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#1676 Re: Planetary transportation » Entomopters! - Any techinical details? » 2002-01-30 15:51:46

This is a fascinating topic. Here's another link to flying on Mars I just found: http://www.cosmiverse.com/space/01230201.html.

It appears that flapping wings are better than fixed wings because the thin air requires very high takeoff and landing speeds for fixed wing, and because flapping wings generate strong wing vortices that create more lift per square meter of wing surface. This is important because of the thin air as well.

Yes, the reference to a chemical muscle is strange. The article referred to "reciprocating" and "waste gases" making it sound like an engine of some sort.  They may be speaking indirectly to protect their technology.

#1677 Re: Human missions » Entrepreneurs First » 2002-01-28 13:42:03

I am intrigued by the idea of a one-person, one-way shot to Mars. I personally would suggest you at least have ONE person with you so that someone can help you when you get a toothache (anyone who has seen the recent movie where Tom Hanks gets stranded on an island for a few years will know what I mean).

I don?t think this project could be done cheaply any time soon. Maybe the baseline vehicle needed could be constructed from the Earth Return Vehicle in Mars Direct (The Case for Mars, page 93). The ERV there is described as follows:

Cabin structure

#1678 Re: Martian Politics and Economy » Mars, Government, and Rights » 2002-01-26 02:04:26

I apologize, but I don't completely understand. You note that conditions on Mars will be tough. In what sense? For example, when the Erie Canal, Transcontinental Railroad, and Panama Canal were built, conditions were tough; i.e., food was dangerous to eat, no one was treated for disease adequately, and thousands died of illnesses (especially on the two canals listed). But I doubt anyone will be eating rotten (literally) food on Mars, nor will there be huge problems with illnesses. Because of the potential media coverage such problems will receive, they will be avoided.

People will have to work hard, and there will be shortages of necessary items. But if a mining company on Earth wanted to open a Mars operation, the reaction wouldn't be to refuse the offer or confiscate the equipment after it arrived. Rather, the extra hands and equipment would be welcomed. And since the sending agency would be embedded in terrestrial culture, capitalism would be alive and well; in other words, refusal to allow capitalism on Mars would simply dry up the investment capital that will expand the place.

Do you see my confusion?

                       -- RobS

#1679 Re: Water on Mars » Water ice on Mars. - Elaborate breakdown of the polar caps. » 2002-01-25 00:42:18

Well, actually, I think my posting made the problem worse, not better. So now I'm confused, too.

                        -- RobS

#1680 Re: Martian Politics and Economy » Mars, Government, and Rights » 2002-01-25 00:39:23

There have been many speculations about Martian government in science fiction novels, Mars Society conventions, e-mail listservs and bulletin boards, and even in NASA reports. The subject of government is dictated by several related variables: population size, economic basis for settlement, the extent and nature of terrestrial involvement, the legal basis for government and ownership, and other factors. In exploring the evolution of Martian government and society over time, it might be useful to think in terms of three or four time periods. They could be labeled chronologically: initial, medium term, and eventual. Or they could be labeled demographically: the station, the hamlet, the village, the town, and the nation. The first stages are smallest, closest to us in time, and the most predictable, while the last stages are the most speculative, the possibilities cover the greatest range, and the possible departure from Earth models is the greatest. In the following I will use the demographic terms, which reflect the size of the Mars population (less than about 12; 12 to about 150; 150 to about 1000; 1000 to several thousand; more than several thousand).

1. The Station. Whenever a crew touches down on Mars for the first time?probably four people, though it could be three or as many as six?the ?government? will be quite simple. Someone will be the commander, someone else the vice commander. Both of those people will also be occupied full time by other tasks: geologist, mechanic, or whatever. They will stay one ?cycle? (that is, arrive on one opposition and depart on the next) and will be replaced by a second crew of similar size. But at some point a crew will be able to stay more than one cycle. This is probably dependent on partial food production and recycling of wastes on Mars. It could occur as quickly as Mars 2. Note that currently the travel opportunities between Earth and Mars mean that the first crew leaves Mars about nine months before they are replaced. The nine-month gap could be covered if recycling was available to stretch supplies, there was more than one Hab for backup, and an entire crew (or at least two members of one) signed up to stay two cycles. If eventually one aimed for an average stay of three cycles, recruiting crews only from those willing to commit at least six years to Mars, with four people being replaced every cycle, Mars would have a population of twelve. At this size, there is still no need for a ?government? per se, though there will be a need for staff meetings. If the missions were being sent out the way NASA sends them now, we can roughly predict the sort of structure the Mars station would have, with a couple of heads of departments (?bosses?) and a fairly informal, egalitarian environment. If the crew is ethnically diverse, one hopes the Mars experience will weld them into a more or less unified whole.

2. The Hamlet. The Mars population could grow beyond a dozen or so if the Hab (as described in The Case for Mars) were expanded into a three or four story ?Habcraft? (as described in The Case for Mars, pages 231-232). A habcraft can hold 24 people and would weigh about twice as much as a Hab, or seventy tonnes. It would require a nuclear rocket or a solar thermal rocket supplemented by chemical engines to get to Mars on the same 145-tonne lift vehicle as Mars Direct uses. Presumably for safety purposes it would be wisest to send two Habcraft at once, so if trouble developed with one, the other could serve as an emergency shelter. It might also be wise to send the Earth Return Vehicle along in parallel, so that three vehicles were available in emergencies. It would probably also be important to launch a ?cycler? which would be a space vehicle in a permanent twenty-four month orbit around the sun. It would pass Earth when the mission departed from there and would fly to Mars in six months. The Habcrafts and ERV would dock to it. It could be as simple as a spare Habcraft with a docking module, emergency consumables, fuel, and solar panels. It could even have a greenhouse that could be operated remotely when no one was on board. The cycler might need some fuel to modify its orbit to reach Earth at the right time; I don?t know celestial mechanics well enough to know how much Mars?s gravity can do.

At Mars, that planet?s gravity would bend the cycler?s orbit so it returned to Earth in twenty months instead of eighteen, in time for the next mission. Another cycler with a Habcraft attached to it would pass Mars at the time a flight was returning to Earth to provide a similar backup capacity and ample space for the return trip. On reaching Mars, one of the two Habcraft could remain on Phobos to provide a return vehicle; the other Habcraft and the ERV would land on Mars, together carrying all the passengers down.

Under these circumstances, the Mars population, renewed at the rate of 48 people per cycle, and assuming an average stay of three cycles, would grow to 144. If Habcrafts cost about the same as Habs, the budget for the operation would be similar to the budget to send four to Mars, except it might involve three heavy lift vehicles every cycle. Presumably at some point as tourism develops in Earth orbit, the cost of Mars flights will drop. The biggest expense for any space venture is to reach to low earth orbit. Right now with the Space Shuttle the cost runs about $10,000 per kilogram. If the cost drops to $1,000 per kilogram, then the big expense is cut to a tenth of what it is currently.

What government does a hamlet of 13-144 need? Presumably at this size, agriculture has been developed and it may be possible for some couples to stay and raise a family. Small children probably should not fly in interplanetary space, but college students could, so once a couple had children on Mars they?d have to stay at least 15-20 years. If their living quarters were under several meters of regolith, radiation levels would be close to Earth normal, so it is feasible to have children. There are possible problems: Martian gravity may be bad for developing bodies; and children exposed to no cold and flu germs for twenty years might have to spend their first year on the Earth in the hospital, battling all sorts of microorganisms.

A hamlet will need a clinic, a school, family housing, and probably a store, among other things. The school might include provisions for graduate education, as people might arrive half way through their doctorates and would have to finish them up under the watchful eyes of a local geologist or exobiologist. It would definitely have to include full day care for children as young as three months, so as to free up as many people to do work as possible. In many ways, it might function like an Israeli kibbutz. A hamlet would also have the ability to process local materials to fabricate metal, plastic, fiberglass, and glass parts, an ability that could require the importation of hundreds of tonnes of additional cargo. Some of that would include automated equipment and robots. We are close to developing robots to carry out tasks like picking tomatoes; presumably tasks such as that will fall to robots on Mars.

It may make sense for the Commander (appointed by the sending space agency) to have to interact with a Council elected by the hamlet?s residents. If the elections occurred every cycle several months after the new mission arrived, it could represent the new arrivals as well as the old hands. At this point, since the people arriving are not all staying a long time and because the weight of terrestrial cultures will still be heavy, it seems likely that the elections will be similar to those on Earth. An alternative would be to use a New England-style town meeting to serve as a legislative body. With a population of 144 (perhaps 200, if there are a lot of children) there will also be the need to register marriages and births, oversee divorces, and settle disputes. A part-time judge may be needed, who would receive legal advice from terrestrial judges selected by the space agency. The hamlet would therefore possess rudimentary executive, legislative, and judicial branches.

