共查询到19条相似文献，搜索用时 140 毫秒
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提出了关于地球生命起源的新模型---星云中继假说, 它是宇宙胚种论的修改版本. 在这个模型中, 作为宇宙``种子''的原始生命起源于太阳系的前身恒星系统中的生物化学过程, 并且在前身恒星死亡后充满整个原太阳星云. 地球生命的起源可以分为3个阶段: 太阳前身恒星的原始生命起源, 原太阳星云时期和太阳系形成与地球生命时期. 这个模型最主要的推论是原始生命(或其后裔)以及它们的化石存在于太阳系内各种天体之中. 相似文献
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分析在聚合形成机制下,巨分子云在刚体自转盘中的形成过程．研究结果表明,形成的巨分子云主要由其附近的分子云组成．由于速度弥散的作用,非弹性碰撞和自引力使分子云聚会在一起,以这种方式形成的巨分子云是小质量的．如果较差自转存在,这些小质量的巨分子云便有更多的机会聚合在一起形成更大质量的巨分子云．这进一步说明,较差自转在巨分子云的形成中起了很大的积极作用． 相似文献
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分析在聚合形成机制下,巨分子云在刚体自转盘中的形成过程。研究结果表明,形成的巨分子云主要由其附近的分子云组成,由于速度弥散的作用,非弹性碰撞才自引力使分子云聚合在一起,以这种方式形成的巨分子云是小质量的,如果较差自转存在这些小质量的巨分子云便有更多的机会聚合在一起形成更大质量的巨分子云,这进一步说明,较差自转在巨分子云的形成中起了很大的积极作用。 相似文献
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本文分析了在巨分子云聚合形成机制下旋臂扰动的影响 .结果表明 ,在巨分子云聚合形成过程中 ,当不考虑恒星形成引起的巨分子云的碎裂时 ,旋臂的存在使分子云在绕星系中心作自转运动时 ,在旋臂区域分子云的密度大大增加而使较多的大质量分子云由于碰撞而形成 ,特别能促使一些质量更大的巨分子云形成 .但当这些聚合形成的大质量分子云走出旋臂区域进入臂间区域时 ,它们又会自动瓦解 .因此在整个星系盘上 ,与没有旋臂扰动情况相比 ,F(M )∝logM的曲线只是相应地往上有一平移 ,而对形成的中间质量的巨分子云的数量基本没有影响 相似文献
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本分析了在巨分子云聚合形成机制下旋臂扰动的影响，结果表明，在巨分子云聚合形成过程中，当不考虑恒星形成引起的巨分子云的破裂时，旋臂的存在使分子云在绕星系中心作自转运动时，在旋臂区域分子云的密度大大增加而使大质量分子云由于碰撞而形成，特别能促使一些质量更大的巨分子云形成。但当这些聚合形成的大质量分子云走出旋臂区域进入臂间区域时，它们又会自动瓦解。因此在整个星系盘上，与没有旋臂扰动情况相比，Ｆ（Ｍ）〈 相似文献
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星系中的巨分子云(GMCs)是恒星形成的主要区域,因此它的形成和演化对于星系的演化是至关重要的。本文中将介绍分子云的基本特性、分子云之间的碰撞和巨分子云的形成、碎裂和寿命以及其他环境因素,如旋臂扰动、较差自转等在巨分子云的形成和演化中的作用。同时也探讨在采用数值模拟研究巨分子云演化时所取分子云数目的影响。 相似文献
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太阳系原始同位素组成是研究太阳系起源和演经的基础,评述了太阳星云的原始放射性核素丰度特征及解释此丰度特征的分子云自增丰模型,ＡＧＢ星污染模型和散裂反应模型,阴石包体中前太阳矿物颗粒的同位素组成异常表明,前太阳颗粒只氏密度石墨,Ｘ型碳硅石可能来源于超新星爆发,而ＡＧＢ星或红巨星被认为尖晶石和碳硅石的最可能的恒星来源,太阳系中比较特殊的氖和氙的同位素组成异常出现与超新星爆发密切相关。 相似文献
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宋国玄 《中国天文和天体物理学报》1989,(1)
巨分子云的碰撞造成了大质量恒星在碰撞分子云中的形成,这些大质量恒星的形成产生了膨胀的HII区域,从而使巨分于云碎裂成小质量的分子云。这是本文提出的巨分子云碎裂机制。因此巨分子云的寿命也主要由区分子云间的碰撞几率所决定。我们的分析表明,巨分子云的寿命有赖于巨分子云所在的旋涡星系中的不同位置。寿命的最大可能存在区间为8.18×10~7yr与2.45×10~8yr。利用我们提出的机制可以在分子云研究的数值计算与数值模拟中得到应用。 相似文献
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Hsu Wei-biao 《Chinese Astronomy and Astrophysics》2003,27(4):365-373
This paper reviews the evidence for short-lived radionuclides in the early solar system and evaluates the models of their origin. The stellar model requires that some freshly-nucleosynthesized radionuclides were injected into the proto-solar cloud shortly before it began to collapse. The spallation theory suggests that these nuclides were the products of interaction between energetic particles and gas/dust in the proto-solar cloud or solar nebula. A brief discussion is given to a new theory for the X-wind model of solar system formation. 相似文献
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Comets seem to be composed of matter, which is supposed to have the same molecular composition as protosolar nebula. Although there are no unbiased evidence that cometary nuclei retain the molecular composition inherited from the protosolar cloud, the observed properties of comets indicate that there is at least a resemblance between cometary composition and the material properties of dense interstellar clouds. Therefore the origin of comets could be searched in the cold stages of the protosolar nebula and molecular abundances of grain mantles in this nebula may be similar to those in the cometary dust. It is suggested that comets may contain pristine, virtually unaltered protosolar material and their study might be very relevant way to more information about processes in early stages of the solar nebula. Our knowledge about composition of the cometary nucleus is still relatively scarce, but we can partly