New Mars Forums

Official discussion forum of The Mars Society and MarsNews.com

You are not logged in.

Announcement

Announcement: This forum is accepting new registrations via email. Please see Recruiting Topic for additional information. Write newmarsmember[at_symbol]gmail.com.
  1. Index
  2. » Search
  3. » Posts by JoshNH4H

#151 Re: Terraformation » Water as a greenhouse gas and source of Methane and Ozone possibly. » 2018-12-13 10:20:31

My understanding is that removing all the water in the atmosphere would result in a substantially cooler planet, but the marginal effect of additional water vapor is up for debate.  Water also tends to have a pretty short lifetime in the atmosphere, falling as rain or snow in a short time.

As far as irrigation and the like goes, that may have some effect on local weather if done at a large scale but I don't think it has a very significant effect on the global climate.

As far as where to get fluorine:  Most fluorine reserves on Earth take the form of fluorite, CaF2.  Here's the series of reactions you would use to produce CF4 from that:

CaF2 + H2SO4 -> CaSO4 + 2 HF

Then, you have two options.  Option 1:

4 HF + C -> CF4 + 2 H2 (in an electrolytic cell admixed with KF)

Option 2:

2 HF -> H2 + F2 (in an electrolytic cell admixed with KF)

2 F2 + CO2 -> CF4 + O2

Neither of these is easy per se, but CF4 is such an effective greenhouse gas that the temperature return on doing this is pretty high.

#152 Re: Terraformation » Water as a greenhouse gas and source of Methane and Ozone possibly. » 2018-12-12 14:12:43

Hey Void,

The remaking of a planet is a gigantic project, orders of magnitude beyond anything humans have ever done in its scale.  What this means, in my opinion, is that we need to be looking for ways to leverage our capabilities to get the planet to do much of the work for us.  It's very much an open question what the best things to do are, although there have been lots of interesting ideas put out there.

To the extent that I question or challenge you idea it's because I think it's worth engaging with.

So, here we go:

Correct me if I am wrong: Your proposal is to keep the water in the upper atmosphere by condensing it into clouds, right?

Clouds are not gaseous.  They are suspensions of liquid water or water ice in atmospheric gas.  What this means (to the best of my understanding) is that its absorption/transmission properties in the infrared are more like water and ice.  On net it's my understanding that clouds actually cool a planet because the greenhouse effect associated with them is cancelled out by the degree to which they reflect sunlight away from the planet.

Creating methane is good but at a guess (a pretty uninformed guess) the actual rates will be low.  Methane has a higher global warming potential than CO2 (around 25 to 100 vs. 1 for CO2*).  This is higher, but not so much higher that small amounts can make a big difference for climate.  I would look towards seeding the upper atmosphere with fluorine as a better way to generate warming: CF4 is an extremely powerful greenhouse gas, with a GWP around 5,000 to 10,000 times higher than CO2.

*Global Warming Potential is a measure of how much warming comes from each tonne of gas when released into Earth's atmosphere as compared to CO2.  It is a function of a lot of variables and the precise number is really only meaningful for Earth and for a specified period of time (100 years is the standard).  When looking at GWP, I would group gases into four basic categories: Weaker than CO2 or negligible warming effect (Nitrogen, Oxygen, and the noble gases), similar to CO2 (CO2 and water), mildly stronger than CO2 (methane and ammonia), and much stronger than CO2 (chlorofluorocarbons etc).

#153 Re: Terraformation » Water as a greenhouse gas and source of Methane and Ozone possibly. » 2018-12-12 11:41:08

Hey Void,

On Earth, we have a lot of water in the atmosphere and not so much CO2.  This means that the frequencies water absorbs are mostly blocked already, while the ones CO2 absorbs are only partially blocked.  Adding additional CO2 to the atmosphere on Earth therefore has a larger marginal effect on the temperature than more water vapor.

