论文标题
近地小行星的物理表征(52768)1998 OR2:冲击的证据1变暗/冲击熔体
Physical Characterization of Near-Earth Asteroid (52768) 1998 OR2: Evidence of Shock 1 Darkening/Impact Melt
论文作者
论文摘要
我们在2020年4月对地球的近距离方法中进行了近地小行星(52768)1998 OR2的光度和光谱表征。我们的光度测量证实了小行星的旋转周期为4.126 +/- 0.179小时,与先前发布的值为4.112 +/-0.001小时一致。通过将我们的可见光谱测量值(0.45-0.93微米)与近红外光谱(0.78-2.49微米)附近的档案密特尼斯结合在一起,我们将小行星分类为Bus -Deme分类法中的XN型。组合频谱显示了两个弱吸收带:在0.926 +/- 0.003微米和2.07 +/- 0.02微米的频带I分别为4.5 +/- 0.15%和4.0 +/- 0.21%。带面积比为1.13 +/- 0.05。这些光谱带参数在gaffey s- asteroid亚型的S(IV)区域的尖端图中绘制图,表明对普通软骨陨石有亲和力。我们使用中心的橄榄石和辉石的化学性质计算为20.1 +/- 2.3 mol%fayalite和18.2 +/- 1.5 mol%二铁硅粉,与H软骨一致。 1998年OR2合并可见频谱的主要成分分析落在α线的C/x复合侧,靠近冲击变暗趋势的结束,与其弱吸收带(带深度<5%)一致。我们使用一种空中混合模型,并与冲击黑暗的H5软管chergach进行实验室测量,以限制小行星表面上的冲击黑暗材料的量,以〜63%的深色岩性和〜37%的光岩性学。
We conducted photometric and spectroscopic characterization of near-Earth asteroid (52768) 1998 OR2 during a close approach to the Earth in April of 2020. Our photometric measurements confirm the rotation period of the asteroid to be 4.126 +/- 0.179 hours, consistent with the previously published value of 4.112 +/- 0.001 hours. By combining our visible spectroscopic measurements (0.45 - 0.93 microns) with archival MITHNEOS near infrared spectra (0.78 - 2.49 microns), we classify the asteroid as an Xn-type in the Bus-DeMeo taxonomy. The combined spectrum shows two weak absorption bands: Band I at 0.926 +/- 0.003 microns and Band II at 2.07 +/- 0.02 microns with band depths of 4.5 +/- 0.15% and 4.0 +/- 0.21%, respectively. The band area ratio is 1.13 +/- 0.05. These spectral band parameters plot at the tip of the S(IV) region of the Gaffey S-asteroid subtypes plot suggesting an affinity to ordinary chondrite meteorites. We calculated the chemistry of the olivine and pyroxene using the Band I center to be 20.1 +/- 2.3 mol% fayalite and 18.2 +/- 1.5 mol% ferrosilite, consistent with H chondrites. Principal component analysis of 1998 OR2's combined visible-NIR spectrum fall on the C/X-complex side of the alpha-line, near the end of the shock darkening trend, consistent with its weak absorption bands (band depth < 5%). We use an aerial mixing model with lab measurements of the shock darkened H5 chondrite, Chergach, to constrain the amount of shock darkened material on the asteroid's surface at ~63% dark lithology and ~37% light lithology.