共查询到20条相似文献，搜索用时 359 毫秒
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《天文研究与技术》2004,(1)
《云南天文台台刊》 (PublicationsoftheYunnanObservatory)作为中国科学院云南天文台主办的面向国内外发行的学术性科技出版物 (CN 5 3- 10 5 2 /P ,ISSN 10 0 1- 75 2 6 ) ,自1977年创刊以来 ,至 2 0 0 3年末已出版发行 97期。《云南天文台台刊》所刊登的学术论文涵盖了天文学及相关学科的各个研究领域 ,包括天文和天体物理的观测研究、实测技术和方法、天文新发现和专题述评等方面的内容。至今《云南天文台台刊》作为中国科技核心期刊之一 ,被中国科技核心期刊 (遴选 )数据库、中国学术期刊综合评价数据库和国际天文数据库ADS和CD… 相似文献
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随着新一代巡天观测、时域观测等天文项目的推进,当前的天文数据量越来越大。面对天文领域日益增长的大数据集和大数据流,需要一些高效的数据存储和数据处理方法来对数据进行管理。天文数据库以及在其基础上提供的数据服务的出现部分解决了这样的问题。借助于计算机技术和信息技术的进步,一些更加专业的针对天文领域的数据发现、数据挖掘、数据交互等工作正在逐步标准化。基于虚拟天文台技术和天文信息学的新型天文数据服务正深入天文用户的日常科研生活中。首先简单回顾了天文数据库的历史,然后通过对几个典型天文数据库的举例分析,从天文数据库的类型、提供的服务等方面介绍了当前天文数据库的特点和最新进展,并对今后天文数据库的发展做了展望。 相似文献
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由北京天文学会山西小组、山西大学天文协会及太原师院天文协会等联合举办的山西省第19次天文科技信息交流会于12月15日在山西大学举行。 相似文献
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因最近几年连续举办“北京地区天文奥赛预赛”在北京天文科普活动领域而日渐闻名的北京市八一中学是北京百所“科技教育示范校”之一,坐落于北京中关村科技园区核心区。八一中学历来重视学生的科技教育,让学生全面发展、学有所长”是学校一贯的办学宗旨。该校连续多年开设天文观星等科技实验班和天文校本课程。可以说天文校园科技活动做的风生水起。 相似文献
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1999年下半年 ,上海市举办了一次全市性的中小学生天文知识方面的学习竞赛活动。尽管青少年学生对于生肖邮票、黄道十二宫、外星人和ＵＦＯ等天文主题非常感兴趣 ,但真正关于天文科学知识方面的科技活动却一直很少开展。即使为迎接哈雷彗星回归、彗木相撞、日全食和流星雨 ,也是相隔好几年才难得遇到机会组织一些有特定内容的活动。为了在尽可能广的范围内展开一个普及性的关于天文基础知识的学习活动 ,在上海市天文学会指导下 ,上海市少年科技指导站、中国福利会少年宫和《中学科技》杂志社联合组织了一次以中小学生为对象的天文仪器小制作… 相似文献
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尹在洪 《紫金山天文台台刊》1994,(4)
近几十年,在建设天文数据库,特别是空间天文数据库方面美国科学家们做了大量的工作,积累了丰富的数据资料。这是美国,也是全世界天文学家的共同宝藏。本文概略介绍了这些美国大型天文数据库的收藏内容、存取方式、以及所提供的服务,旨在使我国天文工作者更加重视这些珍贵的资料,进而去充分开发和利用它们。 相似文献
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山东师范大学是山东省省属重点大学 ,该校不仅在专业教育上雄居本省前列 ,而且在学生素质教育方面也非常重视 ,多年来天文科技活动一直在校园内积极开展 ,深受同学们的欢迎。通过开展校园天文科技活动 ,一方面拓宽了各专业学生的知识面 ,更重要的是提高了在校大学生的科学素质 ,为培养 2 1世纪合格的中学教师 ,奠定了良好的基础。1 999年可以说是山东师大“校园天文”最为火爆的一年 ,关注天文事件、探寻天文知识、参与观测活动、选修天文课程 ,几乎每一位同学在这一年里都与天文或多或少地建立了联系 ,分析其原因主要有两条 :首先是“98年… 相似文献
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自1995年第一颗类太阳恒星周围的系外行星发现以来,随着已发现的系外行星数目的增多,对系外行星性质的统计分析变得重要和有意义。截至2011年6月9日,共发现系外行星555颗。以这些系外行星的轨道参数为依据,对系外行星的性质进行统计分析,得出了一些有意义的结论。同时简要介绍现有的行星形成与演化模型并依据得出的行星统计性质对其进行检验,这对于系外行星的进一步探测具有一定的指导作用。 相似文献
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《Physics and Chemistry of the Earth, Part C: Solar, Terrestrial & Planetary Science》1999,24(5):553-556
Giant planets in circumstellar disks can migrate inward from their initial (formation) positions at several AUs. Inward radial migration of the planet is caused by torques between the planet and the disk; outward radial migration of the planet is caused by torques between the planet and the spinning star, and by torques due to Roche lobe overflow and consequent mass loss from the planet. We present self-consistent numerical considerations of the problem of migrating giant planets by summing torques on planets for various physical parameters of the disk and of planets. We find that Jupiter-mass planets can stably arrive and survive at small heliocentric distances, thus reproducing observed properties of some of the recently discovered extra-solar planets. The range of fates of massive planets is broad, and some perish by losing all their mass onto the central star during Roche lobe overflow, while others survive for the lifetime of the central star. Surviving planets cluster into two groups when examined in terms of final mass and final heliocentric distance: those which have lost mass and those which have not. Some of the observed extrasolar planets fall into each of these two exclusive classes. We also find that there is an inner boundary for planets' final heliocentric distances, caused by tidal torques with the central star. Planets in small orbits are shown to be stable against atmospheric loss. 相似文献
