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Polarization of ultra-cool dwarfs

机译:超冷矮种的极化

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Ultra-cool dwarfs with effective temperatures between≈1400K and ≈2200 K are knownto have dusty atmospheres. Asymmetries of the dwarf surface may arise from rotationally-inducedflattening and dust-cloud coverage, and may result in non-zero linear polarisation through dustscattering. Here we present our linear polarimetric imaging measurements using FORS 1 at the VeryLarge Telescope, in Paranal, in the Bessel I filter, and for a subset of our sample in the Bessel R andthe Gunn z filters. We report a polarisation degree of (-0.31 + +0.07)% for LHS102BC. We fail todetect linear polarisation in the rest of our sample, with upper-limits on the polarisation degree ofeach object of 0.09% to 0.76% (95% of confidence level), depending on the targets and the bands.For six targets, our data indicate polarisation degrees smaller (at the 2-σ level) than previouslyreported.
机译:众所周知,具有有效温度的超冷矮水,均为尘土飞扬的环境。矮化表面的不对称可能来自旋转诱导和灰尘云覆盖,并且可以通过灰尘散射产生非零线性偏振。在这里,我们在贝塞尔I滤波器中,在Peranerg望远镜,在贝塞尔I滤波器中,以及在贝塞尔R和GUNN Z过滤器中的样品子集中,在斯拉尔的望远镜上使用1在普通望远镜上的线性偏振成像测量测量。我们报告了LHS102BC的(-0.31 + + 0.07)%的偏振度。我们在其余的样品中未能在其余的样品中进行线性极化,对象的偏振度的上限为0.09%至0.76%(置信水平的95%),具体取决于目标和频段。六个目标,我们的数据表示比预先报告更小的(在2-Σ电平)上的偏振度。

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