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1.
收集了142个射电类星体(28个射电宁静类星体、114个射电噪类星体)、43个核占优型射电类星体、82个瓣占优型射电类星体和80个Seyfert星系的样本,基于Logistic非线性回归分析的方法对红移和热光度、黑洞质量、5 GHz射电光度、爱丁顿吸积率、核主导参数R的关系进行研究,拟合出相应的演化曲线,得到如下结论:(1)射电类星体的演化是从射电噪类星体(RLQ)演化到射电宁静类星体(RQQ),当演化到一定阶段射电类星体过渡到Seyfert星系;(2)核占优型射电类星体(CDQ)和瓣占优型射电类星体(LDQ)之间并没有明显的随红移演化. 相似文献
2.
以Kang等的星系形成的半解析模型为基础,研究星系和中心大质量黑洞的共同形成和演化.假设类星体的活动性由星系并合引起,通过引入黑洞吸积率,确定了红移区间0z4.5的类星体的热光度函数,并分别从爱丁顿比率、黑洞质量函数和两点相关函数3个方面对模型进行限制,模型预言的光度函数能在整个红移、整个光度范围内与观测相符合.结果显示,常数爱丁顿比率不能很好地描述黑洞吸积,爱丁顿比率需要在一定红移范围内随红移增加;星系主并合是触发类星体活动性的有效机制,而次并合只对低光度和中等光度的类星体有影响,对高光度类星体影响很小;在z=1.0处,极高光度的类星休比其他类星体具有更强的成团性. 相似文献
3.
通过搜集了457个活动星系核样本,根据活动星系核的演化实质是指宇宙时标上的变化,讨论了红移量与活动星系核演化的关系,最终证明了活动星系核的演化分为两个序列:(1)从类星体到Seyfert星系之间的演化;(2)平谱射电类星体(FSRQ)—BL Lac天体—射电星系(RG)的演化。 相似文献
4.
本文对前人的类星体光学演化函数进行改进，使其适用于更大的红移范围，可达Ｚ＝３以上。其物理考虑是：一方面包括核心黑洞质量和吸积率变化而引起光度演化；另一方面在高红移时类星体诞生所引起的密度演化，并且这种演化率与光度有关。这种型式更利于与类星体演化的动力学模型相衔接。新的演化函数通过三种检验来决定，即（１）类星体直到ｍ＝２２＾ｍ．０的星等计数，（２）以ΔＺ＝０．１为间隔的红移分布，（３）Ｚ〉２的类星体 相似文献
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黑洞自旋及其参量能提供黑洞合并及吸积的信息。从文献资料中收集了112个Blazar源,这些源包含了67个FR II射电星系(RG),11个FR II射电噪类星体(RLQ),27个核占优星系(CD)。通过样本数据研究黑洞自旋能量与红移的相关性。研究结果表明:(1)112个Blazar的黑洞自旋能量与红移存在相关性,尤其在爱丁顿磁场条件下(B=BEDD),黑洞自旋能量与红移的相关性最为明显;(2)FR II射电星系(RG)、FR II射电噪类星体(RLQ)、核占优星系(CD)的黑洞自旋能量在3种磁场条件下(B=BEDD,B=104G,B∝j)与红移的相关性强弱上存在差异,但总体趋势较为相似,均呈现正比关系;(3)黑洞自旋能量与红移的强相关性表明,黑洞自旋能量在一定程度上给出黑洞并合与吸积的信息。这些研究结果与其他人用其他方法获得的结果是一致的。 相似文献
7.