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Andrew W. Smith 《Icarus》2009,201(1):381-58
An investigation of the stability of systems of 1 M⊕ (Earth-mass) bodies orbiting a Sun-like star has been conducted for virtual times reaching 10 billion years. For the majority of the tests, a symplectic integrator with a fixed timestep of between 1 and 10 days was employed; however, smaller timesteps and a Bulirsch-Stoer integrator were also selectively utilized to increase confidence in the results. In most cases, the planets were started on initially coplanar, circular orbits, and the longitudinal initial positions of neighboring planets were widely separated. The ratio of the semimajor axes of consecutive planets in each system was approximately uniform (so the spacing between consecutive planets increased slowly in terms of distance from the star). The stability time for a system was taken to be the time at which the orbits of two or more planets crossed. Our results show that, for a given class of system (e.g., three 1 M⊕ planets), orbit crossing times vary with planetary spacing approximately as a power law over a wide range of separation in semimajor axis. Chaos tests indicate that deviations from this power law persist for changed initial longitudes and also for small but non-trivial changes in orbital spacing. We find that the stability time increases more rapidly at large initial orbital separations than the power-law dependence predicted from moderate initial orbital separations. Systems of five planets are less stable than systems of three planets for a specified semimajor axis spacing. Furthermore, systems of less massive planets can be packed more closely, being about as stable as 1 M⊕ planets when the radial separation between planets is scaled using the mutual Hill radius. Finally, systems with retrograde planets can be packed substantially more closely than prograde systems with equal numbers of planets. 相似文献
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日冕是太阳大气活动的关键区域,是日地空间天气的源头.受观测限制,对日冕低层大气等离子体结构和磁场状态的研究非常欠缺,国际上对于可见光波段日冕低层大气的亮度分层研究很少.利用丽江日冕仪YOGIS(Yunnan Green-line Imaging System)的日冕绿线(FeⅩⅣ5303?)观测资料,对内日冕区域(1.03R☉-1.25R☉,R☉表示太阳半径)亮结构及其中冕环进行了有效的强度衰减分析.对亮结构的强度在太阳径向高度上进行了指数衰减拟合,比较这些拟合结果发现所得到的静态内冕环的衰减指数在一固定值附近.然后将比较明显的冕环提取出来,通过对不同高度的绿线强度进行指数拟合,得出的衰减指数与亮结构中也比较相近,这对进一步研究日冕中的各项物理参数演化提供了参考. 相似文献
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We numerically investigate the stability of systems of 1 \({{\rm M}_{\oplus}}\) planets orbiting a solar-mass star. The systems studied have either 2 or 42 planets per occupied semimajor axis, for a total of 6, 10, 126, or 210 planets, and the planets were started on coplanar, circular orbits with the semimajor axes of the innermost planets at 1 AU. For systems with two planets per occupied orbit, the longitudinal initial locations of planets on a given orbit were separated by either 60° (Trojan planets) or 180°. With 42 planets per semimajor axis, initial longitudes were uniformly spaced. The ratio of the semimajor axes of consecutive coorbital groups in each system was approximately uniform. The instability time for a system was taken to be the first time at which the orbits of two planets with different initial orbital distances crossed. Simulations spanned virtual times of up to 1 × 108, 5 × 105, and 2 × 105 years for the 6- and 10-planet, 126-planet, and 210-planet systems, respectively. Our results show that, for a given class of system (e.g., five pairs of Trojan planets orbiting in the same direction), the