论文标题
K2-38行星系统的表征。揭开迄今已知的最密集的行星之一
Characterization of the K2-38 planetary system. Unraveling one of the densest planets known to date
论文作者
论文摘要
我们表征了使用新代梯形光谱仪板旋转G2V星K2-38的过渡行星系统。我们对该恒星的可用K2光度光曲线进行了光度分析,以测量其两个已知行星的半径。使用43个浓度高精度的径向速度测量值8个月以及先前发表的14个雇员RV测量值,我们通过MCMC分析对这两个行星的轨道进行了建模,从而显着改善了他们的质量测量值。使用浓缩咖啡光谱,我们得出了恒星参数,$ t _ {\ rm eff} $ = 5731 $ \ pm $ \ pm $ 66,$ \ log g $ = 4.38 $ \ pm $ 0.11〜dex和$ [fe/h] $ = 0.26 $ = 0.26 $ \ pm $ 0.05〜dex和mass and Mass and Mass and Mass and Mass of K2-38,美元我们确定两个行星的行星特性的新值。 We characterize K2-38b as a super-Earth with $R_{\rm P}$=1.54$\pm$0.14~R$_{\rm \oplus}$ and $M_{\rm p}$=7.3$^{+1.1}_{-1.0}$~M$_{\oplus}$, and K2-38C作为$ r _ {\ rm p} $ = 2.29 $ \ pm $ 0.26〜r $ _ {\ rm \ oplus} $和$ m _ {\ rm p} $ = 8.3 $ = 8.3 $^{+1.3} _ { - 1.3} $ { - 1.3} $ _ {我们得出了$ρ_{\ rm p} $ = 11.0 $^{+4.1} _ { - 2.8} $ 〜g cm $^{ - 3} $的平均密度为$ρ_{\ rm p} $ = 11.0 $^{+4.1} _ { - 2.8} $ 〜g cm $^{ - 3} $ for K2-38b和$ρ_{\ rm P}对于K2-38C,确认K2-38B是迄今已知的最密集的行星之一。 K2-38B组成的最佳描述来自类似铁的汞模型,而K2-38C的岩石模型则可以更好地描述H2信封的岩石模型。最大碰撞剥离边界表明,巨大影响如何成为K2-38B高密度的原因。每个星球收到的辐照将它们放在半径谷的相对侧。我们在径向速度时间序列中找到了长期信号的证据,其起源可以与0.25-3〜m $ _ {\ rm j} $行星或恒星活动相关。
We characterized the transiting planetary system orbiting the G2V star K2-38 using the new-generation echelle spectrograph ESPRESSO. We carried out a photometric analysis of the available K2 photometric light curve of this star to measure the radius of its two known planets. Using 43 ESPRESSO high-precision radial velocity measurements taken over the course of 8 months along with the 14 previously published HIRES RV measurements, we modeled the orbits of the two planets through a MCMC analysis, significantly improving their mass measurements. Using ESPRESSO spectra, we derived the stellar parameters, $T_{\rm eff}$=5731$\pm$66, $\log g$=4.38$\pm$0.11~dex, and $[Fe/H]$=0.26$\pm$0.05~dex, and thus the mass and radius of K2-38, $M_{\star}$=1.03 $^{+0.04}_{-0.02}$~M$_{\oplus}$ and $R_{\star}$=1.06 $^{+0.09}_{-0.06}$~R$_{\oplus}$. We determine new values for the planetary properties of both planets. We characterize K2-38b as a super-Earth with $R_{\rm P}$=1.54$\pm$0.14~R$_{\rm \oplus}$ and $M_{\rm p}$=7.3$^{+1.1}_{-1.0}$~M$_{\oplus}$, and K2-38c as a sub-Neptune with $R_{\rm P}$=2.29$\pm$0.26~R$_{\rm \oplus}$ and $M_{\rm p}$=8.3$^{+1.3}_{-1.3}$~M$_{\oplus}$. We derived a mean density of $ρ_{\rm p}$=11.0$^{+4.1}_{-2.8}$~g cm$^{-3}$ for K2-38b and $ρ_{\rm p}$=3.8$^{+1.8}_{-1.1}$~g~cm$^{-3}$ for K2-38c, confirming K2-38b as one of the densest planets known to date. The best description for the composition of K2-38b comes from an iron-rich Mercury-like model, while K2-38c is better described by a rocky model with a H2 envelope. The maximum collision stripping boundary shows how giant impacts could be the cause for the high density of K2-38b. The irradiation received by each planet places them on opposite sides of the radius valley. We find evidence of a long-period signal in the radial velocity time-series whose origin could be linked to a 0.25-3~M$_{\rm J}$ planet or stellar activity.