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1.
耀斑伽玛射线谱中色含着作用区太阳大气元素丰度及加速高能粒子元素丰度的重要信息。综述了这一刚刚兴起的伽玛射线谱诊断元素丰度的新领域及其所获得的若干新结果。 相似文献
2.
太阳耀斑伽玛射线能谱是加速粒子与太阳大气介质原子碰撞的结果,它是研究太阳耀斑中加速粒子和高能电子最为直接的手段.通过分析伽玛射线能谱,可以获得耀斑过程中加速粒子的成分、能谱、角分布及太阳大气元素丰度等重要信息.TALYS程序是一套模拟核反应的软件,对核反应过程中的所有信息均能完整地描述.利用TALYS计算得到了完整的太阳耀斑伽玛射线的核反应截面数据,开发了一套新的耀斑伽玛射线谱计算程序.详细介绍了耀斑伽玛射线计算的理论模型,并简单探讨了耀斑伽玛射线的特性,为未来的耀斑伽玛射线能谱分析奠定了理论基础. 相似文献
3.
强磁场中的共振逆康普顿散射(RICS)是产生伽玛射线的有效机制．在前文工作的基础上，导出强磁场中子星中具有幂律能谱的大量相对论电子沿中子星磁轴向外运动时在变化磁场中产生的集体RICS辐射谱(RICS谱光度)的基本公式．由此得到在中子星周边几种典型的低频辐射场中集体RICS辐射谱形的简单解析表示(如热轫致辐射场、黑体辐射场，以及非热低频幂律谱辐射场)，以便与实际观测谱形比较．计算表明：在满足匹配条件(即近似共振条件)下，RICS辐射效率很高，其谱形都是两段式(折断的)的幂律谱形式，与周边低频场性质无关．通过计算，再一次论证RICS机制是伽玛射线脉冲星和伽玛暴(GRBs)在高能射线段(硬X-射线和伽玛射线)辐射的一个理想的高效辐射机制。 相似文献
4.
Swift卫星的X射线望远镜观测揭示部分伽玛暴的早期余辉光变曲线有一个缓慢衰减的成分,而相当一部分却没有这样的成分.研究比较这两种暴的观测性质发现两类暴的持续时间、伽玛辐射总流量、谱指数、谱硬度比峰值能量等物理量均没有显著差异.然而有该成分的那些伽玛暴谱比较软、早期X射线余辉比较弱、伽玛射线辐射效率显著高于没有这个成分的那些暴.结果表明两类暴的前身星和中心机制一致,是否呈现这个缓慢衰减成分可能取决于外部介质. 相似文献
5.
强磁场中相对论电子的共振逆康普顿散射(RICS)是产生伽玛射线的有效机制.以前的工作曾论证,伽玛暴(GRB)的早期伽玛射线辐射可能主要由该机制产生.利用此辐射机制,伽玛暴研究中的一些困惑有可能得到较好的解释.例如,观测统计给出的"Amati关系"的起源,两段式(折断式)幂律谱的形成,特别是其中"死线问题"的解决方案,还有偏振的存在等.这里将重点讨论折断幂律谱形成问题.基于单个电子的RICS谱功率公式,导出了强磁场中大量相对论电子穿过周边低频辐射场时产生的集体RICS辐射谱(RICS谱光度)的简化解析公式,并将它应用于中子星周边几种典型的低频场(如黑体辐射场、幂律辐射场以及热轫致辐射场),以便与实际观测谱形比较.计算表明:在满足匹配条件(即近似共振条件)下,RICS辐射效率很高,其谱形普遍为两段式的幂律谱形式,与周边低频场性质无关.还论证RICS机制可能是伽玛暴、软伽玛重复暴和伽玛射线脉冲星在高能射线波段(硬X射线和伽玛射线)的一个理想的高效辐射机制. 相似文献
6.
本文简要回顾了ＳＭＭ／ＧＲＳ对耀斑伽玛射线的观测，并就耀斑伽玛射线的产生，伽玛射线发射的时间结构及解释，高能粒子的能谱及作用模型，高能辐射的方向性及粒子的加速机制，加速粒子的元素丰富度以及电子占优事件的性质等方面，简述了目前的研究状况。 相似文献
7.
王建民 《紫金山天文台台刊》1999,18(3):271-273
频繁的超新星爆发可用以解释活动星系核与类星体的超高金属丰度。星团中的恒星与吸积盘相互作用导致致密天体中子星和黑洞的形成率很高,这些致密天体与红巨星很容易形成双星系统,而后形成（ＮＳ／ＢＨ,ＮＳ／ＢＨ） 双星由于引力辐射最终导致并合而形成伽玛射线爆发。我们估计了伽玛射线爆的爆发频率,发现与观测相符。 相似文献
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9.
