You are not logged in.
Tom Kalbfus,
1,000,000 trips with the largest possible drawing board tanker at 12 years per trip.
If we have 1 or 2 thousand tankers operating at the same time then 50,000 years or so, that is collecting 60 bars from Jupiter the closest possible place.
Jupiter has a more massive gravity well than earth and not pure hydrogen, so you might want to add a year or two on each 12 year trip back and forth from Venus to Jupiter, fuel for transport is almost as massive a problem.
The idea of collecting hydrogen at sedna might not be a bad one, if we dismantled it and used it for collection, processing and transport then the few century single trip is possible.
Collision with Venus, might alter the spin and change most of Venus into h20, but the impact of gas on gas will still leave a molten Venus.
The shell could be used as a sunshade, and the contents simply left in low unstable orbit to distribute themselves to the surface.
...
samy,
Why pump all the way from the surface?
If you have a couple km long pipe, one end in space the other in very thin atmosphere it will self pump towards space.
Will it self pump at escape velocity though?
If not gravity will simply pull co2 back.
Tom Kalbfus,
I don't want to put you off the idea that a water world isn't the way we should approach Venus.
Karov had some very good ideas about importing hydrogen directly from the sun, so importation might not be as big a problem as i perceive it.
I'm probably being a bit generous with the two times heat retention for Venus.
On earth the ocean temperature is quite a low average.
On a newly terra formed Venus it will certainly be twice and probably many times the earths ocean temperatures for a very long period of time.
With the additional radiations on the water at Venus this would probably settle into twice the earth ocean temperature even though we shade.
The slow spin rate is also an unknown factor, it might cause little problem at all or simply overheat on the day side, or cause massive hurricanes on a planetary scale as warm moves to cold.
I agree that a sun shaded Venus is a much better target to terra form, but shielding it to a useful percentage is a massive effort itself.
That 1/2 bar experiment shows how close Venus is to a runaway on any terra formed Venus we have, if the bar pressure goes up so does the temperature, if the bar pressure decreases so does the boil point.
Nitrogen is quite a poor greenhouse gas so we can probably keep all of it without much of a temperature difference.
On earth we have about 50c lea way to a runaway, on a terra formed Venus maybe 20c if everything is perfect.
Venus can be terra formed, its just a question of what steps and for how long.
No expert exists on terra forming Venus, so right now all ideas are good until they are picked apart, Venus chemistry is very good at doing that. ![]()
Tom Kalbfus,
Good idea but how would you implement such a thing?
As you point out as the water vapor on Venus increases so does the temperature, 1% water as steam equates to around an additional 15% temperature .
To create a water world you will need to import around 60 bars of hydrogen to convert the CO2 into C and H2O.
With an all out space effort to transport hydrogen from everywhere possible, i think we could do that in about 50,000 years.(maybe 50% of GNP spending from every country on earth on the effort to move hydrogen for 50,000 years)
You would also need to have Venus sun shaded to the point below the boiling point of water and the additional heat created from the water creation reaction itself before you start importing hydrogen, then wait until the temperature is below 112c at the equator.
On a total water world i would guess you would need to be around 1/2 bar pressure to avoid a runaway, as evaporation would be at least twice that of earth, or twice the temperature retention of earth if sunlight conditions are similar.
You will also need to convert 2/3 of the nitrogen into nitrate or something useful.
Twice the temperature of Earth equator high would be near 100c, on a 1/2 bar world water will boil at around 95c.
You would also have to address the surface radiation problems, but a few meters of water depth works as a good shield.
Anything in the top 10 meters or so of ocean will be sterilized.
So many catch 22s on trying to teraform Venus its a wonder anyone has any good ideas on it ![]()
atitarev,
Thank you ![]()
I'm also in the doubtful group about making any substantial change in the spin of Venus.
If we could double the spin speed over many thousands of years i think that is the best we could hope for.
We probably don't need to alter the spin rate anyway to alter Venus, curtains make wonderful day night. ![]()
All depends on the planetary heat transfer of a 3 bar Venus, might or might not be a problem.
