by @ulaulaman about #exoplanets #planetary_transit #kepler_mission #nasa #astronomy
The search for extrasolar planets (or
exoplanets) had its first success in 1991 with the discovery of some planets orbiting around the pulsar PSR1257+12
(1, 2, 3), measuring the variations of the radio pulses coming from the star. The second important milestone in exoplanet research takes place in 1995, with the discovery around the star 51 Pegasi (a star like our Sun) of a Jupiter-like planet, found at a distance closer than Mercury's orbit in our Solar System
(4).
(51 Pegasi via
BBC)
These initial discoveries, and many other up to 2009
(5, 6) were made using the method of
radial velocity or
Doppler oscillation, in practice it is assumed that the radial velocity of a star is affected by the presence of a planet orbiting the star itself. In this way, the frequence from the star will be blue when the planet moves in its orbit toward the Earth, tending to red when the planet moves away
(7). With the radial velocity, however, is rather difficult to determine the exact orbit of a planet (or at least something that comes close), and then effectively allows us to determine the period of rotation around the star and the orbital eccentricity (i.e. the deviation by a circle) of the orbit of the planet itself. And I must remember that the method is effective especially for massive planets.
Luckly, the transit method is a more effective method to discover and study exoplanets: it is based on the examination of the light emitted by the studied star and it is considered by
Dimitar Sasselov(8) the method of observation more fruitful: when this light decreases, this means that the star is passing in front of an object. In this way it is possible to determine the radius of a planet and its orbital period. Using essentially the same tools used for the detection of the planet, it is also possible to study the atmosphere of the planet itself, determining its composition, temperature and the presence and formation of clouds.
(
comparison between radial velocity and transit
(7))
The Kepler mission is based just on this latter method: launched on March 6, 2009
(5), has found 3845 candidate planets to April 2014, with the first findings published in
Science in 2010
(5) and the
first Earth-like planet announced a couple of days ago:
Looking the following plots and the
plunet-hunting infographic, we can see that astronomers are looking for a kind of light holes, which allow them to determine a bit of data from the planet candidate as its mass, the orbital period and other typically stuff:
(The first transit of Kepler
(5))
(Transits of the planets of Kepler-11
(9))
The research about Kepler-11
(9) is interesting because, in addition to combining the data for the studied system, it also collects information on a particular planet, Kepler-11g, and also offers deductions, based on the data, about the composition and formation of the planetary system, thus providing, as well as a number of interesting scientific data, a good example of the potential of the mission in general.
The Kepler mission, therefore, was in the last years, a source of interesting news and it can be didactically interesting to use Kepler to start bringing astronomy into the classroom. The advantages of this approach with regard to the teaching of physics are multiple and we can emphasize some of these rather than others based on the order and degree of the school. For example, we can introduce students to the study of the direct data of astronomical experiments, almost all public and freely available, some even in simple formats to read even with the usual text editor. In this way, for example, they get used to the development of real data and to their statistical processing
(11, 12), but it is also possible to create a sort of miniature Kepler mission
(10):