O-star winds in the Magellanic Clouds and the Milky Way

UV P-Cygni profiles of OB-stars in the Magellanic Clouds (observed with HST), and the galaxy (observed with IUE) are analyzed empirically using a line formation procedure similar to the one described by Lamers et al. (1987). The assumption of a constant microturbulencev _turb throughout the wind is dropped and replaced by a radially increasing turbulence parameterv _turb(v), thus improving the fit for the emission peaks substantially, and at the same time avoiding the need for a justification of extremely supersonic turbulence in the vicinity of the wind's sonic point. The Sobolev optical depth is determined interatively at fixed velocities in the wind, which removes the bias introduced by the choice of a specific parameterization function. Where it was possible and necessary a full photospheric spectrum was used to illuminate the wind line. The terminal velocitiesv are are found to be largest in the Galaxy, smallest in the Small Magellanic Cloud, and intermediate or similar to galactic in the Large Cloud.     

运输类飞机包含EWIS的区域安全性分析研究

为了解决运输类飞机EWIS设计过程中的安全性评估问题,针对包含EWIS的区域,提出了一种区域安全性分析方法。在对ARP4761标准的区域安全性分析和AC25-27的强化区域分析流程的基础上,考虑EWIS物理失效模式及失效对EWIS自身和区域内系统/设备的影响,给出了分析流程,为EWIS满足适航要求的设计提供技术参考。     

北纬30°N中间层和低热层大气平均风中频雷达观测

利用武汉(30.5°N,114.4°W)中频雷达在2001年1月1日至3月18日、2002年2月5日至3月18日、2002年10月18日至12月31日期间,日本Yamagawa(31.2°N,130.6°W)中频雷达在1997年1月1日至10月17日期间的数据,分析北纬30°N地区上空60-98km高度的中间层、低热层大气平均风的变化规律,结果表明平均纬向风和经向风都具有明显的季节变化.平均纬向风在冬季基本为西风,随高度增加,西风减弱,甚至在上部会出现微弱的东风;夏季中间层表现为强烈的东风,低热层则为西风,风向转换高度在80km附近;春季和秋季为转换季节,在春季出现舌状东风结构.80km附近的平均经向风场在冬季以南风为主,在夏季则以北风为主.不同年份的平均风场存在年际变化性,但其气候变化特点非常相似.中频雷达观测结果与HWM93模式结果的气候变化特点符合很好,与其他纬度的平均纬向风气候变化特点基本类似.     

深埋洞室围岩破坏区域碎裂化的非均匀弹性分析

根据实验研究发现，在深部开挖的围岩中观察到的区域周期结构，是以巷道围岩中的破裂区域和相对完好区域交替出现，这种现象被称为区域碎裂化现象。区域碎裂化现象是深部岩体工程响应的特征和标志，在分析深部岩体工程围岩变形、破裂和稳定性时必须要考虑区域碎裂化现象和破裂区的残余强度，它决定了深部岩体工程开挖、支护方案特点和原理，同时，区域碎裂化现象的产生并不是岩石达到一定深度而产生的突变过程，而是蕴涵着地下工程变形破坏的一种本质特征，只是在一定的应力作用下的明显体现，因此对深部岩体工程区域碎裂化结构形成规律的研究不仅对深部开采具有重要的工程意义，同时也对浅部地下工程建设具有重要的实际意义，本文通过力学分析对区域碎裂化形成机理进行理论研究。     

The case for massive,evolving winds in black hole X-ray binaries

In the last decade, high-resolution X-ray spectroscopy has revolutionized our understanding of the role of accretion disk winds in black hole X-ray binaries. Here I present a brief review of the state of wind studies in black hole X-ray binaries, focusing on recent arguments that disk winds are not only extremely massive, but also highly variable. I show how new and archival observations at high timing and spectral resolution continue to highlight the intricate links between the inner accretion flow, relativistic jets, and accretion disk winds. Finally, I discuss methods to infer the driving mechanisms of observed disk winds and their implications for connections between mass accretion and ejection processes.     

