge gained by studying the destruction of the Earth's biosphere can be applied to engineering a new biosphere on Mars; releasing enough CFCs or similar greenhouse gases into the atmosphere should do the trick. The building blocks of CFCs are available on the surface of Mars, and we could engineer some automated method of synthesizing them in-situ and releasing them into the atmosphere. About 39 million tons would be required, roughly three times what was produced on Earth during the 20 years CFCs were used in industry. Two other methods of warming the planet have been proposed: sending ammonia- or methane-rich asteroids to collide with it (these are greenhouse gases) or building gigantic mirrors in orbit to reflect more sunlight onto those frozen carbon dioxide deposits. Of the three methods, CFCs do seem the most feasible, but the other two may provide a helping hand. If a [[Resources in space#Mining the moon|lunar mining colony]] is in place, launching a thin aluminium mirror of sufficient size would not be unfeasible. | How do we create this 4°C increase? Ironically, the very scientific knowledge gained by studying the destruction of the Earth's biosphere can be applied to engineering a new biosphere on Mars; releasing enough CFCs or similar greenhouse gases into the atmosphere should do the trick. The building blocks of CFCs are available on the surface of Mars, and we could engineer some automated method of synthesizing them in-situ and releasing them into the atmosphere. About 39 million tons would be required, roughly three times what was produced on Earth during the 20 years CFCs were used in industry. Two other methods of warming the planet have been proposed: sending ammonia- or methane-rich asteroids to collide with it (these are greenhouse gases) or building gigantic mirrors in orbit to reflect more sunlight onto those frozen carbon dioxide deposits. Of the three methods, CFCs do seem the most feasible, but the other two may provide a helping hand. If a [[Resources in space#Mining the moon|lunar mining colony]] is in place, launching a thin aluminium mirror of sufficient size would not be unfeasible. | ||
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* {{wp|O%27Neill_cylinder|O'Neill cylinder habitat}} | * {{wp|O%27Neill_cylinder|O'Neill cylinder habitat}} | ||
* [[Resources in space]] | * [[Resources in space]] | ||
+ | * [http://www.spacehabs.com Space Habitats Gallery] - Great art of Mars habitats, asteroid mining equipment, orbital habitats and more. | ||
* Marshall T. Savage's [http://www.amazon.com/Millennial-Project-Colonizing-Galaxy-Eight/dp/0316771635/ref=sr_1_1?ie=UTF8&s=books&qid=1251836768&sr=8-1 The Millenial Project: Colonizing the Galaxy in eight easy steps] - employing known technology. (Forward by {{wp|Arthur_C._Clarke|Arthur C. Clarke}}) | * Marshall T. Savage's [http://www.amazon.com/Millennial-Project-Colonizing-Galaxy-Eight/dp/0316771635/ref=sr_1_1?ie=UTF8&s=books&qid=1251836768&sr=8-1 The Millenial Project: Colonizing the Galaxy in eight easy steps] - employing known technology. (Forward by {{wp|Arthur_C._Clarke|Arthur C. Clarke}}) | ||
{{br}} | {{br}} | ||
{{detailed tour|Colonising Space|AdCiv:About}} | {{detailed tour|Colonising Space|AdCiv:About}} | ||
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Latest revision as of 20:21, 21 June 2013
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