伽玛射线暴是一种来自宇宙空间随机方向的短时间内伽玛射线突然增亮的现象。伽玛射线暴虽然早在1967年就由Vela卫星观测到,但直到1997年人们才通过余辉观测确定其寄主星系,并通过寄主星系的红移最终确定了伽玛射线暴的宇宙学起源。对伽玛射线暴研究概况进行了评述:详细介绍了伽玛射线暴及其余辉的观测进展,特别是近期Swift卫星和Fermi卫星带来的新发现;系统描述了伽玛射线暴标准火球模型、伽玛射线暴余辉物理(相对论性外流与暴周环境介质的相互作用过程、辐射产生机制等)及伽玛射线暴的前身星等。也对伽玛射线暴的未来研究进行了展望。 相似文献
10.
本文收集了ＳＭＭ运行期间（１９８０．２－１９８９．１１）与地面观测相对应的太阳白光耀斑ＨＸＲＢＳ和ＧＲＳ观测资料，就白光耀斑与硬Ｘ－射线发射及伽玛射线发射之产的关系进行了初步的统计研究，结果表明：白光耀斑与伽玛射线发射之间不存在对应关系；白光耀斑也并非全具有强硬Ｘ－射线发射，对那些只具有对较弱的硬Ｘ－射线发射的白光耀斑，我们发现低能粒子具有足够的能量驱动连续发射，因而它们可能起源于色球，而对那些具 相似文献
11.
Nathalia Alzate 《Icarus》2011,211(2):1274-1283
Central pit craters are common on Mars, Ganymede and Callisto, and thus are generally believed to require target volatiles in their formation. The purpose of this study is to identify the environmental conditions under which central pit craters form on Ganymede. We have conducted a study of 471 central pit craters with diameters between 5 and 150 km on Ganymede and compared the results to 1604 central pit craters on Mars (diameter range 5-160 km). Both floor and summit pits occur on Mars whereas floor pits dominate on Ganymede. Central peak craters are found in similar locations and diameter ranges as central pit craters on Mars and overlap in location and at diameters <60 km on Ganymede. Central pit craters show no regional variations on either Ganymede or Mars and are not concentrated on specific geologic units. Central pit craters show a range of preservation states, indicating that conditions favoring central pit formation have existed since crater-retaining surfaces have existed on Ganymede and Mars. Central pit craters on Ganymede are generally about three times larger than those on Mars, probably due to gravity scaling although target characteristics and resolution also may play a role. Central pits tend to be larger relative to their parent crater on Ganymede than on Mars, probably because of Ganymede’s purer ice crust. A transition to different characteristics occurs in Ganymede’s icy crust at depths of 4-7 km based on the larger pit-to-crater-diameter relationship for craters in the 70-130-km-diameter range and lack of central peaks in craters larger than 60-km-diameter. We use our results to constrain the proposed formation models for central pits on these two bodies. Our results are most consistent with the melt-drainage model for central pit formation. 相似文献
12.
The Tractus Fossae region of Mars is a wide area dominated by grabens, normal faults and pit crater chains. In this work, based on previous studies on the area and the new interpretation of topographic data and morphological units based on images as a geologic framework we present a new insight on the origin of the graben structures as well as on the processes associated with the formation of the volcanic features. Here we propose a new model for this region, on the basis of new measurements of graben extension and geological interpretations, together with a reinterpretation of the stratigraphy and the geologic history of the area. Finally, it is postulated that this region underwent a tectonic regime analog to an asymmetric rift system on Earth. 相似文献
13.
Sarah J. Morrison Peter C. Thomas Matthew S. Tiscareno Joseph A. Burns Joseph Veverka 《Icarus》2009,204(1):262-270
High-resolution images from the Cassini Imaging Science Subsystem (ISS) show parallel sets of grooves on Epimetheus and Pandora. Grooves have previously been observed on other satellites and asteroids, including Phobos, Gaspra, Ida, Eros, and minor occurrences on Phoebe. Sets of parallel grooves are so far observed only on satellites known or likely to be subject to significant tidal stresses, such as forced librations. Grooves on asteroids and on satellites not subject to significant forced librations occur in more globally disorganized patterns that may reflect impacts, varying internal structures, or even thermal stresses. The patterns and individual morphologies of grooves on the tidally-affected satellites suggest fracturing in weak materials due to tidal stresses and forced librations. 相似文献
14.