deduce it from data obtained either by ground-based spectroscopy or by in situ mass spectrometry from space experiments. Most important were the discovery of fluffy CHON particles composed partly or even completely from compounds containing light elements. No consensus concerning the presence of interstellar pristine matter in comet has been reached from various approaches to determine the relationship between comets and interstellar grains. Most of these studies are based on infrared spectroscopy. Another method is the comparison on the chemical models of the protosolar nebula with the volatile compounds of the cometary nuclei. Both gas-phase and grain-surface chemistry are considered and initial gas-phase atomic abundances are assumed to be protosolar. The cometary matter is certainly not identical with the typical material of dense interstellar cool dense clouds, but it is closer to it than any other type of matter in solar system so far accessible to us. The data from comets combined with models of chemical evolution of matter in environment similar as prevailed the early stage of presolar nebula may at least impose constrains on the condition for comet formation. Here presented study is a preliminary contribution to such studies. 相似文献
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A. J. Westphal J. C. Bridges D. E. Brownlee A. L. Butterworth B. T. De Gregorio G. Dominguez G. J. Flynn Z. Gainsforth H. A. Ishii D. Joswiak L. R. Nittler R. C. Ogliore R. Palma R. O. Pepin T. Stephan M. E. Zolensky 《Meteoritics & planetary science》2017,52(9):1859-1898
Recent observations indicate that >99% of the small bodies in the solar system reside in its outer reaches—in the Kuiper Belt and Oort Cloud. Kuiper Belt bodies are probably the best‐preserved representatives of the icy planetesimals that dominated the bulk of the solid mass in the early solar system. They likely contain preserved materials inherited from the protosolar cloud, held in cryogenic storage since the formation of the solar system. Despite their importance, they are relatively underrepresented in our extraterrestrial sample collections by many orders of magnitude (~1013 by mass) as compared with the asteroids, represented by meteorites, which are composed of materials that have generally been strongly altered by thermal and aqueous processes. We have only begun to scratch the surface in understanding Kuiper Belt objects, but it is already clear that the very limited samples of them that we have in our laboratories hold the promise of dramatically expanding our understanding of the formation of the solar system. Stardust returned the first samples from a known small solar system body, the Jupiter‐family comet 81P/Wild 2, and, in a separate collector, the first solid samples from the local interstellar medium. The first decade of Stardust research resulted in more than 142 peer‐reviewed publications, including 15 papers in Science. Analyses of these amazing samples continue to yield unexpected discoveries and to raise new questions about the history of the early solar system. We identify nine high‐priority scientific objectives for future Stardust analyses that address important unsolved problems in planetary science. 相似文献
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Thérèse Encrenaz 《Astronomy and Astrophysics Review》1999,9(3-4):171-219
Summary. The exploration of Jupiter, the closest and biggest giant planet, has provided key information about the origin and evolution
of the outer Solar system. Our knowledge has strongly benefited from the Voyager and Galileo space missions. We now have a
good understanding of Jupiter's thermal structure, chemical composition and magnetospheric environment.