On Mars, the situation is reversed: There's a lot of CO2 and very little water vapor.  Adding water vapor to the atmosphere therefore has a bigger effect on the temperature.  The problem, as you noted, is that the cold temperatures cause the water to freeze out quickly.  I don't know that your suggestion of sending it up into the upper atmosphere would help all that much: My guess (which admittedly is all this is) is that it would slowly freeze into very fine ice particles that would actually cool the planet.  The other thing is that you actually want your greenhouse gases to be near ground level so that they warm the part of the atmosphere where people are.

It's true that water is a greenhouse gas, but to me it's best seen as a byproduct of other interventions, because it's not much use as a greenhouse gas until the atmosphere has already warmed substantially.

#154 Re: Terraformation » The Moon » 2018-12-11 10:42:26

I would agree that there's some historical value in retaining the Moon's current appearance.  But I would argue that there's much more value in creating a Moon's worth of habitable land.  Per my post above, the Moon has has much land area as the US, Canada, China, the EU, and India combined.   The value of that much land is simply immense, incalculably so, both in the sense of profitability and in the sense of its value to humanity.  And on top of that it's just three days' journey from here to there on a minimum energy trajectory, less if you have better engines (it's vaguely conceivable, although not with current technology, that you could go to the Moon for a weekend).

It's true that the Moon is quite beautiful as it is, but it's also true that living worlds are quite beautiful. 

It's true that there are huge challenges in remaking the Moon (as there are in terraforming any world), including "known unknowns" (Where is the water and gas inventory to come from? What do you do about the low gravity and slow rotation?) and "unknown unknowns".  However, it's such an incredible project that it will surely be worth it if you set your time horizons long enough.

#155 Re: Terraformation » The Moon » 2018-12-10 16:39:14

Hey knightdepaix,

If I understand correctly, this is what you're proposing:

  1. Transport the CO2 from Venus to the Moon

  2. Send some gases back to Venus from the Moon?

  3. Also send some gases to Mars?

Frankly I don't really understand what you're trying to say there.

Fundamentally, yes, bringing CO2 from Venus to the Moon would be a great step towards terraforming the Moon.  It's true that CO2 is a greenhouse gas.  On the other hand, water is also a greenhouse gas and likely to be in short supply.  What the actual temperature would be if you introduced 300 mb of CO2 to the Moon I do not know.

Even if the global temperature is high, the poles will be cooler.  If there is sufficient water, nitrogen, phosphorus, etc. to support ecosystems at the poles they will slowly fix the CO2 into biomass and Oxygen.  This will lower global temperatures and increase the region of viability in an accelerating process.  Come back in a few thousand years and the Moon might be a comfortable place.

#156 Re: Life support systems » Mobile Energy Storage in a Mars Colony » 2018-12-10 14:03:07

Methyl formate is an option, sure.  If we're going that route though I would think we might go for Methanol.  Methanol is produced by reacting H2 with CO over a zinc catalyst at elevated temperature and pressure.  It freezes at 175 K and boils at 338 K (under one atmosphere).  Of course you still need an oxidizer, which is the real problem.  LOX boils around 90 K, way below Martian ambient.  You'd probably want something more like the kind of oxidizer used in solid rockets: A peroxide, perchlorate, or nitrate.  The problem is that all of these are complicated to make, corrosive, and use up a lot of energy.  You could store Oxygen as a compressed gas.  At Martian temperatures and 100 atm, the density would be around 175 kg/m^3 according to the ideal gas law, which isn't awful.  Worth mentioning that Oxygen will be a supercritical fluid at this temperature/pressure so the ideal gas law is likely to be way off.  High-pressure gas tanks are heavy and expensive too.

#157 Re: Planetary transportation » Steam powered rovers » 2018-12-05 18:37:50

SpaceNut-

I think the Mars Atmosphere Kinetic Engine is the one I had in mind originally.

kbd512-

I'm very excited by that 150 lb per 10 MW number but I've been having trouble finding it in any of the references.  Can you point me to where you found it?

#158 Re: Human missions » Apollo 11 REDUX » 2018-12-05 10:31:09

I would say the Democratic party is generally favorable towards him, seeing as he's the electric car/solar power billionaire.  The Democratic Party is distinct from the entire universe of left-of-center Americans, of course.  My understanding is that the farthest leftward people (perhaps 1% of the actual population or less although disproportionately loud online) dislike him.  I would expect continuing support from elected dems unless spaceflight becomes a polarized political issue.

