Marcy Geoffrey W, Weiss Lauren M, Petigura Erik A, Isaacson Howard, Howard Andrew W, Buchhave Lars A
Department of Astronomy, University of California, Berkeley, CA 94720;
Institute for Astronomy, University of Hawaii at Manoa, Honolulu, HI 96822; and.
Proc Natl Acad Sci U S A. 2014 Sep 2;111(35):12655-60. doi: 10.1073/pnas.1304197111. Epub 2014 May 27.
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 + 3:19 R=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.
大小为地球1至4倍的小行星在类日恒星周围极为常见,而令人惊讶的是,在我们的太阳系中却没有这类小行星。最近的探测已经获得了关于这类系外行星的足够信息,从而能够开始描绘它们的出现率、轨道、质量、密度和内部结构。开普勒任务发现最小的行星最为常见,因为26%的类日恒星拥有小型的、半径为1至2个地球半径(R⊕)且轨道周期小于100天的行星,还有11%的类日恒星拥有半径为1至2个地球半径的行星,这些行星接收到的恒星入射通量是使地球变暖的入射通量的1至4倍。这些地球大小的行星在轨道距离上(对数形式)均匀分布,最远可达地日距离的0.4倍,甚至可能更远。对33颗半径为1至4个地球半径的凌日行星进行的质量测量表明,其中最小的行星,即半径R < 1.5 R⊕的行星,具有岩石行星预期的密度。它们的密度随着半径的增加而增大,这可能是由引力压缩导致的。将太阳系行星包括在内可得出一个关系:ρ = 2.32 + 3.19 R/R⊕ [克/立方厘米]。半径在1.5至4.0个地球半径范围内的较大行星,其密度随着半径的增加而下降,这表明在围绕岩石核心的包层中低密度物质(氢和氦或冰)的含量不断增加,符合“迷你海王星”这一称谓。气态巨行星优先出现在富含重元素的恒星周围,而岩石行星则出现在重元素丰度范围各异的恒星周围。在既没有其他地方生命探测结果,也没有对生命生化起源的了解的情况下,定义宜居带仍然很困难。