Abstract

Context. The discovery of about 700 extrasolar planets, so far, has lead to the first statistics concerning extrasolar planets. The presence of giant planets seems to depend on stellar metallicity and mass. For example, they are more frequent around metal-rich stars,with an exponential increase in planet occurrence rates with metallicity. Aims. We analyzed two samples of metal-poor stars (-2.0 \leq [Fe/H] \leq 0.0) to see if giant planets are indeed rare around these objects. Radial velocity datasets were obtained with two different spectrographs (HARPS and HIRES). Detection limits for these data,expressed in minimum planetary mass and period, are calculated. These produce trustworthy numbers for the planet frequency. Methods. A general Lomb Scargle (GLS) periodogram analysis was used together with a bootstrapping method to produce the detection limits. Planet frequencies were calculated based on a binomial distribution function within metallicity bins. Results. Almost all hot Jupiters and most giant planets should have been found in these data. Hot Jupiters around metal-poor stars have a frequency lower than 1.0% at one sigma. Giant planets with periods up to 1800 days, however, have a higher frequency of $f_p = 2.63^{+2.5}_{-0.8}%$. Taking into account the different metallicities of the stars, we show that giant planets appear to be very frequent $(f_p = 4.48^{+4.04}_{-1.38}%)$ around stars with [Fe/H] > -0.7, while they are rare around stars with [Fe/H] \leq -0.7 (\leq 2.36% at one sigma). Conclusions. Giant planet frequency is indeed a strong function of metallicity, even in the low-metallicity tail. However, the frequencies are most likely higher than previously thought.

Highlights

  • Since the discovery of the first extrasolar planet in 1995 (51 Peg b, Mayor & Queloz 1995), the search for extrasolar planetary systems accelerated

  • Taking into account the different metallicities of the stars, we show that giant planets appear to be very frequent around stars with [Fe/H] > −0.7, while they are rare around stars with [Fe/H] ≤ −0.7 (≤2.36% at one sigma)

  • With these limits and the number of planets found in the samples, a statistical analysis can be made of the giant planet frequency as a function of stellar metallicity

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Summary

Introduction

Since the discovery of the first extrasolar planet in 1995 (51 Peg b, Mayor & Queloz 1995), the search for extrasolar planetary systems accelerated. Current numbers, based on the CORALIE and HARPS samples, suggest that around 25% of the stars with twice the metal content of our Sun are orbited by a giant planet This number decreases to ∼5% for solar-metallicity objects (Sousa et al 2011b; Mayor et al 2011). The Neptune-mass planets found so far seem to have a rather flat metallicity distribution (Sousa et al 2008, 2011b; Mayor et al 2011) This observed metallicity correlation favors the coreaccretion model for the formation of giant planets (Ida & Lin 2004; Udry & Santos 2007; Mordasini et al 2012) because the higher the grain content of the disk, the easier it is to build the cores that will later accrete gas. Radial velocity measurements from two different samples of metal-poor, solar-type stars were used in this paper

The HARPS sample
36 G80-15
The KECK-HIRES sample
The combined sample
Methodology
Stars with at least six measurements
Stars with at least ten measurements
Planet frequency
Findings
Conclusions and discussion
Full Text
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