Return-path: X-Andrew-Authenticated-as: 7997;andrew.cmu.edu;Ted Anderson Received: from hogtown.andrew.cmu.edu via trymail for +dist+/afs/andrew.cmu.edu/usr11/tm2b/space/space.dl@andrew.cmu.edu (->+dist+/afs/andrew.cmu.edu/usr11/tm2b/space/space.dl) (->ota+space.digests) ID ; Sun, 30 Jun 91 02:33:22 -0400 (EDT) Message-ID: Precedence: junk Reply-To: space+@Andrew.CMU.EDU From: space-request+@Andrew.CMU.EDU To: space+@Andrew.CMU.EDU Date: Sun, 30 Jun 91 02:33:15 -0400 (EDT) Subject: SPACE Digest V13 #749 SPACE Digest Volume 13 : Issue 749 Today's Topics: Re: The Adaptive Optics Myth, was Re: HST vs Ground b BITNET mail from MORILLON at FRESE51 Re: Platinum-group metal concentrations in earth-crossing objects Re: Excavating (mining) gold in the space by NASA. Re: Platinum-group metal concentrations in earth-crossing objects Administrivia: Submissions to the SPACE Digest/sci.space should be mailed to space+@andrew.cmu.edu. Other mail, esp. [un]subscription requests, should be sent to space-request+@andrew.cmu.edu, or, if urgent, to tm2b+@andrew.cmu.edu ---------------------------------------------------------------------- Date: 14 Jun 91 14:33:02 GMT From: mcsun!ukc!ox-prg!oxuniv!clements@uunet.uu.net Subject: Re: The Adaptive Optics Myth, was Re: HST vs Ground b >>While it is true that HST does make *some* improvements on the resolution >>achievable by normal ground based telescopes, I would expect that we could do >>a *lot* better by putting the 1.5 billion dollars HST cost into adaptive and >>active optics. These techniques actively correct for the distortions introduced >>by the atmosphere. > But work only in the Near Infrared! The farther towards the visual, let alone > UV you go, the worse the seeing gets and you run out of photons and cannot > analyze the wavefront errors anymore. [I detailed that two years ago in a > letter to 'Nature' which was *accepted* (I even got a proof sheet) but then > never made it into print (or has someone seen it?) - strange...] This is true if you use the photons from you (faint) astronomical object to provide the correction information. Recently published papers (AAS meeting Seatle, 1991) from the declassified SDIO studies in adaptive optics use a laser to generate a fake bright 'star' in the ionosphere which is then used to calculate the necessary wavefront corrections. This, I am lead to believe, has proved very successful, and is *still* much cheaper than HST even at its first guess price. > >>The NTT (New Technology Telescope) at ESO regularly gets >>resolutions well below 1 arcsecond, by using only relatively simple correction >>techniques. The CFHT on Mauna Kea has now been sed to image stars in Virgo galaxies, a project originally slated for HST but shot down by the mirror flaw. > Which have nothing at all to do with Adaptive Optics: the NTT uses Active > Optics which is a *much* slower analyzing & correcting process which ignores > the Seeing completely. [See my article in Sky&Tel Sept.1989 for details.] > This Adaptive Optics plus an excellent site plus an ingenious seeing-reducing > pseudo-dome give the NTT 0.5" regularly and 0.3" at times. HST, BTW, would > have been some 5 to 10 times better, not to speak of its UV capabilities > beyond the atmospheric barrier. > OK. I always get confused between active and adaptive optics. The points remains the same. The UV stuff that HST is still very capable of doing is a unique facility, which should yield some great science. But HST is a very expensive 'super IUE' in that case... >>Other possibilities for beating HSTs resolution on the ground >>include optical interferometry (like the radio mapping that the VLA does but >>in the optical). The ESO VLT will use 4 linked 8 metre optical telescopes to >>get resolutions better than HST will achieve *even if it was built right*, and >>it will cost about 1/10th as much. > The VLTI (VLT Interferometer) is indeed a tremendously exciting prospect for > the early years of the 21st century, but getting actual *images* with 1/10000" > resolution this way will be a *BIG* task. ESO's press people love to show > around the sharpest Neptune images by Voyager 2 and promise that the VLTI will > be able to repeat that (with Adaptive Optics) - unlikely, to say the least. I think you're being a bit doctrinaire in what you call an image. Interferometry is certainly *the* way to get really great resolution. VLTI is not the only way to do it either. A group at Cambridge have got a map of Arcturus using the Hershel in an interferometer mode (mask off most of