There is still debate about the nature of the heating source responsible for the high thermospheric temperatures (precipitating
particles and/or gravity waves). The measurement of elemental abundance ratios (C/H, N/H, S/H) gives strong support to the
“nucleation” formation model, according to which giant planets formed from the accretion of an initial core and the collapse
of the surrounding gaseous protosolar nebula. The D/H and He/He ratios are found to be representative of their protosolar value. The helium abundance, in contrast, appears to be slightly
depleted in the outer envelope with respect to the protosolar value; this departure is interpreted as an evolutionary effect,
due to the condensation of helium droplets in the liquid hydrogen ocean inside Jupiter's interior.
The cloud structure of Jupiter, characterized by the belt-zone system, is globally understood; also present are specific features
like regions of strong infrared radiation (“hot spots”), colder regions (“white ovals”) and the Great Red Spot (GRS). Clouds
were surprisingly absent at the hot spot corresponding to the Galileo probe entry site, and the water abundance measured there
was strongly depleted with respect to the solar O/H value. This probably implies that hot spots are dry, cloud-free regions
of subsidence, while “normal” air, rich in condensibles, is transported upward by convective motions. As a result, the Jovian
meteorology, still based on Halley-type cells, seems to be much more complex than a simple zone-belt system. The nature of
the GRS, a giant anticyclonic storm, colder and higher than its environment, has been confirmed by the Galileo observations,
but its internal structure appears to be very complex.
Strong winds, probably driven by the Jovian internal source, were measured at deep tropospheric levels. The troposphere might
be statically stable at pressures higher than 18 bars, but the extent of this putative radiative layer is still unknown.
Received 23 November 1998 相似文献
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The solar activity can be quantified by solar modulation parameter Φ that affects the heliospheric magnetic field. This activity influences the intensity of the galactic cosmic ray (GCR) particle flux within the solar system, and consequently, the differential primary particle spectra depend on the solar modulation parameter Φ (MeV). The modulation parameter Φ shows spatial and temporal variations (Leya and Masarik 2009). Some of the solar activity variations are cyclic and result in measurable effects as for example the 11‐year solar cycle. Variations in solar activity only induce small effects on the production of long‐lived cosmogenic radionuclides. This is due to the fact that activities measured in meteorites usually correspond to saturation values and represent long‐term average values. Long‐lived radionuclides often require millions of years of irradiation by GCR to reach saturation and therefore activity cycles average out. In contrast, one can expect strongly pronounced variations for saturation values caused by primary flux intensity variations, if short‐lived radionuclides with half‐lives ranging from days to a few years are investigated. Short‐lived cosmogenic nuclides were the subject of many experimental and theoretical investigations (e.g., Evans et al. 1982; Spergel et al. 1986; Neumann et al. 1997; Komura et al. 2002; Laubenstein et al. 2012). The aim of this work is to develop formulae for calculating production rates of radionuclides with short half‐life, taking into account temporal variations in the primary cosmic ray intensity. The developed formulae were applied to the Kosice and Chelyabinsk meteorites. The results for the Ko?ice meteorite were already published (Povinec et al. 2015). Here, we give a full explanation of underlying model. 相似文献
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Henri E. Mitler 《Icarus》1973,20(1):54-71
This article is a critical summary of the solar-system aspects of a meeting held in August 1972. The purpose of the meeting was to review work done sonce the 1967 Paris meeting on the Origin of the Elements.The principal topics discussed were element abundances; the structure and composition of comets, of the terrestrial and the outer planets, of the Moon, of exospheric dust, and of meteorites; planetary atmospheres; evidence for a protosolar magnetic field from remanent meteorite magnetism, abiotic synthesis of organic molecules; nucleosynthesis; solar cosmic rays; and meteorite ages.The principal results were these: There have been a number of significant changes in the estimated solar abundances—especially D, He, B, and Fe. A great deal of progress has been made in our understanding of the temperature and pressure conditions in the protosolar nebula during planetary formation, and of the condensation of solids in it. It is believed that the bulk chemistry of the terrestrial planets is now understood on the basis of equilibrium (slow) cooling of the nebula. Their atmospheres are consistent with this model, and that of Jupiter, with inhomogeneous accretion. The structure of Jupiter is also better understood. There is disagreement on the deep structure and composition of the Moon, though of course an enormous amount has been learned, especially about the surface layers. Not so much progress has been made in understanding comets. 相似文献