Even at the hamlet level, economic forces will play a role in the further development of Martian settlement. Antarctica?s population balloons to several thousand people every summer, a demonstration of the money attached to pure science; but each Antarctic resident costs tens of thousands of dollars to put there, not tens of millions. If, when Mars gets to the hamlet level, it costs two billion dollars per cycle to send 48 people there, then the cost would be $40 million per person. It would be possible to get many nations to shell out $40 million to place a national citizen on Mars, so that might be one source of funds. The development of scientific and tourist facilities on the moon will also help drive down the cost of Mars settlement because travel times to the moon are much shorter and the same equipment could be used in both environments. But further expansion of Mars inevitably will require some economic incentives and return on the money invested there. Where can those economic incentives be found? Several come to mind.

A. Methane/oxygen fuel from Phobos. In another paper posted on the bulletin board I describe the value of developing a refueling station on Phobos. A Hab, a 4.5 tonne nuclear reactor, a drill, some tanks, and a gas processing unit?mostly items developed for Martian exploration or possibly lunar polar exploration?could inject reactor waste heat into a shaft drilled a hundred or more meters into Phobos, breaking down hydrated minerals and carbonaceous compounds, releasing water vapor, carbon dioxide, methane, and hydrocarbons that could be processed into methane and oxygen fuel. The first use of the fuel would be to replace the two-stage ERV proposed for Mars Direct with a reusable single-stage-to-orbit vehicle of roughly the same mass. A twenty-tonne vehicle (empty) fueled with a hundred tonnes of methane and oxygen fuel could carry about thirty tonnes of cargo to Phobos, where the vehicle could refuel with another hundred tonnes of fuel and head for Earth.

Extra methane and oxygen could be accumulated on Phobos and sent to Earth every cycle. A hydrogen tank used by a solar thermal or nuclear thermal rocket and storing one hundred tonnes of hydrogen propellant could store about 1,600 tonnes of liquid methane and liquid oxygen instead. If some of the fuel were burned to get the rest on a minimum energy course back to Earth, and more burned to lower it into low earth orbit, and if gentle aerobraking were used over a six month period to lower the orbit without use of fuel, one could get about a third of the total into low earth orbit, or about 500 tonnes. That would be more than enough propellant to send the entire next Mars expedition to Mars. If the fuel were worth $1,000 per kilogram in low earth orbit, its total value would be a half billion dollars.

B. Rare materials from the Martian surface. A reuseable ERV/Mars shuttle and a Phobos refueling station would allow transportation of very large loads back to low Earth orbit. Gold is worth about $10,000 per kilogram (ten million dollars per tonne) and if remote sensing allowed the discovery of a Martian Klondike or Sutters Mill, astronauts might be able to pick up a tonne or more of gold as nuggets on the surface. It would be well worth importing a centrifugal sorting machine into which a Martian front-end loader could pour gold-rich regolith. Deuterium is of a similar value and is easier to extract from Martian water than terrestrial water because of a six-fold enrichment factor. The Martian surface is littered with millions of tonnes of nickel-iron meteorites; the first asteroid mining will occur on its surface.

If uranium deposits are found, it might make sense, in the hamlet or village phase, to send to Mars either compact centrifugal separation equipment to concentrate the useful Uranium 235 isotope from the far less reactive U-238, or to send a small breeder reactor to Mars to convert U-238 to Plutonium. The transport of radioactive substances into space is one of the most controversial aspects of space flight in general and the Mars Direct project specifically, because of the perceived danger to the terrestrial environment if the rocket explodes. If Mars could provide the fuel for reactors, RTGs (radioactive heat sources for making electricity), and nuclear engines, then unfueled devices could be lifted to low earth orbit and fueled there. But the ability of a Mars base to supply uranium and plutonium is a function of how much the necessary tasks can be automated (to reduce the personnel necessary), how much the equipment?s weight and power demands can be reduced, how much money can be invested in the necessary technology, and how much the resulting technology can be declassified. Otherwise, Mars could have security agents and spies disguised as planetary geologists before it has policemen.

The final, obvious export Mars has is rocks. A search of the web reveals that right now Mars rocks recovered from Antarctica sell for hundreds of dollars per gram. If Mars rocks were flown to Earth and sold at the local mall for $25 for a one-ounce (25 gram) sample, and $10 made its way back to the Mars mission, and a million people worldwide bought such samples, then 25 tonnes of rocks would be needed and they would raise $10 million dollars. If fossils are ever found on Mars, a large fossiliferous rock outcrop could be chopped up and sent here and sold for possibly several times more.

C. Land. The sale of Martian land would be feasible as soon as Mars has a permanent settlement, and as the population and facilities there grow, demand for land will gradually increase. One psychologically important factor would be to develop ?roads? on Mars as soon as possible. These need only be bulldozer tracks that push rocks aside and smooth the surface for wheeled vehicles. It would relatively simple to develop vehicles on Mars that can drive themselves down cleared roads, either navigating from barcoded pole to barcoded pole, or using image recognition software and an image of the entire route, or following the coordinates fed to it from a Mars global positioning system. Roads connecting stations to each other and to interesting geological sites would be the most intensively photographed sections of the planet, and thus if the land were sold, the owners would have access to images of their property. If land were sold for $1,000 per square kilometer, it would be possible for Mars enthusiasts to buy their own little corner of desert. Multinational corporations could spend millions and buy thousands of square kilometers. If owners had to pay an annual claim maintenance fee of $25 per square kilometer, the money could be used to provide them services or to pay for the hamlet?s budding school. Some of the residents in the Mars hamlet would devote their time to exploring the planet, with a priority given to purchased land so that the owners acquire more information about their property. If something valuable was found on someone?s land?say, exposed chunks of nickel-iron meteorite?those resources could be given priority for exploitation and the owners paid a royalty for them. While this approach costs money, it probably would generate more money than it costs, because people are more likely to buy something if they think they might get a return on it.

The ultimate right of a landowner is the voting right. As landowners begin to increase in number, it would make sense to create a second legislative body that they would elect. Thus a ?Mars Council? would be elected by the residents, a ?Mars Assembly? by the landowners. This approach again makes the ownership of Martian land attractive. If even small-scale owners have a vote, one has the potential to create a large, diverse, grassroots movement on Earth that supports Martian settlement. Individuals with great enthusiasm could buy their own square kilometer and vote. Those wishing to keep Mars red could buy a square kilometer and be heard. Multinational corporations could have one vote as well, and would be heard.


3. The Village. The village will develop when the various economic returns listed above gradually mature, developing a stronger financial basis for Martian settlement. The village will have something the hamlet and station might never have had?senior citizens, persons who arrived in their early adulthood, raised families, and remained. The village (population, 150-1,000) will be possible only if transportation costs continue to drop. The use of solid core nuclear engines could reduce the cost of flying hydrogen to low earth orbit from the moon, or an airbreathing, fully reusable single stage to orbit vehicle might have been developed. If launch costs to low earth orbit fall to the $100 to $200 per kilogram range, tourism to hotels in low Earth orbit will be possible for $50,000 to $100,000. Flights to the moon will drop under $1 million per passenger, meaning that rich tourists could go for a month at a time, and university professors teaching lunar geology could get research grants to spend their summer hiking around Tycho. One-way flights to Mars could drop to $2 million (150 tonnes of fuel would cost $30 million to put into orbit and a nuclear engine could use it to push a Habcraft with 24 people plus maybe forty tonnes of cargo to Mars), meaning faculty with large research grants and a two-year leave of absence could go to Mars, corporations wishing to develop a presence on the Red Planet could send teams, media conglomerates could send a journalist, and wealthy private settlers could be accepted.

One consequence is that the entire population, or the vast majority, would no longer be working for the sending agency, forcing new questions to arise: can corporations own their own property? What about individuals? Should residents be allowed to buy their apartments and sell them later to the highest bidder? Should individuals who paid their own way to Mars be charged income and property taxes? Should agency employees be allowed to quit, stay on Mars, and set up their own companies to mine minerals, raise crops, or provide services to other residents? Under what nation?s laws would they incorporate and sign contracts? If an individual wanted to stay on Mars permanently and wanted to fly up grandmother?s Steinway piano, how much should he or she be charged? Should antiquated agency equipment be sold to a resident who wanted to set up her own company? What if the aging equipment were a Mars shuttle and the person or company wanted to set up a private flight service to Phobos and Deimos? What currency should be used in the village store? What if someone wanted to open a competing store? If a Hollywood company wanted to shoot a movie on Mars, could agency employees moonlight as actors and extras? What if a family wanted to buy an old Hab and roll it 1,000 kilometers down Route 7, and settle way out in the wilderness, all by themselves? What if Denmark?or North Korea?wanted to fly up a dozen people to set up their own station? At what point should the village have its own public access cable television channel? How will health care and retirement costs be paid for? When will welfare and unemployment services be needed? At what point should one resident be allowed to sue another, requiring the establishment of a formal court? When will Mars need resident lawyers, heart surgeons, acupuncturists, a ballet troupe (whose dancing would be spectacular in Martian gravity), an intramural basketball league, a professional hair stylist, and an undertaker? Where will churches worship, and can they buy or build their own structures? When will Mars get its first McDonalds?