收集了117个类星体(20个射电宁静类星体和97个射电噪类星体)的红移、热光度、H_β发射线宽度、5 100 A的单色光度、射电噪度.利用反响映射法计算了样本的黑洞质量和爱丁顿比,利用总的5 GHz流量密度计算出射电光度.分析了它们之间的相关性,得到的结论如下:(1)射电宁静类星体的黑洞质量和热光度、射电噪度、射电光度之间具有弱相关性,而射电噪类星体黑洞质量和热光度、射电噪度、射电光度之间具有强相关性;(2)射电宁静类星体热光度和射电光度、5 100 A的单色光度之间具有弱的相关性,而射电噪类星体热光度和射电光度、5 100 A的单色光度之间具有强的相关性;(3)射电宁静和射电噪类星体的黑洞质量、发射线宽度和爱丁顿比分布有差异.基于这些结果得到:射电宁静和射电噪类星体发射线宽度的差异可能是导致它们黑洞质量不同的原因;射电宁静和射电噪类星体本质的不同是由于内秉物理性质的不同造成的;黑洞质量、黑洞自旋、爱丁顿比和寄主星系形态是解释射电噪度起源和双峰状分布的重要参量;射电喷流和盘的吸积率之间具有紧密的关系. 相似文献
8.
研究了低红移SDSS类星体(0.025z0.5)的辐射效率。首先利用类星体中心黑洞的质量估计,通过薄盘吸积模型估计了每一个类星体的吸积率。其次根据光学波段的观测光度,利用经验的类星体全波段模板谱估计了每个类星体的热光度。最后由估计的吸积率和热光度得到了每个类星体的辐射效率。发现低红移SDSS类星体的辐射效率与黑洞质量强相关,并满足ε∝M0.63。这一结果与Davis和Laor(2011)对PG类星体样本得到的结果一致。进一步讨论由于辐射效率估计中各种假设可能引入的偏差及其对ε与M关系的可能影响。 相似文献
9.
在此工作中,分析了一个类星体样本的吸收线红移和发射线红移之间的关系。结果表明这两类红移之间存在显著的相关。主要结论:a)反常吸收线红移的主要部分是宇宙学红移;b)吸收体相对于类星体的运动是弱的;c)结果表明产生这些反常吸收线红移的吸收体位于类星体寄主星系或者类星体内部并且朝着类星体运动。 相似文献
10.
在“等级式成团”（hierarchical clustering)宇宙学演化框架下,早型星系（E／SO）的形成和演化不是如经典的“整体塌缩”（monolithic collapse)演化模式所描述的是由高红移处的短时间剧烈恒星形成过程一次性完成的;相反,它们可能是在大尺度结构形成过程中由盘星系间的相互合并演化而来,特别是对于质量相当的盘星系间的剧烈合并过程。目前的数值模拟和高分辨成像观测都已证实了这种可能性,而且红移巡天的结果也更多地支持这种演化模式。在此提出一个星系合并过程中核区星暴和中心黑洞共生演化的模型,来解释由空间望远镜（HST）和地面CCD高分辨测光所得的早型星系“黑洞／核球”统计线性相关,也即中心黑洞质量约为其核球体质量的0．6％;同时,该演化模型还可以进一步合理地解释在类星体的近红外成像观测中统计得出的相似的线性相关性,即类星体中心亮度与其母星系质量成正比。并给出此模型计算的极限情况和模型的解析估计。 相似文献
11.
L. S. Marochnik 《Astrophysics and Space Science》1983,89(1):61-75
The solar system's position in the Galaxy is an exclusive one, since the Sun is close to the corotation circle, which is the place where the angular velocity of the galactic differential rotation is equal to that of density waves displaying as spiral arms. Each galaxy contains only one corotation circle; therefore, it is an exceptional place. In the Galaxy, the deviation of the Sun from the corotation is very small — it is equal to ΔR/R ⊙≈0.03, where ΔR=R c ?R ⊙,R c is the corotation distance from the galactic center andR ⊙ is the Sun's distance from the galactic center. The special conditions of the Sun's position in the Galaxy explain the origin of the fundamental cosmogony timescalesT 1≈4.6×109 yr,T 2?108 yr,T 3?106 yr detected by the radioactive decay of various nuclides. The timescaleT 1 (the solar system's ‘lifetime’) is the protosolar cloud lifetime in a space between the galactic spiral arms. The timescaleT 2 is the presolar cloud lifetime in a spiral arm.T 3 is a timescale of hydrodynamical processes of a cloud-wave interaction. The possibility of the natural explanation of the cosmogony timescales by the unified process (on condition that the Sun is near the state of corotation) can become an argument in favour of the fact that the nearness to the corotation is necessary for the formation of systems similar to the Solar system. If the special position of the Sun is not incidental, then the corotation circles of our Galaxy, as well as those of other galaxies, are just regions where situations similar to ours are likely to be found. 相似文献
12.
