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1.
311P/PANSTARRS是一颗活动小行星, 具有小行星和彗星的双重特征, 是中国``天问二号''的探测目标之一. 311P/PANSTARRS直径较小, 约为400 m, 非引力效应可能会对其长期动力学演化产生较大的影响. 通过假定不同表面组分, 研究了Yarkovsky效应对311P/PANSTARRS轨道演化的影响, 讨论了密近交汇、 非破坏性碰撞和YORP (Yarkovsky-O''Keefe-Radzievskii-Paddack)效应等非引力效应, 计算了小行星与大行星密近交汇及碰撞概率, 估计了311P/PANSTARRS达到自转周期分裂极限的时标. 模拟结果显示与纯引力模型相比, Yarkovsky效应可能会加快311P/PANSTARRS离开当前共振区域, 大约在10Myr以后311P/PANSTARRS会离开当前所在共振带, 在表面覆盖风化层的情况下有机会通过v6长期共振成为越火小行星; 在考虑YORP效应的情况下, 311P/PANSTARRS在2 Myr时标内可达到自转周期分裂极限; 在考虑Yarkovsky效应及YORP效应等因素的情况下, 311P/PANSTARRS在10 Myr时标内仍可保持其动力学稳定性, 且YORP效应不会显著影响其半长径偏移量. 相似文献
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小行星(234)Barbara 为彼得(Peters)在1883年所发现.惕乾曾根据1883,85,86年三次冲日的观测,并计算木星对它的摄动,求得一组轨道根数,且继续计算木星摄动至1898年为止.但在1920年该星赤经的观测与预告的值,即 O—C 值,竟达到 10~m.3之多,所以斯特拉克重新近似计算木星摄动至1923年为止.求得该星的轨道根数为: 相似文献
4.
流星监测网是小尺寸近地小天体撞击监测、判断陨石落点的主要工具. 提出了一种基于多站布局的全天视频相机组网监测系统, 并在江苏及周边构建了一个区域级原型系统, 实现了火流星监测组网控制、视频数据采集、数据处理及流星体定轨的完整流程. 通过1yr的实测运行表明, 该系统可观测流星极限视星等为-1.0等, 可以实现绝对星等-2.5等流星的完备检测; 根据监测数据得到火流星通量为2.68×10-7km-2 ·h-1;群流星和偶发流星占比分别为46%和54%,偶发流星中类小行星轨道和类彗星轨道比例分别为27.1%和72.9,统计结果与国际主要流星监测网相接近,验证了监测网系统在实际组网使用中的监测能力. 相似文献
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在以前研究的基础上继续研究了双星两子星的自转对轨道变化的后牛顿效应，给出自转对轨道产生的长期摄动效应和周期摄动效应。理论结果表明，两子星的自转对轨道半长轴、轨道偏心率、近星点角和平近点经度均产生周期摄动效应，但对前两个轨道根数不产生长期摄动效,人对后两个轨道根数产生长期摄动效应，并利用理论结果对6颗双星系：EK Cep、GT Cep、NY Cep、V448 Cyg和V451 Oph中两子星的自转对轨道产生周期和长期摄动效应做了数值计算，数值结果显示：对于两个质量较大快速自转的双星系，由此产生的后牛顿铲应是不能忽视的。 相似文献
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研究了双星多方模型的形状对同步子星轨道要素的摄动影响，假定两子星在同一轨道面上运动，推出了主星对伴星的轨道要素的摄动量，理论结果表明，双星多方模型对轨道半长轴和偏心率只有周期项摄动，无长期摄动，但对近星点和历元平近点角除有周期摄动外还有长期摄动效应。文中将理论结果应用于同步双星βＰｅｒ（大陵五双星）的计算上，除计算了两个子星的形状（椭率）外对同步子星的轨道要素变化的周期项振幅和长期项的效应做了数值 相似文献
7.
