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1.
给出了1997年4月15日至17日在北京天文台用2．16m望远镜卡焦光谱仪观测获得的6颗激变变星（ABBoo;UXUMa,TCrBAHHer,ZCam和V426Oph）及3颗相关天体（UMa3,EGUMa和Leo3）的CCD光谱,并同时拍摄了5颗晚型星（3Dra,Vir,Leo,34Boo和36Corn）的CCD光谱,作为晚型星参考谱．测量了观测样本星的Hα和近红外CaII的三重线（8498,8542和8662）的等值宽度（EW）,谱线半极大全宽（FWHM）和现向速度（Vr）,并分析了这些星的活动性． 相似文献
2.
Ⅴ1159 Ori 是SU UMa 型中 ER UMa 亚型激变变星,BZ UMa 介于 U Gem 型和 WZ Sge 型之间,但又具有 SU UMa 的周期特征,存在争议.在2008年2月24日和 25日,用云南天文台 1 米 RCC(Ritchey-Chretien-Coude)望远镜对两者的测光观测显示: Ⅴ1159 Ori 在正常爆发的下降阶段存在 superhump,这为 superhump 现象普遍存在于 ER UMa 型星中提供了观测证据;BZ UMa 观测时处于爆发极大,并未观测到确凿的 superhump 周期,而 AAVSO(American Association of Variable Star Observers)近年的 BZ UMa 观测亦从未发现明确的 superhump;两者均表明 BZ UMa 可能并非 SU UMa 型星.基于星等变化幅度考虑,BZ UMa 较 WZ Sge 更为接近. 相似文献
3.
《天文学报》2010,(1)
V1159 Ori是SU UMa型中ER UMa亚型激变变星,BZ UMa介于UGem型和WZ Sge型之间,但又具有SU UMa的周期特征,存在争议.在2008年2月24日和25日,用云南天文台1米RCC(Ritchey-Chretien-Coude)望远镜对两者的测光观测显示:V1159 Ori在正常爆发的下降阶段存在superhump,这为superhump现象普遍存在于ER UMa型星中提供了观测证据;BZ UMa观测时处于爆发极大,并未观测到确凿的superhump周期,而AAVSO(American Association of Variable Star Observers)近年的BZ UMa观测亦从未发现明确的superhump;两者均表明BZ UMa可能并非SUUMa型星.基于星等变化幅度考虑,BZ UMa较WZ Sge更为接近. 相似文献
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依据观测获得的５颗晚型星：λＡｎｄ,κＣｅｔ,６１ＣｙｇＡ,αＣａｓ和βＣｅｔ的高分辨率、高信噪比的光谱,采用谱线塞曼致宽的谱线轮廓叠加法和利用大量ＦｅＩ的多重线统计分析方法,成功地测定了这些星的磁场和磁场覆盖因子,并对这两种磁场测定方法做了简述和讨论 相似文献
6.
对１９９５年１１月和１９９６年３、４月间观测获得的ＨＲ５５５３、７０Ｏｐｈ和εＥｒｉ给出了高分辨率,高信噪比的阶梯光栅光谱资料。确定了这３颗晚型活动星的大气参数,采用谱线细致分析方法求出了铁、锂、钙、钪、钛、钒、铬、锰、钴、镍、钇、锆和钡１３种金属元素的丰度。采用多重线统计方法测定了这３颗晚型活动星的磁场和磁场覆盖因子。 相似文献
7.
给出了１９９７年４月１５日至１７日在北京天台用２．１６ｍ望远镜卡焦光谱仪观测获得的６颗激变变星（ＡＢ Ｂｏｏ,ＵＸ ＵＭａ,Ｔ ＣｒＢ,ＡＨ Ｈｅｒ,Ｚ Ｃａｍ和Ｖ４２６ Ｏｐｈ）及３颗相关天体（ＵＭａ３,ＥＧ ＵＭａ和Ｌｅｏ３）的ＣＣＤ光谱,并同时拍摄了５颗晚型星（３Ｄｒａ,ｖ Ｖｉｒ,ψＬｅｏ,３４Ｂｏｏ和３６Ｃｏｍ）的ＣＣＤ光谱,作为晚型星参考谱,测量了观测样本星的Ｈα和近红外ＣａⅡ的三重 相似文献
8.
1981年3月及1983年3月期间对44i Boo做了光谱观测。发现CaⅡ的K线和CaⅠ的4227谱线的等值宽度随位相不同而有周期性的变化,而且随之H_α谱线轮廓也有显著变化。本文根据我们的观测资料及最近的IUE的结果做了初步分析,提出了有关44i Boo(B)大气模型的简易设想及密近双星上的恒星活动规律。 相似文献
9.
