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Occurrence and core-envelope structure of 1–4× Earth-size planets around Sun-like stars

机译:太阳类恒星周围1–4×地球大小的行星的发生和核心包络结构

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摘要

Small planets, 1–4× the size of Earth, are extremely common around Sun-like stars, and surprisingly so, as they are missing in our solar system. Recent detections have yielded enough information about this class of exoplanets to begin characterizing their occurrence rates, orbits, masses, densities, and internal structures. The Kepler mission finds the smallest planets to be most common, as 26% of Sun-like stars have small, 1–2 R⊕ planets with orbital periods under 100 d, and 11% have 1–2 R⊕ planets that receive 1–4× the incident stellar flux that warms our Earth. These Earth-size planets are sprinkled uniformly with orbital distance (logarithmically) out to 0.4 the Earth–Sun distance, and probably beyond. Mass measurements for 33 transiting planets of 1–4 R⊕ show that the smallest of them, R < 1.5 R⊕, have the density expected for rocky planets. Their densities increase with increasing radius, likely caused by gravitational compression. Including solar system planets yields a relation: ρ = 2.32 + 3.19R/R⊕ [g cm−3]. Larger planets, in the radius range 1.5–4.0 R⊕, have densities that decline with increasing radius, revealing increasing amounts of low-density material (H and He or ices) in an envelope surrounding a rocky core, befitting the appellation ‘‘mini-Neptunes.’’ The gas giant planets occur preferentially around stars that are rich in heavy elements, while rocky planets occur around stars having a range of heavy element abundances. Defining habitable zones remains difficult, without benefit of either detections of life elsewhere or an understanding of life’s biochemical origins.
机译:小小的行星是地球大小的1-4倍,在类似太阳的恒星周围非常普遍,令人惊讶的是,因为它们在我们的太阳系中不存在。最近的探测已经获得了有关此类系外行星的足够信息,可以开始表征它们的发生率,轨道,质量,密度和内部结构。开普勒任务发现最小的行星是最常见的,因为26%的类太阳恒星具有较小的,1-2个R⊕行星,其轨道周期小于100 d,而11%的1-2个R⊕行星具有1–2个使地球变暖的恒星通量的4倍。这些地球大小的行星均匀地以轨道距离(对数)散布到地球与太阳的距离为0.4的范围内,甚至可能更大。对33个1-4R⊕的过渡行星的质量测量表明,其中最小的R <1.5R⊕具有岩石行星所期望的密度。它们的密度随半径的增加而增加,这很可能是由重力压缩引起的。包括太阳系行星产生的关系为:ρ= 2.32 + 3.19R /R⊕[g cm -3 ]。较大的行星,半径范围为1.5–4.0 R planet,其密度随半径的增加而下降,从而揭示了包围岩心的包层中低密度物质(H,He或冰)的含量不断增加,与称呼“迷你”相称。气体巨行星优先出现在富含重元素的恒星周围,而岩石行星优先出现在具有大量重元素丰度的恒星周围。没有发现其他地方的生命或了解生命的生化起源,就很难定义可居住的区域。

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