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1.
吴月芳  张华伟 《天文学报》1994,35(3):288-304
本文给出了39个不同类型的恒星脉泽源的近红外测光结果,以所获的的J、H、K波段流量密度,结合IRAS分光测量数据及低分辨光谱指数等资料,得出了各类源在不同波段的双色图上的分布特点,计算了光谱斜率和红外光度,同时从红外及射电辐射得出了中心星质量损失率及质量损失历经时间,并对不同源的各类参数进行了比较分析,结果表明随着在AGB上的演化,中心星质量损失率不断增加,脉泽源的红外特性和包层结构呈系统变化,进  相似文献   

2.
本文给出35个不同类型含SiO(v=1,J=1-0)脉泽发射的AGB星的近红外观测结果(其中包括6个Ⅰ型OH星,13个Ⅱ型OH星,9个仅有SiO脉泽的星以及7个无OH脉泽但有SiO和H2O脉泽的星).得出了它们的JHK星等和流量.同时经认证找出了它们对应的IRAS观测数据.通过对它们的近红外、中远红外以及OH射电资料的同时分析,得出了不同类型SiO脉泽星的色指数、谱斜率以及在近红外波段上拟合的等效黑体温度Teq.由红外及OH射电资料导出了其中心星的质量损失率M,并在此基础上结合已知的SiO脉泽源资料,找出了不同类型SiO脉泽星各量之间的关系.计算结果表明,SiO脉泽具有普遍性,在各类脉泽星中都可出现.SiO脉泽的光度与质量损失率弱相关,并且从(Mira)SiO到(OH/IR)SiO逐渐增加.SiO脉泽的流量与近红外“色”以及等效黑体温度Teq的关系较为密切.SiO脉泽积分流量的上限与IRAS在12μm和25μm上流量分别都相关.本文对SiO脉泽在AGB演化中的地位和特殊性进行了简单讨论.  相似文献   

3.
陈培生  汪洵浩 《天文学报》1999,40(2):174-182
利用IRAS低分辨率光谱(LRS)观测资料,从近2000个具有1612MHzOH发射的IRAS源中,发现9个具有碳化硅特征拱星壳层的OH/IR星的候选者.进一步的研究表明其中的6个确实或极有可能既是显示11.3μm碳化硅发射特征的碳星,也是表现1612MHzOH脉泽发射的OH/IR星  相似文献   

4.
本文作者用澳大利亚Parkes 64m射电望远镜观测了OH17.7-2.0的拱星OH脉泽辐射,在观测中共测得了三个峰,其中一个峰是我们新发现的弱源,两个峰是过去发强源,用二维Gaussian拟合我们发现强源位置与一个IRAS点源位置相一致,弱源位置在这个IRAS点源位置的西南方,强源的两个峰的速度位置和峰值流量密度都是比较稳定的。  相似文献   

5.
本文作者用澳大利亚Parkes64m射电望远镜观测了OH17.7-2.0的拱星OH脉泽辐射。在观测中共测得了三个峰,其中一个峰是我们新发现的弱源,两个峰是过去发现的强源。用二维Gaussian拟合我们发现强源位置与一个IRAS点源位置相一致,弱源位置在这个IRAS点源位置的西南方。强源的两个峰的速度位置和峰值流量密度都是比较稳定的。  相似文献   

6.
本对36颗不同质量、不同演化阶段的年轻星体进行了J,H,K波段测光,并结合其它光学、近红外、IRAS、亚毫米、毫米波段的观测结果,计算了它们的红外色指数、能谱分布指数、红外光度等参量,得到近红外和远红外双色图,比较了不同类别源的参量分布。最后,在前人工作的基础上,改进了低质量主序前星的辐射模型,对一些源进行了计算并分析其星周状况。  相似文献   

7.
本文发表继探测到恒星形成区的10个新H2O脉泽[1]后,再发现和证认的7个银河系星际H2O脉泽及其有关参量和谱线图。这些新H2O脉泽是与CO分子外流源[2-5]AFGL5142,HH-3,AFOL5157,NGC2023,RNO73,20126+4104,L1251-A成协的。它们与相应的外向流的中心IRAS点源间的平均位置差为|△α|=24''.8,|△δ|=27''。  相似文献   

8.
向德琳 《天文学报》1995,36(1):107-113
本文发表继探测到恒星形成区的10个新H2O脉泽后,再发现和证认的7个银河系星际H2O脉泽及其有关参量和谱线图,这些新H2O脉泽是与CO分子外流源AFGL5142,HH-3,AFGL5157,NGC2023,RNO73,20126+1+4104,L1251-A成协的。它们与相应的外向流的中心IRAS点源间的平均位置差为|Δα|=24''8,|Δδ|=27''。  相似文献   

