混合移频静刚度法和直接扰动迭代法

本文对混合移频动柔度法的失代式进行等价变换，从而得到一个“变种”，该变种不包含混合移频系统的动柔度式F^△（λ*），这便消除了F^△（λ*）带来的近似性，另外，对直接扰动法也进行等价变换，引出可以省时地用于许多特征向量导数计算的直接扰动迭代法。最后，为了供读者参数，本文还导出了三种混合移频动柔度法的非迭代式，其中有两种恰好是另外两种动柔度法经混合移频后的非迭代式，这实际上已将另两种动柔度法也扩展到密集根情况了。     

密集根之特征向量导数的改进高精度动柔度法

作者曾为许多特征向量导数计算，提出过一种介于直接法（指直接求解线代方程组的，以Nelson为代表的一类方法）和模态法之间的高精度动柔度法。这种方法与作者建立的一般动柔度法一样，不能用于密集根之特征向量导数的计算。为使该方法扩展到密集根状态，本文将作者发展的混合移频技术应用于原高精度动柔度法，并重新推导了混合移频系统 的高精度动柔度式，从而形成能适用于许多密集根之特征向量导数计算的改进高精度动柔度法。     

New multifrequency measurements of the spectrum of the cosmic background radiation

New measurements of the Cosmic Background Radiation temperature at 12 cm, 6.3 cm, 3 cm, 0.9 cm and 0.3 cm have made in July 1982 from the White Mountain High Altitude Research Station. The results are presented and the existence of spectral distortions discussed.     

Two magnetars: SGR 1627–41 and 1E 1547–5408

We describe the results obtained with Target of Opportunity observations of the galactic sources SGR 1627–41 and 1E 1547–5408. These two transients show several similarities supporting the interpretation of Anomalous X-ray Pulsars and Soft Gamma-ray Repeaters as a single class of strongly magnetized neutron stars.     

Very Long Baseline Interferometry: Dependencies on Frequency Stability

Very Long Baseline Interferometry (VLBI) is a differential technique observing radiation of compact extra-galactic radio sources with pairs of radio telescopes. For these observations, the frequency standards at the telescopes need to have very high stability. In this article we discuss why this is, and we investigate exactly how precise the frequency standards need to be. Four areas where good clock performance is needed are considered: coherence, geodetic parameter estimation, correlator synchronization, and UT1 determination. We show that in order to ensure the highest accuracy of VLBI, stability similar to that of a hydrogen maser is needed for time-scales up to a few hours. In the article, we are considering both traditional VLBI where extra-galactic radio sources are observed, as well as observation of man-made artificial radio sources emitted by satellites or spacecrafts.     

一种主动悬架式火星车稳定裕度优化控制策略

针对火星车在非结构化环境下行驶存在的稳定性不足而导致倾覆的风险,提出针对一种六轮主动悬架式火星车的稳定裕度优化控制方法。首先,考虑了火星车悬架机构调整过程中车轮与接触地面滑移和侧倾等运动关系,建立和完善了六轮主动悬架式火星车行驶的运动学模型。然后,以火星车夹角调整机构角度为变量,推导火星车在非结构环境下的稳定裕度模型。之后,使用内点法求解火星车稳定裕度的最优解,并获得期望的夹角调整机构关节角度。在此基础上,对夹角调整机构的关节角度进行规划和控制,实现火星车悬架机构构型的调整,从而提高火星车在非结构化环境下行驶的稳定裕度。最后,对火星车稳定裕度优化控制策略的有效性进行仿真验证,结果表明,所提出的控制方法可有效提高火星车在非结构化环境下行驶的稳定裕度。     

The radiation environment in the ISS-USLab measured by ALTEA: Spectra and relative nuclear abundances in the polar,equatorial and SAA regions

We present here the energy spectra relative to different geomagnetic regions as measured by the ALTEA (Anomalous Long Term Effects on Astronauts) detector in the International Space Station – USLab from August 2006 to July 2007.     

Volatile Trapping in Martian Clathrates

Thermodynamic conditions suggest that clathrates might exist on Mars. Despite observations which show that the dominant condensed phases on the surface of Mars are solid carbon dioxide and water ice, clathrates have been repeatedly proposed to play an important role in the distribution and total inventory of the planet’s volatiles. Here we review the potential consequences of the presence of clathrates on Mars. We investigate how clathrates could be a potential source for the claimed existence of atmospheric methane. In this context, plausible clathrate formation processes, either in the close subsurface or at the base of the cryosphere, are reviewed. Mechanisms that would allow for methane release into the atmosphere from an existing clathrate layer are addressed as well. We also discuss the proposed relationship between clathrate formation/dissociation cycles and how potential seasonal variations influence the atmospheric abundances of argon, krypton and xenon. Moreover, we examine several Martian geomorphologic features that could have been generated by the dissociation of extended subsurface clathrate layers. Finally we investigate the future in situ measurements, as well as the theoretical and experimental improvements that will be needed to better understand the influence of clathrates on the evolution of Mars and its atmosphere.