Four-month Moon and Mars crew water utilization study conducted at the Flashline Mars Arctic Research Station,Devon Island,Nunavut

A categorized water usage study was undertaken at the Flashline Mars Arctic Research Station on Devon Island, Nunavut in the High Canadian Arctic. This study was conducted as part of a long duration four-month Mars mission simulation during the summer of 2007. The study determined that the crew of seven averaged 82.07 L/day over the expedition (standard deviation 22.58 L/day). The study also incorporated a Mars Time Study phase which determined that an average of 12.12 L/sol of water was required for each crewmember. Drinking, food preparation, hand/face, oral, dish wash, clothes wash, shower, shaving, cleaning, engineering, science, plant growth and medical water were each individually monitored throughout the detailed study phases. It was determined that implementing the monitoring program itself resulted in an approximate water savings of 1.5 L/day per crewmember. The seven person crew averaged 202 distinct water draws a day (standard deviation 34) with high water use periods focusing around meal times. No statistically significant correlation was established between total water use and EVA or exercise duration. Study results suggest that current crew water utilization estimates for long duration planetary surface stays are more than two times greater than that required.     

A review of observed variability in the dayside ionosphere of Mars

Recent measurements by Mars Global Surveyor and Mars Express have greatly increased the number of observations of the martian dayside ionosphere available for study. Together with earlier measurements from the Viking era, these datasets have been used to investigate variations in well-known properties of the martian dayside ionosphere and to discover new ionospheric features. The dayside ionosphere includes the main peak, called the M2 layer, and a lower layer, called the M1 layer. In the topside, above the M2 layer, electron densities exponentially decrease with increasing altitude.     

火星空间大尺度电流体系分布特征

在MHD模型基础上, 对火星空间环境的电流分布进行了模拟. 结果表明, 火星空间存在着弓激波电流、磁堆积区电流、电离层电流和磁尾电流. 弓激波电流在激波曲面上均由北向南自成体系, 电流密度在弓激波顶区域较大. 在向阳面磁堆积区边界电流与电离层电流彼此耦合形成完整的回路, 在背阳面磁堆积区边界电流与磁尾中心电流片耦合形成完整的回路.     

计算风工程中 k-ε模型的边界条件研究

从 k-ε湍流模型控制方程入手,对两类满足平衡大气边界层理论要求的入口边界条件进行了详细分析,比较了二者的理论差异。然后以我国公路桥梁抗风规范中建议的 A 类风场为来流条件,定义了相应的 k-ε模型常数与壁面条件,使用两类边界条件进行数值模拟。计算结果表明：两类边界条件结合相应的模型常数与壁面条件,均能在数值模拟中构建基本满足规范要求的平衡大气边界层,但各有其适用范围。在此基础上,对模型常数 C 1和湍动能耗散率与数值模拟结果之间的关系进行了研究,采用修改模型常数与边界条件的方法,改善了数值模拟结果。     

航空发动机燃油系统及其附件爆炸大气试验技术研究

燃油系统及其附件爆炸大气试验在航空发动机研制过程中极其重要。简述了航空发动机燃油系统及其附件爆炸大气试验技术的特点及国内外发展现状,分析了其试验技术发展需求。详细给出了航空发动机燃油系统及其附件爆炸大气试验的分类、试验要求、试验条件、试验方法和试验判据,并开展了某型航空发动机燃油系统液压机械装置爆炸大气试验验证。结果表明:该试验方案可行、数据可靠、结果有效,为航空发动机燃油系统及其附件爆炸大气试验的研究验证工作提供了依据。     

火星探测无动力借力飞行轨道研究

对无动力情形的借金星引力辅助变轨进行了研究,并完成了火星探测轨道的设计;首 先使用Jacobi积分得到了蒂塞朗准则,在利用速度矢量图对借力飞行轨道的特性进行分析后 ,得到了Williams提出的C3匹配法,证明了蒂塞朗准则和C3匹配的同一性;在 搜索借力飞行的可行性转移轨道中,采用C3匹配对借金星引力的火星探测轨道进行了 仿真,并对结果进行了分析,最后使用蒂塞朗准则对C3匹配的仿真结果进行了检验。     

生长军官学员学风评价研究

根据军队院校教育的特点和规律构建了生长军官学员学风评价的指标体系,提出了学风评价的数学模型,依据指标体系和数学模型对某军校进行了学员学风实测,在此基础上进行了分析研究。     

Ozone chemical equilibrium in the extended mesopause under the nighttime conditions

For retrieval of atomic oxygen and atomic hydrogen via ozone observations in the extended mesopause region (～70–100?km) under nighttime conditions, an assumption on photochemical equilibrium of ozone is often used in research. In this work, an assumption on chemical equilibrium of ozone near mesopause region during nighttime is proofed. We examine 3D chemistry-transport model (CTM) annual calculations and determine the ratio between the correct (modeled) distributions of the O₃ density and its equilibrium values depending on the altitude, latitude, and season.The results show that the retrieval of atomic oxygen and atomic hydrogen distributions using an assumption on ozone chemical equilibrium may lead to large errors below ～81–87?km. We give simple and clear semi-empirical criterion for practical utilization of the lower boundary of the area with ozone’s chemical equilibrium near mesopause.     

火星表面风沙物理过程及沙尘暴的起动风速

通过建立风吹动地表沙粒运动的模型并根据大气湍流边界层风速廓线规律,计算了火星上沙尘暴的起动风速和沙尘暴发生时空中悬浮沙尘粒径的大小,并对沙粒从地面跳起进入气流的方式进行了验证.发现当大气为中性层结时,火星沙尘暴的起动需要离地面2m高处的风速达到28.7m·s^-1.在起动临界风速下,地表沙粒需要滚动一个粒径的距离才能跳起,沙尘暴发生后,火星大气中悬浮沙尘的粒径小于30μm.     

用于火星表面生命信息探测的激光拉曼技术进展

生命信息探测一直是深空探测中重要的一个部分。简要介绍了拉曼光谱技术探测有机物的优势和火星生命信息探测进展,以及常见的火星生命信息探测技术;重点概述了国内外用于火星有机物和生命信息探测的激光拉曼光谱技术的进展,分析总结了火星表面有机物质探测技术的发展趋势;最后简要概述了拉曼光谱技术在火星探测领域的发展前景。