the 4m reflector and use a few holes in the mask to do interferometry and achieve diffraction limited resolution). The same group are also working on COAST (Cambridge Optical Aperture Synthesis Telescope) whichj they hope to ave working with baslines of 50 to 100 m. This will be streets ahead of HST in rsolution... (when it works). Dave I'll do the .sig later. ------------------------------ Date: 14 JUN 91 19:57:30.45-GMT From: MORILLON%FRESE51.BITNET@vma.cc.cmu.edu Subject: BITNET mail from MORILLON at FRESE51 UNSUBSCRIBE SPACE ------------------------------ Date: 16 Jun 91 02:47:47 GMT From: sequent!muncher.sequent.com!szabo@uunet.uu.net Subject: Re: Platinum-group metal concentrations in earth-crossing objects In article <1991Jun16.000359.10311@world.std.com> webber@world.std.com (Robert D Webber) writes: [Excellent article re: asteroid mining] >In the absence of a container the composition of the GaAs crystal comes >out wrong... This is an interesting statement; why does this occur? >>First, we should find grains with the above concentrations or better >>in a high-metal regolith (a task for space exploration). We >>extract the metal grains with a magnetic rake. Next, we process >>the metal regolith with the gaseous carbonyl process, as follows: > >You will need to break the hunk of rock down in size quite a bit, first... I agree that breaking down the solid metal is difficult. I don't propose to do that for the first mining projects. I am looking for metal regolith (dust and flakes) that is ready to melt. This is known to exist in very small percentages scattered on the Lunar surface, and probably exists in much higher concentrations, perhaps up to >90%, on the surface of metallic asteroids. Alternatively, brittle chondrites contain up to 30% metal flakes and this can be crushed and raked with a magnet to get nearly pure metal regolith. Exploration can make the mining operations much simpler by pointing out the most easily processed material. >So how much does it cost to get the carbon monoxide and water up there >in the first place? Good question. The answer is that comets, carbonaceous chondrite asteroids, and possibly comet fragments in meteor showers contain carbon compounds including carbon monoxide, and also contain abundant water. The ice can be captured using solar thermal engines and the ice itself as reaction mass. The ice-mining operation will have to pay for itself in terms of reaction mass, shielding, heat sinks, and fuel manufactured from the ice materials and used in Earth orbit. I call this "ice bootstrapping" since ice as reaction mass can be used to lift more equipment to catch more chunks of ice, etc. until the cost of fuel, heat sinks, and shielding in Earth orbit is very low. As you point out rock and metal processing is quite non-trivial. In comparison, however, ice mining requires little more than a mirror, bag, and simple distillery. After the ice bootstrapping takes place, it will be much easier to lift heavy mining equipment out to the asteroids, or alternatively bring raw asteroid regolith to Earth orbit and process it there. The ice also provides the water and carbon monoxide needed for the carbonyl process. Volatile mining will likely be the first use of extraterrestrial materials, but it cannot occur until we have explored the earth-crossing asteroids and meteor showers sufficiently to find good sources of ice, or, failing that, the highest concentrations of water of hydration and carbon in chondrites. >Incidentally, you will need a fair bit of material for the >carbonyl process fixtures as well. The units I saw on a tour of the >Inco facilities in Sudbury were pretty massive, though I'll grant you >that a space facility can be less concerned about accidental carbonyl >releases than an earth-based one. This is a rather underated aspect of space industry. In the long run, it can replace many Earthside industries that really should not be conducted in the middle of an ecosystem. In the short run, the ability to work outside the ecosystem can make some processes significantly cheaper. I am not sure to what extent the carbonyl process is an example; can any readers shed more light on this? >>If we want to get the pure elements additional processing is >>required. > >No kidding?! :-) At this point the impure mixture of platinum-group elements, gallium, arsenic, and other stuff is already worth $20,000/kg. The rest of the processing can be done on Earth. If we want to use any of these in the pure form in orbit, we need the "additional