At the village level regulations and policies will proliferate. The job of Commander would be a full time. Possibly his/her appointment by the agency would have to be affirmed by the Mars Council and Assembly, or by popular vote. It seems inevitable that there will be private property, mortgages, taxes, health insurance, and a bank branch with ATMs. Consumer goods will still be rare and expensive, but a few will now be manufactured on Mars, and some of them might bear designer labels.

4. The Town. Expansion of the Mars population over 1,000 will require the establishment of a real economy. While Mars might still be receiving annual subsidies?probably of billions of dollars?it would also be exporting by the time it reaches the town phase. With automated manufacturing, a population of 1,000 could provide considerable support for asteroid missions. It might be providing occasional flights to Venus orbit and Mercury to ship fuel, cheap manufactured goods, and raw materials to stations there. A Venus orbital station studying that planet robotically and by remotely controlled aircraft and balloons might be growing their food and recycling their wastes in agricultural units using reprocessed regolith from Phobos. The Venus station might be accumulating water in the Venus clouds using solar powered aircraft, concentrating the deuterium?which is far richer on Venus than on Mars?then selling the deuterium to Earth. The Mercury station might be mining Helium 3 from the Mercury regolith, where it should be far more concentrated than in lunar soils, and the equipment it uses might be made on Mars and shipped via Phobos.

By the time Mars has a town, advanced nuclear or ionic propulsion will have reduced travel times and transportation costs further. It might be possible to send an item from the Earth to Mars for $100 per kilogram. Gaseous core nuclear engines or high-powered plasma engines might be able to fly to Mars in three months, wait a month, then fly back to Earth in three more months, making tourism, grant-funded individual scientific research, and the visits to Mars of medical specialists possible.

5. The Nation. It is difficult to say how many more steps would be necessary before a nation-state (or several nation states) emerge on Mars. Because of the extreme shortage of services, for a long time Mars will probably have a single large population center where the hospital, high school, bank, store, etc., are located. This argues in favor of the eventual emergence of a single nation. Alternately, if Earth?s age-old rivalries are transplanted to the Red Planet, a single central population concentration might not emerge; rather, separate American, European, Chinese, and perhaps Russian villages and towns could emerge, speaking their own languages and selling goods and services to each other. There is likely a relationship between financial self-sufficiency and independence; once the colonies begin to cover their own costs, independence becomes likely.

A nation state might be possible with only a few thousand people. When the Massachusetts Bay Company set out with less than a thousand settlers for New England in 1630, it was setting up a de facto independent settlement that was not brought under royal control for a generation. Cleverly, the charter of the Massachusetts Bay Company?approved by the King?did not specify where the annual meeting of the stockholders would be held. Thus while wealthy English merchants owning shares in the Virginia Company met in London every year to select a governor of their private colony, the middle class Puritan small businessmen investing their life savings in the Massachusetts Bay Company boarded the ships themselves, sailed for Boston, and held their annual stockholders? meeting there, and the company?s governor was elected by the colonists themselves. By 1640 religious persecution had driven 10,000 Puritans to New England, where they had imported America?s first printing press, established its first college, elected its first local and regional governments, and built an economic base on the export of codfish and foodstuffs to the Caribbean.

For Mars, a planet of unexploited mineral wealth and the promise of mineral wealth in the asteroid belts might provide a similar economic base. The promise of an entire planet of land to settle, the prospect of nearly free land, and mature technologies for reliably extracting water and oxygen from local resources could open much of Mars to settlement, and if relatively inexpensive transportation becomes available, millions could emigrate to Mars, just as they did to the Americas in the late nineteenth century. The steady development of economies of Earth may make it inevitable. If per capita productivity in the United States were to grow 3% per year?as it did in the 1990s--in twenty-four years Americans will be twice as wealthy in real terms as they are today; in forty-eight years, four times as wealthy; in seventy-two years, eight times as wealthy; in ninety-six years, sixteen times wealthier than they are today. As fantastic as this seems, Americans in 2000 are about sixteen times as wealthy as their grandparents were in 1900. Average national annual incomes of half a million dollars in current dollars may be seen by the end of this century. How many will want to save for a trip to Mars? How many parents might help their children buy a ticket for Mars as a graduation present? Only time will answer these questions.

#1681 Re: Mars Gravity Biosatellite » Go Translife » 2002-01-25 00:33:50

Here's the formula for calculating gravity: F = (0.0011)W2R where F is in gravities, W is the spin rate in rpm, and R is the radius (spin arm) in meters. This is found in Zubrin, *The Case for Mars,* page 123. He also notes the following on that page:
for making Martian gravity, 1 rpm requires an r of 345 meters; 2 rpm requires an r of 86 meters, 4 rpm requires an r of 22 meters, 6 rpm requires an r of 10 meters.

I also favor centrifugal gravity. Weightlessness produces effects similar to prolonged bedrest and aging: oseoporosis, cardiovascual weakening, muscular weakness, etc. Millions of dollars is being poured into ameliorating those conditions.

Zubrin also notes that many spinning spacecraft have performed midcourse corrections without despinning first; the correction is chopped into a series of computer-controled short bursts and are timed for the moment the engine is pointed the right way. He favors putting useless weight at the other end of the tether, not a vital part of the mission.

                     -- Rob S

#1682 Re: Water on Mars » Water ice on Mars. - Elaborate breakdown of the polar caps. » 2002-01-25 00:21:02

An extremely important factor is altitude. The northern cap is built on top of the northern lowlands, the southern cap on top of the cratered highlands. The southern cap is thus at a much higher altitude than the northern and experiences a lower atmospheric pressure. The vapor pressure of CO2 is very sensitive to temperature. According to my CRC, page D-150, the vapor pressure of CO2 at -135C is 1 millimeter of Mercury, but at -110C it is 34 millimeters of Mercury. Thus at high altitude, a CO2 cap will sublimate away; while it is colder at a higher altitude, it is not colder enough.

                -- RobS

#1683 Re: Life support systems » We need a brainstorming session! - Bat around a few ideas. » 2002-01-25 00:10:11

Actually, I think Shaun's idea of air shielding is clever. The Earth's atmosphere provides 10 tonnes per square meter of air over our heads, and half of that is in the lower 5 kilometers or so of the atmosphere. Air has a mass of 1.5 kilograms per cubic meter when compressed at 1 atmosphere of pressure. So 100 meters of air would provide 150 kilograms of shielding per square meter of surface. The entire Martian atmosphere provides about half of that. The Hab's radiation shelter on the flight out to Mars provides 350 kg per square meter.

But the simplest, most practical shielding is to build the living and work areas with several tonnes of mass overhead, by loading their roofs with dirt. People are outside only a few hours a day, usually, so their radiation exposure while outside would not be serious. They could always minimize it during solar flares.

I, too, favor transparent domes, though in a posting on another topic I suggested the domes might need to be covered with an insulating shroud at night to help hold in heat. You would want to let in some ultraviolet, if possible, because bees need it to navigate. This was a big problem with Biosphere 2 down in Arizona, because glass does not admit ultraviolet. Bees starved to death and went extinct in Biosphere 2 because they could not navigate from hive to flower and back; they could not see the sun in ultraviolet. Setting up a few uv lights didn't help, either.

One could easily bury a dome's edge so that one could walk right up to it and look out. Perhaps the opposite side of the dome would have housing with big windows, so people could look out over wheat fields to a barren Marscape beyond. The only danger is the ease one makes very serious vandalism.

                       -- RobS

#1684 Re: Mars Gravity Biosatellite » Go Translife » 2002-01-23 15:20:42

These are very interesting questions. Zubrin's book gives a formula for calculating the radius and revolutions per minute for any particular amount of gravity. I seem to recall seeing in a book about space colonies that one can get 1 Earth gee at 1 rpm when the radius is about 900 meters. I'll try to find the details and post them in a few days.

