A sounding rocket experiment on the marangoni convection

During a 6-minutes free flight of a sounding rocket an experiment on the thermal Marangoni convection in a right circular cylindric floating zone was carried out to verify the thermal Marangoni convection by flow visualisation for the first time at 10^?4 g. From the motion picture analysis the velocity distributions are obtained. The interdependence between the two velocity maxima and the S-shaped temperature distribution on the free surface is discussed. The influence of the heat transfer caused by the flow of the surrounding air induced by the thermal Marangoni convection itself is considered briefly.     

Boundary-layer analysis for the convection/diffusion transition in dendritic growth

Earlier ground-based studies have shown that a sharp transition occurs in the dominant mode of heat transport during dendritic solidifcation. Specifically, convective heat transport dominates below the transition supercooling and diffusive heat transport dominates above. Thus the influence of gravitational acceleration on dendritic crystallization depends critically on the overall thermodynamic driving force. Since many practical solidification processes occur at relatively small supercoolings, understanding the nature of the transition in transport mode is essential for both terrestrial and space processing. A boundary-layer analysis has been carried out wherein the diffusion boundary-layer thickness (Stefan length) is compared with the thermal boundary layer thickness determined from the fluid mechanics of natural convection. Our analysis shows that the Stefan length δ_S decreases rapidly with supercooling (ΔT^?2.5) whereas the thermal boundary layer thickness δ_T decreases slowly (ΔT^?.25). The transition supercooling at which the transport mode switches from convective to diffusive occurs where δ_T = δ_S. The influence of gravitational acceleration, and the thermo-physical properties of the molten phase will be discussed, along with avenues for conducting future research.     

A linear stability analysis of large-Prandtl-number thermocapillary liquid bridges

A linear stability analysis is applied to determine the onset of oscillatory thermocapillary convection in cylindrical liquid bridges of large Prandtl numbers (4  Pr  50). We focus on the relationships between the critical Reynolds number Re_c, the azimuthal wave number m, the aspect ratio Γ and the Prandtl number Pr. A detailed Re_c–Pr stability diagram is given for liquid bridges with various Γ. In the region of Pr > 1, which has been less studied previously and where Re_c has been usually believed to decrease with the increase of Pr, we found Re_c exhibits an early increase for liquid bridges with Γ around one. From the computed surface temperature gradient, it is concluded that the boundary layers developed at both solid ends of liquid bridges strengthen the stability of basic axisymmetric thermocapillary convection at large Prandtl number, and that the stability property of the basic flow is determined by the “effective” part of liquid bridge.     

Oscillatory thermocapillary convection in floating zones under normal- and micro-gravity

The thermocapillary convection in a floating zone becomes oscillatory, exceeding a Marangoni number of approximately 10⁴. The oscillatory state of thermocapillary convection has been verified under 1 g and 10^?4 g and the features seem to be fairly independent of the gravity level. The transition point from the laminar to the oscillatory state (critical Marangoni number), however, depends on the magnitude and direction of the buoyant force.     

Study of waves in the magnetotail region with cluster and DSP

The study of the neutral sheet is of fundamental importance in understanding the dynamics of the Earth’s magnetosphere. From the earliest observation of the magnetotail, it has been found that the neutral sheet frequently appears to be in motion due to changing solar wind conditions and geomagnetic activity. Multiple crossings of the neutral sheet by spacecraft have been attributed to a flapping motion of the neutral sheet in the north–south direction, a wavy profile either along the magnetotail or the dawn–dusk direction. Cluster observations have revealed that the flapping motions of the Earth’s magnetotail are of internal origin and that kink-like waves are emitted from the central part of the tail and propagate toward the tail flanks. This flapping motion is shown here to propagate at an angle of ∼45° with x_GSM. A possible assumption that the flapping could be created by a wake travelling away from a fast flow in the current sheet is rejected. Other waves in the magnetotail are found in the ULF range. One conjunction event between Cluster and DoubleStar TC1 is presented where all spacecraft show ULF wave activity at a period of approximately 5 min during fast Earthward flow. These waves are shown to be Kelvin–Helmholtz waves on the boundaries of the flow channel. Calculations show that the conversion of flow energy into magnetic energy through the Kelvin–Helmholtz instability can contribute to a significant part of flow breaking between Cluster and DoubleStar TC1.     

Crystallization of KNO3 under conditions of diffusive and convective regime

Influence of the nature of heat transfer on crystallization from a cooling solution has been investigated. Sodium polymethylacrylate (PMANa) was used to adjust the viscosity of the medium in the desired way. It was shown that the nature of heat transfer influences the crystallization kinetics and that the absence of convection results in enhanced supercooling. These findings corroborate our interpretation of space experiments /1/. The KNO₃-H₂O-PMANa system is suitable for a detailed analysis of the influence of zero gravity on the nucleation and crystallization processes.     

Some recent results on extragalactic X-ray sources from the Einstein observatory

Extragalactic research studies by the Harvard/Smithsonian group with the Einstein Observatory have emphasized quasars and clusters of galaxies. More than 100 QSO's have been detected, including 20 serendipitous discoveries. The ratio of L_x/L_o for radio loud quasars is on the average 3 times that of radio quiet ones. QSO's with a large intrinsic optical luminosity have a smaller ratio of L_x/L_o. X-ray images of clusters of galaxies reveal a variety of morphological types which may correspond to different stages in their evolution. Several examples of bi-modal clusters have been discovered. An X-ray plume associated with M86 is apparently gas being stripped. From X-ray studies, a mass between 1.7 × 10¹³M_θ and 4.0 × 10¹³ M_θ has been derived for M87.     

Vertical distribution of NH3 in the upper Jovian atmosphere from IUE observations

The first unambiguous identification of ammonia in the upper atmosphere of Jupiter has been obtained from the observation of individual NH₃ bands in an IUE high resolution spectrum in the 2100–2400 Å spectral range. The variation with wavelength of the strengths of these NH₃ bands implies that the NH₃ abundance has to be strongly reduced by photolysis in the upper jovian atmosphere. Preliminary analysis by means of scattering models shows that the ammonia mixing ratio cannot be constant with altitude. The mixing ratio NH₃/H₂ ranges from 5 10^?8 to 5 10^?7 at the 250 mb pressure level, and decreases as P or P² toward higher altitudes.     

蒸发效应与热毛细对流耦合现象的实验研究

实验研究了矩形液池中蒸发薄液居中蒸发效应与热毛细对流的耦合机理. 对于单纯的热毛细对流稳定性从实验和理论上已有深入研究,但目前国际上对带有菇发界面的热毛细对流问题尚缺乏研究. 特别是近来的研究发现,气液界面的蒸发对热毛细对流稳定性有很大的影响. 本实验以温度为主要控制参数,测量了不同工况下蒸发界面不同点的蒸发速率和表层温度,并利用 PIV 方法分析得到了液体内的嘛场分布. 实验结果发现,随着沿界面的温差增加,蒸发液体内的流型从稳定的单涡胞结构变为稳定的多祸胞结构,并最终演变为紊流结构. 综合分析以上测量结果并与理论分析结果进行了比较。      

钛合金的离子束改性

钛合金是航空航天工业常用的结构材料,它具有重量轻、强度高、抗腐蚀强等优良性能,但耐磨性较差.为提高其耐磨性,对TC4、TA7航材试件,采用溅射方法在其表面镀上钛膜,并用(N^＋＋N^＋₂)混合离子束进行动态反冲注入及单元素C^＋离子束注入两种方法,进行表面改性.精密摩擦、磨损试验及显微硬度测量结果,试件表面的滑动摩擦系数降低了64%~77%;磨损率减少了22%~48%;显微硬度提高0.3~1.4倍.证明离子注入有效地改善了合金表层的摩擦、磨损性能.对注入样品进行X射线光电子能谱(XPS)分析,发现注入后的钛合金表层,生成了大量的TiO₂,并析出TiN,TiC等金属化合物,这是降低摩擦系数,提高耐磨性的主要因素.添加C^＋离子注入的试件,其力学性能并无进一步改善,原因有待分析.     