processing." >I've often wondered whether any of the people who figure that metallurgical >operations in space would be simple have ever visited an earthside >metals extraction plant. I share your impatience. In the space community there is an underestimation of mining engineering across the spectrum of mining operations. Many "Manned Mars Mission" scenarios, for example, propose extracting fuel from extraterrestrial regolith and assume that the mining engineering is going to be trivial without detailed analysis or, for that matter, even bothering to ask a mining engineer. Mining equipment is itself difficult; mining equipment in vacuum and microgravity will take much engineering and trial and error before we get it right. On the other hand, if we use the abundant thermal energy, microgravity, and vacuum to full advantage, some of the processes become much easier. (Some become much harder, so we don't use those). That is my other pet peeve on this subject. Merely transfering Earth mining techniques into space is stupidity. We need to take full advantage of the new environment. Much work has to be done to determine which processes gain the most advantage, what new processes are made possible, and how much can be done with the least mass of equipment. The actual mines will bear very little outward resemblence to their Earthside counterparts. At $3.4 billion/year for just the platinum-group elements, billions more for space-manufactured semiconductors, alloys, and other products, and potentially tens of billions per year for solar power satellites, there is quite a bit of incentive for that work to get done. -- Nick Szabo szabo@sequent.com Embrace Change... Keep the Values... Hold Dear the Laughter... These views are my own, and do not represent any organization. ------------------------------ Date: 15 Jun 91 20:00:29 GMT From: cis.ohio-state.edu!zaphod.mps.ohio-state.edu!swrinde!cs.utexas.edu!uwm.edu!ux1.cso.uiuc.edu!bryans@ucbvax.Berkeley.EDU (B. Charles Siegfried) Subject: Re: Excavating (mining) gold in the space by NASA. shafer@skipper.dfrf.nasa.gov (Mary Shafer) writes: >The gold and silver that the Spanish brought back from the New World >messed up the European economy quite greviously. Galloping inflation, >with too much money (precious metals, of course) chasing too few goods. >This caused a lot of instability, first economic and then political. When the Spanish brought back their riches, Europe's currency was essentially based on precious metals. Gold and silver do have more influence than most commodities, but an infusion of a larg amount of gold would have little effect on the whole world economy compared to what Europe experienced in the mercatilist age. Besides, the need to open new markets and to grow certainly outweighs any minor dislocations in the process. Europe may have experienced a little shake - up when their metal currency was debased, but the summ effect of colonialization provided a tremendous boost to the European economy. __ Bryan Siegfried Biology and Economics at UIUC zig@uiuc.edu ------------------------------ Date: 16 Jun 91 00:03:59 GMT From: cis.ohio-state.edu!zaphod.mps.ohio-state.edu!think.com!snorkelwacker.mit.edu!world!webber@ucbvax.Berkeley.EDU (Robert D Webber) Subject: Re: Platinum-group metal concentrations in earth-crossing objects In article <1991Jun12.073415.12543@sequent.com> szabo@sequent.com writes: > >The best data we have come from the asteroid samples fallen to Earth, >meteorites, many of which contain metal or metal grains from core >material. The best platinum-group concentrations have been >found in the metal grains of LL-type chondrites, as follows: > [...numbers in the tens of ppm deleted...] > >As an aside, they also contain 1-15 ppm gallium, 200 ppm germanium, and >1.2 ppm arsenic. Space Industries Inc. is currently working on a >wake shield to produce large volumes of very high vacuum, which can >be used with microgravity to create GaAs and other semiconductors >with much greater purity than in Earthside semiconductor fabs. Back in semiconductor fabrication class they always told us the biggest contamination problem came from the container, and that the high vapour pressure of arsenic led to a need for either As pressurization or some kind of complete encapsulation for the melt. In the absence of a container the composition of the GaAs crystal comes out wrong, so I don't see how the "very high vacuum" will help fabrication operations for the materials used to make devices. >Back to platinum: we have a total of 55 ppm