Rotation and cometary activity of KBO (29981) 1999 TD10

We describe observations of the scattered Kuiper Belt object (29981) 1999 TD₁₀ performed during five observing runs at two observatories, over 370 days from 2000 September to 2001 September. They show significant brightness variations that fit a double-peaked lightcurve with period 15.448±0.012 h in V and R bands. The phase effect in V band, 0.09±0.01 mag deg⁻¹, is smaller than that of Pluto but larger than that of several KBOs, while in R band it is 0.030±0.005 mag deg⁻¹. We find color variation between the two bands, which implies a non-homogeneous albedo distribution on the surface. Evidence of surface activity near perihelion in the form of a coma/tail is presented using radial image profiles and a 2D contour map.     

Search for Microflaring Activity in the Magnetic Network

We analyze the temporal behavior of network bright points (NBPs) searching for low-atmosphere signatures of flares occurring on the magnetic network. We make use of a set of data acquired during coordinated observations between ground-based observatories (NSO/Sacramento Peak) and the MDI instrument on board SOHO. Light curves in chromospheric spectral lines show only small-amplitude temporal variations, without any sudden intensity enhancement that could suggest the presence of a transient phenomenon such as a (micro)flare. Only one NBP shows spikes of downward velocity, of the order of 2–4 km s^–1, considered as signals of compression associated with a (micro)flare occurrence. For this same NBP, we also find a peculiar relationship between the magnetic and velocity fields fluctuations, as measured by MDI. Only for this point the B–V fluctuations are well correlated, suggesting the presence of magneto-acoustic waves propagating along the magnetic structure. This correlation is lost during the compression episodes and resumes afterward. An A6 GOES soft X-ray burst is temporally associated with the downward velocity episodes, suggesting that this NBP is the footpoint of a flaring loop. This event has a total thermal energy content of about 10²⁸ erg, and, hence, belongs to the microflare class.     

Search for isotopic anomalies in oldhamite (CaS) from unequilibrated (E3) enstatite chondrites

Abstract— The Ca isotopic compositions of 32 oldhamite (CaS) grains from the Qingzhen (EH3), MAC88136 (EL3), and Indarch (EH4) enstatite chondrites were determined by ion microprobe mass spectrometry. Also measured were the S isotopic compositions of eight oldhamite, two niningerite (MgS), and seven troilite (FeS) grains. The S isotopic compositions of all minerals are normal, but oldhamite grains of the first two meteorites exhibit apparent small ⁴⁸Ca excesses and deficits that are correlated with isotopic mass fractionation as determined from the ⁴⁰Ca-⁴⁴Ca pair. The interpretation of these results is complicated by the fact that none of the established mass fractionation laws can account for the data in the Norton County oldhamite standard. The method of analysis is carefully scrutinized for experimental artifacts. Neither interferences nor any known mass fractionation effect can satisfactorily explain the observed small deviations from normal isotopic composition. If these are truly isotopic anomalies, they are much smaller than those observed in hibonite. The nucleosynthetic origin of Ca isotopes is discussed.     

Search for optical identifications in the 5C4 radio survey

With the aid of a statistical approach regarding only the nearest optical object to a given radio position we have found identification rates of nearly 30 per cent up to the blue and red limits of the Palomar Sky Survey prints covering the region of the 5C4 radio survey. Roughly 60 per cent of these identifications are blue starlike objects and therefore possible quasar candidates. The remainig identifications are galaxies. Probabilities for the first neighbours to be an optical counterpart and finding charts for highly reliable objects are given.     

Search for causes of the low epithermal neutron flux anomaly in the Arabia Terra region (Mars)

A geologic analysis of 274 images acquired by the high-resolution MOC camera onboard the Mars Global Surveyor spacecraft within the Arabia Terra low neutron flux anomaly (which is indicative of an anomalously high abundance of hydrogen: up to 16 wt % of the equivalent amount of water) was performed. Correlation between the enhanced abundance of equivalent water with the presence of dust on the surface was found. Since dust plays a key role in condensation of water from the atmosphere, we suppose that the anomalies could result from the retention of atmospheric moisture. To analyze this suggestion, we performed a theoretical modeling that allowed us to map the planetary-scale distributions of several meteorological parameters responsible for the atmospheric moisture condensation. Two antipodal regions coinciding rather well with the Arabia Terra anomaly and the geographically antipodal anomaly southwest of Olympus Mons were found in the maps. This suggests that the anomalies are rather recent than ancient formations. They were probably formed by a sink of moisture from the atmosphere in the areas where present meteorological conditions support this sink. Geological parameters, primarily the presence of dust, only promote this process. We cannot exclude the possibility that the Martian cryosphere, rather than the atmosphere, supplied the studied anomalies with moisture during their formation: the thermodynamic conditions in the anomaly areas could block the moisture flux from the Martian interior in the upper regolith layer. The moisture coming from the atmosphere or from the interior is likely held as chemically bound water entering into the structure of water-bearing minerals (probably, hydrated magnesium sulfates) directly from the vapor; or the moisture precipitates as frost, penetrates into microfissures, and then is bound in minerals. Probably, another geologic factor—the magnesium sulfate abundance—works in the Arabia Terra anomaly.     

基于伽马射线的类轴子粒子探测及暗物质子晕搜寻研究

目前已经有很多观测证据表明宇宙中存在着大量暗物质,其能量密度占据了目前宇宙总能量密度的1/4.根据高精度的数值模拟和引力透镜观测,我们已经对从矮星系到星系团中的暗物质空间分布有了较好的理解,但是对于暗物质究竟是什么我们还一无所知.由此,物理学家提出了很多假想的粒子模型.     

