热压压力对B/Al复合材料组织结构及力学性能的影响

使用表面覆有B4C涂层的硼纤维，采用大气等离子喷涂法制备连续硼纤维增强铝基复合材料预制片，结合真空热压扩散焊制备了纤维均匀分布的B／Al复合材料。探讨在接近铝基体熔点温度的条件下热压压力对复合材料力学性能与B／Al界面结合的影响，分析了B／Al界面结合状态与断口形貌及力学性能之间的关系。研究表明：热压压力对制备的B／Al复合材料的纤维体积分数、B纤维与Al基体的界面结合状态和拉伸强度有显著的影响；纤维表面的B4c涂层有效地防止了B纤维与Al基体间的界面反应，在温度6500C、压力10MPa的条件下，制备的纤维体积分数为42％的B／Al复合材料拉伸强度达到968MPa，达到了纤维理想强度的77％。     

Studies of anomalous potential drops due to ion density inhomogeneities

The dynamic response of a 1-dimensional plasma diode to an applied step voltage is studied during a few electron transit times by numerical simulations when the initial state has an ion density minimum (an ion density cavity). Depending on the cavity depth and the applied voltage the potential drop distributes over the cavity or concentrates in a cathode sheath. The transistion between the two states as well as the cavity potential profiles are predicted by an analytical model. Simulations with periodic cavities as initial state show that the applied voltage can be shared between the cavities. A double layer, steady on the ion time scale, is created by introducing a steady cavity by ion losses.     

Statistical description of low-latitude plasma blobs as observed by DMSP F15 and KOMPSAT-1

The global distribution of low-latitude plasma blobs was investigated by in-situ plasma density measurements from the Korea Multi-Purpose Satellite-1 (KOMPSAT-1) and Defense Meteorological Satellite Program (DMSP) F15. In the observations, blobs occurred in the longitude sector where the activity of the equatorial plasma bubble (EPB) was appreciable, and additional blobs were found at the lower (KOMPSAT-1) altitude as in the EPBs. However, several notable differences exist between the distributions of EPBs and blobs. First, KOMPSAT-1 found few blobs around 0°E in March and June, as did DMSP F15 from 30°W to 120°E for every season. Second, the overall occurrences in December and March at the DMSP F15 (840 km) altitude were somewhat lower than expected from those of the EBPs. Third, at the DMSP F15 altitude, the occurrence probability of plasma blobs was less controlled by yearly variations in the solar activity. These results imply that topside ionospheric conditions as well as the existence of EPBs control further development of blobs. Additionally, it was found that the blob latitudes became higher as the yearly solar activity increased. Moreover, most of the blobs were encountered in the winter hemisphere, possibly due to the low ambient density.     

A 2-D comparison of ionospheric convection derived from SuperDARN and DMSP measurements

Ion drift vectors measured by the DMSP satellites are compared with plasma convection vectors obtained by the SuperDARN HF radars through the standard Map Potential algorithm of Ruohoniemi and Baker [Ruohoniemi, M., Baker, K.B. Large-scale imaging of high-latitude convection with super dual auroral radar network HF radar observations. J. Geophys. Res. 103, 20797–20811, 1998]. Despite significant data spread, the agreement can be qualified as reasonable for a data set comprising of 149 satellite passes over the Northern Hemisphere at high latitudes. The slope of the best-fit line relating SuperDARN and DMSP velocity magnitudes is of the order of 0.3 with a tendency for the SuperDARN velocities to be smaller. The agreement between the azimuths of the ion drift and convection is better with the slope of the best-fit line being close to 1. It is shown that consistency between the radar and satellite measurements is much better if the SuperDARN line-of-sight velocities are compared with the DMSP cross-track ion drifts for events showing slow spatial and temporal variations of the convection. If areas of strong convection changes are included into comparison, the degree of agreement deteriorates drastically. This result implies that differences in the spatial and temporal resolutions of DMSP and SuperDARN measurements are crucial factors contributing to the observed discrepancies. In addition, some differences are introduced when the SuperDARN line-of-sight velocities are filtered and reprocessed into vectors with the application of a background convection model.     