I've never seen what the plan is for the Mars Direct Project's return. Astronauts have spent six months in zero gee before and they adjust fine over a week or two (well, some have longer term problems, but minor ones). I was wondering whether the burnt out upper stage of the ERV could be used as a counterweight vis a vis the crew cabin. One could gradually spin up the rotation rate from Mars gee to Earth gee, so that the astronauts gradually adjust to the higher gravity.

                  -- RobS

#1685 Re: Human missions » Mars? Moon first. - Mars is too hard and dangerous for now. » 2002-01-23 15:06:28

Josh has indeed gotten a good thread going on water on Mars, located under "Acheron Labs."

Zubrin's *The Case for Mars* has an entire section about how to extract volatiles (mostly water) from Martian regolith. Most of the techniques would work on the moon as well. If equipment can be manufactured that can handle extremely cold materials (it does not matter whether there is a vacuum or not; if regolith is -150 Centigrade and is on a backloader, it will make the backloader blade -150 as well) then the regolith can be processed to remove the volatiles. Loads can be dumped into a furnace and heated with spare reactor heat. Or a plastic tent could be spread over the ground, anchored, and the regolith could be zapped with microwaves, or a mirror could reflect sunlight onto it. The escaping volatiles will inflate the tent and can be pumped into tanks, compressed, separated, etc. Or one could drill a shaft into the volatile-rich regolith, it could be heated, and the escaping gasses captured.

We do not know how much water, CO2, etc., there is at the lunar poles. Paul Spudis, who ran the Clementine experiment, has estimated it, and it was in the millions of tons or billions of tons range, I believe. Interestingly, the poles of Mercury appear to have more.

Most likely lots of fuel can be obtained from the lunar poles. But even at the equator there may be volcanic minerals with water in them, and the surface materials are full of oxygen. It takes a lot of energy to liberate it, but note that hydrogen-oxygen fuel is 90% oxygen by weight, and methane/oxygen fuel is 80% oxygen by weight.

One problem no one has discussed: from Earth, it is comparatively easy to enter an equatorial orbit around the moon, but apparently it is fairly difficult to enter a polar orbit. Does anyone know how much more energy it takes? This makes a big difference in terms of the use of the lunar poles as "gas stations" for interplantary exploration. Otherwise, one imagines convoys of tanker trucks rolling from Aitken to Mare Imbrium every lunar night, carrying liquid hydrogen to the moon's main spaceport. . .

                      --RobS

#1686 Re: Water on Mars » Water ice on Mars. - Elaborate breakdown of the polar caps. » 2002-01-23 12:26:00

Josh, thank you for these data. I wish I could give you a source for this additional information, but it was preweb; probably something I read 1975-77 when I was a graduate student in planetary science at Brown. Or maybe it was in the 1980s. Someone calculated that under the north polar cap, the pressure from the overburden soon gets too high for solid carbon dioxide to exist; it sublimates under pressure unless the temperature gets lower (and with geothermal heat, with increased burial the temperature goes up).

So this makes it impossible for the northern cap to be CO2. But it might be a CO2/H2O "clathrate," which is a combination of the two compounds. There has been some research done on clathrates. One could check the old Icarus abstracts if they are on line, like the new ones are. The article about clathrates on Mars may have been there. I think there have been Icarus articles about clathrates in the Jupiter and Saturn systems, too.

Even if they are clathrates, though, it does not change the total water in the polar cap by an order of magnitude. Maybe by an order of two; but that's still a LOT of water!

                     -- RobS

#1687 Re: Water on Mars » A Soggy World ... Maybe! - Looking at a Globe of Mars » 2002-01-23 12:18:39

I'm not sure whether it is 40% or 10%, but I was surprised to read something recently that said the Earth could face runaway greenhouse effect and head toward a Venus-like future in a mere billion years. I wonder whether 10% would do that. But I am not sure what the projection of future brightness increases is. Thanks for asking.

                             RobS

#1688 Re: Interplanetary transportation » Plasma Rockets - the best propulsion system yet... » 2002-01-22 12:29:45

Can you give a web address where more information can be found? If not, don't worry about it. I am curious how the engine works and how much energy it uses. If it could get us to Mars in three months but it takes six or eight months of energy to power the engine, it doesn't actually speed up the trip. Currently nuclear reactors weigh something like 45 tonnes per thousand kilowatts of electrical output, so if you need 10,000 kilowatts, the reactor gets extremely large (450 tonnes); or you need about 100,000 square meters of solar panels at a minimum of 4 kg per square meter, which is 400 tonnes of solar panels. This may explain why NASA doesn't spend much money on the process, too; there's no reason developing an engine that cannot currently be powered.

                  -- RobS

P.S.: I should add, though, that the figure for the weight of a reactor comes from a 1977 publication about space colonies. Maybe we can do better now (by a factor of 2 or 3?). And solar panels are getting more efficient as well.

#1689 Re: Water on Mars » A Soggy World ... Maybe! - Looking at a Globe of Mars » 2002-01-22 00:28:59

Alas, I have not followed the research in detail for about 20 year, but I gather that a "cold wet Mars" model is also being considered by many people. The large outflow channels could have been formed not by a single flood of a few days, but a constant flow of ground water over many years that freezes as it flows, choking its own channel with ice and therefore forcing it to make the channel wider. That's an argument some have made. A few outflow channels appear to flow uphill, which is possible under a glacier. There appear to be eskers on Argyre Planitia, which are channel deposits formed under a subglacial river.

So it may be that in the first billion years or so, Mars was close to freezing, but usually below. Volcanic activity was much greater than today, with millions of square kilometers being repaved by basalt flows. The flows brought heat to the surface as well as water. So water accumulated in the regolith partly as vapor perculating upward, partly as snow (it may have snowed; this would explain the few gullies that appear to come from meteorological sources) and when volcanic activity occurred in an area vast quantities of permafrost melted, oozed out their water, sometimes gushed out their water. Some of the Mariner Canyons were filled with lakes; the horizontal strata of lakebed deposits seem to be visible in some pictures. As Mars aged, the volcanic activity decreased, more and more water and air escaped into space, and the episodes of water flow and even precipitation grew less and less.

A billion years or so from now, when the sun is 40% brighter than today, Mars may have a brief renaissance, then the atmosphere leaks away at a faster rate and we have a "warm dry" Mars model instead!

                    -- RobS

#1690 Re: Exploration to Settlement Creation » Domed habitats... - ...size, materials, and more. » 2002-01-21 00:37:37

Bill White makes some excellent points. Zubrin, in Case for Mars, also assumes that one would not use hemispheres, but "flatter" structures that do not go as high. I did my calculations with hemispheres because I do not know how to calculate volumes and surface areas of "flatter" structures. Zubrin said the thing to do is to use a portion of a sphere less than a hemisphere, like slicing the "top" or "bottom" off a globe.

Yes, a flattened hemisphere has less surface area and therefore would generate less upward pull, decreasing the amount of dirt needed to anchor a dome somewhat. Since I do not have the ability to calculate the area, I do not know what it will be. Consider that the surface area being domed over is a function of pi r squared but a hemisphere is 2 pi r squared. A flattened hemisphere would fall between those numbers, depending on the flattening.

Multiple layers do not have to decrease the available light. Zubrin says a 1 millimeter thick kevlar layer can hold in air at an entire terrestrial atmosphere of pressure. Let us say we divide the layer into four 1/4 millimeter thick layers, and let each layer approximate a true hemisphere more closely (rise higher and higher from the center of the enclosure). And let us assume that each layer holds in 1/4 of the total pressure underneath. A leak from the bottom layer into the next one would not necessarily exceed its yield strength if the layers were able to accommodate 2 or 3 times their standard design pressure, and by spreading the air out in a larger area the pressure on the second layer would be reduced anyway. Presumably 4 layers 1/4 mm thick block as much sunlight as 1 layer 1 mm thick.

As for multiple levels of plants, this assumes artificial lighting, which assumes an ample source of energy. The surface of the earth receives over 1 kilowatt of sunlight per square meter, constantly during the day. On Mars that is already reduced to less than half, which is a problem for some plants (some vegetables and grains do not grow well when they get only six hours of sunlight per day. I know; my backyard garden is partially shaded). A dome with multiple levels of plants reduces their light exposure even more. If you have to supplement 10,000 square meters of plants with artificial light, you may need 10,000 kilowatts of power to do it! It's easier to spread the plants out under domes and use mirrors to give them some extra light.