9.
本对一批中心星光度大于10^3L⊙质量大于7~8M⊙的大质量年轻星体(YSOs)进行了研究,利用近几年对这批源进行的JHK波段的观测以及其它台站的红外测光和IRAS点源资料,得到了这批源的红外能谱,根据它们在7-23μm间的低分辨率光谱(LRS)确定了其尘埃粒子的类型,并将其分三类;(1)具有9.7μm的硅酸盐特征;(2)具有11.3μm的PAH特征;(3)特征不明显或谱噪音较大,本采用球对称  相似文献   

10.
用中科院射电联合实验室上海天台25米望远镜,对19个已知水脉泽源和20个HII区候选源进行了水脉泽观测和搜寻,共测到水脉泽辐射21个,包括2个首次测到S/N≥3σ的源。结合已知脉泽资料求出了脉泽时变,发现峰值流量的变化比较普遍,包括同一峰强度变化及不同成分置换引起的变化两种情况,峰值速度变化多数由不同成分置换所造成。证认了对应的IRAS源并探讨了脉泽辐射与红外参量的关系,表明红外辐射的强度对脉泽  相似文献   

11.
正Research in Astronomy and Astrophysics publishes original research papers and reviews 011 all liranchcs of astronoiriy and astrophysics.Reviews arc by invitation only.Important new results that require rapid publication can be submitted as a Letter(Letters must be restricted in length  相似文献   

12.
Laura Schaefer 《Icarus》2004,169(1):216-241
We modified the MAGMA chemical equilibrium code developed by Fegley and Cameron (1987, Earth Planet. Sci. Lett. 82, 207-222) and used it to model vaporization of high temperature silicate lavas on Io. The MAGMA code computes chemical equilibria in a melt, between melt and its equilibrium vapor, and in the gas phase. The good agreement of MAGMA code results with experimental data and with other computer codes is demonstrated. The temperature-dependent pressure and composition of vapor in equilibrium with lava is calculated from 1700 to 2400 K for 109 different silicate lavas in the ONaKFeSiMgCaAlTi system. Results for five lavas (tholeiitic basalt, alkali basalt, Barberton komatiite, dunite, and a molten type B1 Ca, Al-rich inclusion) are discussed in detail. The effects of continuous fractional vaporization on chemistry of these lavas and their equilibrium vapor are presented. The predicted abundances (relative to Na) of K, Fe, Si, Al, Ca, and Ti in the vapor equilibrated with lavas at 1900 K are lower than published upper limits for Io's atmosphere (which do not include Mg). We predict evaporative loss of alkalis, Fe, and Si during volcanic eruptions. Sodium is more volatile than K, and the Na/K ratio in the gas is decreased by fractional vaporization. This process can match Io's atmospheric Na/K ratio of 10±3 reported by Brown (2001, Icarus 151, 190-195). Silicon monoxide is an abundant species in the vapor above lavas. Spectroscopic searches are recommended for SiO at IR and mm wavelengths. Reactions of metallic vapors with S- and Cl-bearing volcanic gases may form other unusual gases including MgCl2, MgS, MgCl, FeCl2, FeS, FeCl, and SiS.  相似文献   

13.
14.
正Research in Astronomy and Astrophysics publishes original research papers and reviews on all branches of astronomy and astrophysics.Reviews are by invitation only.Important new results that require rapid publication can be submitted as a Letter(Letters must be restricted in length to 6 printed pages).Authors who submit a paper are expected to be able to certify that the paper is original work,  相似文献   

15.
16.
Laura Schaefer 《Icarus》2005,173(2):454-468
We use chemical equilibrium calculations to model the speciation of alkalis and halogens in volcanic gases emitted on Io. The calculations cover wide temperature (500-2000 K) and pressure (10−6 to 10+1 bars) ranges, which overlap the nominal conditions at Pele (T=1760 K, P=0.01 bars). About 230 compounds of 11 elements (O, S, Li, Na, K, Rb, Cs, F, Cl, Br, I) are considered. The elemental abundances for O, S, Na, K, and Cl are based upon observations. CI chondritic elemental abundances relative to sulfur are used for the other alkalis and halogens (as yet unobserved on Io). We predict the major alkali species in Pele-like volcanic gases and the percentage distribution of each alkali are LiCl (73%), LiF (27%); NaCl (81%), Na (16%), NaF (3%); KCl (91%), K (5%), KF (4%); RbCl (93%), Rb (4%), RbF (3%); CsCl (92%), CsF (6%), Cs (2%). Likewise the major halogen species and the percentage distribution of each halogen are NaF (88%), KF (10%), LiF (2%); NaCl (89%), KCl (11%); NaBr (89%), KBr (10%), Br (1%); NaI (61%), I (30%), KI (9%). We predict the major halogen condensates and their condensation temperatures at P=0.01 bar are NaF (1115 K), LiF (970 K); NaCl (1050 K), KCl (950 K); KBr (750 K), RbBr (730 K), CsBr (645 K); and solid I2 (200 K). We also model disequilibrium chemistry of the alkalis and halogens in the volcanic plume. Based on this work and our prior modeling for Na, K, and Cl in a volcanic plume, we predict the major loss processes for the alkali halide gases are photolysis and/or condensation onto grains. Their estimated photochemical lifetimes range from a few minutes for alkali iodides to a few hours for alkali fluorides. Condensation is apparently the only loss process for elemental iodine. On the basis of elemental abundances and photochemical lifetimes, we recommend searching for gaseous KCl, NaF, LiF, LiCl, RbF, RbCl, CsF, and CsCl around volcanic vents during eruptions. Based on abundance considerations and observations of brown dwarfs we also recommend a search of Io's extended atmosphere and the Io plasma torus for neutral and ionized Li, Cs, Rb, and F.  相似文献   