我们在有些恒星上观测到它们的光亮骤然发生变化,例如和太阳隣近的红矮星(鲸鱼UV型)和属於某一星協的星(金牛T型). 本文先列出20颗确定为鲸鱼UV型的星(表1),然後讨论它们的光变情况,如躍变的幅度,光变曲线(表2),闪光的速度(在上昇到极亮时,速度可达0.25星等/秒),躍变的频率等.跟着我们更讨论这些星不在闪光的时候的变化(表3). 这些星的光谱内常有发射线(H与CaⅡ),闪光的时候,光谱上的连续背景加强,并且出现HeⅠ和HeⅡ的谱线,表示温度增加很高,但是这仅限於星的很小的表皮层(1至3％). 鲸鱼UV型星自身亮度很弱(M_(pg)13),数目很多,属星族Ⅰ. 本文内提到几颗御夫RW型星的迅速变化,并且讨论了金牛区(表5),猎户星雲区(表6)和NGC2264里(表7)的闪光星. 我们研究了光变的情况,特别说明鲸鱼UV型星和金牛T型星之间的关系:例如在光曲线、光谱型和同属星族Ⅰ几个方面.我们也讨论了这两型星在绝对星等、光谱和赫-罗图上的位置三者的差异. 最後我们断定鲸鱼UV型星和金牛T型星实在是相同的一群;我们由观测得到的它们之间的差异,其原因一则由於“观测上的选择性”,再则由於这两型星的演化阶段有所不同. 许多恒星的光亮表现突然的增加,或者说很迅速地发出“闪光”,在几分钟、有时在几秒钟内,星光有显著的增加,跟着变暗,初迅速而渐缓慢. 这种星光的躍变在许多型星都观测到,特别是在绝对亮度微弱的星上面.我们现在只讨论下列的主要两类恒星: 相似文献
10.
使用德国Th(u|¨)ringer Landessternwarte Tautenburg(TLS)的2 m望远镜对Aquila Rift的16个区域进行了Hα、R和I共3个波段的成像观测.这些观测区域大约覆盖了Aquila Rift 7平方度的天区.除去3个数据质量不高的天区,对其余的13个区域进行了测光分析,从中证认出点源,并利用双色图的方法最终证认出7颗Hα发射线星候选体.这7个候选体是从5个观测区域中选出的,其中3颗位于银道面区域,4颗位于银纬高于4°的区域.对于这5个天区,证认了其中点源的2MASS对应体,并利用双色图的方法进一步分析了7个Hα发射线星候选体的性质.这些Hα发射线星候选体的近红外辐射并没有明显的红外超现象,有一颗还落在了主序分支上.这也说明有Hα发射的年轻星并不都伴随有红外超现象.Hα发射线观测和红外超观测的结果是相互补充的.如果将这7颗Hα发射线星候选体作为年轻星候选体,则Aquila Rift区域的年轻星数目是较少的.对于这些候选体的进一步证认还需要后续的光谱观测. 相似文献
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C. M. Andreazza E. P. Marinho P. D. Singh † 《Monthly notices of the Royal Astronomical Society》2006,372(4):1653-1656
The rate coefficients for the formation of carbon monophosphide (CP) and silicon monophosphide (SiP) by radiative association are estimated for temperatures ranging from 300 to 14 100 K. In this temperature range, the radiative association rate coefficients are found to vary from 1.14 × 10−18 to 1.62 × 10−18 cm3 s−1 and from 3.73 × 10−20 to 7.03 × 10−20 cm3 s−1 for CP and SiP, respectively. In both cases, rate coefficients increase slowly with the increase in temperature. 相似文献
13.
DDO photometry and metallic abundances of E and SO galaxies and globular clusters of the LMC and SMC
Horacio A. Dottori Miriani G. Pastoriza Eduardo L. D. Bica 《Astrophysics and Space Science》1983,91(1):79-91
Metallicity of 8 E and SO galaxies as well as that of red globulars of the LMC and SMC were obtained by means of DDO integrated photometry calibrated with galactic globular clusters (Bica and Pastoriza, 1983; hereafter referred to as Paper I). A correction was obtained in order to reduce the colors of the galaxies to zero redshift. The relation metallicity vsM V for the galaxies is analyzed (adding to our sample the observations of McClure and Van den Bergh, 1968; and Faber, 1973a). For the Magellanic Clouds we found metallicity ranging from intermediate to poor. 相似文献
14.
Dale P. Cruikshank 《Icarus》1977,30(1):224-230
Thermal radiation has been detected from four asteroids of the Trojan group, and J6 and J7, the brightest of the outer satellites of Jupiter. The six objects all have exceedingly low geometric albedos of 0.02 or 0.03 according to calculations based on their known visual brightness and the measured thermal fluxes. 624 Hektor, the largest object studied here, has a radius of 110 ± 20 km, though the exact shape of this body is in question. While the sample observed in this work is small (the total number of Trojans larger than 0.25 km in radius is about 1000), the fact that all four studied have similarly low albedos suggests that this property is characterisic of the Trojans and at least two of the outer members of Jupiter's retinue of satellites. The low surface albedo of the Trojans may preclude the proposed origin of the Jovian group of comets among these bodies according to E. Rabe. Updated tables of the dimensions of all the Jovian satellites are given. 相似文献
15.