                     -- RobS

#1691 Re: Interplanetary transportation » Phobos and Deimos - The importance of Mars's moons to explor » 2002-01-21 00:13:08

Phobos and Nuclear-Free Mars Exploration


One of the most controversial aspects of the Mars Direct plan is its use of nuclear power. It is difficult to imagine an alternative power source that is both as efficient, per kilogram of weight, as easy to deploy and control remotely, and as reliable. Solar power on the Martian surface requires large arrays and weights, too large to deploy without direct human intervention, and is diminished by dust storms. Wind power requires enormous blades, elaborate deployment, considerable weight (probably close to a ton per kilowatt), and produces variable outputs, maximal during dust storms and much less except in areas with seasonal winds (such as spring near the polar edges). Solar and wind power complement each other and, together, can meet the needs of Martian settlements, but at a high cost.

If a nuclear reactor were not available, the ?Mars Semi-direct Plan? (Case for Mars, pages 67-69) would have to be used. In this plan, in addition to a Hab, it would be necessary to launch to Mars a ?Mars Ascent Vehicle? (MAV) that would land on the Martian surface fully fueled, and an ?Earth Return Vehicle? (ERV) that would go into Martian orbit, fully fueled, for the return trip to Earth. The MAV would carry the crew to the ERV, which would carry them home.

If nuclear reactors are not available, the Mars Semi-Direct Plan probably becomes inevitable for the first few flights, but it need not be followed forever. Possibly the cheapest and most flexible alternative would be to place a solar power array on Phobos and beam it to the Martian surface using microwaves. If the array were placed at the north or south pole of Phobos it would be in constant sunlight, except when Phobos is in Mars?s shadow (which is up to 38% of each orbit). A Phobosian array will generate more power than a similar one on the Martian surface and can be built to track the sun much more easily because of the moon?s near-zero gravity and no need to consider the force of surface winds on the arrays.

An array to collect 250 kilowatts of sunlight on Phobos, assuming the collection of 0.05 kilowatt per square meter (less than half the collection on Earth) and a mass of 4 kilograms per square meter, would require 5,000 square meters and would have a mass of 20 tonnes. When one takes the effect of Mars?s shadow into consideration, the array collects a continual average of 155 kilowatts. In Phobos?s gravity (6/10,000 that of Earth) the array would weigh 26 pounds. Mirrors, which can be constructed more lightly for use on Phobos than on Mars because of the lack of gravity, can be used to concentrate sunlight onto solar cells. Such mirrors conceivably could cut the mass of the array in half. The solar array will also need a fuel cell system with hydrogen and oxygen or (newer) methane and oxygen tanks to store energy for broadcast when the rectenna is above the horizon.

The technology that could beam the power to the surface of Mars has been studied and tested, but not extensively developed (T. A. Heppenheimer, Colonies in Space [N.Y.: Warner Books, 1977], pages 38 and following). It is basically the technology assumed for power stations in Earth orbit, which were extensively studied in the late 1970s. The direct current produced by the solar cells would be converted into a microwave beam and aimed at a rectenna on the Martian surface, where it would be converted back to direct current electricity. The overall system efficiency is about 60%, which means that of the 155 kilowatts produced on Phobos, 93 kilowatts of useable power arrives on the Martian surface. If the energy is beamed at the surface at a density of half a kilowatt per square meter (much more than would be allowable on Earth, but reasonable on Mars, and just equal to the energy density of sunlight there) and the power can be received ten hours a day (because Phobos is above the horizon only half of the time, and is rather close to the horizon some of the rest) the receiving array would require an area of 450 square meters. The rectenna would have a mass of 5 kg/m2 (Richard Johnson and Charles Holbrow, eds., Space Settlements: A Design Study [NASA, 1977], page 158; much of the information in this paragraph comes from this source) or a total mass of 2.25 tonnes. It might be wise to make the rectenna twice as large to simplify the pointing of the beam. The result?4.5 tonnes?is comparable to the mass of the nuclear reactor proposed for the Mars Direct mission.

The power array on Phobos possibly could be deployed remotely, but more likely it would require a human crew to be set up and tested; if no nuclear reactor is available for Mars exploration, presumably it would be set up on the first flight. But once set up, it would be capable of beaming microwave power to much of the surface of Mars. Phobos rises in the west, passes overhead, and set in the east 5 hours and 33 minutes later; thus it appears in the sky twice a day (Deimos, in contrast, takes 5.5 days from moonrise to moonrise, because it orbits Mars once every thirty hours, close to the length of a Martian day). Phobos is not visible north or south of 70 degrees of latitude (Samuel Glasstone, The Book of Mars [NASA, 1968], page 71; much of my information on the orbits of Phobos and Deimos comes from this source), though it will be rather close to the horizon north or south of 55 degrees, which may be the practical limit of receiving beamed power. Once the beamed power system were established, subsequent Mars missions would only need to bring rectennas along. Mobile crews on the Martian surface could take a small rectenna along, deploy it every night (probably a safe kilometer or two away from them), and pick up the power they need for the next day while sleeping.

Once established and tested by the first crew (using the Mars Semi-Direct plan), the power system would permit a switchover to the Mars Direct plan. To be more precise, it would allow a switchover to an even better system involving the manufacture of methane and oxygen propellant from the carbonaceous chondrite material of Phobos itself, allowing vehicles from the Martian surface to refuel before they flew to Earth (see my previous posting, ?The Importance of Phobos in Mars Exploration?). Solar power capture, conversion, and retransmission will be highly reliable if the solar arrays are located on at least three towers a few hundred meters from each other, if at least three fuel cells and associated fuel tanks for power storage are set up, and at least three transmission antennas are available. Such a system would be capable of beaming power to up to three different locations on the Martian surface. As Mars settlement advances, the Phobos Power Station could be expanded in total output and number of transmission antennas to provide power to more and more places.

Whether the system outlined above will work requires the answering of several questions:

1. Whether it is possible to beam energy with sufficient precision to hit a small target on the Martian surface from an object moving around the planet. If it is not, there is another way to transmit power to the Martian surface: one could manufacture methane and oxygen fuel on Phobos (see my ?The Importance of Phobos in Mars Exploration?) use it to fuel a space vehicle, fly the vehicle remotely to the surface to drop off thirty or forty tonnes of fuel, then return it to Phobos to pick up another load. Once on Mars, the methane and oxygen fuel could be run through fuel cells or internal combustion engines to make electricity.

2. Whether the existing technology can function under Martian conditions (especially low temperatures) or whether expensive modifications are needed.

3. Whether dust storms will effect the transmission. I know little about microwave transmission, but I gather a small amount of dust will not diminish the beam significantly.

Another benefit of the system should be noted:  The microwave transmission system could also be used to warm small areas of the Martian surface (1,000 square meters) and drive volatiles from the regolith. Astronauts would first cover the area with an airtight plastic tent (by burying its edges), then have the area cooked with microwaves for several days to drive out the water.

A similar solar array and microwave transmitter system could be established on Deimos if high-latitude stations need power. Deimos can be seen as far north or south as 83 degrees, and therefore could power stations located up to 68 degrees, perhaps more if special rectenna towers were built.

#1692 Re: Interplanetary transportation » Phobos and Deimos - The importance of Mars's moons to explor » 2002-01-20 07:43:32

I was surprised to see that carbonaceous chondrites had so much water in them. The data comes from the web--not always the best source--but I see no reason to assume they're vastly wrong.

As I noted in another posting somewhere, there are stony asteroids, carbonaceous ones, and metallic ones. The metallic ones won't have much carbonaceous content to provide fuel for a return flight, and the carbonaceous ones don't have much metal. Most likely an asteroid can be found that is a fusion of several from collision that will have all the materials one needs for a good mining colony.

But meanwhile, Mars has all three. If one wants to mine asteroids, one can start mining the zillions of tons scattered across the Martian surface; and that effort would have the advantage of a local infrastructure (maybe even a hospital!) to provide support. Yes, Mars has a gravity well, but in terms of fuel it's much less deep than Earth's, and Phobos is smack dab in the middle of it to serve as a permanent "second stage"; Earth's gravity well is 25,000 miles per hour "deep" and that's 2.5 times the exhaust velocity of hydrogen and oxygen, requiring a mass ratio (fuel to payload) of 11.2 to 1. Mar's gravity well is only 12,000 miles per hour "deep," requiring a mass ratio of 2.3 to 1. The Mars Direct's ERV could be modifed into a reuseable "space shuttle" to shuttle back and forth between the surface and Phobos or Phobos and Earth orbit.

This is not to say that the asteroid belt won't be mined. Just that Mars will be the testing ground, because it's cheaper. It could be mined twenty or thirty years before asteroidal mining is tried, giving it a big advantage. And if you want to raise a family, the cosmic radiation and zero gravity may make that impossible in the asteroid belt; those guys (and gals) will have their spouces on Mars or the Earth.