17.
18.
A special stressed annular polishing technique is proposed to mill the off-axis aspheric sub-mirrors of a large segmented mirror with an annular polishing machine. Based on the basic principle of stressed annular polishing technique, a set of special stressing mechanisms are designed to convert milling the aspheric surfaces of sub-mirrors with different off-axis distances into milling the spherical surfaces with identical radii of curvature, so that they can be pol- ished simultaneously on a continuous polishing machine. It took about contin- uous 40 hours to polish a scaled-down mirror of the planning Chinese Future Giant Telescope (CFGT) using this technique. This mirror has the 330 mm di- ameter, 3.6 m off-axis distance, and the 21.6 m radius of curvature, and its max- imum asphericity is 16 micron. The experiment shows that this method has a high effciency, suits batch manufacturing, especially the batch manufacturing of aspheric sub-mirrors of the segmented primary mirror of an extremely large aperture telescope.  相似文献   

19.
Modern-day synoptic-scale eastern Mediterranean climatology provides a useful context to synthesize the diverse late Pleistocene (60–12 ka) paleohydrologic and paleoenvironmental indicators of past climatic conditions in the Levant and the deserts to its south and east. We first critically evaluate, extract, and summarize paleoenvironmental and paleohydrologic records. Then, we propose a framework of eastern Mediterranean atmospheric circulation features interacting with the morphology and location of the southeast Mediterranean coast. Together they strongly control the spatial distribution of rainfall and wind pattern. This cyclone–physiography interaction enforces the observed rainfall patterns by hampering rainfall generation south and southeast of the latitude of the north Sinai coast, currently at 31°15′.The proposed framework explains the much-increased rains in Lebanon and northern Israel and Jordan as deduced from pollen, rise and maintenance of Lake Lisan, and speleothem formation in areas currently arid and semiarid. The proposed framework also accounts for the southward and eastward transition into semiarid, arid, and hyperarid deserts as expressed in thick loess accumulation at the deserts' margins, dune migration from west to east in the Sinai and the western Negev, and the formation of hyperarid (< 80 mm yr− 1) gypsic–salic soils in the southern Negev and Sinai. Our climatic synthesis explains the hyperarid condition in the southern Negev, located only 200–250 km south of the much-increased rains in the north, probably reflecting a steeper rainfall gradient than the present-day gradient from the wetter Levant into its bordering southern and eastern deserts.At present, the rainiest winter seasons in Lebanon and northern and central Israel are associated with more frequent (+ 20%), deeper Cyprus Lows traversing the eastern Mediterranean at approximately the latitude of southern Turkey. Even these wettest years in northern Israel do not yield above average annual rainfall amounts in the hyperarid southern Negev. This region is mainly influenced by the Active Red Sea Troughs that produce only localized rains. The eastern Mediterranean Cyprus Lows also produce more dust storms and transport higher amounts of suspended dust to the loess area than any other atmospheric pattern. Concurrent rainfall and dust are essential to the late Pleistocene formation of the elongated thick loess zone along the desert northern margin. Even with existing dust storms, the lack of rain and very sparse vegetation account for the absence of late Pleistocene loess sequences from the southern Negev and the formation of hyperarid soils.When the north Sinai coast shifted 30–70 km northwest due to last glacial global sea level lowering, the newly exposed coastal areas supplied the sand and dust to these active eastern Mediterranean cyclones. This enforced the latitude of the northern boundary of the loess zone to be directly due east of the LGM shoreline. This shift of coast to the northwest inhibited rainfall in the southern Levant deserts and maintained their hyperaridity. Concurrently, frequent deep eastern Mediterranean Cyprus Lows were funneled along the northern Mediterranean increasing (probably doubling) the rains in central and northern Israel, Lebanon, southwestern Syria and northern Jordan. These storms and rains formed lakes, forests, and speleothems only a short distance north of the deserts in the southern Levant.  相似文献   

20.
Interferometry in the visible provides milliarcsecond spatial resolution and thus has been used for studying the circumstellar environment of active hot stars. In this paper I will illustrate how the visibility modulus and phase can be used to better constrain the physics of Be disks through results from the VLA, the MkII and the GI2T interferometers. I will insist on the importance and the potential of coupling high angular resolution with high spectral resolution to the study of Be shells. Finally I will present a possible study of the circumstellar disk of Be stars using the VLTI. This revised version was published online in July 2006 with corrections to the Cover Date.  相似文献   

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