#159 Re: Planetary transportation » Steam powered rovers » 2018-12-04 15:12:09

Assuming a reliable working model is built I think this would be a great technology to use in rocket applications and for launch from earth in general.  10 MW in 150 lb works out to roughly 150 kW/kg, an incredibly high number.  The SAFE-400 reactor generated 400 kWt with a reactor mass of 540 kg.  With a 40% efficient scCO2 cycle you could get 160 kWe from this.  Scaling up to 10 MW, you would expect a reactor mass of 13.5 tonnes.  Against this, 150 lb is a rounding error.  No doubt major improvements are possible on the reactor side, especially at scale.

In space, there's also good reason to believe that a system of solar concentrating mirrors will be more reliable and have a lower mass.  What I'm getting at is that this has the sort of power-to-weight ratio that makes short-duration, interplanetary electric propulsion missions begin to look doable (or at least possible), something which I have been deeply skeptical of for a long time.

On-planet, I agree that this would work well with a molten salt thermal battery/solar power tower setup for both daytime and nighttime power generation.  Dust storms are another issue, for which a reserve of chemical energy is probably a better solution.

I think this is a good example of how earth-supply and local manufacture will have different technological results.  For Earth-supply, mass is key and high technology/precise manufacturing is readily available and you'll almost certainly look to something like this.  Local manufacture, on the other hand, will be somewhat rougher.  Land on Mars is nearly free (the only cost really is opportunity cost) and a larger mirror array to compensate for a lower engine efficiency (but correspondingly cheaper manufacture) seems like a good trade to make.

#160 Re: Planetary transportation » Steam powered rovers » 2018-12-03 19:40:49

Hey all,

Sorry for my long absence in this thread.  I was travelling over the holiday and unable to get the time together to have a look at things on the forum and reply.

Anyway, I've gone and had a look at some of the stuff you guys posted about sCO2 as a working fluid.  I think it's a promising technology with a substantial range of applications that may or may not be optimally suited for Mars.  In this post, I will go into more detail on why.

First, the good: The use of sCO2 in a thermodynamic engine has the potential to increase efficiency and decrease size at the same time.  This is a rare case where a new development seems to be strictly better than what came before under all circumstances.  And I want to be clear that under most circumstances, particularly on Earth, I really do think this is better.  However, I don't think it's necessarily better under all circumstances.  To explain why, I will start with two simple numbers: The pressure and temperature of CO2's critical point:

305 K (32 C and 89 F) and 7.4 MPa (74 atm).  No portion of the thermodynamic cycle can operate below that temperature or below that pressure, else you lose the benefits of using a supercritical fluid.

These references all correctly note that denser fluids require less energy to compress, which is a big deal.  The low-temperature engine I described above is not exactly typical, but I'm sure yo all noticed the fact that the low efficiency was due in large part to the work required to freeze CO2 out of the air.

I have three additional observations about this sort of system, one neutral and two drawbacks. 

Neutrally, it seems that much of the efficiency gains come from a higher operating temperature.  There is certainly nothing wrong in the abstract with operating at a higher temperature but it helps to make clear where the efficiency gains are really coming from.

Negatively, the pressures used in this system are likely to be enormous, far larger than comparable systems in use today and maybe even higher than a rocket engine like the SSME.  If the low-pressure portion at the system is at 7.4 MPa, the high pressure portion will be at a substantially higher temperature.  The Sandia report cited a maximum pressure of 14 MPa and the GE report mentioned operating pressures above 25 MPa.  For reference even the SSME operates around 20 MPa.

Also negatively, such high pressures and temperatures operating in a small volume generate a huge challenge in designing a turbine to withstand them.  Turbines already typically operate with advanced materials; this combination of high temperature, high pressure, and extreme force (large changes in pressure over short distances) are going to be really challenging to deal with, possibly at the very limits of materials as they currently exist.  As a point of comparison, the surface of Venus is around 9 MPa and 450 C, which is to say it's actually a less hostile environment in many ways than the interior of such an engine.

