Comment Re: Potential dangers (Score 1) 88
Rei, it's always this way with you. Take the chip off your shoulder.
Firstly, I see you have this notion that martian rocks must all be igneous. This is not correct. That planet has had extensive geologic hydrolysis. Noteworthy shale formations have been found at Jezero and Gale.
https://news.mit.edu/2024/stud...
https://agupubs.onlinelibrary....
The generalized composition profile for windblown dust is very high in basaltic minerals, but many noteworthy sedimentary-dominated structures have been catalogued, as above. Depending on where the regolith is sourced, its composition can vary widely. Blanket statements like 'regolith is not shale!', does not engender notions of superior knowledge. Regolith is the fine to midsized mixture of fractured rocks on the surface. Its composition will be determined by wind erosion and transport patterns, and which rocks became wind eroded. As pointed out above, large surface deposits of hydrolized mineral layers are present on mars.
Rather than pretend I dont know this, I instead correctly asserted that what you do with the collected dust after extracting the perclorate depends entirely on its composition, which will be very site-specific. The one making silly generalizations about the regolith is yourself, Rei.
But, since we are playing 'name the ignorance' in this exchange, your attestation stat perchlorate is 0.5% liberatable oxygen says 'Say i'm ignorant of basic chemistry without saying i'm ignorant of basic chemistry, and am bad at reading too.' The 0.5% statistic comes from the publication at bottom, and is the proportion of the regolith that is perchlorates. This is one of those lemons you seem to have a hard time with, so I'll hold your agitated little hand on this one.
Washing the regolith to remove the perchlorate is a requirement for *any* other use of that regolith. The chlorine it contains is a fouling contaminant for any other industrial process that you put it through. It's not optional. This stuff MUST be washed first. Even at this low of a concentration, its presence would destroy melting crucibles, and deleteriously affect the mechanical properties of resulting products.
Washing it is not optional. It's a required first step for any subsequent process.
As you have rightly pointed out, the water ice on mars is more 'frozen mud'. Cleaning the melt is going to be a necessary first step to using it *regardless*. That means either vacuum distillation, thermal distillation, or reverse osmosis filtration. Again, NOT OPTIONAL. This is necessary equipment that you need to bring, regardless. RO filtration is the least energy intensive of these.
The end products are clean water and perchlorate contaminated mud, and clean mud, with contaminated water.
Since we already have to bring the RO equipment, do it like this:
Permafrost goes in RO unit 1.
clean water and salty mud come out.
Dry, salty regolith, and the dirty mud go in an agitation and settling system. It gets completely cleaned through agitation and settling in a continuous inflow agitator, until water testing shows clean (salt free) water at the outflow. The dirty water is partially re-added to the salty mud in the RO unit, which is processing permafrost, to improve filtration. The remainder is low-sediment saline water, which is fed to another RO unit, giving potable water, and concentrated perchlorate saline solution as products.
This gets you cleaned regolith, concentrated perchlorate brine, and fresh water.
Of those, only one is a lemon. The perchlorate brine. The other two have industrial or immediate uses.
What do we do with this nasty bitter lemon? Do we complain about it, or put it to use? You seem to favor complaining about it, but that's dumb. Instead, it should be made into lemonaide.
Now that we have strongly concentrated the stuff, as a biproduct of producing other things this doomed colony needs, I remind you, the percentage of this stuff is going to be very much higher than 0.6% by weight, so kindly shove that out the airlock, and look at what perchlorate salts *are*: highly oxygenated alkali-earth and transition metal chlorine salts, with a very high recoverable oxygen value.
The very same publication that gives the 0.6% wt value, also gives us a generalized compositional makep of what perchlorates we have. They assay it as predominantly calcium and magnesium perchlorate.
Here are the percentages of oxygen (many wholly liberatable) by weight of various anhydrous perchlorate salts, including calcium and magnesium), and the thermal decomposition temperatures of each. (No electrolysis, just getting it hot enough. Though again, if we have nitrogen, we can use bioreactors for this very cheaply instead. Since thats not guaranteed, here's the thermal decomp route.)
Sodium Perchlorate (NaClO4): 52.3% liberatable oxygen by weight. Thermal decomp at 490-520C at 1atm.
Potassium perchlorate (KClO4): 46.19% liberatable oxygen by weight. Thermal decomp at 550-600C at 1atm.
Calcium perchlorate (Ca(ClO4)2): 53.56% liberatable oxygen by weight. Partial decomp at 150C(!), full decomp at 380-570C at 1atm.
Magnesium perchlorate (Mg(ClO4)2): 57.3% liberatable oxygen by weight (but requires more processing to get it all). Thermal decomp (to MgO) at 369-429C.
Aluminium perchlorate: (Al(ClO4)3): 58.9% oxygen by weight. Aluminium holds oxygen very tightly. Decomposition produces a mix of oxygen and chlorine gasses, with pure aluminium oxide as the end product. This is a useful substance, as it's a principle ore of aluminium, and a useful abrasive in manufacturing. Thermal decomposition begins at 150C, and ends at 450C. (But unlikely to be a major constituent of martian regolith)
Iron(II) perchlorate (Fe(ClO4)2): 50.24% oxygen by weight. Like Aluminium, it holds oxygen tightly. The decomposition initiates a redox reaction that turns iron(ii) into iron(iii), resulting in iron(iii) oxide (Fe2O3), and a mixture of oxygen and chlorine gasses. It functions as a catalyst in the thermal decomposition of other perchlorates. Decomposition starts at 100C(!)
Iron(iii) perchlorate (Fe(ClO4)3): 54.2% liberatable oxygen by weight. Basically the same as iron(ii), but is already oxidized to iron(iii).
Since we need to heat the now cleaned regolith to its melting point *ANYWAY*, (in order to get glasses, basalt fibre, or bisqued shales, as appropriate) we can use the same industrial plant to thermally decompose the perchlorates. If we're building sintering furnaces, we are building sintering furnaces. The decomp temps are comparatively low, compared to the temps needed for melting bassalt. The melting / bisqueing of the regolith will also evolve useful gasses we want to collect and refine later, because of local scarcities *anyway*, so having the equipment in one processing plant makes logistical sense.
Our outputs here are alkali earth oxides (mainly calcium and magnesium oxides, which are useful for making concrete) and chlorides (which are useful for an abundance of chemical processes), oxygen, chlorine, and water vapors, and industrial regolith end products (glasses, basalt fibre, or bisqued shale pellets or bricks, depending on what we fed in.)
Fractional distillation of the gasses will give you distilled water, liquefied oxygen gas, and compressed chlorine gas.
Noteworthy publications: