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1.
用紫金山天文台青海站的１３７ｍ射电望远镜,对１０个行星状星云给出了新的ＣＯ（１－０）谱线观测结果．其中４个行星状星云：ＮＧＣ６４４５,Ｍ１５９,Ｍ４９和Ｍ２５１,已有过ＣＯ（２１）的观测,本文第一次给出了它们的ＣＯ（１０）的测量结果;对２个别人曾经观测过但未测到ＣＯ的行星状星云：Ｓｈ２７１和Ｍ４１８,本文第一次证认了它们的ＣＯ发射;对４个别人从未进行过ＣＯ搜寻的行星状星云：ＶＶ１８,Ｍ２５２,Ｈｅ２４５９和Ｋ３３１,本文第一次进行了观测,并得到了它们的ＣＯ（１０）谱．由ＣＯ的发射谱征可见,ＶＶ１８可能是一个误分类的行星状星云 相似文献
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使用澳大利亚Ｐａｒｋｅｓ６４ｍ射电望远镜,在五个不同的位置上观测了ＯＨ１７．７２．０附近的弱ＯＨ脉泽源．发现了一个新的弱ＯＨ脉泽源,其峰值速度为５２．５ｋｍ／ｓ．利用二维Ｇａｕｓｓｉａｎ拟合技术,得到了这个源的最佳拟合位置 相似文献
3.
在此介绍我们基于ＡＳＣＡ 和ＲＯＳＡＴ 等Ｘ 射线天文卫星,对３Ｃ３９７ 、Ｇ３２７ ．１１ ．１ 、Ｇ２１ ．５０ ．９ 和ＲＸＪ１７１３ ．７３９４６ 等超新星遗迹的物理特性进行的分析,简要地讨论了３Ｃ３９７ 的非平衡电离双热分量和双极泡结构以及Ｇ３２７ ．１１ ．１ 和Ｇ２１ ．５０ ．９ 中隐匿脉冲星的性质,并提出ＲＸＪ１７１３ ．７３９４６ 和ＡＤ３９３ 客星之间可能的关系。 相似文献
4.
ON2中部区域OH1667MHz脉泽的新观测 总被引：1，自引：0，他引：1
利用法国巴黎默东天文台的南锡射电望远镜对ＯＮ２ 中部区域ＯＨ１６６７ ＭＨｚ 脉泽首次进行观测．观测结果表明中部区域的ＯＨ１６６７ ＭＨｚ 脉泽的辐射频谱为典型的双峰结构．这说明ＯＮ２ 中部区域的ＯＨ１６６７ ＭＨｚ 脉泽是位于绕中央星运动的薄盘上．结合模型对中部区域的ＯＨ１６６７ ＭＨｚ 脉泽谱线频谱图进行分析和研究 相似文献
5.
利用紫金山天文台青海观测站１３．７米射电望远镜对源ＩＲＡＳ０５３９１０２１７和ＩＲＡＳ０６５７２０７４２进行了１２ＣＯＪ＝１－０观测,获得了气体的相应参数;用ＩＲＡＳ及其他红外观测资料,获得了尘埃热结构;探讨了云中气体的热平衡．对于ＩＲＡＳ０５３９１０２１７中由远红外得出的Ｔｄ＜Ｔｋ的情形,考虑了几种可能的加热机制．光电加热对该云可能是比较重要的;激波可能是另一种加热途径． 相似文献
6.
张澍 《中国天文和天体物理学报》1998,(2)
利用直接解调方法分析了ＣＯＭＰＴＥＬ对γ暴ＧＲＢ９１０６０１的观测数据,发现该γ暴的直接解调成像定位较ＣＯＭＰＴＥＬ用最大似然法分析得到的结果更接近于ＵｌｙｓｅｓＢＡＴＳＥ系统联合定位的圆环．结果表明,采用直接解调方法对γ暴这类信噪比高、统计性差的瞬变源进行成像分析是完全可行的,而且,γ暴的成像定位精度可由此而获得提高． 相似文献
7.
本文详细计算了在不同的观测条件下（大气视宁度,天光背景）,对于不同的观测对象（椭圆星系、旋涡星系和恒星等）光纤定位中心位置偏差对光谱观测结果的影响．根据ＬＡＭＯＳＴ的主要设计参数,给出了在不同条件下观测所得信噪比的具体数值结果．本文同时也给出了采用不同光纤尺寸对观测结果的影响 相似文献
8.
根据贫金属星个别重元素丰度的观测值和太阳系重核素的ｒ过程和ｓ过程分量的丰度分布,计算了贫金属星ＨＤ２０３６０８和ＨＤ２１１９９８的重元素丰度并与观测进行了比较。结果表明,太阳系纯ｒ过程和ｓ过程元素丰度均不能拟合出这二颗样品星的丰度观测值,而应同时考虑ｒ过程和ｓ过程的贡献 相似文献
9.
作者认为,有五种误差会影响ＬＡＭＯＳＴ工程光纤定位：（１）光纤的机械定位误差;（２）输入星表与导星星表的误差;（３）焦面坐标系与理想坐标系的转换误差;（４）较差大气折射对观测目标的影响;（５）导星的跟踪误差。并提出在ＬＡＭＯＳＴ工程中有关天体测量的三个研究课题：（１）星表系统差的研究,以提供适合ＬＡＭＯＳＴ使用的导星星表和输入星表;（２）望远镜光学系统畸变的研究以及焦面坐标与理想坐标间关系的确定,提出用国内外观测资料,建立５°×５°的几个标准天区;（３）从现有的光学图象和测光资料中给出ＬＡＭＯＳＴ输入星表中星象的类别,如双星、聚星、变星、星系等。建议ＬＡＭＯＳＴ工程中采用ＧＳＣ－Ⅱ作为导星星表,而输入星表的精度应好于０．５４”。 相似文献
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5个新发现的X选BL Lac天体 总被引：1，自引：0，他引：1
利用ＲＯＳＡＴＶＬＡ方法筛选，从ＲＯＳＡＴＸ射线源中选出了一批新的ＢＬＬａｃ天体和类星体的候选体．１９９６年１２月８日至１７日，利用北京天文台２．１６ｍ望远镜和新从美国引进的ＯＭＲ摄谱仪，对这批新候选体进行了光谱认证．经ＳＵＮ工作站处理，又发现了５个新的Ｘ选ＢＬＬａｃ天体．此外，还对去年作者在ＯＭＲ引进之前发现的ＢＬＬａｃ天体进行了检验，结果发现，去年发现的７个ＢＬＬａｃ天体中，２３２２＋３４３的ＣａＩＩＨ＆Ｋ“Ｂｒｅａｋｓｔｒｅｎｇｔｈ”为２６．９％，稍大于判据２５％，因此，２３２２＋３４３到底是ＢＬＬａｃ天体还是射电星系还有待于进一步测光及偏振观测的验证． 相似文献
11.
M. Sobotka 《Astronomische Nachrichten》2003,324(4):369-373
Sunspots and pores appear as a consequence of interactions between strong magnetic fields and moving plasma. A wide variety of small‐scale features, presumably of convective origin, are observed in photospheric layers of sunspots and pores: Umbral dots, light bridges, penumbral filaments, and penumbral grains. Each type of features has specific morphological, photometric, spectral, and kinematic characteristics. Spots and pores modify velocity fields in adjacent photosphere and sub‐photospheric layers. Recent high‐resolution spectral, broad‐band, and helioseismic observations of the structure, dynamics, and magnetic fields of sunspots and pores, together with theoretical interpretations, are discussed in this review. 相似文献
12.
Alexander N. Krot Tasha L. Dunn Michail I. Petaev Chi Ma Kazuhide Nagashima Jutta Zipfel 《Meteoritics & planetary science》2024,59(4):809-835
We report on the primary and secondary mineralogies of three coarse-grained igneous calcium-aluminum-rich inclusions (CAIs) (Compact Type A [CTA], Type B [B], and forsterite-bearing type B [FoB]) from the Northwest Africa (NWA) 5343 (CK3.7) and NWA 4964 (CK3.8) carbonaceous chondrites, compare them with the mineralogy of igneous CAIs from the Allende (CV3.6) chondrite, and discuss the nature of the alteration processes that affected the CK and CV CAIs. The primary mineralogy and mineral chemistry of the CK3 CAIs studied are similar to those from Allende; however, primary melilite and anorthite are nearly completely absent. Although the secondary minerals identified in CK CAIs (Al-diopside, andradite, Cl-apatite, clintonite, forsterite, ferroan olivine, Fe,Ni-sulfides, grossular, ilmenite, magnetite, plagioclase, spinel, titanite, and wadalite) occur also in the Allende CAIs, there are several important differences: (i) In addition to melilite and anorthite, which are nearly completely replaced by secondary minerals, the alteration of CK CAIs also affected high-Ti pyroxenes (fassaite and grossmanite) characterized by high Ti3+/Ti4+ ratio and spinel. These pyroxenes are corroded and crosscut by veins of Fe- and Ti-bearing grossular, Fe-bearing Al,Ti-diopside, titanite, and ilmenite. Spinel is corroded by Fe-bearing Al-diopside and grossular. (ii) The secondary mineral assemblages of grossular + monticellite and grossular + wollastonite, commonly observed in the Allende CAIs, are absent; the Fe-bearing grossular + Fe-bearing Al-diopside ± Fe,Mg-spinel, Fe-bearing grossular + Fe,Mg-olivine ± Fe,Mg-spinel, and Ca,Na-plagioclase + Fe-bearing Al-diopside + Fe-bearing grossular assemblages are present instead. These mineral assemblages are often crosscut by veins of Fe-bearing Al-diopside, Fe,Mg-olivine, Fe,Mg-spinel, and Ca,Na-plagioclase. The coarse-grained secondary grossular and Al-diopside often show multilayered chemical zoning with distinct compositional boundaries between the layers; the abundances of Fe and Ti typically increase toward the grain edges. (iv) Sodium-rich secondary minerals, nepheline and sodalite, commonly observed in the peripheral portions of the Allende CAIs, are absent; Ca,Na-plagioclase is present instead. We conclude that coarse-grained igneous CAIs from CK3.7–3.8 s and Allende experienced an open-system multistage metasomatic alteration in the presence of an aqueous solution–infiltration metasomatism. This process resulted in localized mobilization of all major rock-forming elements: Si, Ca, Al, Ti, Mg, Fe, Mn, Na, K, and Cl. The metasomatic alteration of CK CAIs is more advanced and occurred under higher temperature and higher oxygen fugacity than that of the Allende CAIs. 相似文献
13.
F.W. Taylor 《Planetary and Space Science》2011,59(10):889-899
Spacecraft studies of the three terrestrial planets with atmospheres have made it possible to make meaningful comparisons that shed light on their common origin and divergent evolutionary paths. Early in their histories, all three apparently had oceans and extensive volcanism; Mars and Earth, at least, had magnetic fields, and Earth, at least, had life. All three currently have climates determined by energy balance relationships involving carbon dioxide, water and aerosols, regulated by solar energy deposition, atmospheric and ocean circulation, composition, and cloud physics and chemistry.This paper addresses the extent to which current knowledge allows us to explain the observed state of each planet, its planetology, climatology and biology, within a common framework. Areas of ignorance and mysteries are explored, and prospects for advances in resolving these with missions within the present planning horizon of the space agencies are considered and assessed. 相似文献
14.
