射电源的谱指数

文章研究了162个射电源,其中包括了47个BL Lacs ,21个galaxies ,94个平谱射电类星体( FSRQs ) ,这些源是通过Michigan大学的26m的射电望远镜观测的。大多数源都包含了3个波段的观测数据:4 .8GHz ,8GHz和14 .5GHz。文中计算了3个子类的平均的流量密度,并且得到了相应的谱指数(αwei) ,αBL=0 .08±0 .28 ,αGAL=-0 .91±0 .32 ,αFSRQ=-0 .14±0 .4。同时也讨论了这些源的射电性质,其中包含了谱指数,流量密度和红移之间的关系,流量密度和谱指数之间的关系。     

平谱射电类星体3C 454.3中长周期有效谱指数特性研究

耀变体是一种非常活跃的活动星系核,研究它的有效谱指数是认识其内部结构和辐射机制的有效方法。文中数据来源于目前已公布的SMARTS(Small and Medium Aperture Research Telescope System)数据库,共682组具有B, V, R, J和K波段的准同时性的观测数据,用LSP(LombScargle Periodogram)方法研究了其有效谱指数的特性,研究结果表明,3C 454.3光学和红外波段光变之间呈正相关;光学和红外波段光变存在两个主导周期,分别约为1.2年和4.5年;双黑洞结构模型中双黑洞质量比约为2∶1。     

AO 0235+164射电波段宽带谱指数周期性变化的研究

收集了AO 0235+164天体射电4.8 GHz和14.5 GHz波段的光变测量数据,并获得了长期的光变曲线,从光变曲线可以看出其活动是非常剧烈的。利用Jurkevich方法和自相关函数方法分别对AO 0235+164射电波段宽带谱指数进行周期性分析,并对流量和谱指数进行相关性分析,研究结果表明:(1)AO 0235+164天体射电波段4.8 GHz～14.5 GHz对应的宽带谱指数,可能存在5.30年的光变周期,与Liu等人用功率谱法在射电波段发现其流量密度可能存在5.59±0.47年的光变周期基本吻合;(2)宽带谱指数与流量密度之间存在相关性。     

Blazar多波段有效谱指数关系研究

从相关文献中获得Fermi耀变体(blazar)的射电(R)1.4 GHz、光学(O)4.68×10~(14)Hz、X-ray(X)1 ke V和γ-ray(γ)1 Ge V辐射流量密度,计算了上述波段两两之间的6个有效谱指数α_(RO)、α_(RX)、α_(Rγ)、α_(OX)、α_(Oγ)、α_(Xγ).研究了blazar总样本及其子类FSRQ(Flat Spectral Radio Quasar),蝎虎天体(BL Lac)含高同步峰频BL Lac(HBL)和低同步峰频BL Lac(LBL)样本的任意两个有效谱指数之间的关系.结果表明:(1)除HBL样本及α_(OX)与α_(Rγ)之间关系外,两两有效谱指数之间均存在较强的相关,这种相关可用4个波段能谱分布的结构关系得到解释;(2)在有效谱指数相关的散点图中,FSRQ与LBL分布在相同的区域,但HBL与FSRQ(LBL)分布在不同的区域;(3)在不同的有效谱指数相关散点图中,HBL与FSRQ(LBL)分布的分离程度(区分度)不相同,这种区分度与决定2个有效谱指数的频率有关.     

AO0235＋164射电波段宽带谱指数周期性变化的研究

收集了AO0235＋164天体射电4．8GHz和14．5GHz波段的光变测量数据,并获得了长期的光变曲线,从光变曲线可以看出其活动是非常剧烈的。利用Jurkevieh方法和自相关函数方法分别对AO0235＋164射电波段宽带谱指数进行周期性分析,并对流量和谱指数进行相关性分析,研究结果表明：（1）AO0235＋164天体射电波段4．8GHz-14．5GHz对应的宽带谱指数,可能存在5．30年的光变周期,与Liu等人用功率谱法在射电波段发现其流量密度可能存在5．59±0．47年的光变周期基本吻合;（2）宽带谱指数与流量密度之间存在相关性。     

射电选和X射线选BL Lacertae天体的射电性质

收集了射电选和X射线选BL Lac天体的射电数据(包括核和延展光度), 并计算了它们的核主导系数R.研究显示: 射电选BL Lac(RBLs)天体的总射电光度是X射线选BL Lac(XBLs)天体的2个量级.详细分析得到这种差别主要是来自于核光度的差别因为延展光度差别只有1个量级.研究RBLs和XBLs的核(延展元)光度与核主导系数之间的关系, 发现延展元光度与核主导系数负相关, 而核(总)光度几乎与核主导系数没有相关.     

