Showing posts with label Meteorite. Show all posts
Showing posts with label Meteorite. Show all posts

Thursday, December 18, 2025

Mining asteroids for water and metals explored

Carbonaceous chondrite meteorite
Credit: J.M.Trigo-Rodríguez/ICE-CSIC
Licence type: Attribution (CC BY 4.0)



The potential for space mining – including identifying asteroids close to Mars and Jupiter best suited for extracting precious metals and water – has been explored in a new study.

Research published in Monthly Notices of the Royal Astronomical Society looked into how viable the idea would be in the future.

Much is still unknown about the chemical composition of small asteroids but their potential to harbour valuable metals, materials from the early solar system, and the possibility of obtaining a geochemical record of their parent bodies makes them promising candidates for future use of space resources.

A team led by the Institute of Space Sciences (ICE-CSIC) in Spain analysed meteorites that had fallen to Earth, including from NASA’s Antarctic collection, to determine the chemical composition of the six most common groups of carbonaceous chondrites.

Their findings support the idea that these asteroids can serve as crucial material sources and identify their parent bodies, as well as for planning future missions and developing new technologies for resource exploitation.

Several proposals have already been put forward, such as capturing small asteroids that pass close to Earth and placing them in a circumlunar orbit for exploitation.

“For certain water-rich carbonaceous asteroids, extracting water for reuse seems more viable, either as fuel or as a primary resource for exploring other worlds,” said Dr Josep Trigo-Rodríguez, first author of the study and astrophysicist at ICE-CSIC, affiliated to the Institute of Space Studies of Catalonia (IEEC).

“This could also provide science with greater knowledge about certain bodies that could one day threaten our very existence. In the long term, we could even mine and shrink potentially hazardous asteroids so that they cease to be dangerous.”

Carbonaceous chondrites are relatively rare – making up just 5 per cent of meteorite falls – and many of them are so fragile that they fragment and are never recovered. Those that have been are usually found in desert regions, such as the Sahara or Antarctica.

“The scientific interest in each of these meteorites is that they sample small, undifferentiated asteroids, and provide valuable information on the chemical composition and evolutionary history of the bodies from which they originate,” Dr Trigo-Rodríguez explained.

Pau Grèbol Tomás, ICE-CSIC predoctoral researcher, said: “Studying and selecting these types of meteorites in our clean room and using other analytical techniques is fascinating, particularly because of the diversity of minerals and chemical elements they contain.

“However, most asteroids have relatively small abundances of precious elements, and therefore the objective of our study has been to understand to what extent their extraction would be viable.”

Study co-author Jordi Ibáñez-Insa, of the Geosciences Barcelona (GEO3BCN-CSIC), said: “Although most small asteroids have surfaces covered in fragmented material called regolith – and it would facilitate the return of small amounts of samples – developing large-scale collection systems to achieve clear benefits is a very different matter.

“In any case, it deserves to be explored because the search for resources in space would likely minimise the impact of mining activities on terrestrial ecosystems.”

Given the diversity present in the main asteroid belt, it is crucial to define what types of resources could be found there.

“They are small and quite heterogeneous objects, heavily influenced by their evolutionary history, particularly collisions and close approaches to the Sun,” said Dr Trigo-Rodríguez.

“If we are looking for water, there are certain asteroids from which hydrated carbonaceous chondrites originate, which, conversely, will have fewer metals in their native state.

“Let's not forget that, after 4.56 billion years since their formation, each asteroid has a different composition, as revealed by the study of chondritic meteorites.”

One of the study's conclusions is that mining undifferentiated asteroids – the primordial remnants of the solar system's formation considered the progenitor bodies of chondritic meteorites – is still far from viable.

On the other hand, the study points to a type of pristine asteroid with olivine and spinel bands as a potential target for mining. A comprehensive chemical analysis of carbonaceous chondrites is essential to identify promising targets for space mining.

However, the team states that this effort must be accompanied by new sample-return missions to verify the identity of the progenitor bodies.

“Alongside the progress represented by sample return missions, companies capable of taking decisive steps in the technological development necessary to extract and collect these materials under low-gravity conditions are truly needed,” Dr Trigo-Rodríguez added.

“The processing of these materials and the waste generated would also have a significant impact that should be quantified and properly mitigated.”

The team is confident of very short-term progress, given that the use of in-situ resources will be a key factor for future long-term missions to the Moon and Mars, reducing dependence on resupply from Earth.

In this regard, the authors point out that if water extraction were the goal, water-altered asteroids with a high concentration of water-bearing minerals should be selected. Exploiting these resources under low-gravity conditions requires the development of new extraction and processing techniques.