Mesospheric H2O and H2O2 densities inferred from in situ positive ion composition measurement

The measurements of positive ion composition in the high latitude D-region have revealed an excess of 34⁺ under distrubed conditions which has been interpreted as H₂O₂⁺. At the same altitude range near the transition height oxonium ions were measured as well. This paper presents a new model for the production and loss of oxonium ions with their production from H₂O₂⁺ + H₂O → H₃O⁺ + HO₂ and their loss by attachment of N₂ and/or CO₂. A reaction constant of 8.5×10^?28 (300/T)⁴ cm⁶s^?1 has been obtained for the three body attachment H₃O⁺ + CO₂ + M → H₃O⁺.CO₂ + M from the measured density profile of 63⁺ in flight 18.1020. Mesospheric H₂O and H₂O₂ densities are inferred from measurements of four high latitude ion compositions based on the oxonium model. The mixing ratios of hydrogen peroxide are up to two orders of magnitude higher compared to previous model calculations. In order to explain the missing production of odd hydrogen, we consider larger O(¹D) densities, surface reactions of O(³P) on particles, and cathalytic photodissociation of water vapor on aerosol particles.     

Highly variable X-ray emitting objects in the Rho Oph dark cloud

The Rho Ophiuchi dark cloud region has been the subject of an extensive guest investigation using the $\text{Einstein}$ Observatory. The set of observations comprise 14 IPC fields and 3 HRI fields. The densest part of the cloud has been observed 6 times. Forty seven sources were detected at a level > 3.5 σ and twenty more above 2 σ. The majority of these sources have optical, IR, or even radio continuum counterparts; nine are identified with known T Tauri stars, while several others are identified with stars showing H α in emission. All show a high degree of time variability; flux variations reach factors of 5 in a few hours, or 25 in a day. Apparent luminosities are in the range 10(30) – 10(31)(1) erg.s^?1. The possibility that the X-ray variability is due to flares is examined. If this interpretation is correct, one source has been the seat of the largest stellar flare ever recorded in X rays [L_x = 10(32) erg.s^?1, E_x ?10(36) ergs^-].     

Positive ion distributions in the morning auroral zone: Local acceleration and drift effects

We report on the typical structure of the large scale ion precipitation in the morning sector of the auroral zone and associated low frequency electromagnetic waves. Data obtained during near radial passes of the AUREOL-3 satellite point to a distinction between two main precipitation regions: 1) In the poleward part of the auroral zone the latitudinal variation of the average energy (or temperature) of the precipitated ions (mainly H⁺) indicate that they are adiabatically accelerated in the outer magnetosphere. This “high energy” (? 3 to > 20 keV) precipitation is usually associated with a low energy (E < 110 eV) upward flowing 0⁺ and H⁺ component, and 2) near the boundary between discrete and diffuse electron aurorae a drastic change in the ion characteristics is observed. The flux of energetic precipitated H⁺ ions is sharply reduced, which suggests the formation of an Alfvén layer. However, intense fluxes of precipitated H⁺, O⁺, and He⁺ ions with energies < 3 keV are observed equatorward of the Alfvén layer, in coincidence with the diffuse aurora and in association with quasi-monochromatic electromagnetic waves with frequencies around the proton gyrofrequency. As the characteristic convection and bounce times of the low energy upward flowing ion component are comparable (τ > 3 hours) we suggest that the precipitation of ionospheric ions inside the diffuse aurora results from convection and corotation of the ions accelerated to suprathermal energies at higher latitudes.     