RPC-MIP: the Mutual Impedance Probe of the Rosetta Plasma Consortium

The main objective of the Mutual Impedance Probe (MIP), part of the Rosetta Plasma Consortium (RPC), is to measure the electron density and temperature of Comet 67P/Churyumov-Gerasimenko’s coma, in particular inside the contact surface. Furthermore, MIP will determine the bulk velocity of the ionised outflowing atmosphere, define the spectral distribution of natural plasma waves, and monitor dust and gas activities around the nucleus. The MIP instrumentation consists of an electronics board for signal processing in the 7 kHz to 3.5 MHz range and a sensor unit of two receiving and two transmitting electrodes mounted on a 1-m long bar. In addition, the Langmuir probe of the RPC/LAP instrument that is at about 4 m from the MIP sensor can be used as a transmitter (in place of the MIP ones) and MIP as a receiver in order to have access to the density and temperature of plasmas at higher Debye lengths than those for which the MIP is originally designed.     

The Cold-Dense Plasma Sheet: A Geotail Perspective

GEOTAIL observations of the low-latitude boundary layer (LLBL) in the tail-flanks show that they are the region where the cold-dense plasma appears with stagnant flow signatures accompanied by bi-directional thermal electrons (< 300 eV). It is concluded from these facts that the tail-LLBL is the site of capturing the cold-dense plasma of the magnetosheath origin on to the closed field lines of the magnetosphere. There are also cases that strongly suggest that the cold-dense plasma entry from the flanks can be significant to fill a substantial part of the magnetotail. In such cases, the cold-dense plasma is not spatially restricted to a layer attached to the magnetopause (that is, the LLBL), but continues to well inside the magnetotail, constituting the cold-dense plasma sheet. Inspired by the fact that these remarkable cases are found for northward interplanetary magnetic field (IMF), a statistical study on the status of the near-Earth plasma sheet is made. The results show that the plasma sheet becomes significantly colder and denser when the northward IMF continues than during southward IMF periods, and that the cold-dense status appears most prominently near the dawn and dusk flanks. These are consistent with the idea that, during northward IMF periods, the supply of cold-dense ions to the near-Earth tail from the flanks dominates over the hot-tenuous ions transported from the distant tail.     

电子环束流对航天器表面电位和等离子体鞘层的影响

采用二维三分量静电粒子模拟程序研究了电子环束流对低轨道磁化等离子体中运行的航天器表面电位和等离子体鞘层结构的影响.当有电子束流平行磁场入射时,航天器表面所带负电位的绝对值将增大.电子束流的速度和密度的增加将使航天器表面负电位绝对值增加很快.与此同时等离子体鞘层的尺度也将增大,形状将由向尾部延伸的“泪滴”状变成向两侧展开的“机翼”状.当电子环束流以相对于磁场成一定角度斜入射时,由于磁场的约束作用,航天器表面负电位的绝对值将随入射角增大而减小.      

小功率电弧等离子体发动机试验及性能研究

电推进技术已应用于航天的多个领域,电弧等离子体发动机（Arcjet)因其高比冲、高推力／功率比以及大的推进剂选择范围等特点成为当前国际上电火箭研究和应用的热点。文章总结小功率Arcjet实验及性能研究,介绍了实验研究系统的主要组成,给出初步的发动机工作性能参数及实验结果分析。     

Charge-product control approach to electrostatic leader-follower formations in LEO plasma wakes

The feasibility of using electrostatic forces to stabilize a close-proximity leader-follower formation is investigated. The leader craft is equipped with a set of affixed spheres whose charge is modulated to hold the charged follower craft along a proscribed trajectory to its nominal leader-relative position. This charge structure and the follower craft are constrained to remain in the plasma wake generated behind all LEO craft because the more-dense ambient plasma outside the wake prevents object charging and electric field propagation. Once the formation is achieved, a controlled electric field is generated by the leader to counter relative accelerations from perturbations like differential drag and solar radiation pressure, holding the follow near its nominal position. Two controllers are derived for the system described, incorporating Coulomb accelerations and linearized gravity and drag accelerations. Simulations are run under unmodeled perturbations and sensor noise for different scenarios, demonstrating the challenges and benefits associated with electrostatic actuation.     

基于碱金属辅助电离的等离子鞘套模拟方法

为解决再入过程中通信黑障与探测异常问题，对等离子体鞘套地面模拟方法进行了研究。以RAM C-II 飞行试验为依据，计算了等离子体鞘套的参数范围。分析现有模拟设备，概括提出了高焓低速风洞的模拟方案，选取相适应的放电方式，并对流量功率进行了计算。针对高温环境对电磁设备造成损坏以及所需功率难以实现的问题，提出添加碱金属的解决方案，并进行了试验验证。试验结果表明，添加碱金属可以使电子密度提升约一个数量级。对方案效果进行评估，预期功率需求降至兆瓦量级。