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X-rays from solar system objects

机译:来自太阳系物体的X射线

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During the last few years our knowledge about the X-ray emission from bodies within the solar system has significantly improved. Several new solar system objects are now known to shine in X-rays at energies below 2 keV. Apart from the Sun, the known X-ray emitters now include planets (Venus, Earth, Mars, Jupiter, and Saturn), planetary satellites (Moon, Io, Europa, and Ganymede), all active comets, the Io plasma torus (IPT), the rings of Saturn, the coronae (exospheres) of Earth and Mars, and the heliosphere. The advent of higher-resolution X-ray spectroscopy with the Chandra and XMM-Newton X-ray observatories has been of great benefit in advancing the field of planetary X-ray astronomy. Progress in modeling X-ray emission, laboratory studies of X-ray production, and theoretical calculations of cross-sections, have all contributed to our understanding of processes that produce X-rays from the solar system bodies. At Jupiter and Earth, both auroral and non-auroral disk X-ray emissions have been observed. X-rays have been detected from Saturn's disk, but no convincing evidence of an X-ray aurora has been observed. The first soft (0.1-2keV) X-ray observation of Earth's aurora by Chandra shows that it is highly variable. The non-auroral X-ray emissions from Jupiter, Saturn, and Earth, those from the disk of Mars, Venus, and Moon, and from the rings of Saturn, are mainly produced by scattering of solar X-rays. The spectral characteristics of X-ray emission from comets, the heliosphere, the geocorona, and the Martian halo are quite similar, but they appear to be quite different from those of Jovian auroral X-rays. X-rays from the Galilean satellites and the IPT are mostly driven by impact of Jovian magnetospheric particles. This paper reviews studies of the soft X-ray emission from the solar system bodies, excluding the Sun. Processes of production of solar system X-rays are discussed and an overview is provided of the main source mechanisms of X-ray production at each object. A brief account on recent development in the area of laboratory studies of X-ray production is also provided.
机译:在过去的几年中,我们对来自太阳系内物体的X射线发射的了解已大大提高。现在已知几个新的太阳系物体会在2 keV以下的能量下以X射线发光。除了太阳,现在已知的X射线发射器还包括行星(金星,地球,火星,木星和土星),行星卫星(月亮,艾欧,欧罗巴和木卫三),所有活动彗星,艾奥托环(IPT) ),土星环,地球和火星的日冕(外层)以及日球层。钱德拉(Chandra)和XMM-牛顿(Newton)X射线天文台更高分辨率的X射线光谱学的出现对推进行星X射线天文学领域具有极大的好处。 X射线发射建模,X射线产生的实验室研究以及横截面的理论计算方面的进展,都有助于我们理解从太阳系物体产生X射线的过程。在木星和地球上,已经观测到极光和非极光盘的X射线辐射。从土星的盘中检测到X射线,但没有令人信服的X射线极光证据。钱德拉(Chandra)对地球极光的第一次软(0.1-2keV)X射线观察表明,它极易变化。来自木星,土星和地球的非极光X射线,来自火星,金星和月球的圆盘以及来自土星环的非极光X射线主要产生于太阳X射线的散射。来自彗星,日球层,电晕和火星晕的X射线发射的光谱特征非常相似,但它们似乎与木卫二极光X射线的光谱特征完全不同。来自伽利略卫星和IPT的X射线主要由木星磁层的撞击驱动。本文回顾了太阳系(不包括太阳)发出的软X射线的研究。讨论了太阳系X射线的产生过程,并对每个对象产生X射线的主要来源机制进行了概述。还简要介绍了X射线产生实验室研究领域的最新发展。

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