I don't mean to claim that it's impossible to build such an engine, or even that it's excessively difficult.  It's not.  What I do want to point out is that the extreme operating conditions will produce an engine that uses advanced materials and requires thorough (read: expensive) design and testing to operate safely and reliably. It's precisely the kind of engine that you would consider for grid power on Earth, where efficiency is critical and system lifetimes are measured in decades.

This is what makes me question whether it's really the best choice for off-planet use.  This scCO2 engine appears to approach a rocket engine in its conditions and complexity, and I'm sure we're all well-aware of the extent to which launches are a critical failure point.  Efficiency, in general, takes a backseat to reliability for pioneering missions or settlements.  This is particularly true of something as critical as an electrical generator.  I am also curious if it would be possible to build a generator small enough to work in the range of our power needs without big losses in efficiency.

When looking at thermodynamic engines, as is often the case, there is no one correct answer but there are many wrong ones.  I would say this falls within the group of reasonable options--the biggest concern to me being that it is not now nor has it in the past been in common use.  Chicken and egg, I know.

#161 Re: Unmanned probes » Mars Communications and Navigation Infrastructure for Crewed Missions » 2018-11-20 19:06:13

I suppose there are questions to be asked about reliability and durability, but a 10-kg, 200 gbps, ~$2 million lasercom satellite seems like a slam dunk compared to a 6400 kg, $600 million satellite, even if its throughput is in the terabit range.

We seem to be converging on Ka/X-band for surface-to-orbit communications and laser systems for orbit-to-Earth communications.  This seems like a solid design choice to me, with each being well-suited to its respective application.

This does create something of a mismatch, though: The Earth-to-Mars orbit leg might have a higher throughput than the Mars Orbit-to-Mars Surface leg.

#162 Re: Planetary transportation » Steam powered rovers » 2018-11-20 16:43:13

SpaceNut wrote:

Since most of the dust will be metal particles the electrostatic will tend to short out quite easily so I would make use of a magnetic sieve and reverse air back wash to remove the particles once the magnet is off.

metal particles

I'm sorry, what?

Planning to have a look at the rest of your references tonight

#163 Re: Interplanetary transportation » excess of propellant for safety margin » 2018-11-20 15:40:29

I don't think there's any guideline in particular. It depends how reliable your engines and navigation are (if your engine is rated for 330 s and it produces 320 s sometimes you need to carry more propellant) and what the failure options are (if you fall short, does human crew die? Or is your satellite just in a somewhat lower orbit? Can you use reaction control fuel as a backup?).

For interplanetary trips, all craft carry "course correction" fuel to change the direction and speed of travel after the main burn.  Orbital craft do a "circularization burn" after orbital insertion. 

I wish I had a better answer for you but basically it seems like we're pretty good at hitting the orbit on the nose without extra fuel.

#164 Re: Planetary transportation » Steam powered rovers » 2018-11-20 15:05:58

Hey SpaceNut,

That's an interesting device that would work for some applications but probably isn't adequate for this one.  The problem here is volume.  A 50 kW overnight system is going to need something in the range of 15-20 tonnes per day of LCO2.  A batch process in which you need to manually scrape frost off of a plate just doesn't have the capacity or the efficiency that would be needed to make this workable.

There are two related technical issues that I see with the process of freezing CO2 out of the atmosphere.

The first is the low density, and therefore low rate of heat transfer, of the Martian atmosphere.

The second is that CO2 frost on solid surfaces will be hard to recapture for use and will reduce the rate of heat transfer from the refrigeration unit to the atmosphere.  This is a problem because the CO2 will tend to frost on precisely the surfaces being used to freeze it.

I believe I may have a solution which addresses both problems: Use the ambient CO2 atmosphere as your working fluid.