I also agree that around 3 bars of mostly nitrogen will keep the radiation at the surface to respectable levels.
I think 3 bars with .9 G would be adaptable for most things.
That should equate to 2.7 bars of earth pressure at ground level.
atitarev,
I agree with almost everything you said in your last post.
The only part that is questionable is the hollowed out asteroid being sent to Venus.
If we were to go to all that trouble to make one then park it very carefully in a Venus low orbit.
I think it would be very technically challenging to do that.
If we need to remove carbon from Venus, then assembling a moon made from carbon right at Venus might be an easier task, we could also use it to alter the spin of the planet to some degree.
We could make the moon as big as we like and take whatever time we liked constructing it, all the while removing carbon from Venus.
We have around 30 bars of carbon as building material, so it would be a substantial sized moon at completion.
The waste O2 from carbon separation makes excellent rocket fuel, and the sun as a source of power for CO2 separation and collection.
As the moon size increases it becomes a launch point for hydrogen collection and a point to add carbon soot in orbit to shade Venus.
With a little luck when the moon is big enough it will begin to tidally effect Venus and maybe start a magnetic field.
This sort of multiple win win no waste plan i think is what we need to alter Venus.
Tom Kalbfus,
Not a direct impact with a large asteroid, just a glancing blow to dump material into geo orbit.
I agree that making a molten Venus is not a good step forward either, but adding a natural sunshade that takes no upkeep is.
I don't think to many people will be living on asteroids in the kb, the temperatures are to say the least cold.
When you open a bottle of liquid nitrogen it wont boil, but might freeze.
If people did live on them we could just pick another, or ask if they would like to be part of Venus new sunshade. *lol*
Cooling Venus i think is a must to start any method of atmospheric reduction on Venus.
Cooling it enough to make carbon chains stable on the surface is all we need to start, then carbon assembling micro clones can reduce the atmosphere with simple copies of themselves using ample sunlight as a power source.
As they fault they simply fall to the surface, but already have made many clones of themselves.
This will only take you so far though as the O2 levels will rise and need to bond with something, preferably hydrogen to form water.
If the O2 levels get to high it will self combust.
Works well for hydrogen importation for many millennia though, and same delivery can remove compressed co2 to Mars.
Or simple sun focused hydrogen importation, or magnetic collection from solar storms.
atitarev,
I did see an idea on this forum about a year ago.
It involved giant carbon balloons made at Venus filled with co2.
After sending a couple to mars no real destination was left for the other 999,998 of them.
Continuing on the asteroid idea, a large asteroid with a glancing blow on Venus deposits a lot of material as a sun shade that lasts for a long time.
This might be step 1 in teraforming Venus.
As you point out though even a 2 or 3 bar Venus would still have lots of troubles.
I wouldn't want to hazard a guess but even on that teraformed Venus near the equator, temperatures would probably boil water and begin a runaway.
Changing the spin of Venus is probably possible with impacts from water ice asteroids, but changing it to more than about twice its spin is doubtful.
Even on a terformed Venus we will still have to deal with the lack of magnetic field to solve the radiation problems.
That can be fixed with a massive ground or space based field generator, but either are massive engineering jobs.
karov,
I will have to believe you on the temperatures because i can't find anything proving or disproving it. ![]()
As i said overheating Venus is easy but doing anything with that new temperature range questionable.
The max i could for see for greenhouse gasses was maybe double the temperature of the current Venus.
Probably a useless addition to temperature on Venus unless some chemical genius can use nitrogen somehow to alter C02 (I couldn't)
I agree that Venus has no need to loose its C02, infarct just dumping it to space would probably cause unforeseen problems in the inner solar system.
Adding hydrogen to Venus from the sun is a excellent idea, but lets not forget that the current Venus retains 12% of its total heat from its far less than 1% of water vapor in the atmosphere.
Creating water vapor on Venus will add heat from the H2O reaction itself in the short term and from the water vapor in the long term.
For this idea to work Venus would have to be at a temperature lower than the steam point of H2O to avoid the original runaway greenhouse condition.
Water as steam is a very powerful greenhouse gas.