platinum group, about 5 >times better than the best Earth ore. This still wouldn't be that >good, given the high costs of launching mining equipment, except >that there exists a process which, taking advantage of the large >amounts of solar-thermal power available in space, could make >extracting the platinum economical. > >First, we should find grains with the above concentrations or better >in a high-metal regolith (a task for space exploration). We >extract the metal grains with a magnetic rake. Next, we process >the metal regolith with the gaseous carbonyl process, as follows: You will need to break the hunk of rock down in size quite a bit, first. On the ground this is generally accomplished by crushing in rather large, heavy machines, then grinding in a mill where balls or rods are raised from and dropped back onto the material to be ground. Obviously the term "dropped" implies the machine's presence in a gravity field. I suppose that some other accelerating field could be substituted. Anyway, the grinding medium in a conventional process needs to be dense so that the individual grinding elements have a lot of kinetic energy for a small surface area: this allows a lot of K.E. to be transformed into the energy of new surfaces during the grinding process in a short period of time. What are you proposing as an alternative to this very much earthbound, heavyweight technology? You definitely need something to get the mineral particles down to liberation size in the process you describe. > >First phase: > >Treat the regolith with CO at c. 5 atm pressure, 100 degrees >C. This forms a vapor of gaseous carbonyl compounds. [...some details of carbonyl processing deleted...] >The water and CO are again recycled. So how much does it cost to get the carbon monoxide and water up there in the first place? I would guess that you can ship up oxygen and make the monoxide on the spot, once you ship up or build the requisite process equipment, but shipping water around seems like a somewhat bad idea. Incidentally, you will need a fair bit of material for the carbonyl process fixtures as well. The units I saw on a tour of the Inco facilities in Sudbury were pretty massive, though I'll grant you that a space facility can be less concerned about accidental carbonyl releases than an earth-based one. One other point: you get metals back out of the carbonyl state by plating them out on metallic seeds. If your particles are all down to liberation size, I'd be willing to bet real money that a lot of platinide dust will end up blowing around in the carbonyl tank and getting trapped by nickel/ cobalt/iron shell growth on a seed. >This technique, called the gaseous carbonyl process, is currently >used at the Sudbury mine in Ontario, primarily to extract the nickel, >and secondarily to extract the c. 5 ppm platinum. By some accounts >the Sudbury ore is actually the remains of an impacted asteroid, >but I won't get into _that_ broohaha. :-) There are several operators and a number of mines and mills in the Sudbury, Ontario area. The carbonyl plant is located (if my memory of my visit hasn't spoiled since it's been defrosted) at one of Inco's facilities, as noted above. However, precious metals are typically recovered from anode slime which collects at the bottoms of electrolytic cells during electrowinning, having precipitated out of molten sulphide as very fine metallic particles. Further separation of gold and platinides is carried out by additional electrochemical processing. The last I heard, the theory was that the high-grade sulphide ore being mined at Sudbury was formed by an upwelling in crustal cracks after a meteor strike. The actual material involved in the meteor seems unlikely to have produced the millions of tons of material which have been mined in the Sudbury area. >If we want to get the pure elements additional processing is >required. No kidding?! I've often wondered whether any of the people who figure that metallurgical operations in space would be simple have ever visited an earthside metals extraction plant. It ain't simple down here, guys, and the size and cost of even crude equipment is pretty staggering for somebody used to stuff like computers. Our state of knowledge for most extraction processes, and for the systems from which we're extracting values, is pretty poor, too: we've come a long way from Agricola, but not as far as it is to what you want to do, and in nowhere nearly as little time. ------------------------------ End of SPACE Digest V13 #749 *******************