Yoshio Kubo 《Celestial Mechanics and Dynamical Astronomy》1982,26(1):97-112
Perturbations in the motion of the Moon are computed for the effect by the oblateness of the Earth and for the indirect effect of planets. Based on Delaunay's analytical solution of the main problem, the computations are performed by a method of Fourier series operation. The effect of the oblateness of the Earth is obtained to the second order, partly adopting an analytical evaluation. Both in longitude and latitude are found a few terms whose coefficient differs from the current lunar ephemeris based on Brown's theory by about 0.01. While, concerning the indirect effect of planets, several periodic terms in the current ephemeris seem to have errors reaching 0.05.As for the secular variations of
and due to the figure of the Earth and the indirect effect of planets, the newly-computed values agree within 1/cy with Brown's results reduced to the same values of the parameters. Further, the accelerations in the mean longitude,
and caused by the secular changes in the eccentricity of the Earth's orbite and in the obliquity of the ecliptic are obtained. The comparison with Brown shows an agreement within 0.3/cy2 for the former cause and 0.02/cy2 for the latter. An error is found in the argument of the principal term for the perturbations due to the ecliptic motion in the current ephemeris.Proceedings of the Conference on Analytical Methods and Ephemerides: Theory and Observations of the Moon and Planets. Facultés universitaires Notre Dame de la Paix, Namur, Belgium, 28–31 July, 1980. 相似文献
13.
E. L. Ruskol 《Earth, Moon, and Planets》1973,6(1-2):190-201
It is suggested that the overall early melting of the lunar surface is not necessary for the explanation of facts and that
the structure of highlands is more complicated than a solidified anorthositic ‘plot’. The early heating of the interior of
the Moon up to 1000K is really needed for the subsequent thermal history with the maximum melting 3.5 × 109 yr ago, to give the observed ages for mare basalts. This may be considered as an indication that the Moon during the accumulation
retained a portion of its gravitational energy converted into heat, which may occur only at rapid processes. A rapid (t < 103 yr) accretion of the Moon from the circumterrestrial swarm of small particles would give necessary temperature, but it is
not compatible with the characteristic time 108 yr of the replenishment of this swarm which is the same as the time-scale of the accumulation of the Earth. It is shown that
there were conditions in the circumterrestial swarm for the formation at a first stage of a few large protomoons. Their number
and position is evaluated from the simple formal laws of the growth of satellites in the vicinity of a planet. Such ‘systems’
of protomoons are compared with the observed multiple systems, and the conclusion is reached that there could have been not
more than 2–3 large protomoons with the Earth. The tidal evolution of protomoon orbits was short not only for the present
value of the tidal phase-lag but also for a considerably smaller value.
The coalescence of protomoons into a single Moon had to occur before the formation of the observed relief on the Moon. If
we accept the age 3.9 × 109 yr for the excavation of the Imbrium basin and ascribe the latter to the impact of an Earth satellite, this collision had
to be roughly at 30R, whereR is the radius of the Earth, because the Moon at that time had to be somewhere at this distance. Therefore, the protomoons
had to be orbiting inside 20–25R, and their coalescence had to occur more than 4.0x109 yr ago. The energy release at coalescence is equivalent to several hundred degrees and even 1000 K. The process is very rapid
(of the order of one hour). Therefore, the model is valid for the initial conditions of the Moon. 相似文献
14.