研究了双星多方模型的形状对同步子星轨道要素的摄动影响。假定两子星在同一轨道面上运动，推出了主星对伴星的轨道要素的摄动量。理论结果表明：双星多方模型对轨道半长轴和偏心率只有周期项摄动，无长期摄动，但对近星点和历元平近点角除有周期摄动外还有长期摄动效应。文中将理论结果应用于同步双星βＰｅｒ（大陵五双星）的计算上。除计算了两个子星的形状（椭率）外对同步子星的轨道要素变化的周期项振幅和长期项的效应做了数值计算 相似文献
8.
3C273的光学光变周期 总被引：3，自引：0，他引：3
收录了类星体3C273约110年的光学资料，并在此基础上讨论了光变周期性.当用两种不同方法(Jurkevich方法及DCF(离散相关系数)法)分析时，发现光变曲线中存在周期为2.0年、(13.65±0.20)及(22.5±2.0)年的周期性.同时也讨论了这种周期的可能机制. 相似文献
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研究了地球磁场对带电的非赤道卫星的轨道根数的摄动影响。理论结果表明，地球磁场对带电卫星的轨道半长轴没有摄动影响，既无周期摄动，也无长期摄动，但对轨道偏心率、轨道倾角、升交点赤经、近地点经度和历元平近点角均有周期摄动，且对升交点和近地点经度还有长期摄动效应。通过算例表明，当卫星带有大量电荷时，地球磁场对卫星轨道的摄动影响必须加以考虑。 相似文献
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1°.利用波林(Bohlin)方法计算这颗小行星受木星和土星的普遍摄动并利用惕仁(Tie-tjen)方法作轨道改进.2°.取上面获得结果为第一近似值,再用爱克(Eckert)方法作轨道改进获得平均残差|Δα|=1~s.96,|Δδ|=21″.8. 相似文献
11.
Liu Xie-lin 《Chinese Astronomy and Astrophysics》1987,11(4):312-319
A power spectrum analysis is applied to the yearly statistics of Chinese historical records of fireballs. The results show that sound is an important indicator of origin. Noisy fireballs have the following possible periods in years: 170.6 ± 0.0, 102.4 ± 0.0, 66.1 ± 2.2, 27.3 ± 0.4, 23.3 ± 0.0, 17.9 ± 0.4, 14.8 ± 0.1, 12.4 ± 0.1, 10.5 ± 0.3. Noisy fireballs and meteorite falls have basically the same periods, and both originate in the asteroid belt. We think that the factors affecting both are the Yarkovsky effect and the perturbations by Jupitor. The 10.5-yr, 23.3-yr and 66.1-yr periods are related to the Yarkovsky effect and the 12.4-yr, 17.9-yr, 102.4-yr and 170.6-yr periods, to Jovian perturbations. The 14.8-yr and 27.3-yr periods may be due to the combined effect of the two, or to some other causes. 相似文献
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Abstract— Terminal bursts and fragmentations of meteoritic fireballs in the atmosphere may now be accurately located in four dimensions (three spatial + temporal) using seismic arrival times of their acoustic waves recorded by seismometer, camera, microphone, and/or infrasound stations on the ground. A computer program, SUPRACENTER, calculates travel times by ray tracing through realistic atmospheres (that include winds) and locates source positions by minimization of travel time residuals. This is analogous to earthquake hypocenter location in the solid Earth but is done through a variably moving medium. Inclusion of realistic atmospheric ray tracing has removed the need for the simplifying assumption of an isotropic atmosphere or an approximation to account for “wind drift.” This “drift” is on the order of several km when strong, unidirectional winds are present in the atmosphere at the time of a fireball's occurrence. SUPRACENTER‐derived locations of three seismically recorded fireballs: 1) the October 9, 1997 El Paso superbolide; 2) the January 25, 1989 Mt. Adams fireball; and 3) the May 6, 2000 Morávka fireball (with its associated meteorite fall), are consistent with (and, probably, an improvement upon) the locations derived from eyewitness, photographic, and video observations from the respective individual events. If direct acoustic seismic arrivals can be quickly identified for a fireball event, terminal burst locations (and, potentially, trajectory geometry and velocity information) can be quickly derived, aiding any meteorite recovery efforts during the early days after the fall. Potentially, seismic records may yield enough trajectory information to assist in the derivation of orbits for entering projectiles. 相似文献
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Shiba Y. Shimoda C. Maruyama T. Okumura S. Tomita M. Murasawa A. Ohtsuka K. Tomioka H. Hidaka E. 《Earth, Moon, and Planets》1997,77(1):47-54
Several Leonid fireballs were successfully photographed by the Japanese Fireball Network and by other observers in Japan on
16 November, 1996. A totals of seven of these were simultaneously observed from two or more stations, from which the orbital
and physical data were deduced. The radiant of these fireballs were very small, only 0.1°, similar to that of the 1991 Perseids.