SpaceNut,
Hi
Geesh i didn't even know Venus was hairy ![]()
I can't believe a table of disassociation temperatures doesn't exist somewhere.
While looking for a table i did stumble across a very interesting idea that involved simple carbon machines that self replicated and grew exceptionally.
It looked very promising as a way to soak up carbon from Venus, but still the initial ground temperatures were an issue as the carbon copies failed.
Virus engineering also offered a similar approach to remove carbon.
Tom Kalbfus,
When you make that could we have an ocean on it? and maybe forests?
Just watched that series ![]()
Karov,
Thank you for the escape speed.
~10 km/s
A lot higher than i thought.
No need to figure out the Kelvin temperature to reach escape velocity for c02 as c02 bonds should disassociate long before that temperature.
I can't find any paper or information about c02 disassociating in heat.
O escape velocities are much lower, so we need to know what temperature it will escape at, and will it be lower than the super greenhouse gas disassociating, and will it be a respectable escape temperature for O.
Starting to feel like a chemical experiment with many locked variables dependant on each other for a result.
I think realistically we could double the temperature of Venus for the short term to chemically alter it, but beyond that it would require more input than a realistic amount of super greenhouse gas could contribute.
We probably don't need to remove all the c02 from Venus, as soon as Carbon can accumulate on the surface with lowering temperatures we have a place to work chemically or with machines.
Overheating Venus is easy, doing anything useful with a hotter Venus not so easy.
karov,
All depends on what reactions we get with a slow heating VS a fast one.
Adding a greenhouse gas that self bonds with CO2 shouldn't be to difficult.
Getting it to Venus another story.
If higher temperatures cause 0 and C to separate it might make for a very different teraforming model for Venus.
We might be able to make some interesting chain reactions with free O and much less energy needed as the free atoms occupy more space than CO2, a loss of heating though as CO2 is converted.
I'm curious if very hot CO2 becomes O and O and C or simply escapes as CO2?
Shows how a simple planet heating can have unseen outcomes, and we haven't talked about the heated sulphur or nitrogen yet and what they might do.
What is the escape velocity for CO2 on Venus? what temperature do we need to produce that on Venus and what temperature is the breakpoint of the CO2 bonds on Venus?
That would answer the how much super greenhouse gas question, and the what happens to CO2 when super heated (escape as CO2 or broken bonds and O only escapes)
karov,
I think Venus is a question of making stable carbon chains.
Once Venus is cool enough for any carbon products to survive on the surface it's possible to teraform.
I cant think of a possible importation right now that would lower the temperature of Venus to any degree to allow any stable carbon chemistry.
Other than hydrogen and its beyond practical importation quantities for the current Venus.
snelson5871,
It is a simple process to overheat Venus.
Since Venus has so much free C02 you could easily import the products to create super greenhouse gasses right in the atmosphere.
The importation volumes would be relatively small, but still large quantities for our technology.
It would have to be done pretty quickly as the heating caused would cause problems for the mechanism producing the greenhouse gasses.
When we super heat C02 do we get C02 escaping or 0 escaping as the C02 bonds weaken?
Guess that all depends on how hot how fast.?
Cleaning up the 20 or 30 bars remaining on Venus afterwards could envolve carbon fixing in a number of ways, hydrogen mining or importation, metals mining etc, anything that will capture free 0 or C02.
Once machines could work for extended periods of time on the surface i think teraforming the rest would be quite possible.
Bring the big chemistry set also.
Belinda,
The episodal model of Venus. ![]()
Trapped heat at Venus should make for a more active core, yet Venus has no magnetic field.
This could simply be the spin rate, or Venus didn't get a late large hit to stir it up.
Two planets being so similar ending up so differently just goes to show how small differences can make worlds of difference.
Venus might be the typical earth like planet in the universe.
Without late collisions and correct compositions all earth like places in the universe probably end up like it, or as frozen ice balls.
It doesn't take much for a runaway greenhouse or runaway freeze on any earth like planet.
I think the moon is much more important than we give credit for.
SRAM,
Why wouldn't god go ahead and make molten planets?
Makes as much sense to create them that way.