Bernard H. Foing 《Solar physics》1989,121(1-2):117-133
Stellar spectral diagnostics are of utmost importance to test fundamental concepts of flare physics such as particle beam versus suprathermal heating, atmospheric response, mass motions, microflaring, statistics and recurrence of flares, flare activity and stellar interior. We review some of these diagnostics (from photometry, optical, and ultraviolet spectroscopy at medium- and high-spectral resolution, X-ray, and radio observations). Specific diagnostics from line and continuum fluxes, density sensitive lines, broadening and velocity field effects and the comparison with semi-empirical models are also described.Some results on stellar flares obtained from previous multi-wavelength observing campaigns are presented. Future satellite missions and ground-based observatories, with new techniques for obtaining high spectral and temporal resolution, are discussed in light of their possible contribution to our understanding of solar and stellar flares.Based partially on observations obtained at European Southern Observatory, Canada-France Hawaii Telescope, and with IUE and EXOSAT satellites. 相似文献
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Harry Y. McSWEEN 《Meteoritics & planetary science》1996,31(6):727-738
Abstract— Research on extraterrestrial materials plays a critical role in formulating the science rationale and design for spacecraft missions, and, conversely, spaceflight holds great promise for solving perplexing problems in meteoritics. The connections between meteoritics and sample-return missions are obvious: Meteorite research can define sampling strategies, the capabilities of sampling devices, acceptable levels of chemical contamination and physical alteration of samples, and the conditions under which samples are stored prior to and during recovery. For their part, sample-return missions can provide geologic context for meteorites, increased sampling diversity (including materials not sampled as meteorites, such as unconsolidated regolith, ices, and atmosphere), calibration for crater-counting chronology, and ground truth for remote sensing measurements of meteorite parent bodies. Meteoritics also relates to spacecraft flyby, rendezvous, and lander missions that do not necessarily return samples. Specific illustrations of this mutual relationship, based on a selection of recent or planned spacecraft missions include: Identifying source asteroid classes for ordinary and carbonaceous chondrites and reconstructing their thermal and collisional histories (Galileo, NEAR, Clementine II, and Muses-C); determining the extent to which cometary dust and interstellar grains are found as interplanetary dust particles and assessing volatile abundances, isotopic compositions, and molecular species in cometary nuclei (Stardust and Rosetta); understanding the compositions of ancient Martian crust and the mantle sources for SNC meteorites, as well as inventorying the planet's volatile reservoirs and interactions (Mars Pathfinder, Mars Global Surveyor, and Mars Volatiles and Climate Surveyor); assessing whether lunar meteorites provide a more representative chemical sampling of the highlands crust and of mare volcanism than do Apollo samples (Galileo, Clementine, and Lunar Prospector). Spaceflight is the first priority of the space agencies that fund most research on extraterrestrial materials, and the continued level of support for such research may be linked, in part, to its use in exploration by spacecraft. 相似文献
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The measurement of stellar properties such as chemical compositions, masses and ages, through stellar spectra, is a fundamental problem in astrophysics. Progress in the understanding, calculation and measurement of atomic properties and processes relevant to the high-accuracy analysis of F-, G-, and K-type stellar spectra is reviewed, with particular emphasis on abundance analysis. This includes fundamental atomic data such as energy levels, wavelengths, and transition probabilities, as well as processes of photoionisation, collisional broadening and inelastic collisions. A recurring theme throughout the review is the interplay between theoretical atomic physics, laboratory measurements, and astrophysical modelling, all of which contribute to our understanding of atoms and atomic processes, as well as to modelling stellar spectra. 相似文献
20.
时间频率量的特征及其对时频系统建设的影响 总被引：2，自引：1，他引：1
分析了物理量测量中时间频率量的特点，主要有：时间的流逝性；其基准是自然基准；时间和频率既密切相关又有区别；时间频率具有最高的测量精细度(分辨率)与准确度；其计量标准可通过电磁波发播；其测量精确度与测量时间有关。另外，从基准、守时、授时、时间频率设备的研制、生产和队伍建设等方面阐发了这些特点对时间频率系统建设的影响。 相似文献