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ALMA observations of sulfur-bearing molecules in protoplanetary disks

机译:原文象磁盘中含硫分子的ALMA观察

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It is thought that protoplanets formed in protoplanetary disks excite the orbital motion of the surrounding planetesimals, and the bow shocks caused by the highly excited planetesimals heat their icy component evaporating into gas. We have performed model calculations to study the evolution of molecular abundances of the evaporated icy component, which suggests sulfur-bearing molecules can be good tracers of icy planetesimal evaporation. Here we report the result of our ALMA observations of sulfur-bearing molecules towards protoplanetary disks. The lines were undetected but the obtained upper limits of the line fluxes and our model calculations give upper limits of the fractional abundances of x (H_2S) < 10~(-11) and x(SO) < 10~(-10) in the outer disk. These results are consistent with the molecular abundances in comets in our Solar system.
机译:据认为,在原始板块中形成的原生质网激励周围的星系侧的轨道运动,并且由高兴奋的行星引起的弓形冲击加热它们的冰冷成分蒸发成气体。 我们已经进行了模型计算,以研究蒸发的冰碳分子的分子丰度的演变,这表明硫磺的分子可以是冰冷的行星蒸发的良好示踪剂。 在这里,我们报告了我们的ALMA对硫磺分子朝向原生型盘的结果。 未检测到线,但是所获得的线通量的上限和我们的模型计算提供了X(H_2S)<10〜(-11)和x(SO)<10〜(-10)的分数丰度的上限 外盘。 这些结果与我们太阳系中的彗星分子丰度一致。

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