Search for variability in hydrogen-poor stars

The evolutionary status of hydrogen-poor stars is analyzed.Photoelectric observations of six objects are reported as a first step of a long-term project devoted to search for variability of a large sample of hydrogen-poor stars.The observed stars show phenomena of microvariability with an amplitude of the order of 0^m. 1 or less.Two extreme helium stars have been examined: a period in the range of 0^d.162-0^d.164 has been found for BD+ 10⁰2179, andP=0^d.1079962 for BD+13⁰3324.The mass-losing O subdwarf (sdO) BD+37⁰ 443 presents short-term fluctuations with a time-scale of several minutes and long-term variations on a scale of months. The standard sdO BD+75⁰325 is probably non-variable, although light variations of very small amplitude (m0.03) with a time-scale of about 1 hr might be present. The high gravity sdO BD+25⁰4655, which is very close to the white dwarf stage, also presents variability on a time-scale of about 13 minutes, and might be an analog of the recently discovered pulsating sdO, or hot white dwarf, PG 1159-035.The variability of the intermediate helium star HD 37776 is finally confirmed.     

Spectra of PV Cep and GM1-29 (RNO 125) in 1976-1997

The main spectral characteristics of PV Cep, a T Tau star, and of the variable nebula GM1-29 associated with it are considered. Their variations during 1976-1997, based on observations on the 6-m telescope and literature data, are described. In the period of maximum brightness (1977-1979), the star had a well-developed emission spectrum, typical of classical T Tau stars, with clearly defined P Cyg components in the H and H lines, strong Na D absorption features shifted in the blue direction, and well-defined fluorescence in Fe I emission features. After the end of the latter eruption, the star's spectrum has remained more or less in a stable state; emission lines are considerably weaker. The ejected matter continues to be observed in the form of shifted components in emission lines. There are also indications of the possible existence of a collimated jet 1.5-2 long in the star's immediate vicinity. Also clearly seen is HH215 P1 — the first HH knot in the giant jet emerging from PV Cep. At the epoch of the object's maximum brightness, there were clear signs of spectral asymmetry of the stellar envelope in the nebula's spectrum, due to the directional outflow, manifested in variation of the profiles and intensities of Balmer lines. PV Cep and GM1-29 thereby prove to be another object in which the phenomenon first noted in R Mon and NGC 2261 is observed.     

Search for GRB counterparts in the optical

The history and recent results of searches for optical counterparts to gamma ray burst sources in all three categories (i.e. flaring, fading and quiet) are outlined. The related problems such as background triggers and advantages and drawbacks of previous and recent approaches and investigations are discussed. Although there are some promising results especially in the appearance of optical transients i.e. short-lived star-like objects found in or close to the error boxes of some GRB, there is a need for more and better optical data, especially taken at or close to the times of GRB. Based on recent results, a strategy for further works in this direction is suggested with emphasis on obtaining of simultaneous (wide-field CCD experiments) and quasisimultaneous (robotic telescopes automatically pointed to the positions of newly detected GRB by Internet link) optical data.     

Search for HD in Jupiter and Saturn

Upper limits are placed on the D/H ratio in the observed portions of the atmospheres of Jupiter and Saturn from observations at high S/N over the region of the 5-0 R(1) line of HD. The upper limits of 4 × 10^?5 and 6 × 10^?5 D/H on Jupiter and Saturn, respectively, are not inconsistent with present models for abundance ratios in the primitive solar nebula or with other estimates of this quantity from observations.     

Search for Compact x-ray Sources in sxt Observations

We show the result of a search for compact sources in observations of Soft X-ray Telescope (SXT) aboard the Yohkoh satellite. We focused the search on the highest-resolution SXT images taken with the SXT thick aluminum filter. Non-standard methods have been used in order to avoid data corrupted by spikes or dark current saturation effects. Search criteria and certain questions concerning the SXT database are addressed and discussed in more detail. For the most compact structures found we show also comparison of their brightness spatial distribution with ground calibration data. The search was performed to identify regions with well-localized X-ray emission in SXT images and to gather basic information about them.     

ESO Involvement in the Search for Extrasolar Planets

ESO intends to actively and vigorously support the search for extrasolar planets by designing and commissioning instruments and methods targeted towards this end. High precision radial velocity measurements at La Silla and Paranal, wide-field microlensing imaging in the bulge from Paranal, and very high spatial resolution observations with the VLT Interferometer are but a few of the exciting new techniques ESO plans to bring on line in the next few years. I will discuss in detail the expected or actual performance of each of these methods and review the scientific potential for progress in the field of extrasolar planet research that they are expected to bring.     

Search for Star Groups in the Solar Neighborhood

Two methods are proposed for finding star groups in coordinate and velocity spaces, which were used to investigate stars of the Hipparcos Catalog with known radial velocities in the solar neighborhood with a radius of 125 pc. Thirteen probable nonrandom star groups in coordinate space and five moving groups in velocity space were found. These results are compared with the results of other authors.     

Search for extractable fullerenes in the Allende meteorite

Abstract— In an effort to confirm earlier observations of fullerenes in the Allende meteorite by Becker et al. (1994), we have treated nine separate whole-rock chips of this meteorite with toluene to search for extractable C₆₀ and C₇₀ fullerenes. The analysis was done with high performance liquid chromatography. Less than 1 ppb C₆₀ and C₇₀ were detected in a total of 131.82 g of this meteorite. Becker et al. (1994) have estimated a content of 100 ppm in one Allende sample. Either they have grossly overestimated the C₆₀ content of their sample, or Allende is very inhomogeneous concerning fullerenes.