Originally Posted by
Dreamwoven
The SOCIETY for POPULAR ASTRONOMY
Electronic News Bulletin No. 463 2018 February 18
Here is the latest round-up of news from the Society for Popular
Astronomy.
COMPOSITION OF TRAPPIST-1 PLANETS
ESO
The seven Earth-size planets of TRAPPIST-1 are all mostly made of rock, with some having the potential to hold more water than the Earth. The planets' densities, now known much more precisely than before, suggest that some of them could have up to 5 per cent of their mass in water -- which is 250 times more than the oceans on Earth. The form that water would take on TRAPPIST-1 planets would depend on the amount of heat they receive from their star, which is a mere 9 per cent as massive as our Sun. Planets closest to the star are more likely to have water in the form of atmospheric vapour, while those farther away may have water frozen on their surfaces as ice. TRAPPIST-1e is the rockiest planet of them all, but still is believed potentially to have some liquid water. Astronomers now know more about TRAPPIST-1 than about any other planetary system apart from our own. Since the extent of the TRAPPIST system was recognized in 2017 February, researchers have been working hard to characterize the planets better and to collect more information about them. The new study offers better estimates than were available previously for the planets' densities. The TRAPPIST name comes from the Transiting Planets and Planetesimals Small Telescope in Chile, which discovered two of the seven planets we know of today --announced in 2016. The Spitzer space telescope, in collaboration with ground-based telescopes, confirmed those planets and discovered the other five in the system. Since then, the Kepler space telescope has also observed the TRAPPIST-1 system, and Spitzer began a new programme of 500 additional hours of TRAPPIST-1 observations, which will conclude in March. The new body of data has helped the authors of the study to paint a clearer picture of the system than ever before -- although there is still much more to learn about TRAPPIST-1.
The TRAPPIST-1 planets huddle so close to one another that a person standing on the surface of one of them would have a spectacular view of the neighbouring planets in the sky. Those planets would sometimes appear larger than the Moon looks to an observer on Earth. They may also be tidally locked, meaning that the same side of the planet is always facing the star, with each side in perpetual day or night. Although the planets are all
closer to their star than Mercury is to the Sun, TRAPPIST-1 is such a cool
star that some of its planets could still, in theory, hold liquid water.
It is impossible to know exactly how each planet looks, because they are so
far away. In our own Solar System, the Moon and Mars have nearly the same density, yet their surfaces appear entirely different. TRAPPIST-1b, the innermost planet, is likely to have a rocky core, surrounded by an atmosphere much thicker than the Earth's. TRAPPIST-1c also probably has a rocky interior, but with a thinner atmosphere than planet b. TRAPPIST-1d is the lightest of the planets -- about three-tenths the mass of the Earth.
Scientists are uncertain whether it has a large atmosphere, an ocean or an
ice layer -- all three of those would give the planet an 'envelope' of
volatile substances, which would make sense for a planet of its density.
Scientists were surprised that TRAPPIST-1e is the only planet in the system
slightly denser than the Earth, suggesting that it may have a relatively
larger iron core than our home planet. Like TRAPPIST-1c, it does not
necessarily have a thick atmosphere, ocean or ice layer -- making those two
planets distinct in the system. It is a mystery why TRAPPIST-1e has a much
rockier composition than the rest of the planets. In terms of size, density
and the amount of radiation it receives from its star, it is the planet that
is most similar to the Earth. TRAPPIST-1f, g and h are far enough from the
host star that water could be frozen as ice on their surfaces. If they have
thin atmospheres, they would be unlikely to contain heavy molecules such as carbon dioxide.
Scientists can calculate the densities of the planets because their orbits
happen to be oriented in such a way that they transit in front of their
star, causing a slight dimming of the starlight. The amount of dimming is
related to the radius of the planet. To get the density, scientists take
advantage of what are called 'transit timing variations'. If there were no
other gravitational forces on a transiting planet, it would always cross in
front of its host star in the same amount of time -- for example, the Earth
orbits the Sun every 365 days. But because the TRAPPIST-1 planets are
packed so close together, they change the timing of one another's 'years'
ever so slightly. Those variations in orbital timing are used to estimate
the planets' masses. Then, mass and radius are used to calculate density.
The next step in exploring TRAPPIST-1 will be with the James Webb space
telescope, which may be able to determine whether these planets have
atmospheres and, if so, what those atmospheres are like. A recent study
using the Hubble telescope found no detection of hydrogen-dominated
atmospheres on planets TRAPPIST-1d, e and f -- another piece of evidence for rocky composition -- although a hydrogen-dominated atmosphere cannot be ruled out for good.