“It sounds like science fiction, but it also seemed like science fiction when the first sample return missions were being planned 30 years ago,” said Grèbol Tomàs.

The scientific team from ICE-CSIC selected, characterised, and provided the asteroid samples, which were analysed using mass spectrometry at the University of Castilla-La Mancha by Professor Jacinto Alonso-Azcárate.

This allowed them to determine the precise chemical abundances of the six most common classes of carbonaceous chondrites, fostering the discussion among the scientific community of whether their future extraction would be feasible.

The Asteroids, Comets, and Meteorites research group at ICE-CSIC investigates the physicochemical properties of the materials that make up the surfaces of asteroids and comets and has made numerous contributions in this field over the last decade.

“At ICE-CSIC and IEEC, we specialise in developing experiments to better understand the properties of these asteroids and how the physical processes that occur in space affect their nature and mineralogy,” said Dr Trigo-Rodríguez, who leads this group.

For over a decade he has been involved in selecting and requesting from NASA the carbonaceous chondrites analysed in this study, as well as devising several experiments with them.

"The work now being published is the culmination of that team effort," Dr Trigo-Rodríguez added.




Media contacts:

Sam Tonkin
Royal Astronomical Society
Mob: +44 (0)7802 877 700

press@ras.ac.uk

Dr Robert Massey
Royal Astronomical Society
Mob: +44 (0)7802 877 699

press@ras.ac.uk



Science contacts:

Dr Josep Trigo-Rodríguez
ICE-CSIC

trigo@ice.csic.es



Images & captions

Carbonaceous chondrite meteorite

Caption: Reflected light image of a thin section of carbonaceous chondrite CV3 from NASA's Antarctic collection, analysed in the study. Several chondrules with bright olivine crystals embedded in a carbonaceous matrix can be seen. Credit: J.M.Trigo-Rodríguez/ICE-CSIC



Further information

The paper ‘Assessing the metal and rare earth element mining potential of undifferentiated asteroids through the study of carbonaceous chondrites’ by J.M. Trigo-Rodríguez et al. has been published in Monthly Notices of the Royal Astronomical Society. DOI: 10.1093/mnras/staf1902.



Notes for editors

About the Royal Astronomical Society

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The RAS organises scientific meetings, publishes international research and review journals, recognises outstanding achievements by the award of medals and prizes, maintains an extensive library, supports education through grants and outreach activities and represents UK astronomy nationally and internationally. Its more than 4,000 members (Fellows), a third based overseas, include scientific researchers in universities, observatories and laboratories as well as historians of astronomy and others.

The RAS accepts papers for its journals based on the principle of peer review, in which fellow experts on the editorial boards accept the paper as worth considering. The Society issues press releases based on a similar principle, but the organisations and scientists concerned have overall responsibility for their content.

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Submitted by Sam Tonkin on Wed, 10/12/2025 - 09:00


Wednesday, December 15, 2010

Building Blocks of Life Created in "Impossible" Place

This is a NASA Hubble Space Telescope picture of what was first thought to be a comet but is probably an asteroid collision. The inset picture shows a complex structure that suggests the object is not a comet but instead the product of a head-on collision between two asteroids traveling five times faster than a rifle bullet (about three miles per second). Astronomers have long thought that the asteroid belt is being ground down through collisions, but such a smashup has never before been seen. The filaments are made of dust and gravel, presumably recently thrown out of the 460-foot-diameter nucleus. Some of the filaments are swept back by radiation pressure from sunlight to create straight dust streaks. Embedded in the filaments are co-moving blobs of dust that likely originate from tiny unseen parent bodies. An impact origin would also be consistent with the absence of gas in spectra recorded using ground-based telescopes. At the time of the Hubble observations in January 2010, the object was approximately 180 million miles (300 million km) from the Sun and 90 million miles (140 million km) from Earth. Credit: NASA, ESA, and D. Jewitt (UCLA). Full-resolution copy

GREENBELT, Md. -- NASA-funded scientists have discovered amino acids, a fundamental building block of life, in a meteorite where none were expected.

"This meteorite formed when two asteroids collided," said Dr. Daniel Glavin of NASA’s Goddard Space Flight Center, Greenbelt, Md. "The shock of the collision heated it to more than 2,000 degrees Fahrenheit, hot enough that all complex organic molecules like amino acids should have been destroyed, but we found them anyway." Glavin is lead author of a paper on this discovery appearing December 15 in Meteoritics and Planetary Science. "Finding them in this type of meteorite suggests that there is more than one way to make amino acids in space, which increases the chance for finding life elsewhere in the Universe."

