An international collaboration involving scientists in Tenerife, the US and the UK, are using Diamond, the UK’s world class science institute operating a synchrotron that provides industrial and academic user communities with access to state of the art analytical tools, to investigate Moon rocks recovered during the Apollo Missions in a brand new way.
Dr. Matt Pankhurst of Instituto Volcanológico de Canarias and NASA lunar principle investigator explains; “We have used a new imaging technique developed at Diamond to carry out 3D mapping of olivine – a common green mineral found in the Earth’s sub-surface and in these Moon rock samples. These maps will be used to improve understanding of the Moon’s ancient volcanic systems and help to understand active geological processes here on Earth.
With this new technique, our team may be able to recover from these Moon rock samples information such as what the patterns of magma flow within the volcanic system were, what the magma storage duration was like, and potentially even identify eruption triggers. The data will be analysed using state-of-the-art diffusion modelling which will establish the history of individual crystals.”
When early astronomers looked at the Moon, they mistakenly thought that the darker areas they could see were seas, and named them Mare, the Latin for sea. Around 16% of the lunar surface is covered in this dark material, which we now know is basalt, a volcanic rock. Before the Apollo missions, we believed that these areas meant that they were young, but when the rock samples brought back from the Moon were examined, they were shown to be ancient; the youngest volcanic Moon rock sample is nearly 3 billion years old.
The team have examined samples from the Apollo 12 and 15 missions, using an advanced X-ray speckle imaging technique developed on Beamline B16 at Diamond Light Source. As Dr. Hongchang Wang, Senior Optics Scientist, explains: “Combined with the recently developed fast fly-scan tomography and novel white beam camera, the X-ray speckle imaging technique has allowed us to swiftly and effectively collect 3D information of olivine inside of the lunar rock in much more detail than ever before.” This new technique does not damage the lunar samples.
Dr. Pankhurst continues; “Nearly 50 years after the first humans landed on the Moon, there is still a lot we don’t know about how the Moon formed, and the nature of lunar volcanic activity. We know that, on Earth, volcanic eruptions can be triggered (or ended) by changes in magma (molten rock) in or beneath the planet’s crust. The cause of these changes is often thought to be a result of the mixing of different batches of magma in the ‘plumbing system’ below the volcanoes. Volcanologists are working on detecting and understanding these changes, by examining volcanic rock samples, with the aim of being able to accurately forecast future eruptions.”
The same techniques are now being applied to lunar rock samples, which will provide new insights into how the Moon was formed, and its volcanic history.
In magma, the ratio of iron to magnesium in olivine changes over timeframes ranging from hours to months, and these changes are ‘locked in’ to the mineral as the magma cools. Accurate 3D images of the iron distribution within olivine in the Moon rock samples will ‘unlock’ information about the volcanic processes in which they formed.
NASA has approved the use of 18 lunar samples for these experiments, and similar, well-characterised terrestrial samples have also been scanned, and used to verify the chemical composition of olivine. Samples are loaned to scientists who wish to study them, a process overseen by NASA's Apollo sample curator, Ryan Zeigler. As a scientist who understands the trade-off between studying the samples and preserving them, a balance must be struck in experiment design. These decisions are becoming easier as we develop more powerful, non-destructive techniques. He comments: “The researchers are now using state-of-the-art diffusion modelling to establish the history of individual crystals of olivine from 3D images. These techniques will be applied to the new data gathered during this beamtime. The results will add to our understanding of lunar and planetary formation, topics which have been continually debated since the samples were first returned to Earth.”
Prof Andrew Harrison CEO at Diamond Light Source concludes: “A successful demonstration of the new technique at B16 will pave the way, we hope, for extended collaboration with NASA and maybe next No10* Downing Street and the Natural History Museum might be interested in loaning us their own samples.”
Diamond has a huge amount of experience of investigating priceless heritage items, and gaining new insights from them. Using these techniques, we could study the UK’s Moon rock samples in new ways, and these fresh images would give them more meaning and inspire the next generation of scientists and engineers.