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Multi-epoch Sub-arcsecond [Fe II] Spectroimaging of the DG Tau Outflows with NIFS. I. First data epoch

机译:DG Tau流出的多历元亚弧秒[Fe II]光谱   与NIFs。 I.第一个数据时代

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Investigating the outflows emanating from young stellar objects (YSOs) onsub-arcsecond scales provides important clues to the nature of the underlyingaccretion-ejection process occurring near the central protostar. We haveinvestigated the structures and kinematics of the outflows driven by the YSO DGTauri, using the Near-infrared Integral Field Spectrograph (NIFS) on GeminiNorth. The blueshifted outflow shows two distinct components in [Fe II] 1.644micron emission, which are separated using multi-component line fitting. Astationary recollimation shock is observed, in agreement with previous X-rayand FUV observations. The presence of this shock indicates that the innermoststreamlines of the high-velocity component are launched at a very small radius,0.01-0.15 AU, from the central star. The jet accelerates and expands downstreamof the recollimation shock; the 'acceleration' is likely a sign of velocityvariations in the jet. No evidence of rotation is found, and we compare thisnon-detection to previous counter-claims. Moving jet knots, likely the resultof the jet velocity variations, are observed. One of these knots moves moreslowly than previously observed knots, and the knot ejection interval appearsto be non-periodic. An intermediate-velocity component surrounds this centraljet, and is interpreted as the result of a turbulent mixing layer along the jetboundaries. Such lateral entrainment requires the presence of a magnetic fieldof strength a few mG or less at hundreds of AU above the disc surface, which isargued to be a reasonable proposition. In H2 1-0 S(1) 2.1218 micron emission, awide-angle, intermediate-velocity blueshifted outflow is observed. Bothoutflows are consistent with being launched by a magnetocentrifugal disc wind,although an X-wind origin for the high-velocity jet cannot be ruled out.
机译:研究亚秒尺度上的年轻恒星物体(YSOs)流出的水流,为中央原恒星附近发生的潜在增生-喷射过程的性质提供了重要线索。我们使用GeminiNorth上的近红外积分场光谱仪(NIFS)研究了由YSO DGTauri驱动的流出的结构和运动学。蓝移流出显示出[Fe II] 1.644微米发射中的两个截然不同的成分,使用多成分管线拟合将其分离。与先前的X射线和FUV观察结果相一致,观察到了静止性恢复性休克。这种冲击的存在表明,高速分量的最里面的流线是从中心恒星以很小的半径(0.01-0.15 AU)发射的。射流加速并在再通激休克的下游膨胀; “加速”可能是射流速度变化的迹象。找不到旋转的证据,我们将这种未发现与以前的反诉进行了比较。观察到移动的打结,这可能是喷射速度变化的结果。这些结之一移动的速度比以前观察到的结慢,结弹出的间隔似乎是非周期性的。中间速度分量围绕该中央射流,并且被解释为沿着射流边界的湍流混合层的结果。这种横向夹带需要在盘表面上方数百AU处存在几mG或更小的强度的磁场,这被认为是合理的主张。在H2 1-0 S(1)2.1218微米排放中,观察到广角,中速蓝移流出。尽管不能排除高速射流的X风起源,但两种流出都与磁离心圆盘风产生的一致。

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