                         -- RobS

#1693 Re: Interplanetary transportation » Phobos and Deimos - The importance of Mars's moons to explor » 2002-01-19 00:58:44

The Importance of Phobos in Mars Exploration


A crucial and often underappreciated resource for the exploration and eventual settlement of Mars is Phobos and, to a lesser extent, Deimos, its two moons. Phobos is an average of 22 kilometers in diameter, has a mass of 10 quadrillion tons, and orbits about 6,100 kilometers above the Martian surface. Its surface gravity is six ten thousandths that of Earth; thus a five-ton (10,000 pound) boulder on Phobos has a weight of only six pounds.

From the point of view of delta vee (launch velocity), Phobos is about as ?close? to low earth orbit as the Moon; on average, an object in Martian orbit only needs an additional 2.6 kilometers per second (5,800 mph) to enter a Hohmann transfer trajectory to Earth, whereas from the surface of the moon an object needs 2.4 kilometers per second (5,300 mph) to reach low Earth orbit. But this is not the entire story. Some of the most ?interesting? areas of the moon?its north and south poles, where there may be large quantities of volatiles trapped in the regolith?take more delta vee to reach because an orbital plane change is necessary. Furthermore, while the energy needed to reach low earth orbit from either may be approximately the same, the energies needed to go from low earth orbit to Phobos or to the Moon are radically different, because the Martian atmosphere allows aerobraking. Once a vehicle has entered Mars orbit, a relatively small delta vee is sufficient to land on Phobos; but a 2.4 kilometers per second deceleration using a rocket engine is necessary to land on the Moon. Thus from the point of view of round trip delta vee, Phobos and Deimos are the closest objects to the Earth in the solar system. This advantage is somewhat negated by the fact that a flight to them takes six to nine months, the return flight requires the same length of time, and that a round trip requires a wait at either Phobos or Earth of thirteen to seventeen months.

Phobos is also the closest object, in terms of delta vee, to the Martian surface; a rocket needs about 3.8 kilometers per second to reach Phobos. For a methane/oxygen rocket the resulting mass ratio (fuel to payload) is 1.74 to 1.

Phobos is significant because all evidence suggests it is made of carbonaceous chondrite, a stony material rich in water, carbonaceous compounds, and sulfur. The quantity of water and carbon compounds in carbonaceous chondrite meteorites varies; one website gives the average composition of carbonaceous chondrite as 2% carbon, 0.2% nitrogen, 1.8% metals, 83% silicates, and 11% water (http://www.ibiblio.org/lunar/school /solar_system/minecarb.html). The water typically is bound to the silicates, which are clays. The carbon is largely present as ?kerogen? and the kerogen is 77.5% carbon, 7.5% hydrogen, 1.5% nitrogen, 12.0% oxygen, and 1.5% sulfur.

Carbonaceous chondrites can vary from 1% to 5% carbon. We do not know Phobos?s average composition, but clearly it contains a vast amount of carbon, oxygen, and hydrogen, the elements for making methane (CH4) and oxygen fuel. If only 1% of Phobos?s mass could be converted into fuel, the quantity still amounts to 100 trillion tons.

Can the gasses be profitably and easily extracted from the chondrite? The Mars Direct plan already includes many of the elements necessary to set up a fuel manufacturing station on Phobos. A Hab could be landed on Phobos to provide housing for a crew (presumably, because of the moon?s nearly zero gravity, crews could not remain on Phobos more than three to six months, so a permanently inhabited station would require rotating crews down to Mars. Mars would also be the Phobos station?s principal source of supplies).  Mars Direct?s Earth Return Vehicle has a first stage that is approximately of the correct power to take crews from the Martian surface to Phobos; if the second stage were replaced by a cargo compartment and modifications that allowed the ERV to be reused, the ERV could serve as the Martian equivalent of the space shuttle, hauling perhaps twenty tonnes of cargo from Mars to Phobos per flight.

More importantly, the Mars Direct plan includes a 4.5 tonne nuclear reactor capable of producing 100 kilowatts of electricity and about 2,000 kilowatts of heat energy. One way to use this energy would be to drill into Phobos. Carbonaceous chondrite is very friable (crumbly); meteorites made from it that land on Earth disintegrate into piles of mud after a few rainstorms. A driller weighing a tonne or two would be capable of drilling hundreds of meters, perhaps kilometers, into the moon. The driller would face two obstacles in doing its work:

1. Drills rely on gravity to press themselves against the surface being cut. Gravity is inadequate for the task on Phobos, so the driller will have to be staked and bolted to the rock.

2. Phobos is cold inside; one website says ?112C (http://www.bbc.co.uk/science/space/ solarsystem/mars/phobos.shtml). Drill bits and other equipment will have to be able to handle exposure to cold materials.

Once a suitable shaft has been drilled, adding heat will drive off water, carbon dioxide, and hydrocarbons (methane and longer chain hydrocarbons of the sort found in petroleum and natural gas). Some of the gasses will enter the drill shaft and rise to the surface, where they can be captured and processed; some will escape into cracks and pores in the rock and freeze solid. Phobos has a mean density of 1,900 kilograms per cubic meter, almost twice the density of water, and research suggests the interior consists of matter that is three times or more the density of water plus 10-35% pore space (http://www.psrd.hawaii.edu/Aug99/asteroidDensity.html). This is not unusual; loose sand can have up to 40% porosity. It will be necessary to test a piece of chondrite (or better, a piece of Phobos) to determine exactly how much heat drives off how much of the carbon, hydrogen, and oxygen. Most of the escaping gas will be water vapor, with carbon dioxide second. Methane, ammonia, alcohols, ethane, butane, benzine, and other simple hydrocarbons can be expected to be produced as well. Water vapor can be electrolyzed into hydrogen and oxygen, with the latter being stored; the hydrogen can be run through a Sabatier reactor to make methane and water vapor from carbon dioxide.

The rate at which the methane, oxygen, and other materials are produced is a function of the energy available to liberate them. A cubic meter of Phobos material weighs almost two tons and requires about 1,000 kilocalories to be heated by 1 degree centigrade (I am here assuming rock takes about a half kilocalorie to heat a kilogram one degree Centigrade. This is half the heat capacity of water and is about right, but will vary depending on the minerals.) A thousand kilocalories is equal to 1.16 kilowatt-hours. Thus 100 kilowatts of heat can raise the temperature of a cubic meter of Phobos material 86 degrees centigrade in an hour.

If the heat is being put into the shaft using a simple electric heater, the heat will travel inward through the rock. If the shaft is 100 meters deep, it has 314 cubic meters of rock within 1 meter of the shaft. One hundred kilowatts will heat that quantity of rock about 6.5 degrees a day; in a month it will be heated from ?112 C to 85C, and in another month to 280C. Such a temperature should be sufficient to drive off a large fraction of the volatiles. In four more months the material within two meters of the shaft can be heated to that temperature. As the rock gradually cools by conducting the heat to material farther from the shaft, volatiles will continue to be released, even without additional heat input.

Within 1 meter of the shaft is 628 tonnes of Phobos material, containing about 60 tonnes of water and 12 tonnes of carbonaceous material (based on previously quoted estimates). Tests would be necessary to determine how much of the released volatiles would go up the shaft. The volatiles escaping laterally, however, will largely freeze to ices and can be captured later by shafts driven parallel to the first and a few meters away.

Yields from a shaft can be increased in various ways. If hydrogen and oxygen (from electrolyzed water) are pumped down the shaft and lit to make a flame, and the amount of hydrogen added is in excess to the amount the oxygen can consume, the hot hydrogen will interact with the carbon compounds to make methane and with the silicates to make water vapor. Conversely, if the oxygen is in excess to the amount the hydrogen can consume, the hot oxygen will interact with the carbonaceous materials to make carbon dioxide. Sulfur and nitrogen compounds will also be produced. The gasses escaping from the shaft will have to be separated cryogenically, stored, and then further combined or split to yield the compounds desired.

Once a quantity of volatiles has been accumulated, it would no longer be necessary to use electricity to heat the rock in the shaft; reactor heat could be sent down the hole in the form of steam. Hot water, interacting with rock, will help remove carbon compounds. If hydrogen is added to the steam, methane will result.

A one hundred kilowatt reactor on the Martian surface, working with atmospheric carbon dioxide and imported hydrogen, can make 108 tonnes of methane and oxygen in six months (Mars Direct, page 5). It appears that a similar quantity should be possible on Phobos in the same timeframe. Some of the energy used on the Martian surface must go into splitting carbon dioxide into oxygen and carbon monoxide to augment the oxygen supply This process is probably unnecessary on Phobos, since the literature suggests more water will be produced than carbon dioxide. Thus it appears a reactor on Phobos could produce more fuel than one on Mars.

