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arXiv 0908.2244astro-ph.SR
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CoRoT目标HD175726:具有弱太阳振荡的活动恒星

The CoRoT target HD175726: an active star with weak solar-like oscillations

B. Mosser, E. Michel, T. Appourchaux, C. Barban, F. Baudin, P. Boumier, H. Bruntt, C. Catala, S. Deheuvels, R. A. Garcia, P. Gaulme, C. Regulo, I. Roxburgh, R. … 展开作者

B. Mosser, E. Michel, T. Appourchaux, C. Barban, F. Baudin, P. Boumier, H. Bruntt, C. Catala, S. Deheuvels, R. A. Garcia, P. Gaulme, C. Regulo, I. Roxburgh, R. Samadi, G. Verner, M. Auvergne, A. Baglin, J. Ballot, O. Benomar, S. Mathur

摘要:

上下文CoRoT的短期运行使我们有机会通过它们类似太阳的振荡来观察各种各样的晚型恒星。我们报告的恒星HD 175726,持续了27天,在第一次短期运行的任务。时间序列揭示了一个高活性的信号和功率谱呈现出过剩,由于太阳般的振荡与低信噪比。目标。我们的目标是确定最有效的工具,以提取尽可能多的信息,从功率密度谱。方法.最有效的方法似乎是时间序列的自相关性,计算为滤波频谱的频谱。这种方法是有效的,非常快速的计算,并将是有用的其他目标的分析,观察与CoRoT或即将到来的任务,如开普勒和柏拉图。结果测得的平均大间隔为97.2 ± 0.5微赫兹,略低于根据太阳定标律确定的预期值,我们也给出了大间隔随频率变化的强有力的证据。对于径向模式,测辐射热模式振幅仅为1.7 ± 0.25 ppm,比预期小1.7倍。由于低信噪比,模式识别是不可能的HD 175726的可用数据集。结论.这项研究表明,尽管信噪比只有0.37,提取地震信号的可能性。对这样一个目标的观测显示了CoRoT数据的效率,以及更长时间观测运行的潜在好处。

英文摘要:

Context. The CoRoT short runs give us the opportunity to observe a large variety of late-type stars through their solar-like oscillations. We report observations of the star HD175726 that lasted for 27 days during the first short run of the mission. The time series reveals a high-activity signal and the power spectrum presents an excess due to solar-like oscillations with a low signal-to-noise ratio. Aims. Our aim is to identify the most efficient tools to extract as much information as possible from the power density spectrum. Methods. The most productive method appears to be the autocorrelation of the time series, calculated as the spectrum of the filtered spectrum. This method is efficient, very rapid computationally, and will be useful for the analysis of other targets, observed with CoRoT or with forthcoming missions such as Kepler and Plato. Results. The mean large separation has been measured to be 97.2+-0.5 microHz, slightly below the expected value determined from solar scaling laws.We also show strong evidence for variation of the large separation with frequency. The bolometric mode amplitude is only 1.7+-0.25 ppm for radial modes, which is 1.7 times less than expected. Due to the low signal-to-noise ratio, mode identification is not possible for the available data set of HD175726. Conclusions. This study shows the possibility of extracting a seismic signal despite a signal-to-noise ratio of only 0.37. The observation of such a target shows the efficiency of the CoRoT data, and the potential benefit of longer observing runs.

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