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在丽江高美古前期选址工作的基础上^[1-2],二期选址的望远镜地面高度的确定工作于2000年11月3日至2000年12月16日进行,采用30m铁塔的温度脉动测量装置,对6#选址观测点的近地面大气湍流进行反复多次测量,得到近地面不同高度(4-30m和8-22m)上每夜温度结构系数CT^2的平均值,对观测取得的资料作进一步处理和分析,得到高美古6#观测点的望远镜地面高度为13~15m。 相似文献
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利用乌鲁木齐南山站25m望远镜6cm系统对观测站周边的地面辐射做了仔细的观测。发现该系统对地面辐射的响应在天空的不同方向有显著的变化。望远镜俯仰为8°时,南方由于高山的影响,对地面辐射的响应已经饱和;甚至在望远镜指向高俯仰(60°)时,总功率响应随不同方位的起伏也可达到0.3K,大于银道面0.01~0.1K的响应,因此它对射电天文观测有显著的影响。根据这些观测数据,建立了6cm系统在不同方向处对地面辐射的响应模型。此模型能够大致描述地面辐射的特征,但尚不能用来完全消除地面辐射的影响。 相似文献
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空间太阳望远镜1m主镜支撑结构的研究 总被引:8,自引:0,他引:8
本文对正在预研中的空间太阳望远镜的关键部件之一1m主镜,提出一种合理的支撑结构系统,此系统可以兼顾空间太阳望远镜光学系统的地面装校调试的有效性和火箭发射力学环境中的安全性以及入轨后正常观测时的高精度性。 相似文献
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激光测月中的地球和月球参考架 总被引:2,自引:0,他引:2
本讨论了激光测月 算地面台站坐标和月面反射器的月面坐标过程中初值的影响及迭代求解的稳定性问题。并指出影响地面台站坐标中地心经度分量的精度有两方面的原因,一是平差时采用的UT1值有误差,二是月球的赤经误差,后将引起地面台站产生一个沿经度方向的系统旋转,而这是所采用的月球星历表的误差所致。通过实例迭代运算表明, 测站坐标结果可以收敛到2cm左右,月面反射器在月面柱坐标中的σ和Z分量的结果可以稳定在10cm左右,而其λ分量目前只能达到米级。 相似文献
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1m红外太阳塔是我国未来重点发展的地面太阳观测设备,本文的所有工作均围绕着与此相关的红外波段太阳观测技术方法展开。1.针对望远镜实验平台-云台太阳光谱仪,建立了光谱仪分光流量,工用多种实验手段验证了其可靠性。利用该模型计算了Fe Ⅰ1.56μm红外太阳光 谱的分光流量,分析了实验观测的可行性及改进方案。2.针对探测器实验平台-PtSi红外焦平面阵列相机,建立了FeⅠ1.56μm光谱观测信噪比模型,模拟了各种噪声对观测的影响。在此基础上,在国内首次成功进行了FeⅠ1.56μm红外太阳光谱的面阵观测实验。3.在红外观测实验所处的高背景低对比度条件下,讨论了红外太阳光谱观测的图像处理方法,分析了观测中出现的干涉条纹的来源及解决办法,初步建立起了一整套红外太阳光谱与成像的定标方法和图像处理方法。4.首次利用PVA材料,设计研制了一套FeⅠ1.56μm近红外Stokes参量偏振仪,并将该偏振仪安装在美国国立天文台McMath望远镜上进行了观测实验。针对一太阳黑子,通过扫描进行了二维的Stokes参量观测。同时建立了一套从Stokes参量反演磁矢量场的方法,并将反演的结果与怀柔太阳磁场望远镜的观测结果进行了比对。5.针对1m红外太阳塔的太阳光谱仪系统,给出了垂直多波段光谱仪和红外大色散光谱仪的光、机初步设计。6.针对1m红外太阳塔的科学目标,提出了多波段光谱仪探测器系统方案,对红外大色散光谱仪所使用的红外探测器也进行了初步方案设计。 相似文献
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苏定强 《紫金山天文台台刊》2003,(1)
目前 ,已有 1 0架口径 8~ 1 0m的地面大望远镜建成并投入科学观测。在近红外波段 ,自适应光学和干涉术已在大望远镜上获得成功。Hubble空间望远镜发射至今已逾 1 2年。为了研究早期宇宙 ,探测类地行星等 ,2 0 0 2年 9月NASA已与TWR公司签约 ,研制口径≥ 6m的下一代空间望远镜JWST ,计划2 0 1 0年发射。许多口径 30~ 1 0 0m的地面未来巨型望远镜FGT项目已经提出。本报告 ,也介绍了我国正在研制或预研中的三个大项目 :LAMOST、FAST和SST ,这些项目虽较小 ,但完成后都会对天文学的一个方面作出有份量的贡献。最后 ,报告人建议我国参与到与国外合作研制FGT或NGST的工作中 ,特别强调要有天文学家和工程专家参与进去 相似文献
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A. M. Boichenko 《Astrophysics》2004,47(1):134-142
Observational data on the dynamics of stars in the neighborhood of the sun indicate the existence of a third integral besides the integrals of the angular momentum and energy. The Poincaré integral is proposed as a third integral. The consequences of this assumption are derived and compared with available astrophysical data. 相似文献
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介绍和论述了在后牛顿引力理论(PPN形式)中在优越参考系和非优越参考系中经过参数化后引力常数变化对地球自转产生的效应,其中特别重点介绍了年周期变化的效应。此外也将理论结果同观测结果相对比。 相似文献
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Range of values of the Sun's mass quadrupole moment of coefficient J2 arising both from experimental and theoretical determinations enlarge across literature on two orders of magnitude, from
around 10-7 until to 10-5. The accurate knowledge of the Moon's physical librations, for which the Lunar Laser Ranging data reach an outstanding precision
level, prove to be appropriate to reduce the interval of J2 values by giving an upper bound of J2. A solar quadrupole moment as high as 1.1 10-5 given either from the upper bounds of the error bars of the observations, or from the Roche's theory, is not compatible with
the knowledge of the lunar librations accurately modeled and observed with the LLR experiment. The suitable values of J2 have to be smaller than 3.0 10-6.
As a consequence, this upper bound of 3.0 10-6 is accepted to study the impact of the Sun's quadrupole moment of mass on the dynamics of the Earth-Moon system. Such as