Mid-latitude thermospheric zonal winds during the equinoxes

The diurnal variation of the mid-latitude upper thermosphere zonal winds during equinoxes has been studied using data recently generated from CHAMP measurements from 2002 to 2004 using an iterative algorithm. The wind data was separated into two geomagnetic activity levels, representing high geomagnetic activity level (Ap > 8) and low geomagnetic activity level (Ap ? 8). The data were further separated into two solar flux levels; with F10.7 > 140 for high and F10.7 ? 140 for low. Geomagnetic activity is a correlator just as significant as solar activity. The response of mid-latitude thermospheric zonal winds to increases in geomagnetic disturbances and solar flux is evident. With increase in geomagnetic activity, midday to midnight winds are generally less eastward and generally more westward after the about midnight transitions. The results show that east west transitions generally occurred about midnight hours for all the situations analyzed. The west to east transition occurs from 1400–1500 MLT. Enhanced westward averaged zonal wind speeds going above 150 ms⁻¹ are observed in the north hemisphere mid-latitude about sunrise hours (∼0700–1100 MLT). Nighttime winds in the north hemisphere are in good agreement with previous single station ground observations over Millstone Hill. Improved ground observations and multi satellite observations from space will greatly improve temporal coverage of the Earth’s thermosphere.     

航天员舱外相对航天器运动轨迹摄动研究

用轨道根数描述载人航天器运动,在其轨道坐标系(LVLH)中,建立了含地球J2项引力和大气阻力摄动加速度的航天员质心相对航天器的运动模型。在参考轨道存在小偏心率时,对基于圆参考轨道假设推导的航天器编队飞行的线性时变系统状态矩阵进行了修正。仿真结果表明:对偏心率为0.002的航天器轨道,修正后模型所得航天员相对轨迹摄动量在离舱300 s后达到0.8%,是修正前模型的5倍,但计算量增加不超过5%,更适于航天员舱外飞行和近距离编队飞行建模。     

中频雷达风场的双谱分析

对中纬度中频雷达１９９７年６月８２ｋｍ高度的小时平均风场数据进行了动态谱分析和双谱分析,得到了中层顶区域谱行为具有多样性和各向异性的特点,以及行星波,潮汐波和重力波之间相位相干的现象,讨论了中层顶行星波,潮汐波和重力波之间存在非线性相互作用的可能性。     

Observations of the atmospheres and winds of O-stars,LBVs and Wolf-Rayet stars

This review summarises recent studies of O-stars, Luminous Blue Variables (LBVs) and Wolf-Rayet (WR) stars, emphasising observations and analyses of their atmospheres and stellar winds yielding determinations of their physical and chemical properties. Studies of these stellar groups provide important tests of both stellar wind theory and stellar evolution models incorporating mass-loss effects. Quantitative analyses of O-star spectra reveal enhanced helium abundances in Of and many luminous O-supergiants, together with CNO anomalies in OBN and Ofpe/WN9 stars, indicative of evolved objects. Enhanced helium, and CNO-cycle products are observed in several LBVs, implying a highly evolved status, whilst for the WR stars there is strong evidence for the exposition of CNO-cycle products in WN stars, and helium-burning products in WC and WO stars. The observed wind properties and mass-loss rates derived for O-stars show, in general terms, good agreement with predictions from the latest radiation-driven wind models, although some discrepancies are apparent. Several LBVs show similar mass-loss rates at maximum and minimum states, contrary to previous expectations, with the mechanism responsible for the variability and outbursts remaining unclear. WR stars exhibit the most extreme levels of mass-loss and stellar wind momenta. Whilst alternative mass-loss mechanisms have been proposed, recent calculations indicate that radiation pressure alone may be sufficient, given the strong ionization stratification present in their winds.