If god is the creator then he could do whatever he wanted, not for us to decide what he did, just for us to understand the process.
Belinda,
A molten Mars cooling works well for Mars but not well for Venus.
If it is all dictated just from size then Venus should be an active world like earth.
Our moon might be the answer to that riddle.
SRAM,
Specific gravity will force all the heavy atomic elements to the center of the earth, as long as the medium is liquid.
At the exact center of the earth where gravity is near 0 who is to guess what is there, but likely its heavy atoms also from simply being churned.
Our sun isn't at the center of our solar system, Jupiter, Saturn etc all perturb the sun.
You have some interesting ideas and i would be the first to agree that science is a long way from being able to make any relevant statement about anything.
Most people forget that just a short time ago people were burning people just for thought, and now we ridicule people with ideas that don't fit what is believed to be true.
Sad to think that technology has come this far, but mans mind has not taken any giant leaps.
Belinda,
I wouldn't go as far as to say all kb binary objects are the product of capture only.
Some binary objects in the kb are probably the result of collision also.
In fact Pluto charon and its second moon make even the collision scenario tough to explain.
Two moons circling a small planet is tough to explain with any one mechanism.
In a belt of objects traveling at similar speeds it is much easier for one body to capture another and impacts a regular occurrence.
If we remove all the red giant stars, tiny red stars, brown dwarfs, white dwarfs, hot blue stars, radiation spewing stars, multiple stars , stars younger than 1 billion years and unstable yellow stars, we are left with maybe 1 in 50 to 1 in 100 pretty stable yellow stars with good habitable zones.
I personally believe that if an earth like place exists its 100% chance of life, bacteria and virus.
I also believe that 99.99% of those earth 2s 3s etc will be just that, bacteria and virus and slime, even the lucky ones with nice moons.
I also believe that with all the chance happenings for earth/moon and the range of stars in our galaxy only a handful of other earths will exist in each galaxy, and only a handful of intelligent life forms will exist at one time in all the universe.
LOL as kirk says (no intelligent life here...beam me up scottie) ![]()
Agreed, Earth 2 was good and bad, kind of like earth 1.
Actually the Lava one was for SRAM, but you did an excellent job of explaining how lava gets to the surface past the crust.
Makes sense to me that if the earth is mostly molten then the heaviest objects Led Gold Iron etc migrate to the center to form a molten core, if not your Lava explanation might need a total rework. ![]()
Belinda,
Other than Pluto Charon system the rest is all captured items.
Small objects traveling at similar velocities can gravitationally perturb each other slowly.
Large sized worlds cant capture each other, they either perturb and collide, or simply perturb each other and both feel the gradational effects of the pass bye.
For an earth mars sort of collision to happen, first a planet has to be perturbed from its original orbit, then collide with another planet in the correct place at the correct time.
Forming a moon and earth from it requires a precise angular collision or you get one big world with no moon, or very small moon.
The odds pile up against earth 2 if you factor in the % of stars that are not good for life anywhere near them.
Probably making my guess at more like one in 50 billion, and i haven't even touched on the life starts %.
If earth like places are required for intelligent life then we might be searching forever for Et as 99% of the time earth has been here it had no intelligent life, and not to sure about now either. ![]()
SRAM,
Lava?
Where does that come from?
Just a wild guess at finding another earth moon type system
Chance of earth sized planet at right stellar place 1/10 ... systems
Chance that said planet is a water world 1/10 ...wet
Chance of planetary crash that forms large moon 1/1,000,000 ... crashes
Chance that end product is earthlike 1/10 ... atmospheric remains of crash, spin composition etc
1 in a billion stars.
Might be a long look for earth 2
Tholzel,
The tidal action on the core of the earth isn't much now, but a billion or two years ago its was immense.
This might be the reason we still have a molten core now.
If we look at similar moonless planets in our solar system Mars and Venus they are long dead and simply might have run the course for heat they could produce.
I'm amazed no one has thought about a few billion years of tidal action on earths core caused by the moon.
When we start closely looking for places that have life in the universe, i think we will be looking at moons around Jovian type planets more than earth like places with moons.
