From The European Southern Observatory [Observatorio Europeo Austral] [Observatoire européen austral][Europäische Südsternwarte] (EU)(CL): “Astronomers find missing link for water in the Solar System”
3.8.23
John J. Tobin
National Radio Astronomy Observatory
Charlottesville, USA
Email: jtobin@nrao.edu
Margot Leemker
Leiden Observatory
Leiden, the Netherlands
Email: leemker@strw.leidenuniv.nl
Juan Carlos Muñoz Mateos
ESO Media Officer
Garching bei München, Germany
Tel: +49 89 3200 6176
Email: press@eso.org
Water in the planet-forming disc around the star V883 Orionis (artist’s impression)
ALMA images of the disc around the star V883 Orionis, showing the spatial distribution of water (left, orange), dust (middle, green) and carbon monoxide (blue, right). Because water freezes out at higher temperatures than carbon monoxide, it can only be detected in gaseous form closer to the star. The apparent gap in the the water and carbon monoxide images is actually due to the bright emission of the dust, which attenuates the emission of the gas. Credit: ALMA (ESO/NAOJ/NRAO); J. Tobin, B. Saxton (NRAO/AUI/NSF)
This artist’s impression shows the planet-forming disc around the star V883 Orionis. In the outermost part of the disc water is frozen out as ice and therefore can’t be easily detected. An outburst of energy from the star heats the inner disc to a temperature where water is gaseous, enabling astronomers to detect it. Credit: L. Calçada/ESO.
Using the Atacama Large Millimeter/submillimeter Array (ALMA) [below], astronomers have detected gaseous water in the planet-forming disc around the star V883 Orionis. This water carries a chemical signature that explains the journey of water from star-forming gas clouds to planets, and supports the idea that water on Earth is even older than our Sun.
“We can now trace the origins of water in our Solar System to before the formation of the Sun,” says John J. Tobin, an astronomer at the National Radio Astronomy Observatory, USA and lead author of the study published today in Nature [below].
This discovery was made by studying the composition of water in V883 Orionis [depictions above], a planet-forming disc about 1300 light-years away from Earth. When a cloud of gas and dust collapses it forms a star at its centre. Around the star, material from the cloud also forms a disc. Over the course of a few million years, the matter in the disc clumps together to form comets, asteroids, and eventually planets. Tobin and his team used ALMA, in which the European Southern Observatory (ESO) is a partner, to measure chemical signatures of the water and its path from the star-forming cloud to planets.
Water usually consists of one oxygen atom and two hydrogen atoms. Tobin’s team studied a slightly heavier version of water where one of the hydrogen atoms is replaced with deuterium — a heavy isotope of hydrogen. Because simple and heavy water form under different conditions, their ratio can be used to trace when and where the water was formed. For instance, this ratio in some Solar System comets has been shown to be similar to that in water on Earth, suggesting that comets might have delivered water to Earth.
The journey of water from clouds to young stars, and then later from comets to planets has previously been observed, but until now the link between the young stars and comets was missing. “V883 Orionis is the missing link in this case,” says Tobin. “The composition of the water in the disc is very similar to that of comets in our own Solar System. This is confirmation of the idea that the water in planetary systems formed billions of years ago, before the Sun, in interstellar space, and has been inherited by both comets and Earth, relatively unchanged.”
But observing the water turned out to be tricky. “Most of the water in planet-forming discs is frozen out as ice, so it’s usually hidden from our view,” says co-author Margot Leemker, a PhD student at Leiden Observatory in the Netherlands. Gaseous water can be detected thanks to the radiation emitted by molecules as they spin and vibrate, but this is more complicated when the water is frozen, where the motion of molecules is more constrained. Gaseous water can be found towards the centre of the discs, close to the star, where it’s warmer. However, these close-in regions are hidden by the dust disc itself, and are also too small to be imaged with our telescopes.
Fortunately, the V883 Orionis disc was shown in a recent study [Nature (below)] to be unusually hot. A dramatic outburst of energy from the star heats the disc, “up to a temperature where water is no longer in the form of ice, but gas, enabling us to detect it,” says Tobin.