Recent advances in upper atmospheric structure

A possible quantitative explanation of the semi-annual variation in thermospheric density has been obtained in terms of a semi-annual variation in the computed globally averaged vertical energy carried by propagating tides from the lower and middle atmosphere into the thermosphere. The effect is primarily due to seasonal changes in the distribution of water vapor and in the solar declination angle and Sun-Earth distance. An MSIS-83 empirical model of the thermosphere, representing a revision of the earlier MSIS models, has been prepared. The database used covers a wider range of solar activity than previous models and an improved magnetic storm representation is included. Atomic oxygen profiles in the 100 to 160 km altitude region of the auroral thermosphere have been recalculated from measured quenching of N₂(A³∑_u⁺) using the latest laboratory rates and the results are in good agreement with the mean CIRA 1972 profile. A new empirical model of thermospheric variations with geomagnetic activity has been developed incorporating variations with local magnetic time, latitude dependent terms which can vary with the magnitude of the geomagnetic disturbance, and an altitude dependent expression for the equatorial wave. A new index ML, derived from the AL index, has been developed that appears to have promise to represent the variations of thermospheric species with geomagnetic activity. Satellite measured values of solar UV flux, ground-based observations of CaK plages, sunspot numbers and 10.7 cm solar radio flux have been analyzed for temporal variations. Some differences have been identified and the significance to empirical and theoretical upper atmosphere models is discussed.     

Effect of gravity on coupled convective and interfacial instabilities during directional solidification

We investigate the role of gravity in a linear stability analysis of the onset of coupled convective and morphological instabilities during directional solidification at constant velocity of a dilute alloy of tin in lead. For solidification vertically upwards, the temperature gradient alone would cause a negative density gradient and the solute gradient alone would cause a positive density gradient. Two types of instability are found, a convective type that occurs for long wavelengths and a morphological type that occurs for short wavelengths. In general, these are coupled but the morphological instabilities are practically independent of gravity and thus correspond to the predictions of previous morphological stability theory in which density changes and convection are neglected. The convective instabilities depend strongly on gravity; for a growth velocity of V = 1 μm/s and a temperature gradient in the liquid of G_L = 200 K/cm, the critical concentrations for convective instabilities are 3.1 × 10^?4, 3.1 × 10^?2 and 2.39 wt. % for g_e = 980 cm/s², 10^?4 g_e and 10^?6 g_e, respectively. For low velocities, the convective instabilities occur at much lower solute concentrations than the morphological instabilities whereas at high velocities, the reverse is true. At intermediate velocities where the changeover takes place, there are oscillitory instabilities of mixed character whose periods range from 60 s at g_e to 6 × 10⁴ s at 10^?6 g_e.     

The N4,5 - OO Auger and “N3” N4,5O2,3 Coster-Kronig spectra of xenon induced by electron impact

The N_4,5OO Auger electron spectrum in the kinetic energy region (14–37) eV has been measured with high resolution at electron incident energies between 71 eV and 2019 eV. The Auger and satellite lines are assigned by comparison with previous literature data. Several states which correspond to the resonant Auger transitions from the 4d_{3/2, 5/2} 6p states are observed. The PCI effects on the N₅-O_2,3O_2,3(¹S₀) Auger peak when the incident electron energy approaches to the N₅ edge (67.55 eV) is investigated and it is found that the dependence of the energy shift on the excess energy, E_exc, is well represented by the function E_exc^β with β = (-1.40 ± 0.05). The ^“N₃^” N_4,5O_2,3 Coster-Kronig spectrum is measured at various electron incident energies. The assignments of the features are made in comparison with a similar spectrum from synchrotron radiation measured by Kivimäki et al. [J. Electron Spectrosc. Relat. Phenom. 1999, 101–103, 43–47]. The Auger spectrum in the kinetic energy regions (68–78) eV and (90–138) eV is observed for the first time in an electron impact experiment and a comparison is made with the photoionization experiment by Hikosaka et al. [Phys. Rev. A 2007, 76, 032708].     