活动星系核X射线本征谱指数与爱丁顿比关系的研究进展

活动星系核是中央核区有剧烈活动的(河外)星系总称。随着观测技术不断进步,人们对活动星系核的研究越来越多,对其理解也越来越深刻。总结整理了近年来对活动星系核X射线本征谱指数与爱丁顿比关系的观测结果,揭示出如下V形关系图像:随着爱丁顿比由大变小,X射线本征谱指数与爱丁顿比由存在正相关关系,转变为存在负相关关系。一般认为,这一观测现象反映了随着吸积率的降低,黑洞吸积模式发生了变化,由高吸积率时的标准薄盘吸积变为低吸积率时的辐射无效吸积流。这表明,基于标准薄盘的最基本的活动星系核统一模型虽然能够成功地解释较高光度活动星系核的很多观测现象,但却需要做一定的修正,以解释低光度活动星系核的一些观测性质。同时,将来有希望利用这一相关关系估算活动星系核一些重要参数,如中央超大黑洞质量、吸积率等,从而帮助人们更好地理解活动星系核的辐射机制和演化过程。最后对这一领域的研究进行了总结与展望。     

γ噪Blazar天体的复合谱指数研究

收集了66个有γ射线噪的Blazar在高态下的多波段流量数据,研究了Blazar复合谱指数之间的相关性.分析了BL Lac天体和平谱射电类星体(FSRQs) 复合谱指数之间的相关性.结果表明(1)高态下Blazar的复合谱指数与αr,ir与αir,γ、αr,ir 与αo,γ、αr,o与αo,x、αr,o与αo,γ之间有强相关性,αr,x与αx,γ之间有强负相关性.(2)平谱射电类星体(FSRQs)在高态下αr,o与αo,x、αr,o与αo,γ有强相关性.(3)BL Lac天体在高态时αr,o与αo,γ之间有强相关性,αr,x与αx,γ、αir,x与αx,γ有强负相关性.(4)γ射线很可能产生于同步自康普顿(SSC)过程.     

一种研究空间谱指数变化的新方法

本文介绍了一种用于射电天文学谱指数研究的新方法－双色微分图解法，在进行谱指数分析所使用的多频图中，一般存在有不同的背景分量及大尺度缓变分量，使用本文介绍的新万法得到的结果不受这两种成分的影响，这种新方法还可用于热及非热射电辐射分离，本文还给出了应用实例，首次精确计算了SNRG78．2＋2．1的多频空间谱指数分布。     

费米耀变体峰值参量、康普顿主导、谱指数之间相关性的研究

使用一个具有(准)同时性宽带能谱数据的Fermi耀变体样本,对其进行同步和逆康普顿峰峰值参量、康普顿主导以及高能谱指数等参量之间的相关性分析,以获得耀变体整体和子类相关性之间差异的来源、耀变体喷流中粒子冷却的主导机制和电子能谱形状等方面的解释。分析结果表明,耀变体的整体相关性至少有部分来自平谱射电类星体和蝎虎天体由于物理性质不同而在参数平面上具有不同分布区域这一特性贡献,因此针对两个子类的相关性分析是必需的。蝎虎天体为快冷却机制,谱指数图的结果支持对数抛物线形状的电子能谱。     

A thermodynamic model of high temperature lava vaporization on Io

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.     

Instructions for authors

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,     

Alkali and halogen chemistry in volcanic gases on Io

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.     

The climatic and physiographic controls of the eastern Mediterranean over the late Pleistocene climates in the southern Levant and its neighboring deserts

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.     

Active hot star shells

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.     

Fitting X-ray Afterglow Light curves of Gamma-ray Bursts by Using the Magnetar Energy Injection Model

The central compact object for some gamma-ray bursts (GRBs) may be a strongly magnetized millisecond pulsar. It can inject energy to the outer shock of the GRB by through the magnetic dipole radiation, and therefore causes the shallow decay of the early afterglow. Recently, from a large number of GRB X-ray afterglows observed by Swift/XRT(X-ray telescope), it is revealed that many of them exhibit the shallow decay about 10²∼10⁴ s after the burst prompt emission. We have fitted the X-ray afterglow light curves of 11 GRBs by using the energy injection model of a magnetar with the rotation period in the millisecond order of magnitude. The obtained result shows the validity and universality of the magnetar energy injection model in explaining the shallow decay of afterglows, and simultaneously provides some constraints on the magnetic field strength and rotation period of the central magnetar.     

Born–Infeld type phantom model in the ω–ω′ plane

In this paper, we investigate the dynamics of Born–Infeld (B–I) phantom model in the ω–ω′ plane, which is defined by the equation of state parameter for the dark energy and its derivative with respect to N (the logarithm of the scale factor a). We find the scalar field equation of motion in ω–ω′ plane, and show mathematically the property of attractor solutions which correspond to ω _φ ∼−1, Ω _φ =1, which avoid the “Big rip” problem and meets the current observations well.      

Shear and vorticity in a combined Einstein-Cartan-Brans-Dicke inflationary lambda-Universe

A combined BCDE (Brans-Dicke and Einstein-Cartan) theory with lambda-term is developed through Raychaudhuri’s equation, for inflationary scenario. It involves a variable cosmological constant, which decreases with time, jointly with energy density, cosmic pressure, shear, vorticity, and Hubble’s parameter, while the scale factor, total spin and scalar field increase exponentially. The post-inflationary fluid resembles a perfect one, though total spin grows, but the angular speed does not (Astrophys. Space Sci. 312: 275, 2007d).