An alternative method may need to be considered if the shaft leaks too much volatiles back into Phobos, reducing the yield out the top of the hole. A robotic digging device could be operated from the Martian surface which would transport a tonne or two of Phobos material to an oven attached to the reactor, where it would be baked and chemically treated, its gasses extracted, and then the slag dumped. The advantage of this method is the degree of control gained over the processing; rock temperature and the application of hydrogen and oxygen can be monitored and tailored to the composition of the material, and yield maximized. The disadvantages include the greater involvement of scarce human resources and the problem of controlling vehicles and materials in near zero gravity. Whereas a well shaft would produce relatively little dust but could release a lot of gasses into the space around Phobos, the use of vehicles and ovens could produce dust clouds and create waste disposal issues.

If the assumptions above are approximately correct, they imply that a 100-kilowatt reactor should be capable of producing several hundred tonnes of methane and oxygen propellant per year. Solar arrays erected at the north or south pole of Phobos where there is perpetual sunlight could increase the available electricity, allowing more reactor heat to be pumped down the various shafts, which could be extended deeper and expanded outward in ever larger arrays.

How could the propellant be used? An example may illustrate the implications. The current space shuttle?s external tank weighs a bit less than 30 tonnes and can hold 2,000 cubic meters of propellant. When divided appropriately between hydrogen and oxygen, it can carry 780 tonnes of the two. If the same stage transported liquid hydrogen only, it would hold 143 tonnes. If it carried methane and oxygen it could hold 2,100 tonnes. In all these cases the gasses need to be segregated in tanks of appropriate size, but if the interior space were divided into four or five tanks of different sizes, all the above combinations could be accommodated.

Perhaps half the external tank?s weight is necessary because it must hold together during accelerations of 2 or 3 gees while tearing through the terrestrial atmosphere at thousands of miles an hour. An expert would have to redesign the tank for use exclusively between planets, but I suspect the tank?s weight could be reduced to fifteen tonnes, maybe less.

A tank of size similar to this could be flown to Mars if a nuclear engine were used to push cargo or people to the Red Planet. A 1.5 tonne solid core nuclear engine generating forty-five tonnes of thrust (such as the Timberwind design, specific impulse, 1,000 seconds) could use a tank such as this, with 143 tonnes of liquid hydrogen, to push three hundred tonnes to Mars. Alternately, the tank itself could be pushed to Mars with about twice as much fuel as its final weight (thirty tonnes of liquid oxygen and hydrogen, if the tank?s weight were reduced to fifteen tonnes). The tank could be ?landed? on Phobos ( twenty tonnes of mass weigh 26 pounds there!) and over the next year it could be filled with 2,100 tonnes of liquid oxygen and methane (assuming the facilities on Phobos were designed to produce that much). At the next opposition the tank could take off from Phobos (2,100 tonnes of mass would weigh 2,772 pounds!) and head back to Earth on a Hohmann trajectory. It would arrive nine months later with about 900 tonnes of fuel, and if a series of gentle, incremental aerobraking maneuvers can bring it to low earth orbit with a minimal expenditure of energy, when it arrives it could possibly be the largest object ever placed in low earth orbit in a single launch. Nine hundred tonnes of methane and oxygen could propel four hundred tonnes of cargo back to Mars or soft land 250 tonnes of payload on the moon.

If, instead, the stage flew from Phobos to Venus, it would arrive with 403 tonnes of methane and oxygen, or any other payload desired. If fuel were burned to place a payload into a high Venus orbit (delta vee of perhaps 1 kilometer per second; the payload might be water, carbon dioxide, and processed Phobosian regolith to serve as a basis for agriculture and radiation shielding in a permanent orbiting scientific station) it could deliver about 300 tonnes. If instead the stage flew past Venus and used that planet to bend its trajectory to Mercury, it could arrive in Mercury orbit (delta-vee of 4.3 kilometers per second) with 122 tonnes of payload. This would be enough to send a Hab and crew back to Earth via Venus.

This example shows the potential of Phobos (and Deimos as well) to serve as the ?gas station of the solar system,? as someone once called it. It suggests the following about the exploration of Mars:

1. An expedition to Phobos and Deimos should be mounted as early as possible, possibly the first or second manned mission. It would be easiest to visit the moons upon arrival when the Hab could be landed, then later sent to the Martian surface. If the missions arrived at Mars during its northern hemisphere spring, when dust storms are common, two weeks on either moon could be a valuable use of orbital time.

2. A goal of the first expedition to either moon should be to determine its efficacy for propellant manufacturing. This would be accomplished by extensive sampling, seismic study of the moons? interiors, and possibly drilling.

3. A follow-up expedition should be scheduled for the third or fourth manned mission to Mars with the goal of leaving a reactor, remotely operated drill, gas processing plant, and cryogenic storage tanks, perhaps ten tonnes of equipment altogether.

4. By the fourth or fifth manned mission to Mars, a Hab could be left on Phobos (and later on Deimos) with the astronauts landing on the planet in the ERV instead (to stay in one of the Habs placed on Mars by earlier crews).

5. Possibly as early as the fourth or fifth manned mission, the two-stage ERV could be replaced by a one stage ?Mars shuttle? that could visit Phobos and Deimos at least once during the eighteen-month stay on Mars. Astronauts returning to Earth would fly the shuttle to Phobos, refuel, and then continue to Earth.

6. The capacity to refuel on Phobos opens up the possibility of hauling cargo back to Earth. If a single-stage ERV refueled on Phobos, it probably would be able to transport about twenty tonnes of cargo from the Martian surface to Earth. Twenty tonnes of gold nuggets would be worth about 200 million dollars and could cover a tenth the cost of an expedition. If Mars rocks were sold to eager collectors for ten dollars a gram (that?s about $1000 for four ounces), twenty tonnes of Mars rocks would also be worth $200 million. Current prices for Mars meteorites are in this range, though twenty tonnes might flood the market. If fossiliferous strata are found on Mars, in particular, Mars rocks could be sold for that much or more.

7. If Mars develops the capacity to place 900 tonnes of liquid oxygen and methane into low Earth orbit every 26 months, it revolutionizes transport costs to Mars, reducing the cost of future expeditions significantly, and reduces the cost of other orbital tasks. Currently launch costs are nearly $10,000 per kilogram to low earth orbit. Even if the costs have dropped to $1,000 per kilogram at the time of Mars exploration, 900 tonnes of propellant would be worth almost a billion dollars.

8. Longer term, Phobos and Deimos could be sites for various important experiments. Solid core and gaseous core nuclear engines could be tested on them at sites far from any habitation. Very heavy orbital structures?such as stations with hundreds or thousands of tonnes of rock for radiation shielding and agriculture?could be constructed near them from their materials and transported using their fuel. Phobos and Deimos should play a major role in making transportation from the Martian surface to low earth orbit cheaper and may play an important role in opening Venus, Mercury, the asteroids, and possibly even the near-Jupiter environment to human exploration.

#1694 Re: Human missions » Mars? Moon first. - Mars is too hard and dangerous for now. » 2002-01-19 00:51:08

On the subject of whether people could live in the asteroid belt, I think the zero gee problem is the big one. Ceres has about one twenty-fifth the gravity of the Earth, I think. I'm not sure resources are that much of a problem. One problem is that some asteroids are nickel iron and great for mining, but would be lousy for agriculture or extracting indigenous fuel; the stony and chondritic asteroids, on the other hand would be adequate for agriculture if you can concentrate the sunlight with mirrors, and could make lots or methane and oxygen fuel, but would lack nickel-iron for construction and export. Fortunately the regolith layer of all asteroids is made out of the stuff that has fallen on them, and that's a mix of the types, so stony asteroids will have chunks of nickel-iron and nickel-iron asteroids will have chunks of stony and chondritic material.

Before you mine the asteroids for metals for Martian factories, remember that there are a few zillion tons of asteroid material littering the Martian surface. Since it's a big place--the size of all of Earth's dry land--explorers will soon know that there's a thousand tons of nickel iron exposed by erosion in crater X and other things exposed in other craters as well. With minimal weather for the last billion years, most of the stuff that's fallen to Mars is still intact, rather like the meteorites in Antarctica.

                  -- Rob S

#1695 Re: Exploration to Settlement Creation » Domed habitats... - ...size, materials, and more. » 2002-01-19 00:38:04

The weights of the kevlar are all from Zubrin's *The Case for Mars,* page 178, where there is a section about domes. I was assuming a hemisphere when I gave volumes (formula, 2/3 pi r cubed).