Nusselt number for convection driven by tidal and radiogenic heating

The ‘traditional’ formulas giving the Nusselt number Nu as a function of Rayleigh number Ra cannot be used for low and moderate values of Ra. Moreover, the recent progress in 3D numerical modeling makes possible to determine the Nusselt number Nu as a function of Rayleigh number Ra for convection driven by radiogenic and tidal heating. We found that for low and moderate Ra: Nu(Ra) = ε(Ra+ξ)^λ where λ depends on rheology and boundary conditions, ε depends only on the mode of heating, and ξ = ε^−1/λ · Nu(Ra) makes possible to develop a parameterized theory of convection in medium size icy satellites. We also indicate some differences between convection driven by tidal and radiogenic heating and convection driven exclusively by radiogenic heating.     

F-Region ion composition modeling

Measurements of the principal ion species of the F₁- and F₂- regions have been used to develop an empirical model of the ion composition for altitudes between 150 and 500 km. The species measured by the S3-1 satellite include N⁺, O⁺, N₂⁺, NO⁺ and O₂⁺. The data were obtained near the minimum of the solar cycle, thus limited information on the ionospheric variation with solar flux is available. However, the range of latitude, altitude, local time and geomagnetic activity does provide a useful basis for modeling the F-region. The ion composition measurements have been used to provide a model for relative ion composition which is compatible with the total ion density from the International Reference Ionosphere model.     

Field-aligned plasmaspheric flows at moderate latitudes

In a model of the plasmasphere, coupled time-dependent continuity, momentum and energy equations are solved for thermal O⁺, H⁺ and electrons. The field-aligned mass flow coupling and thermal coupling of conjugate ionsopheres via the protonosphere are studied. For solstice conditions, thermal coupling between conjugate hemispheres gives rise to very strong upward flows of O⁺ in the topside ionosphere of the summer hemisphere at the time of sunrise in the conjugate (winter) ionosphere; a less marked effect (but with downward flow) occurs in the summer ionosphere at winter sunset. In addition, there are strong upward and downward flows of O⁺ at local sunrise and sunset, respectively, in both hemispheres. At both L = 1.5 and L = 3, the 24-hour time-integrated interhemispheric H⁺ flux is in the summer - winter direction. At L = 1.5 its magnitude is in good agreement with the magnitude of the time- integrated field-aligned plasma (O⁺ + H⁺) flux at 1000 km altitude; there is no such agreement at L = 3.     

The galactic center black hole: Clues for the evolution of black holes in Galactic nuclei

The evidence for a black hole located at the dynamical center of the Milky Way and identified with the unusual radio source, Sgr A¹, is now very compelling. Proper motion and radial velocity surveys of stars clearly demonstrate the presence of a non-luminous concentration of 2.6 × 10⁶ M_⊙ within a volume of radius ∼0.01 pc centered on Sgr A¹. At present, the accretion rate onto this object is rather small, leading to a total accretion luminosity at radio through far-IR wavelengths < 10³ L_⊙. The accreted material apparently originates in the winds of nearby massive stars. However, neither the stellar nor the gaseous environments are static. The surrounding cluster of massive stars, most lying well within a parsec, is only a few million years old, and is destined to fade substantially within another 10⁷ years. How did such a cluster form in the immediate and tidally stressed vicinity of a supermassive black hole? The circumnuclear disk of gas, which presently has an inner radius of 1 pc, seems destined to migrate inwards and eventually cause a much higher accretion rate onto Sgr A¹, with a consequent flurry of new activity. Because the young stars and gas in the vicinity of the black hole interact with each other, the episodes of recurrent activity there can be described in terms of a limit cycle, which effectively controls the growth of the central black hole. In addition to describing the steps of this cycle, we identify several key observations which serve as potential clues to the past activity not only of our Galactic center, but to the activity of gas-rich nuclei in general.