The 1996 Leonids showed a lower magnitude distribution index similar to those obtained in the 1961 and 1965 Leonids. All of
these showers occurred before perihelion passage of the parent comet. We conclude that we have already encountered the elongated
front part of the dust trail of the Leonid parent comet, where the trail is probably composed of larger dust particles.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
14.
Abstract— We explore the orbital dynamics of Earth‐crossing objects with the intent to understand the time scales under which an “orbital stream” of material could produce time‐correlated meteorite falls. These “meteoroid streams” have been suggested to be associated with three well‐known meteorite‐dropping fireballs (Innisfree, Peekskill, and P?íbram). We have performed two different analyses of the statistical significance of the “orbital similarity,” in particular calculating how often orbits of the same level of similarity would come from a random sample. Secondly, we have performed extremely detailed numerical integrations related to these three cases, and we find that if they were streams of objects in similar orbits, then they would become “decoherent” (in the sense that the day‐of‐fall of meteorites of these streams become almost random) on time scales of 104–105 yr. Thus, an extremely recent breakup would be required, much more recent that the cosmic ray exposure ages of the recovered falls in each case. We conclude that orbital destruction is too efficient to allow the existence of long‐lived meteoroid streams and that the statistical evidence for such streams is insufficient; random fall patterns show comparable levels of clustering. 相似文献
15.
Plausible meteorite mass distributions imply that in the Prairie Network data there must be many fainter fireballs produced by meteorites with physical properties that, except for mass, are very similar to the recovered ordinary chondrite (H5) Lost City. Four criteria are proposed for identifying these other meteorites among the fireballs. These are: deceleration to final velocity ≤8 km/sec; a photometric mass/dynamic mass ratio within a factor of 2 of that of Lost City, agreement of the observed and theoretical single body end heights (calculated using dynamic mass), and a lightcurve no more irregular than those of the three recovered fireballs. These criteria can be related to the PE criterion of Ceplecha and McCrosky, but include a wider range of observational data, and also differ from the PE criterion in avoiding inclusion of data not helpful to the particular problem of identifying ordinary chondrite fireballs. By use of our criteria, 27 Prairie Network fireballs are identified as being meteorites comparable to or greater in strength and density to Lost City, most of these should be ordinary chondrites. The orbital element distributions of these objects span a wide range, include those of recovered fireballs, and show that the 4.0-AU aphelion of the Pribram meteorite is not unusually large. Perihelia are concentrated near 1.0 AU, in agreement with previous inferences from time-of-fall and radiant distributions, demonstrating the usefulness of these data based on visual observations. 相似文献
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Ian Halliday Arthur A. Griffin Alan T. Blackwell 《Meteoritics & planetary science》1996,31(2):185-217
Abstract— We present data for 259 meteoric fireballs observed with the Canadian camera network, including velocities, heights, orbits, luminosities along each trail, estimates of preatmospheric masses and surviving meteorites (if any) as well as membership in meteor showers. Some 213 of the events comprise an unbiased sample of the 754 fireballs observed in a total of 1.51 × 1010 km2 h of clear-sky observations. The number of fireballs and the amount of clear sky in which they were recorded are given for each day of the year. We find at least 37% of the unbiased sample are members of some 15 recognized meteor showers. Preatmospheric masses, based on an assumed luminous efficiency of 0.04 for velocities >10 km s?1, range from 1 g for some very fast fireballs up to hundreds of kilograms for the