As for processing the Martian regolith, there are various ways to do it. You might want to erect the dome over an area where you don't have to clear rocks, like an ancient Martian lakebed (there are a few; Zubrin mentions a "paleolake site" in passing in a chart on page 142). A lakebed might be mostly clay, which is easy to excavate, and it probably will contain permafrost or ice layers underneath. Rather than hauling the dirt in through airlocks after you erect the dome, you make a pile of dirt in the middle of your future dome first, build the dome around it, inflate it with compressed Martian air, then place the plastic "dropcloth" and bulldoze the dirt over it. The easiest way to get excess salts from the regolith, once it has warmed up and is in a pressurized environment, is to soak it with water, let the water run off, collect it, desalt it with reactor heat, and irrigate the regolith again. Zubrin says Martian regolith is pretty good in terms of minerals for plants (page 196). Adding nitrogen will be essential and the most difficult, unless the ancient Martian lakebeds include nitrate deposits (possible).  My guess is that a good year of work by one or two people would be necessary to prepare the soil fully, but even slightly salty soil will grow some crops (the Israelis have been experimenting with salt-tolerant crops).

                 -- RobS

#1696 Re: Exploration to Settlement Creation » Domed habitats... - ...size, materials, and more. » 2002-01-16 16:15:37

I have a few thoughts about domes that might help one visualize them. Zubrin's book on Mars Direct notes that a 100-meter in diameter sphere of kevlar (one of the strongest and toughest plastics ever developed) would weigh 64 tonnes. A hemisphere (half a sphere) would therefore weigh 32 tonnes. It would enclose 7854 square meters or .7854 hectares, which is about two acres. Its volume would be 2/3 pi r3 or 261,800 cubic meters. Since the mass of air at a third of an atmosphere of pressure is about half a kilogram per cubic meter, the air inside would weigh 130,000 kg or 131 tonnes. The reactor Mars Direct postulates could make that much oxygen from CO2 in less than a year.

Another useful statistic: the suface area of a hemisphere is 15,708 square meters. Each square meter, at a third of an atmosphere of pressure, will have about 3.3 tonnes of force on it (33,000 newtons, if you are a purist), so the dome will have an upward force on its outer edge of about 50,000 tonnes. The perimeter is 314 meters long, so that's an upward force of 165 tonnes per meter. If you assume a ten meter wide sleeve on the ground and Martian rock "weighs" about a tonne per cubic meter (the mass is about 2-2.5 tonnes per cubic meter, but the weight is that times Martian gravity, 0.38) then you would have to bury the sleeve under 16.5 meters (54 feet) of dirt and rock to hold it down. You could also anchor stakes in the regolith to help hold it down, reducing the dirt pile to some extent. The obvious place to put housing is under the dirt pile perimeter, so that the housing opens onto the interior space and the regolith reduces cosmic ray and solar radiation exposure to almost terrestrial levels. It's amazing you can do all that with 32 tonnes of kevlar and a bulldozer!

The floor probably should have plastic liner to help make it air tight; on top of that you'd pile processed Martian regolith. You'd want to build the dome somewhere there are ample supplies of eolian drift and clay. The big problem probably is desalting the regolith, though you might find regolith with low enough salt levels so that you don't have to desalt it for plants to grow in it. You'd have to add nitrogen and maybe phosphorous.

A landscape architect friend of mine who was designing a rooftop garden once told me you put 9 inches (23 centimeters) of dirt on a rooftop garden. That would take about half a tonne of soil per square meter, or 15,000 tonnes total. That would take machinery quite a long time to prepare; probably a year or two. Meanwhile, you could get away with less and start on one side of the floor only.

Biosphere 2, in Arizona, had an intensive agriculture area of 2233 square meters that was able to feed eight volunteers inside. Thus this hemisphere could feed about 24 people. Presumably any Mars station building such big enclosures would have several, in case one were temporarily damaged, so a 100-meter hemisphere would be built by stations of 100 or so people.

What shape would you like the dome's floor to take? It could be flat, but probably you want it sloping to a low point for drainage. The obvious thing to do would be to put a pond somewhere at the lowest point--maybe in the middle. You'd raise fish in the pond, flood a rice paddy next to it, swim in the pond for fun, and have a small barbeque patio there as well. A barbeque would put a lot of smoke in the interior, but not a dangerous quantity (assuming you had all 261,000 cubic meters of air space inside).

The dome would probably be layered; in other words, instead of one dome, you'd want a minimum of two, maybe three or four, nested inside each other. That way if one leaks the air just leaks out to the next dome, an alarm goes off, and someone has to go find the leak and fix it. If you had three or four domes, the spaces between the others could be used to store nitrogen, argon, and other inert gasses you might want to use for other purposes. Multiple domes also are essential for insulation against the frigid exterior temperatures.

I am guessing, but you may also want to draw a black insulating shroud over the dome at night to hold in the heat. If that is the case, you'd have to have it retract if you wanted to look at the stars or moons. Maybe the computer could be programmed to pull the shroud over the dome every evening at 9 p.m., giving people two hours to look at the stars.

In the morning, you'd want to pull the shroud back on the east side only and leave the west side covered with the shroud, which would be silvered on the inside. This would reflect the morning light into the dome and increase total sunlight. With skillful computerized control of a silvered shroud over the outer dome, one could raise the total sunlight inside almost to terrestrial levels. In the afternoon, the shroud would cover the eastern side of the dome.

#1697 Re: Planetary transportation » Martian Scale Design - Little Planet, Big Trucks » 2002-01-16 15:45:25

One thing that has occurred to me about surface transportation on Mars: self-driving vehicles could be built more reliably than on earth, especially if a very simple global positioning system could be deployed on Mars. There is already reseach being done on self-driving tractors; the farmer programs in the corners of the field in GPS coordinates and the coordinates of any obstacles (fields sometimes have bedrock outcrops or even trees in them) and the tractor would then plow the field itself. This technology would work well on Mars once you've bulldozed a route through the rocks and programed in the dips and rises (and filled in ravines, of course). On Earth you can't program for fallen trees, tumbleweeds, deer running in front of your vehicle, or other vehicles. But if you have a 5,000 kilometer route connecting, say, Hellas and Isidis and it is bulldozed to some sort of basic standard (3 or 4 meters wide, for instance), and there are no other vehicles on it, you could program a vehicle to drive at 25 miles per hour from one place to the other and the crew could sit inside, playing cards, eating, sleeping, etc., while the vehicle traveled 600 miles a day for them.

Actually, you might not even need global positioning system (gps). You might be able to use the technology the military has developed for air-to-surface missiles for terrain recognition. You'd program in an image of the entire route and the software would navigate by recognizing prominent boulders. You could supplement the terrain recognition with an occasional road sign bearing a bar code for the rover's computers to recognize.

Rather than Maglev trains, the first "trains" might be a nuclear powered truck towing four or five trailers behind it automatically, carrying people and cargo from place to place.

#1698 Re: Interplanetary transportation » Launch Vehicles - Energia, Ares, Magnum etc. » 2002-01-16 15:32:32

I have two questions about the Energia Launch System:

1. Is there information on the web about the system? I am curious about the sizes and weights of the various stages, thrust, the various options, etc.

2. Does anyone have any idea how much it would cost to launch an Energia with, say, a 140 or 150 tonne payload; that is, the Mars Direct payload?

#1699 Re: Life support systems » Power generation on Mars » 2002-01-16 00:01:47

I am new to this forum, so I hope I am not missing some context. If nuclear power is not available for a surface Mars station, probably the best way to go is a combination of wind and solar, because dust storms that obscure the sun and decrease the efficency of solar arrays also can generate wind power.

I was searching about wind power on the web a few months ago and came across the specifications for the BWC XL-50 wind turbine. Its blades are 46 feet in diameter and it produces 50 kilowatts of power in a 25 mile per hour wind. The wind turbine sells for about $70,000 and installation adds another $15,000 or so. The start-up speed of the turbine is a 4.5 mile per hour wind.

I did some calculations (don't ask me how; it was a few months ago now) and figured that if the length of the blades were doubled to 92 feet, the windmill would make 1.5 kilowatts in a 25 mile per hour wind on Mars. If you increase the blade length another fifty percent to 138 feet (diameter, not radius) then in a 25 mph wind the turbine can generate 3.5 kilowatts on Mars. The start-up speed would probably be about 11 mph, but the wind turbine only makes 0.3 kw at that speed.

I don't know what the weight of such a wind turbine would be, but the blades would probably be fiberglass or could be made out of very light-weight substances, so it would probably be only a few tons. While the first wind turbines would have to be brought from earth, once there is any manufacturing capability at all, they would probably be pretty easy to make, as they are mechanically simple devices.

                    -- Rob Stockman

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