The team used ALMA, an array of radio telescopes in northern Chile, to observe the gaseous water in V883 Orionis. Thanks to its sensitivity and ability to discern small details they were able to both detect the water and determine its composition, as well as map its distribution within the disc. From the observations, they found this disc contains at least 1200 times the amount of water in all Earth’s oceans.
In the future, they hope to use ESO’s upcoming Extremely Large Telescope [below] and its first-generation instrument METIS.
This mid-infrared instrument will be able to resolve the gas-phase of water in these types of discs, strengthening the link of water’s path all the way from star-forming clouds to solar systems. ”This will give us a much more complete view of the ice and gas in planet-forming discs,” concludes Leemker.
More information
This research was presented in a paper to appear in Nature [below]
The team is composed of John J. Tobin (National Radio Astronomy Observatory, USA), Merel L. R. van’t Hoff (Department of Astronomy, University of Michigan, USA), Margot Leemker (Leiden Observatory, Leiden University, the Netherlands [Leiden]) , Ewine F. van Dishoeck (Leiden), Teresa Paneque-Carreño (Leiden; European Southern Observatory, Germany), Kenji Furuya (National Astronomical Observatory of Japan, Japan), Daniel Harsono (Institute of Astronomy, National Tsing Hua University, Taiwan), Magnus V. Persson (Department of Space, Earth and Environment, Chalmers University of Technology, Onsala Space Observatory, Sweden), L. Ilsedore Cleeves (Department of Astronomy, University of Virginia, USA), Patrick D. Sheehan (Center for Interdisciplinary Exploration and Research in Astronomy, Northwestern University, USA) and Lucas Cieza (Núcleo de Astronomía, Facultad de Ingeniería, Millennium Nucleus on Young Exoplanets and their Moons, Universidad Diego Portales, Chile).
Nature 2016
Nature
From the science paper
Abstract
Water is a fundamental molecule in the star and planet formation process, essential for catalysing the growth of solid material and the formation of planetesimals within disks[1*],[2]. However, the water snowline and the HDO:H2O ratio within proto-planetary disks have not been well characterized because water only sublimates at roughly 160 K (ref. 3), meaning that most water is frozen out onto dust grains and that the water snowline radii are less than 10 AU (astronomical units)[4],[5]. The sun-like protostar V883 Ori (M* = 1.3 M⊙)[6] is undergoing an accretion burst[7], increasing its luminosity to roughly 200 L⊙ (ref. 8), and previous observations suggested that its water snowline is 40–120 AU in radius[6],[9],[10]. Here we report the direct detection of gas phase water (HDO and H218O) from the disk of V883 Ori. We measure a midplane water snowline radius of approximately 80 AU, comparable to the scale of the Kuiper Belt, and detect water out to a radius of roughly 160 AU. We then measure the HDO:H2O ratio of the disk to be (2.26 ± 0.63) × 10−3. This ratio is comparable to those of protostellar envelopes and comets, and exceeds that of Earth’s oceans by 3.1σ. We conclude that disks directly inherit water from the star-forming cloud and this water becomes incorporated into large icy bodies, such as comets, without substantial chemical alteration.
*References in the science paper.
For further illustrations see the science paper.
See the full article here .
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European Southern Observatory(EU) , Very Large Telescope at Cerro Paranal in the Atacama Desert •ANTU (UT1; The Sun ) •KUEYEN (UT2; The Moon ) •MELIPAL (UT3; The Southern Cross ), and •YEPUN (UT4; Venus – as evening star). Elevation 2,635 m (8,645 ft) from above Credit J.L. Dauvergne & G. Hüdepohl atacama photo.
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Part of ESO’s Paranal Observatory the VLT Survey Telescope (VISTA) observes the brilliantly clear skies above the Atacama Desert of Chile. It is the largest survey telescope in the world in visible light, with an elevation of 2,635 metres (8,645 ft) above sea level.
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European Space Agency [Agence spatiale européenne][Europäische Weltraumorganisation](EU) The open dome of The black telescope structure of the‘s Test-Bed Telescope 2 peers out of its open dome in front of the rolling desert landscape. The telescope is located at ESO’s La Silla Observatory, which sits at a 2400 metre altitude in the Chilean Atacama desert.
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