largest events. We present plots and equations for the flux, as a function of initial mass, for the entire group of fireballs and for some subgroups: meteorite-dropping objects; meteor shower members; groups that appear to be mainly of asteroidal or cometary origin; and for very fast objects. For masses of a few kilograms, asteroidal objects outnumber cometary ones. Cometary objects attain greater peak brightness than asteroidal ones of equal mass largely due to higher velocity, but also because they fragment more severely. For 66 fireballs, we estimate the meteoroid density using photometric and dynamic masses. Presumed cometary objects have typical densities near 1.0, while asteroidal values show two groups that suggest meteoroids similar to carbonaceous and ordinary chondrites. Our basic data may be used by others for further studies or to reexamine our results using assumptions different from those employed in this paper. 相似文献
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Peter Brown Valerie Marchenko Danielle E. Moser Robert Weryk William Cooke 《Meteoritics & planetary science》2013,48(2):270-288
We propose that the Taurid meteor shower may contain bodies able to survive and be recovered as meteorites. We review the expected properties of meteorite‐producing fireballs, and suggest that end heights below 35 km and terminal speeds below 10 km s?1 are necessary conditions for fireballs expected to produce meteorites. Applying the meteoroid strength index (PE criteria) of Ceplecha and McCrosky (1976) to a suite of 33 photographically recorded Taurid fireballs, we find a large spread in the apparent meteoroid strengths within the stream, including some very strong meteoroids. We also examine in detail the flight behavior of a Taurid fireball (SOMN 101031) and show that it has the potential to be a (small) meteorite‐producing event. Similarly, photographic observations of a bright, potential Taurid fireball recorded in November of 1995 in Spain show that it also had meteorite‐producing characteristics, despite a very high entry velocity (33 km s?1). Finally, we note that the recent Maribo meteorite fall may have had a very high entry velocity (28 km s?1), further suggesting that survival of meteorites at Taurid‐like velocities is possible. Application of a numerical entry model also shows plausible survival of meteorites at Taurid‐like velocities, provided the initial meteoroids are fairly strong and large, both of which are characteristics found in the Taurid stream. 相似文献
19.
Ichiro Hasegawa 《Earth, Moon, and Planets》1995,71(3):311-316
Chinese and Japanese historical records of daytime fireballs, and world-wide daytime meteorite falls in the catalogue have been investigated. Among them, there are 253 and 104 records of great daytime fireballs in China and in Japan respectively, and 506 meteorite falls in the daytime are recorded in the Catalogue of Meteorites (1985).The same trends of seasonal and daily variations in the flux of daytime fireballs are clearly seen in both Chinese and Japanese records, and then the distributions of the daytime fireballs seem to suggest the association with meteorites and near-earth minor planets rather than with comets.Possible relations with minor planets, such as (1566) Icarus, (3671) Dionysius, (4450) Pan, (4486) Mithra and others are suggested. 相似文献
20.
Ichiro Hasegawa 《Earth, Moon, and Planets》1996,72(1-3):311-316
Chinese and Japanese historical records of daytime fireballs, and world-wide daytime meteorite falls in the catalogue have been investigated. Among them, there are 253 and 104 records of great daytime fireballs in China and in Japan respectively, and 506 meteorite falls in the daytime are recorded in the Catalogue of Meteorites (1985). The same trends of seasonal and daily variations in the flux of daytime fireballs are clearly seen in both Chinese and Japanese records, and then the distributions of the daytime fireballs seem to suggest the association with meteorites and near-earth minor planets rather than with comets. Possible relations with minor planets, such as (1566) Icarus, (3671) Dionysius, (4450) Pan, (4486) Mithra and others are suggested. 相似文献