Both Uranus and Neptune are thought to have strong zonal winds with velocities of several 100 m s−1. These wind velocities, however, assume solid-body rotation periods based on Voyager 2 measurements of periodic variations in the planets’ radio signals and of fits to the planets’ magnetic fields; 17.24 h and 16.11 h for Uranus and Neptune, respectively. The realization that the radio period of Saturn does not represent the planet’s deep interior rotation and the complexity of the magnetic fields of Uranus and Neptune raise the possibility that the Voyager 2 radio and magnetic periods might not represent the deep interior rotation periods of the ice giants. Moreover, if there is deep differential rotation within Uranus and Neptune no single solid-body rotation period could characterize the bulk rotation of the planets. We use wind and shape data to investigate the rotation of Uranus and Neptune. The shapes (flattening) of the ice giants are not measured, but only inferred from atmospheric wind speeds and radio occultation measurements at a single latitude. The inferred oblateness values of Uranus and Neptune do not correspond to bodies rotating with the Voyager rotation periods. Minimization of wind velocities or dynamic heights of the 1 bar isosurfaces, constrained by the single occultation radii and gravitational coefficients of the planets, leads to solid-body rotation periods of ∼16.58 h for Uranus and ∼17.46 h for Neptune. Uranus might be rotating faster and Neptune slower than Voyager rotation speeds. We derive shapes for the planets based on these rotation rates. Wind velocities with respect to these rotation periods are essentially identical on Uranus and Neptune and wind speeds are slower than previously thought. Alternatively, if we interpret wind measurements in terms of differential rotation on cylinders there are essentially no residual atmospheric winds. 相似文献
16.
Amir Babak Aazami Priyamvada Natarajan 《Monthly notices of the Royal Astronomical Society》2006,372(4):1692-1698
Gravitational lensing of a background source by a foreground galaxy lens occasionally produces four images of the source. The cusp and the fold relations impose conditions on the ratios of magnifications of these four-image lenses. In this theoretical investigation, we explore the sensitivity of these relations to the presence of substructure in the lens. Starting with a smooth lens potential, we add varying amounts of substructure, while keeping the source position fixed, and find that the fold relation is a more robust indicator of substructure than the cusp relation for the images. This robustness is independent of the detailed spatial distribution of the substructure, as well as of the ellipticity of the lensing potential and the presence of external shear. 相似文献
17.
R. Rummel 《Earth, Moon, and Planets》2004,94(1-2):103-111
Planetology serves the understanding on the one hand of the solar system and on the other hand, for investigating similarities
and differences, of our own planet. While observational evidence about the outer planets is very limited, substantial datasets
exist for the terrestrial planets. Radar and optical images and detailed models of gravity and topography give an impressive
insight into the history, composition and dynamics of moon and planets. However, there exists still significant lack of data.
It is therefore recommended to equip all future satellite missions to the moon and to planets with full tensor gravity gradiometers
and radar altimeters. 相似文献
18.
B. P. GLASS D. W. MUENOW B. F. BOHOR G. P. MEEKER 《Meteoritics & planetary science》1997,32(3):333-341
Abstract— An examination of data collected over the last 30 years indicates that the percent of glass fragments vs. whole splash forms in the Cenozoic microtektite strewn fields increases towards the source crater (or source region). We propose that this is due to thermal stress produced when tektites and larger microtektites fall into water near the source crater while still relatively hot (>1150 °C). We also find evidence (low major oxide totals, frothing when melted) for hydration of most of the North American tektite fragments and microtektites found in marine sediments. High-temperature mass spectrometry indicates that these tektite fragments and microtektites contain up to 3.8 wt% H2O. The H2O-release behavior during the high-temperature mass-spectrometric analysis, plus high CI abundances (0.05 wt%), indicate that the North American tektite fragments and microtektites were hydrated in the marine environment (i.e., the H2O was not trapped solely on quenching from a melt). The younger Ivory Coast and Australasian microtektites do not exhibit much evidence of hydration (at least not in excess of 0.5 wt% H2O); this suggests that the degree of hydration increases with age. In addition, we find that some glass spherules (with <65 wt% SiO2) from the upper Eocene clinopyroxene-bearing spherule layer in the Indian Ocean have palagonitized rims. These spherules appear to have been altered in a similar fashion to the splash form K/T boundary spherules. Thus, our data indicate that tektites and microtektites that generally contain >65 wt% SiO2 can undergo simple hydration in the marine environment, while impact glasses (with <65 wt% SiO2) can also undergo palagonitization. 相似文献
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V. Bumba 《Solar physics》1996,169(2):303-312
We have compiled the results of our long-term studies of the local magnetic field and its activity development, derived from investigating sunspot group evolution, photoelectrically measured longitudinal magnetic and velocity fields, and measurements of sunspot proper motions. We estimate certain regularities according to which the magnetic and velocity fields, and photospheric, as well as chromospheric activities develop. We speculate about the physical background of such processes.Dedicated to Cornelis de Jager 相似文献