I mentioned refrigeration very briefly in post #26.  I would like to go into somewhat more detail here.  Refrigerators (or heat pumps, which is the more general term) are thermodynamic engines very similar to the power generating cycles we've been discussing in this thread.  However, instead of generating power while transferring heat from hot to cold, they transfer heat from cold to hot while consuming power.  Here's how a refrigeration cycle works, idealized and in the abstract.  Note that the "fluid" in this case usually means a gas:

  1. Isentropic compression: In this stage, the working fluid is compressed with no heat transfer.  Compression causes the fluid to heat up to above the ambient temperature.

  2. Heat Rejection: In this stage, the working fluid is cooled by releasing heat to the environment

  3. Isentropic Expansion: In this stage, the working fluid expands through a piston or turbine and cools, returning some (but not all) of the work done in stage 1.  At the end of this stage, the fluid is cooler than it was originally.

  4. Heat Absorption: In this stage, the working fluid absorbs heat from the cold side.  At the end of this stage the fluid is at the same temperature and pressure as it was at the beginning of stage 1.  The cycle then repeats.

In general, the system works best when the "cold" temperature corresponds to the condensation of the working fluid at the operating pressure of the system.  The reason for this is that this creates a uniform temperature on the cold side and increases the density of the fluid.  All else being equal, both of these improve heat transfer.

This drives the choice of fluid for the system.  Historically, some of the first refrigerators used Ammonia.  Later, new gases were developed: Chlorofluorocarbons (CFCs).  These were banned for environmental reasons and replaced with fluorocarbons (FCs) and hydrofluorocarbons (HFCs).  These gases also raise some environmental concerns and lately there has been a movement to consider some other gases.

One refrigerant gas which saw some use in the early years and sees increasing use today is Carbon Dioxide (which is known as R744 when it's being used in a refrigerator/heat pump).  This makes it sorta convenient for our use: We can, in some senses, use Carbon Dioxide to refrigerate itself.

Here's how I propose to do that, in the abstract:

  1. Start with ambient air and filter out the fines to the extent that it's possible to do so.  An electrostatic system seems like the best way to get the really fine particles out to me.  This air isn't intended for human consumption so it's a question of machine wear vs. filtering cost.

  2. Compress the air using a turbine.  In this case the pressurization we're looking at is pretty mild: As an example, assuming you want to pressurize from 230 K to 270 K (and assuming CO2 behaves like an ideal gas) the pressure differential will be by a factor of two.  In the case of Martian ambient, that means you're pressurizing from 0.7 kPa to 1.4 kPa.

  3. Cool the gas back down to ambient: Use a heat exchanger that radiates to the surrounding environment to cool the gas back down towards 230 K.  Ammonia might be a good working fluid for this purpose because of its condensation temperature/pressure curve.

  4. Expand the gas through a second turbine and allow it to cool.  Ideally the parameters of this first stage would be such that the gas would cool to the sublimation temperature of 195 K

  5. Compress the gas a second time and remove the heat a second time

  6. Expand the gas through a turbine.  In the first instance, the gas ended up at a lower temperature than when it entered.  In this instance, the temperature can't fall because the gas already started at its sublimation temperature.  Instead, some of the gas condenses out as dry ice.  By cleverly designing the gas flow you can get this dry ice to be deposited at certain select points, where it can be moved batch by batch into the melting chambers.

  7. No more than roughly 10% of the gas can condense out in any one cycle for the turbine to work correctly.  Of the remaining gas, some is tapped off to be used as feedstock for N2 and Ar [this will be more energy intensive because the CO2 needs to be removed entirely but will also produce some dry ice along with useful quantities of Nitrogen and Argon buffer gases] or released to the atmosphere (this is necessary to prevent the mass of gas in the system from increasing forever as N2 and Ar build up) and most is redirected back to the input for the second stage, where it is mixed in an appropriate ratio with gas from the first stage.

My knowledge of refrigeration and chemical process (this system straddles the boundary) is not great, but I think this is the best way to meet our requirements.

#165 Re: Interplanetary transportation » Best RCS propulsion for NTR spaceship » 2018-11-19 17:30:56

kbd512 wrote:

...artificial gravity...

Can you clarify what you mean by this?

