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X-ray observations of MeV electron precipitation with a balloon-borne germanium spectrometer.

机译:用气球载锗光谱仪对MeV电子沉淀进行X射线观察。

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摘要

The MAXIS (MeV Auroral X-ray Imaging and Spectroscopy) balloon payload was launched on a long duration balloon from McMurdo, Antarctica on Jan. 12, 2000. The high spectral resolution germanium spectrometer aboard MAXIS detected nine X-ray bursts with significant flux extending above 0.5 MeV during the 18 day flight. The X-rays are bremsstrahlung produced by precipitating electrons and the events are characterized by an extremely flat X-ray spectrum (∼E−2) similar to the first MeV event discovered in 1996, indicating relativistic parent electrons. The bursts were detected between magnetic latitudes 58°–68° (IGRF L-values of 3.8–6.7) with durations varying from several minutes to several hours and occurred only in the late afternoon/dusk sectors (14:30–00:00 MLT) while softer precipitation was detected at all magnetic local times. In addition, the MeV events were associated with substorm activity and several events showed Ultra Low Frequency (mHz) modulation of the X-ray count rate. Spacecraft and ground-based observations indicate the presence of ULF wave activity near the time and location of the events which may be causing the modulation by some mechanism that is not understood.; The MeV events are well modeled by a very flat exponential precipitating electron distribution and the average flux of precipitating electrons with E ≥ 0.5 MeV is estimated to be ∼360 cm−2 s−1. This corresponds to about 5 × 1025 precipitated electrons in this latitude range during the eight day observing interval compared to ∼2 × 10 25 trapped 0.5–3.6 MeV electrons estimated using GPS electron measurements. The MAXIS observations indicate that these electron precipitation events are common and may be the primary loss mechanism for outer zone relativistic electrons. Individual events were also compared with measurements of the trapped electrons from which it is estimated that only a few percent of the loss cone is being filled by the mechanism acting to precipitate the particles. This indicates that if the mechanism is wave-particle interaction, it is not in the strong diffusion regime.; Looking towards the future, a Compton telescope for imaging MeV X-ray bursts at high energies is also investigated. Such an instrument may also be used to measure polarization and thus may provide a method for inferring the precipitating electron pitch angle distribution.
机译:2000年1月12日,从南极麦克默多的一个长时球气球上发射了MAXIS(MeV极光X射线成像和光谱学)球囊有效载荷。MAXIS上的高光谱分辨率锗光谱仪检测到9个X射线爆发,通量范围扩大在18天的飞行中高于0.5 MeV。 X射线是通过电子沉淀产生的致辐射,这些事件的特征是非常平坦的X射线光谱(〜E −2 ),类似于1996年发现的第一个MeV事件,表明相对论母电子。在58°–68°的纬度(IGRF L值3.8–6.7)之间检测到爆发,持续时间从几分钟到几小时不等,仅在下午/黄昏时段(美国中部时间14:30-00:00)发生),而在所有磁场局部时间都检测到较软的降水。另外,MeV事件与亚暴活动有关,一些事件显示了X射线计数率的超低频(mHz)调制。航天器和基于地面的观测表明,在事件的时间和位置附近存在ULF波活动,这可能是由于某种未知的机制引起的调制。 MeV事件由非常平坦的指数沉淀电子分布很好地模拟,E≥0.5 MeV的沉淀电子的平均通量估计为〜360 cm −2 < italic> s -1 。在八天的观测间隔内,这对应于该纬度范围内约5×10 25 个沉淀电子,而使用GPS估算的约2×10 25 捕获的0.5–3.6 MeV电子电子测量。 MAXIS的观察结果表明,这些电子沉淀事件很常见,并且可能是外层相对论电子的主要损耗机制。还将各个事件与捕获电子的测量结果进行了比较,据估计,捕获电子的作用机理仅使百分之几的损耗锥被填充,从而使粒子沉淀。这表明如果机理是波粒相互作用,那么它就不在强扩散状态。展望未来,还研究了一种康普顿望远镜,用于对高能MeV X射线突发成像。这样的仪器还可以用于测量极化,并且因此可以提供用于推断沉淀的电子俯仰角分布的方法。

著录项

  • 作者

    Millan, Robyn Margaret.;

  • 作者单位

    University of California, Berkeley.;

  • 授予单位 University of California, Berkeley.;
  • 学科 Physics General.; Geophysics.
  • 学位 Ph.D.
  • 年度 2002
  • 页码 p.4212
  • 总页数 244
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 物理学;
  • 关键词

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