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Robert H. NICHOLS Frank A. PODOSEK Brad S. MEYER Cristine L. JENNINGS 《Meteoritics & planetary science》1999,34(6):869-884
Abstract— The presence of several short-lived (now extinct) radionuclides in the early solar system demands that they were synthesized and added to preexisting solar system materials shortly (on a time scale on the order of the relevant radionuclide lifetime) before formation of solar system solids. For diverse reasons, it is often suggested that the solar system distributions of these radionuclides were radically heterogeneous, perhaps because of the late addition. Much attention has been given to the astrophysical circumstances that might govern the synthesis and distribution of these short-lived radionuclides, but comparatively little attention has been devoted to the distribution of cosynthesized isotopes. The focus of this paper is a systematic, quantitative evaluation of the collateral consequences in stable and long-lived isotopes that might be expected if short-lived radionuclides, in particular 26Al or 53Mn, were injected at their canonical levels and inhomogeneously distributed in the early solar system. We mix model massive star yields of Meyer et al. (1995) and Woosley and Weaver (1995) into a reservoir of cosmic composition, as tabulated by Anders and Grevesse (1989). To mitigate the effects of systematic deviations that may be present in these mixtures due to uncertainties in model stellar yields, we follow Timmes and Clayton (1996) and also mix into a “renormalized” proxy solar system composition computed from a galactic chemical evolution model based primarily on the stellar yields of Woosley and Weaver (1995). The results are very unfavorable to the likelihood of heterogeneously distributed 26Al derived from supernova ejecta. If a massive star is invoked to account for 26Al, its ejecta must have been rather uniformly distributed, as inferred from the lack of measured collateral anomalies in several elements, notably Ca, Cr, and Ni. Conversely, if 26Al were indeed radically heterogeneously distributed, some other nucleosynthetic source more efficient at producing 26Al is required. In principle, a similar statement applies to 53Mn, but the situation is more complicated. The inferred anomalies at 53Cr will depend not only on how much 53Mn is added by a heterogeneous component, but also more sensitively on the contributions to the associated stable nuclides, 53Cr, 52Cr, and 50Cr. Consideration of predicted collateral anomalies provides no direct support for heterogeneously distributed supernova-derived 53Mn, but the required quantity of supernova contribution, and thus also the collateral anomalies, are much less for 53Mn than for 26Al. With allowance for model calculation uncertainties, it could be argued that anomalies collateral to heterogeneous 53Mn might be small enough to have evaded detection. 相似文献
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A. B. Makalkin 《Solar System Research》2004,38(6):491-507
The problem of angular-momentum and mass transport in the disk is discussed and the disk viscosity is estimated. The evolution of the gas-dust protoplanetary disk at the stage of its formation inside the protostellar (protosolar) accretion envelope is considered. The conditions for the radial growth of the disk are estimated. For the subsequent period, when the central star (young Sun) is in the T Tauri phase, the temporal variations of the radius, mass, and the surface density of the disk, as well as the total mass flux from the disk onto the star (Sun), i.e., the mass accretion rate, are evaluated. The constraints on the initial value of the angular momentum of the protoplanetary circumsolar disk (that is, on the angular momentum of the protosolar cloud) are discussed with due regard for cosmochemical data.Translated from Astronomicheskii Vestnik, Vol. 38, No. 6, 2004, pp. 559–576.Original Russian Text Copyright © 2004 by Makalkin. 相似文献