Academics from Milton Keynes based Open University, have discovered the spectral signature of water ice that reveals new information about how ice forms and evolves during the birth of stars and planets.
A team of astronomers, including Open University (OU) academics, Helen Fraser and Hugh Dickinson and OU PhD student Zak Smith, have discovered the spectral signature of water ice that reveals new information about how ice forms and evolves during the birth of stars and planets. Their findings have been published today in the journal Nature Astronomy.
A spectral signature is like the fingerprint of a molecule; it is unique to a particular chemical and occurs in this case at a specific infrared wavelength that reflects the motion of oxygen and hydrogen atoms in the water molecule, relative to each other.
Astronomers used the James Webb Space Telescope (JWST) to reveal the ‘dangling OH’ features of water ice using observations with the NIRCAM (Near Infrared Camera).
The ‘dangling OH’ signatures reveal water molecules that aren’t fully locked into the ice but are hanging out of the ice surface. This indicates that the material is porous, fluffy and chemically reactive.
This discovery opens a new window on studying star and planet formation since these newly discovered features allow scientists to build up an idea of the spatial distribution and structure of ices, as well as how they evolve on their journey from molecular clouds to planets.
OU scientists from the School of Physical Sciences were instrumental in this discovery as they used local high-performance computing to process the telescope data and analysed their findings with data recorded in the OU astrochemical laboratories.
The detection of dangling OH bonds described in the paper, led by Dr Jenny Noble from the French National Centre for Scientific Research (CNRS), are significant because these spectral features have been observed for decades in the laboratory but never before in star-forming regions in space.
The ‘dangling OH’ features occur at infrared wavelengths that are impossible to observe with ground-based telescopes but are accessible to JWST. Although it was thought that these features should be observed in the icy material in star-forming regions, this is the first time they have actually been spotted in observations.
Dr Helen Fraser, Senior Lecturer in Astronomy and Director of Research in the School of Physical Sciences, who leads the OU astrochemistry group said, “Historically, it was possible to measure intense absorption features linked with major ice species in star-forming clouds, namely water, carbon dioxide, carbon monoxide, methanol, and ammonia. Thanks to JWST’s unprecedented spectral, spatial and flux sensitivity, we can now measure super-weak spectral features, perhaps 1/100th the intensity of the bulk ice bands.”
Researchers used an ice mapping technique developed by Dr Helen Fraser and her team to study ice in a nearby cloud region called Chamaeleon I. This technique allowed them to analyse light from hundreds of stars behind the cloud, revealing how much ice was present in the molecular cloud. By looking specifical at the ‘dangling OH’ spectral feature, they were able to map the distribution of these surface water molecules and found that they were concentrated around the densest regions encircling a core of gas and dusty material, inside which it is possible a new star has formed that is only a few thousand years old.
This discovery opens a view on the structure of icy material in space, and its potential to catalyse the formation of more complex chemical species as star and planet formation progresses. Research is ongoing in the OU Astrochemistry group to illustrate the power of interstellar ice-mapping.