In this paper we first emphasize why it is important to know the successive zonal harmonics of the Sun's figure with high
accuracy: mainly fundamental astrometry, helioseismology, planetary motions and relativistic effects. Then we briefly comment
why the Sun appears oblate, going back to primitive definitions in order to underline some discrepancies in theories and to
emphasize again the relevant hypotheses. We propose a new theoretical approach entirely based on an expansion in terms of
Legendre's functions, including the differential rotation of the Sun at the surface. This permits linking the two first spherical
harmonic coefficients (J
2 and J
4) with the geometric parameters that can be measured on the Sun (equatorial and polar radii). We emphasize the difficulties
in inferring gravitational oblateness from visual measurements of the geometric oblateness, and more generally a dynamical
flattening. Results are given for different observed rotational laws. It is shown that the surface oblateness is surely upper
bounded by 11 milliarcsecond. As a consequence of the observed surface and sub-surface differential rotation laws, we deduce
a measure of the two first gravitational harmonics, the quadrupole and the octopole moment of the Sun: J
2=−(6.13±2.52)×10−7 if all observed data are taken into account, and respectively, J
2=−(6.84±3.75)×10−7 if only sunspot data are considered, and J
2=−(3.49±1.86)×10−7 in the case of helioseismic data alone. The value deduced from all available data for the octopole is: J
4=(2.8±2.1)×10−12. These values are compared to some others found in the literature.
Supplementary material to this paper is available in electronic form at http://dx.doi.org/10.1023/A:1005238718479 相似文献
15.
B. P. Kondratyev 《Solar System Research》2013,47(1):1-10
A two-component theoretical model of the physical libration of the Moon in longitude is constructed with account taken of the viscosity of the core. In the new version, a hydrodynamic problem of motion of a fluid filling a solid rotating shell is solved. It is found that surfaces of equal angular velocity are spherical, and a velocity field of the fluid core of the Moon is described by elementary functions. A distribution of the internal pressure in the core is found. An angular momentum exchange between the fluid core and solid mantle is described by a third-order differential equation with a right-hand side. The roots of a characteristic equation are studied and the stability of rotation is proved. A libration angle as a function of time is found using the derived solution of the differential equation. Limiting cases of infinitely large and infinitely small viscosity are considered and an effect of lag of a libration phase from a phase of action of an external moment of forces is ascertained. This makes it possible to estimate the viscosity and sizes of the lunar fluid core from data of observations. 相似文献
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M. V. Samokhin 《Astrophysics and Space Science》1979,62(1):159-183
In order to understand the reason of the existence of the electric field in the magnetosphere, and for the theoretical evaluation of its value, it is necessary to find the solution of the problem of determination of the magnetosphere boundary form in the frameworks of the continuum medium model which takes into account part of the magnetospheric plasma movement in supporting the magnetospheric boundary equilibrium. A number of problems for finding the distribution of the pressure, the density, the magnetic field and the electric field on the particular tangential discontinuity is considered in the case when the form of discontinuity is set (the direct problem) and a number of problems for finding the form of the discontinuity and the distribution of the above-mentioned physical quantities on the discontinuity is considered when the law of the change of the external pressure along the boundary is set (for example, with the help of the approximate Newton equation). The problem which is considered here, which deals with the calculation of the boundary form and with the calculation of the distribution of the corresponding physical quantities on the discontinuity of the 1st kind for the compressible fluid with the magnetic field with field lines which are perpendicular to the plane of the flow in question, concerns the last sort of problems. The comparison of the results of the calculation with the data in the equatorial cross-section of the magnetosphere demonstrates that the calculated form of the boundary, the value of the velocity of the return flow and the value of the electric field on the magnetopause, agree satisfactorily with the observational data. 相似文献
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