relationship between orbit crossing times and planetary spacing is well fit by the functional form log(t c /t 0) = b β + c, where t c is the crossing time, t 0 = 1 year, β is the separation in initial orbital semimajor axis (in terms of the mutual Hill radii of the planets), and b and c are fitting constants. The same functional form was observed in the previous studies of single planets on nested orbits (Smith and Lissauer 2009). Pairs of Trojan planets are more stable than pairs initially separated by 180°. Systems with retrograde planets (i.e., some planets orbiting in the opposite sense from others) can be packed substantially more closely than can systems with all planets orbiting in the same sense. To have the same characteristic lifetime, systems with 2 or 42 planets per orbit typically need to have about 1.5 or 2 times the orbital separation as orbits occupied by single planets, respectively. 相似文献
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Adrián Rodríguez Cristian A. Giuppone Tatiana A. Michtchenko 《Celestial Mechanics and Dynamical Astronomy》2013,117(1):59-74
In this paper, we study the behavior of a pair of co-orbital planets, both orbiting a central star on the same plane and undergoing tidal interactions. Our goal is to investigate final orbital configurations of the planets, initially involved in the 1/1 mean-motion resonance (MMR), after long-lasting tidal evolution. The study is done in the form of purely numerical simulations of the exact equations of motions accounting for gravitational and tidal forces. The results obtained show that, at least for equal mass planets, the combined effects of the resonant and tidal interactions provoke the orbital instability of the system, often resulting in collision between the planets. We first discuss the case of two hot-super-Earth planets, whose orbital dynamics can be easily understood in the frame of our semi-analytical model of the 1/1 MMR. Systems consisting of two hot-Saturn planets are also briefly discussed. 相似文献
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A rich population of low‐mass planets orbiting solar‐type stars on tight orbits has been detected by Doppler spectroscopy. These planets have masses in the domain of super‐Earths and Neptune‐type objects, and periods less than 100 days. In numerous cases these planets are part of very compact multiplanetary systems. Up to seven planets have been discovered orbiting one single star. These low‐mass planets have been detected by the HARPS spectrograph around 30 % of solar‐type stars. This very high occurrence rate has been recently confirmed by the results of the Kepler planetary transit space mission. The large number of planets of this kind allows us to attempt a first characterization of their statistical properties, which in turn represent constraints to understand the formation process of these systems. The achieved progress in the sensitivity and stability of spectrographs have already led to the discovery of planets with masses as small as 1.5 M⊕ (© 2011 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim) 相似文献
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A number of extrasolar planets have been detected in close orbits around nearby stars. It is probable that these planets did
not form in these orbits but migrated from their formation locations beyond the ice line. Orbital migration mechanisms involving
angular momentum transfer through tidal interactions between the planets and circumstellar gas-dust disks or by gravitational
interaction with a residual planetesimal disk together with several means of halting inward migration have been identified.