Amino acids are used to make proteins, the workhorse molecules of life, used in everything from structures like hair to enzymes, the catalysts that speed up or regulate chemical reactions. Just as the 26 letters of the alphabet are arranged in limitless combinations to make words, life uses 20 different amino acids in a huge variety of arrangements to build millions of different proteins. Previously, scientists at the Goddard Astrobiology Analytical Laboratory have found amino acids in samples of comet Wild 2 from NASA’s Stardust mission, and in various carbon-rich meteorites. Finding amino acids in these objects supports the theory that the origin of life got a boost from space -- some of life’s ingredients formed in space and were delivered to Earth long ago by meteorite impacts.

When Dr. Peter Jenniskens of the SETI Institute, Mountain View, Calif., and NASA's Ames Research Center, Moffett Field, Calif., approached NASA with the suggestion to search for amino acids in the carbon-rich remnants of asteroid 2008 TC3, expectations were that nothing was to be found. Because of an unusually violent collision in the past, this asteroid's ingredients for life were a "culinary disaster" and now mostly in the form of graphite. The small asteroid, estimated at six to fifteen feet across, was the first to be detected in space prior to impact on Earth on October 7, 2008. When Jenniskens and Dr. Muawia Shaddad of the University of Khartoum recovered remnants in the Nubian Desert of northern Sudan, the remnants turned out to be the first Ureilite meteorites found in pristine condition.

A meteorite sample was divided between the Goddard lab and a lab at the Scripps Institution of Oceanography at the University of California, San Diego. "Our analyses confirm those obtained at Goddard," said Professor Jeffrey Bada of Scripps, who led the analysis there. The extremely sensitive equipment in both labs detected small amounts of 19 different amino acids in the sample, ranging from 0.5 to 149 parts per billion. The team had to be sure that the amino acids in the meteorite didn’t come from contamination by life on Earth, and they were able to do so because of the way amino acids are made. Amino acid molecules can be built in two ways that are mirror images of each other, like your hands. Life on Earth uses left-handed amino acids, and they are never mixed with right-handed ones, but the amino acids found in the meteorite had equal amounts of the left and right-handed varieties.

The sample had various minerals that only form under high temperatures, indicating it was forged in a violent collision. It's possible that the amino acids are simply leftovers from one of the original asteroids in the collision – an asteroid that had better conditions for amino acid formation. Dr. Jennifer Blank of SETI has done experiments with amino acids in water and ice, showing they survive pressures and temperatures comparable to a low-angle comet-Earth impact or asteroid-asteroid collisions.

However, the team thinks it's unlikely amino acids could have survived the conditions that created the meteorite, which endured higher temperatures – more than 2,000 degrees Fahrenheit (over 1,100 Celsius) – over a much longer period. "It would be hard to transfer amino acids from an impactor to another body simply because of the high-energy conditions associated with the impact," said Bada.

Instead, the team believes there’s an alternate method for making amino acids in space. "Previously, we thought the simplest way to make amino acids in an asteroid was at cooler temperatures in the presence of liquid water. This meteorite suggests there’s another way involving reactions in gases as a very hot asteroid cools down," said Glavin. The team is planning experiments to test various gas-phase chemical reactions to see if they generate amino acids.

Infrared image taken by the Meteosat 8 satellite of asteroid 2008 TC3 exploding. The path of the asteroid is shown with a yellow arrow; red-yellow blob on arrow is infrared from the explosion. Credit: EUMESTAT

A typical example of a meteorite remnant linked to asteroid 2008 TC3, with a dark scruffy texture. Credit: Peter Jenniskens. Full-resolution copy

Fragments of 2008 TC3 are collectively called "Almahata Sitta" or "Station Six" after the train stop in northern Sudan near the location where pieces were recovered. They are prized because they are Ureilites, a rare type of meteorite. "An interesting possibility is that Ureilites are thought by some researchers to have formed in the solar nebula and thus the findings of amino acids in Almahata Sitta might imply that amino acids were in fact synthesized very early in the history of the solar system," adds Bada.

The Goddard analysis team includes Glavin and Drs. Jason Dworkin, Michael Callahan, and Jamie Elsila. This research was funded by the NASA Astrobiology Institute, which is managed by NASA Ames; the Goddard Center for Astrobiology, and the NASA Cosmochemistry and Astrobiology: Exobiology and Evolutionary Biology programs.

Contact

Nancy Neal-Jones / Bill Steigerwald
NASA's Goddard Space Flight Center, Greenbelt, Md.
301-286-0039 / 5017
Nancy.N.Jones@nasa.gov / William.A.Steigerwald@nasa.gov