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This HST image of the first-magnitude star Fomalhaut (in the constellation Pisces) has had the star itself blocked out by a device called a coronagraph. With the glare from the star much reduced, it is possible to spot a planet (Fomalhaut b; see inset) orbiting the star at a distance of about 115 AU (115 times the Earth's distance from the Sun). Fomalhaut b is definitely a planet, not a brown dwarf – it is estimated to weigh no more than 3 times as much as Jupiter. It is unusually bright for its mass, and some astronomers speculate that it may have icy rings like Saturn's. Image by the HST Advanced Camera for Surveys; credit NASA/ESA
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Summary of Lecture 13 – Detection of Extrasolar Planets
- There are various ways of attempting to detect planets around other stars:
- direct observation is very difficult with current
technology, because the star's light swamps the much fainter planet:
- 42 "planets" in 39 systems as of December 2 2013;
- all very massive (smallest is 2 Jupiter masses,
see picture, and several are >10 Jupiter masses and
so probably brown dwarfs) and far from their
stars (a couple at around 3 AU actually orbit
brown dwarfs; the closest to a "proper" star is at 8.5 AU,
comparable to Saturn, and the most distant at
2500 AU, 80 times further than Neptune!);
- astrometry relies on detecting the orbital motion of
the star across the sky caused by the gravitational force
between star and planet:
- the oldest method, but very difficult, with several claimed
discoveries subsequently retracted;
- most sensitive to massive planets orbiting
relatively far from low-mass
stars;
- only works for nearby stars (otherwise
motion not detectable, similar to parallax);
- unsuccessful so far – only one or two unconfirmed
detections;
- spectroscopic methods rely on detecting (by Doppler
shift) the orbital motion of the star in the line of sight:
- most sensitive to massive planets orbiting
close to stars;
- not dependent on distance, except that fainter stars are
harder to get the necessary high-precision spectra for;
- because we detect only line-of-sight motion,
which depends on tilt of orbit to line of sight, only
minimum mass of planet can be determined
(mass that planet would have in ideal case of edge-on orbit);
- the most successful method to date: 538 planets
in 404 systems discovered as of December 2
2013;
- transit observations rely on detecting the
drop in brightness of the star caused by a planet's
passing in front of it:
- requires extremely precise measurements of stellar brightness,
best done from space (to remove effect of atmosphere);
- most sensitive to large planet (bigger dip)
close to star (more frequent dips);
- but can see much smaller objects – best
hope at present of detecting Earth-size objects around
normal stars;
- measures orbital period and
radius of planet, but provides
no information on mass unless combined with
other information, e.g. spectroscopy;
- requires very nearly edge-on orbit;
- best combined with spectroscopy: transit implies edge-on
orbit, so spectroscopy gives exact mass – combine
with size from transit to get density, and hence
information on chemical composition;
- 424 planets in 321 systems discovered as
of December 2 2013 – number increasing rapidly;
- timing of regular variables can be used in a similar
way to spectroscopy:
- extremely sensitive if the parent star's variation is
fast and regular;
- smallest planet discovered this way (orbiting a pulsar)
weighs only about the same as the Moon!
- but can only be used with rapidly and regularly
varying parent star;
- 15 planets in 12 systems
(three pulsars, one sdB pulsating variable, seven short-period
eclipsing binaries, and one from timing variations in
the transit of another planet);
- gravitational microlensing detects planets when
their gravity amplifies the light from a background star:
- one-off event – only get one chance to see it;
- limited information – mass of planet, and projected
distance from star, but no details about orbit,
unless lensing event lasts long enough to see orbital
motion;
- where information available, planets fairly far from
their stars (few AU, periods 5-10 years);
- masses similar to other exoplanets: 0.01 to 3.5
Jupiter masses;
- 25 planets in 23 systems as of December 2 2013.
- Properties of the planets:
- The 1047 extrasolar planets in 794 systems (as of 02/12/13)
so far observed around other stars:
- are fairly massive
(49% more massive than Jupiter;
only 11% 10 Earth masses or less;
13% of transiting planets 2 Earth radii or less);
- are mainly gas giants like Jupiter and Saturn,
in those cases where their density can be measured (transiting
planets), although some of the super-Earths
with masses <10 Earth masses are icy or rocky;
- are fairly close to their stars (63%
closer to their star than the Earth, over ⅓ closer
than 0.1 AU; only 7% further out than Jupiter);
- often have quite eccentric orbits (least
circular orbit of a major solar system planet is Mercury's,
with eccentricity 0.2: about
40% have orbits less circular than this);
- tend to orbit Sun-like stars high
in heavy elements (just over half
the stars are within 20% of the Sun's mass, whereas in a fair
sample of nearby stars about 70% are class M, i.e. much less
massive than the Sun; also, a similar fraction are
higher in heavy elements than the Sun, whereas a typical
local star is about the same as the Sun).
- These properties are biased by the detection
methods:
- massive planets close to stars are the easiest to
detect, so they will be over-represented;
- low-mass planets like Earth are almost impossible to
detect, so they will be missing;
- planets with very long periods will be missed by
most techniques (except direct imaging), because we haven't been
watching for long enough yet;
- spectroscopic techniques are easier with Sun-like stars than
with class M stars, which have very complicated
spectra (also, astronomers looking for extrasolar planets
really want to find another Earth, so they preferentially
look at stars like the Sun!).
The preference for high-metallicity stars and the non-circular orbits
aren't obviously biased, but may be common specifically for massive
planets in close orbits, not for planetary systems in general.
- The hot Jupiters (massive planets in very close
orbits) were unexpected:
- theory says gas giant planets should form far from stars,
like Jupiter;
- likeliest idea is that the planets do form out there
and then migrate inwards
- (modern models of solar system formation suggest
this also happened to Jupiter, but orbital
resonance with Saturn moved it out again –
see PHY106)
- The preference for stars high in heavy elements was expected:
- planets believed to form when dust grains in the dusty disc
around a young star coalesce into larger bodies;
- dust is made from heavy elements, not hydrogen and helium;
- therefore stars high in heavy elements likely to have more
circumstellar dust, therefore more likely to have planets;
- however, planets have been found around stars
quite low in heavy elements, e.g. HD155358, an old Sun-like
star (class G0) with only one-fifth of the Sun's heavy
element content;
- Some of the stars with detected planetary systems are members of
binary pairs:
- slightly unexpected – many people thought that collapsing
gas cloud would form either binary system (if it
rotated so fast it tore itself apart) or planetary
system (if rotating less fast), but not combination;
- however simulations do show circumstellar discs formed
around members of (not too close) binary systems,
suggesting that planets could form;
- several planets found in wide orbit around both
stars of a close binary (very weird).
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