
The purpose of this paper is to present a detailed 
analysis  of  the  three  approaches  for  locating 
exoplanets: radial velocity, transit and direct imaging. 
In  order  to  offer  a  analytically  and  systematically 
sumamry of the current state of exoplanet detection 
research  as  well  as  possible  directions  for  future 
development,  this  paper  examines  the  guiding 
principles, detector structures and current results of 
these methods. The main part of the paper introduces 
the three exploration methods in detail, including the 
principle of each method, the structure of the probe 
and the specific results in recent years. In addition, 
the limitations of current planetary research and the 
future prospects of this field are analysed. 
2. DESCRIPTIONS OF PLANET 
SEARCHING 
Planet  searching  involves  many  aspects  to  be 
analyzed  and  studied,  and  they  provide  important 
information to further analyze the characteristics and 
potential  habitability  of  newfound  planets.  The 
elements  to  be  determined  include  the  planetary 
properties and the potential habitability of discovered 
exoplanets. Planetary properties include radius, mass, 
density  and  atmospheric  composition  of  a  planet. 
Both  radius  and  mass  are  measured  at  the  first  to 
further  obtain  the  density  and  atmospheric 
composition.  For  the  measurement  of  the  radius, 
scientists usually use transit method. When a planet 
transits,  it  causes  dimming  of  the  star’s  light.  By 
transit,  the  planet’s  size  relative  to  the  star  can  be 
determined. Regarding to the measurement of mass, 
velocity method is used in most cases.  
By  knowing  the  planet’s  mass  and  radius,  the 
density of the planet can be calculated using density 
formula.  Besides,  the  density  can  also  provide  the 
information of an exoplanet’s composition. A planet's 
atmosphere  absorbs  some  starlight  as  it  passes 
through its star, which can be used to determine the 
composition  of  the  atmosphere.  As  for  detailed 
atmospheric condition, missions like the JWST will 
provide strong support (Pepe, et al., 2020). 
The  factors  to  assess  whether  a  planet  could 
support life include the planet's location within the 
habitable zone, surface temperature, and geological 
activity. With  measurement  of the  star’s  luminosity 
and  the  planet’s  distance  from  the  star,  whether  its 
location  is  within  the  habitable  zone  can  be 
determined.  However,  even  if  a  planet’s  location  is 
determined as the habitable  zone, it doesn’t mean a 
guarantee of habitability since it merely indicates the 
signature of water.  
Surface  temperature  can  be  affected  by  several 
factors including the distance, its atmosphere, and its 
reflectivity. For those planets with thick atmosphere, 
closer distance and smaller reflectivity, their surface 
temperature is greater; and vice versa (Shields, et al., 
2016). Geological activity is also very important to 
maintain  a  planet’s  habitability  in  the  long  run.  It 
generally includes two main factors: volcanism and 
plate tectonics. They both contribute to producing and 
recycling carbon and other elements, which is crucial 
for climate stability and nutrient distribution. 
3  RADIAL VELOCITY 
Because of the planet's gravitational pull, a star with 
planets orbiting it moves in a small orbit, making it 
impossible  for the star  to  remain  stationary.  This 
movement  is  caused  by  the  Doppler  effect,  which 
periodically shifts the star's spectral lines. The star's 
light spectrum has redshift when it moves away from 
Earth and blueshift when it moves closer to the planet. 
This observation forms the basis of the approach. The 
existence of a planet and details about it, like its mass 
and  orbit,  can  be  determined  by  measuring  those 
changes in the star's color lines (Ribas, et al., 2018; 
Smith, et al., 2021). 
The velocity change () can be calculated using 
the Doppler formula: 
             (1) 
            (2) 
where i is the inclination of the orbit, t is the time of 
observation, t
0
 is the time of periastron, and P is the 
orbital period, G is the gravitational constant, M
p
 and 
M
*
 are the mass of the planet and star, and e is the 
eccentricity. 
Detection  using  radial  velocity  measurements 
basically  depends  on  the  spectrograph.  There  are 
three  important  components  of  the  spectrograph. 
These  fibers maintain  a  steady  and  uniform  light 
delivery  while  guiding starlight  into 
the spectrograph.  In  order  to preserve the accuracy 
required for radial velocity measurements, stabilized 
optical fibers are used to reduce any possible signal 
loss  or distortion.  Accurate  measurements  of  radial 
velocity  require  extremely  stable  wavelength 
calibration.  Reference light sources, such as  Th-Ar 
(thorium-argon)  lamps  and  laser  frequency  combs, 
are  used  to  achieve  this.  To  measure  the  star's 
spectrum, these calibration systems provide a set of 
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