#166 Re: Interplanetary transportation » Best RCS propulsion for NTR spaceship » 2018-11-19 14:55:31

It means that you need to know the precise location of the spacecraft better, in order to use such a gentle force over such a long period of time to put it on the right course given the ongoing effect of various gravitational fields.  It's a heavier computational load too.

I don't know exactly where our capabilities lie here but it should be doable.

#167 Re: Science, Technology, and Astronomy » Three Scientific Standards Redefined » 2018-11-19 14:52:43

Isn't it the case that we can't actually measure either of those and that they're calculated from things we can measure or calculate? Makes it kind of hard to use them as standards of measurement

#168 Re: Planetary transportation » Steam powered rovers » 2018-11-19 14:49:35

tahanson43206 wrote:

While there is plenty of water ice at the poles, (I gather), my business plan did not include harvesting any of it.

Can you point me to a post or a link that explains how water ice might occur when dry ice sublimes?

It might make sense to harvest water ice while collecting dry ice.  That is a different question

No substance in nature is pure. There is dry ice at the poles and there is water ice at the poles. Any attempt to mine the one will therefore also produce the other.  Admittedly, I do not know what the ratio of the one to the other will be, but I'm fairly confident that whatever you mine will be less than 100% pure.  Water admixed into the dry ice presents both potential benefits and potential challenges.

Only the real world will tell, but competition between different technologies only works when the two technologies are close enough to parity that they can both be profitable at the same time.  For example, it's possible to get from New York to Los Angeles on foot, on bike, by plane, by train, and by car. People do the latter three to varying degrees, but only do the former extremely rarely because it's so much harder.  Nobody will open a business to bring cargo to LA by bike because it couldn't possibly be profitable.

It's important to mention that mining by teleoperation is not a labor-free activity.  In general the use of robots requires substantial setup and oversight.  Just because the workers aren't out on the cap with a pickaxe doesn't mean their labor doesn't count.

#169 Re: Planetary transportation » Steam powered rovers » 2018-11-19 14:35:53

Terraformer wrote:

Would the system exhaust to ambient pressure, or are there benefits from using a (very large...) tank to hold it at say 100mb? What's the efficiency penalty of going from 10 bars to 1 bar, rather than 10 bar to ambient? It would certainly be easier to repressurise it, no?

I've been assuming the system exhaust would be at ~100 mbar and 195 K and released to ambient.

The exhaust pressure determines the number of reheat cycles you can do, which strongly influences the efficiency of the system.  So, for example, here's the system EROI (Work out divided by work in) and isentropic efficiency and exhaust pressure as a function of the number of heating cycles.  Note that the pressure declines by 62% after each heating cycle.  I assumed an initial pressure of 10 bar.

0PQqh6Q.png

Negative efficiency values correspond to an EROI less than one.  All chemical batteries have negative efficiencies when measured in this way (although it's not clear that you could calculate an actual numerical value for the efficiency because the denominator, heat input, is zero).  All of these values will be lower in a real system: Inefficiencies will make the work input higher and the work output lower. Furthermore, friction between stages will cause pressure loss.

For an input pressure of 10 atm, I would use 5 heating cycles to release gas at 80 mbar.  This means you can get roughly twice as much energy out of each kg of CO2 as if you release at 1000 mbar.

If we were using compressor pumps it would absolutely be the case that pressurizing from 7 mbar to 1000 mbar would be the most energy intensive portion. Work is path dependent, which means that when you go straight from 7 mbar to 10,000 mbar in a small, constant volume (as when you're melting dry ice) you don't do a lot of it.

There's also the consideration of storage: Gases at one bar really are not dense.  Our hypothetical 50 kW overnight power system would require 27 tonnes of LCO2, which at 1 bar and 200 K will take up about 11,000 m^3. Using the same assumptions as for the 10 bar LCO2 tank (post #17) this tank will mass roughly 270 tonnes and have a diameter of 30 meters.

#170 Re: Planetary transportation » Steam powered rovers » 2018-11-19 10:25:40

Hey tahanson,

It's certainly conceivable that mining dry ice at the poles could be economical, but it's hard (for me) to imagine that it would actually make sense unless the end user is actually at the poles.