Our moon the size it is with an earth like planet in the right stellar place will be quite rare.
karov,
Very interesting ideas on altering the Venus chemistry.
Cooling Venus is a must for anything useful to happen with its chemistry, so your idea of a cooling process as the chemistry happens is very interesting.
I can see a problem with the beaming of hydrogen as the thermal temperatures increase, it will be very difficult to avoid steam with the production of h20.
Also we are talking about beaming 30 or so bars of hydrogen, not impossible but long term.
Some additional cooling process might be required as liquid water starts to accumulate in the atmosphere.
If not the steam effect on Venus will start to become a bigger and bigger problem with heating as co2 is converted in greater quantities of h20 and C.
Maybe instead of common h20 we can produce heavy water? and instead of free C we produce Carbon monoxide?
Both of them will alter the heating process and both soak up more bar pressure.
Both would lead to additional steps for Venus though.
karov,
I agree Venus=chemistry problem.
Other than fine tuning near the end of a teraformation the main solution will need to be a chemistry one.
Big question for me is bond the O or bond the C, both are very difficult with current surface temperatures, both well bound to each other.
Carbon monoxide might be a good solution to lower the surface temperature, but just 1 step in many for sure.
neilzero,
Many thousands or millions of years to make an earth like place.
Venus probably got the way it is when its oceans boiled into its atmosphere, free hydrogen without a good magnetic field was lost to space, then the carbon was liberated from the crust as the temperature rose and bonded with the free O.
ALA co2 atmosphere.
Adding hydrogen to Venus now will produce water, but water on Venus just produces steam, a very powerful greenhouse gas.
Adding iron asteroids has its potential, but enough to alter that much co2 is a doubtful project, and still you need to break the co2 bonds so the iron has free oxygen to bond with.
Even if all the C on Venus boned to something it produces a 75mb Oxygen atmosphere so something even more plentiful will also need to bond to it.
Cooling Venus just produces vast quantities of co2 ice, maybe 200 miles thick planet wide.
Even if we could find a solution to all that ice we would still require a few million years for a natural plant cycle to produce an earthlike place.
Maybe something as simple as altering the co2 into carbon monoxide is the solution Venus needs to get things started.
carbon monoxide and free oxygen will occupy a much larger volume than co2, i doubt if Venus can hold an atmosphere much bigger than its current size.
At best though even a simple solution like it will leave you 50 times the volume of earths atmosphere or more.
Carbon monoxide bonds more readily with metal than co2 so lots of it at that point might reduce the atmosphere further.
Carbon monoxide (smog) is great at reflecting light, and nowhere near as good a greenhouse gas.
Unless we do something radical with Venus it will be a very long term stepped project. IMHO
Austin,
Certainly dumping 95% of the co2 reduces the temperature and the atmospheric pressure problems.
Importation of the equivalent of 1 earth atmosphere of hydrogen at that point makes an earth like Venus.
The energy to dump 95 earth pressures and the time involved are seldom looked at.
Freezing Venus also creates the same problem of 95 earth pressures of co2 ice, then what to do with it.
Heating Venus up a bit more might be the best solution of all to dump atmosphere.
relatively small quantities of super greenhouse gasses added to The Venusian atmosphere could really heat things up to the point that co2 escapes.
I came to the same problem with radiation to break the bonds of the co2.
The bonds do break easily with radiation, but with no input of energy the bonds rejoin.
Unless the o2 can bond to something else or the C can be locked into heat resistant things then its pointless.
Trying to transport 45 atmospheres of something for o2 to bond to is not realistic.
At best with something that makes many 02 bonds we would still need 10 or so atmospheres importation, again not realistic.
No additional carbon on Venus vs earth, just in a bad form as co2.
The two worlds have very similar amounts of carbon.
The black hole idea is rather non thinkable, but the radiation input has some possibilities.
Creating a constant radiation disaster on Venus or in orbit might be a promising way to lock co2 away or break the co2 bonds or create new heat resistant carbon chains.
With pretty high constant radiation in any spectrum we choose and a free source of power in the sun we should be able to alter the chemistry of Venus atmosphere.?
Ideas?