effect (with J2 = 5.5±1.3 × 10-6) has been already tested in 1983 by Campbell & Moffat using analytical approximate equations, and thus for the orbits of
Mercury, Venus, the Earth and Icarus. The approximate equations are no longer sufficient compared with present observational
data and exact equations are required. As if to compute the effect on the lunar librations, we have used our BJV relativistic
model of solar system integration including the spin-orbit coupled motion of the Moon. The model is solved by numerical integration.
The BJV model stems from general relativity by using the DSX formalism for purposes of celestial mechanics when it is about
to deal with a system of n extended, weakly self-gravitating, rotating and deformable bodies in mutual interactions.
The resulting effects on the orbital elements of the Earth have been computed and plotted over 160 and 1600 years. The impact
of the quadrupole moment of the Sun on the Earth's orbital motion is mainly characterized by variations of
,
, and
. As a consequence, the Sun's quadrupole moment of mass could play a sensible role over long time periods of integration of
solar system models.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
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Wu Lin-xiang 《Chinese Astronomy and Astrophysics》1992,16(4):427-433
By means of a simple relation between the velocity v of the fluid particle and the velocity vf of the photospheric footpoint of the magnetic field line vz and Bz being respectively the components of v and the magnetic field B normal to the photospheric surface, it is shown formally that through the phtospheric surface the transport of all the quantities attributed to the magnetic field, such as the magnetic flux, the magnetic energy and the helicity, is independent of vz, and vf is the only kinematical quantity on which the transport depends. In addition, in the neighborhood of the neutral line the velocity vl of the moving curve of constant Bz is found to be equal approximately to the component of v or vf in the direction of vl. Since vl can be measured or extimated, so can the components of v and vf near the neutral line. 相似文献
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I. Ilyin K.G. Strassmeier M. Woche F. Dionies I. Di Varano 《Astronomische Nachrichten》2011,332(8):753-758
We present the design concept of the spectropolarimeter for the high‐resolution echelle spectrograph PEPSI tobe installed at the 2 × 8.4 m Large Binocular Telescope (LBT) in Arizona. We discuss the optical key elements, the principles of operations of the instrument and its instrumental polarization effects (© 2011 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim) 相似文献
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Arbab I. Arbab 《Astrophysics and Space Science》2008,314(1-3):35-39
We have developed a cosmological model for the Earth rotation and planetary acceleration that gives a good account (data)
of the Earth astronomical parameters. These data can be compared with the ones obtained using space-base telescopes. The expansion
of the universe has shown to have an impact on the rotation of planets, and in particular, the Earth. The expansion of the
universe causes an acceleration that is exhibited by all planets. 相似文献
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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
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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
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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