You used coal as an analogy, and it's a pretty decent one.  However, rather than showing the potential value of CO2 mining I believe it shows why it probably won't be worthwhile.

I believe the appropriate comparison is the system we were discussing before: a refrigeration system that uses energy to freeze CO2 out of the atmosphere.  Here are the costs and benefits of such a system:

Costs:

  • Requires industrial equipment

  • Consumes energy

  • System has not been designed fully yet

Benefits:

  • Generates ~1 kg per kWh of inert gas (primarily Nitrogen and Argon)

  • Works equally well anywhere on Mars

Now, by comparison, here are the costs and benefits of pole-mining:

Costs:

  • Requires an ongoing supply of human labor (All mining does)

  • Consumes energy

  • Requires shipment over thousands of kilometers

  • Requires industrial equipment

  • System for mining a substance that sublimes at 195 K has never been built and would require some tweaks to existing techniques

Benefits:

  • Will produce water as a byproduct

In my view, the question is: Is more labor and thousands of km of shipping worth saving yourself 150 kJ/kg?  In my opinion, it is not.  It's good to compare this to coal:  Coal on Earth has an energy content of 30 MJ/kg, 200 times greater than the energy you save.  Because the energy content is so high, it really is worth pulling out out of the ground and shipping it to the point of use (or at least it was in times past).  I question whether mining CO2 from the poles would save any energy at all.

#171 Re: Planetary transportation » Steam powered rovers » 2018-11-19 00:20:09

I mean, mining dry ice at the pole to use later is an idea but I don't think it's worth doing from an energy perspective unless your settlement is physically located at the poles.

I don't see why you would want to capture the CO2 once you've used it: The low temperature, low-pressure gas output of the system is not really any more valuable than the gas in the atmosphere.  Plus, the volume will be huge: A 50 kW system operating overnight will generate 1.2 million cubic meters of ambient-pressure gas, enough to fill a cube 100 meters on a side.

#172 Re: Unmanned probes » Mars Communications and Navigation Infrastructure for Crewed Missions » 2018-11-18 22:53:24

It would be incredibly frustrating if the FCC felt the need to block people from using certain frequencies in certain ways, but that's life I suppose.

Anyway I don't know a ton about this stuff. If you were creating a network for Martian communications with Earth on a minimum budget, how would you do it?

#173 Re: Planetary transportation » Steam powered rovers » 2018-11-18 22:28:39

The biggest problem with freezing CO2 is volume.  A system able to generate 50 kW at night probably needs to be freezing 600-1000 g per second of CO2 during the day, which is a substantial volume of atmosphere.  I'm not sure exactly what the right way to do it is.

#174 Re: Meta New Mars » New Mars Articles » 2018-11-18 22:23:40

Hey guys!

I took the engine we were talking about in the "Steam Engines on Mars" thread and wrote it up into an article on Newmars:

http://newmars.com/2018/11/on-mars-air- … r-storage/

Hopefully more to come!

#175 Re: Planetary transportation » Steam powered rovers » 2018-11-18 18:42:37

On reliability:

I haven't figured out exactly how I think the freezer system should work.  There's a couple big challenges with that part.  The first challenge is the low density of the Martian atmosphere: To get a single kilogram of CO2 you'll need to process roughly 65 cubic meters of Martian air. 

The second is the heat transfer, specifically how you get dry ice in a useful form (i.e. not as frost on your cooling element). 

Presuming this can be handled in a simple, reliable way, the next least reliable system will be the freezer.     Freezers are in general pretty reliable and in general have long lifetimes (how old is your oldest refrigerator?).

One thing worth pointing out: The design pressure for the tank I specified was 10 atmospheres. You could halve the mass by reducing the design pressure to 5 atmospheres.  I also specified a safety factor of 5, which is standard for Terran pressure vessels but could be reduced in principle.

  1. Index
  2. » Search
  3. » Posts by JoshNH4H

Board footer

Powered by FluxBB