Lava tubes and basaltic caves are common features in volcanic terrains on Earth. Lava tubes and cave-like features have also been identified on Mars based on orbital imagery and remote-sensing data. Caves are unique environments where both secondary mineral precipitation and microbial growth are enhanced by stable physico-chemical conditions. Thus, they represent excellent locations where traces of microbial life, or biosignatures, are formed and preserved in minerals. By analogy with terrestrial caves, caves on Mars may contain a record of secondary mineralization that would inform us on past aqueous activity. They may also represent the best locations to search for biosignatures. The study of caves on Earth can be used to test hypotheses and better understand biogeochemical processes, and the signatures that these processes leave in mineral deposits. Caves may also serve as test beds for the development of exploration strategies and novel technologies for future missions to Mars. Here we review recent evidence for the presence of caves or lava tubes on Mars, as well as the geomicrobiology of lava tubes and basaltic caves on Earth. We also propose future lines of investigation, including exploration strategies and relevant technologies. 相似文献
15.
In this paper the tidal phenomena on the Earth are concisely specified, including solid tides, ocean tides and atmospheric tides due to the luni-solar tide-generating force, and the Earth pole tide due to the motion of the Earth's rotation axis (polar motion); as well as their effects on the Earth rotation. The outcomes of scientific researches of Chinese astronomers on these topics are described in some detail. These researches deal with the mechanisms responsible for tidal effects on the earth rotation, and on the measurements of the Earth rotation parameters. Finally, the effects discovered by Chinese researchers on the measurements of the period and change in period of pulsars are discussed. These effects are very small in magnitude but not negligible. 相似文献
16.
C.J. Howe D. Drummond B. Maddison R. Parker J. Spencer M. Grande J. Huovelin J. Gow L. d’Uston 《Planetary and Space Science》2009,57(7):735-743
The UK-built Chandrayaan-1 X-ray Spectrometer (C1XS) is flying as an ESA instrument on India's Chandrayaan-1 mission to the Moon. The Chandrayaan-1 mission launched on the 22nd October 2008 and entered a 100 km polar lunar orbit on the 12th November 2008. C1XS builds on experience gained with the earlier D-CIXS instrument on SMART-1, but will be a technically much more capable instrument. Here we describe the instrument design. 相似文献
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18.
We review the present status of how astronomical observations allow to constrain the evolution of fundamental constants of
nature. The main observational constraints on the variation of the gravitational constant, on the fine structure constant
and on the proton-to-electron mass ratio are reviewed. We also elaborate on some theoretical schemes which naturally lead
to such variations. 相似文献
19.
我国雷暴活动对太阳耀斑响应的东西不对称性 总被引：3，自引：0，他引：3
本文研究了１９７１—１９８０年间发生在日面东部的１６４个和西部的１３２个２级以上耀斑对我国１８５个气象站上空雷暴活动的影响．结果表明，日面东部耀斑爆发后雷暴活动减弱且通过优于０．１的置信度检验测站数远多于日面西部耀斑，而日面西部耀斑爆发后雷暴活动增强，通过优于０．１的置信度检验测站数远多于日面东部耀斑．这种与地磁活动和日球扰动相似的雷暴活动对太阳耀斑响应的东西不对称性，可能借助于大气电环境并通过行星际磁场和磁层，将太阳和对流层的确耦合起来了． 相似文献
20.
Minerals mapping of the lunar surface with Clementine UVVIS/NIR data based on spectra unmixing method and Hapke model 总被引：2，自引：0，他引：2
The distribution of minerals on the lunar surface is information which could contribute to studying lunar origin and evolution. In this paper, the distribution of clinopyroxene, orthopyroxene, olivine, ilmenite, and plagioclase on the lunar surface has been mapped based on Hapke radiative transfer model and linear unmixing of spectra with Clementine UVVIS/NIR data. The results have been validated on the basis of minerals modal abundance data of the Apollo samples, and problems in the minerals abundance mapping have been analyzed. The validation based on analysis data of Apollo samples indicates that plagioclase mapped in this paper represents the total abundance of plagioclase and agglutinitic glass. The minerals mapping results show that the lunar surface is mainly composed of pyroxene, plagioclase, agglutinitic glass, and ilmenite. Basalt in the lunar mare is mainly composed of clinopyroxene and ilmenite, and lunar highland is mainly composed of plagioclase and agglutinitic glass. Orthopyroxene is mainly distributed on the north of Mare Imbrium, on the south of Maria and Aitken Basin. According to our results, there is probably no large area of olivine distribution on the lunar surface which is different from earlier published results. Therefore, emphasis should be put on the olivine distribution in the minerals mapping using hyperspectral data such as M3 of Chandrayaan-1 and IIM of ChangE-1. 相似文献