These offer plausible schemes to explain the orbits of observed extrasolar giant planets and giant planets within the Solar
System. Recent advances in numerical integration methods and in the power of computer workstations have allowed these techniques
to be applied to modelling directly the mechanisms and consequences of orbital migration in the Solar System. There is now
potential for these techniques also to be applied to modelling the consequences of the orbital migration of planets in the
observed exoplanetary systems. In particular the detailed investigation of the stability of terrestrial planets in the habitable
zone of these systems and the formation of terrestrial planets after the dissipation of the gas disk is now possible. The
stability of terrestrial planets in the habitable zone of selected exoplanetary systems has been established and the possibility
of the accretion of terrestrial planets in these systems is being investigated by the author in collaboration with Barrie
W. Jones (Open University), and with John Chambers (NASA-Ames) and Mark Bailey of Armagh Observatory, using numerical integration.
The direct simulation of orbital migration by planetesimal scattering must probably await faster hardware and/or more efficient
algorithms.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
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We have tested the implications and limitations of Program ACRETE, a scheme based merely on Newtonian physics and accretion with unit sticking efficiency, devised by Dole in 1970 to simulate the origin of the planets. The dependence of the results on a variety of radial and vertical density distribution laws, on the ratio of gas to dust in the solar nebula, on the total nebula mass, and on the orbital eccentricity, ?, of the accreting grains are explored. Only for a small subset of conceivable cases are planetary systems closely like our own generated. Many models have tendencies toward one of two preferred configurations: multiple-star systems, or planetary systems in which Jovian planets either have substantially smaller masses than in our system or are absent altogether. But for a wide range of cases recognizable planetary systems are generated, ranging from multiple-star systems with accompanying planets, to systems with Jovian planets at several hundred astronomical units, to single stars surrounded only by asteroids. Many systems exhibit planets like Pluto and objects of asteroidal mass, in addition to usual terrestrial and Jovian planets. No terrestrial planets were generated more massive than five Earth masses. The number of planets per system is for most cases of order 10, and, roughly, inversely proportional to ?. All systems generated obey a relation of the Titius-Bode variety for relative planetary spacing. The case with which planetary systems are generated using such elementary and incomplete physical assumptions supports the idea of abundant and morphologically diverse planetary systems throughout the Galaxy. 相似文献
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L. V. Ksanfomality 《Solar System Research》2007,41(6):463-482
In this paper, we consider the physical properties and characteristic features of extrasolar planets and planetary systems, those, for which the passage of low-orbit giant planets across the stellar disk (transits) are observed. The paper is mostly a review. The peculiarities of the search for transits are briefly considered. The main attention in this paper is given to the difference in the physical properties of low-orbit giant planets. A comparison of the data obtained during the transits of “hot Jupiters” points to the probable existence of several distinct subtypes of low-orbit extrasolar planets. “Hot Jupiters” of low density (HD 209458b), “hot Jupiters” with massive cores composed of heavy elements (HD 149026b), and “very hot Jupiters” (HD 189733b) are bodies that probably fall into different categories of exoplanets. Dissipation of the atmospheres of low-orbit giant planets estimated from the experimental data is compared with the calculated Jeans atmospheric losses. For “hot Jupiters”, the expected Jeans mass losses due to atmospheric escape on a cosmogonic time scale hardly exceed a few percent. Low-orbit giant planets should have a strong magnetic field. Since the orbital velocity of “hot Jupiters” is close to the magnetosonic velocity (or can even exceed it), the moving planet should actively interact with the “stellar wind” plasma. The possession of a magnetic field by extrasolar planets and the effects of their interaction with plasma can be used to search for extrasolar planets. 相似文献