有关阿姆斯特朗的传闻和真相

传闻：选择阿姆斯特朗做“阿波罗11”登月宇航员，是因为他的平民身份。白宫更希望第一个登陆月球的是普通老百姓，而不是军人。 真相：阿姆斯特朗能成为“阿波罗11”号的指令长。是因为他的不断进步。以及他在“双子座”航天飞机及早期“阿波罗”飞行任务中的表现。没人知道，他在成为“阿波罗11”号机组成员之前需要完成多少任务。     

人类行为：杀戮本性

“有人说，我们从我们的动物祖先身上继承了发动战争的倾向……战争以及其他所有的暴力行为都是在基因水平上被设定好，并且烙印在人类天性之中的……人类有一个‘暴力的大脑’……这些说法从科学上来讲都是不正确的。”     

“阿波罗11”号与UFO

“阿波罗11”号登月才过去几十年，但这一事件已经成为历史课本中的传奇，标志着人类第一次在另一个世界登陆，同时也展示了20世纪60年代美国的科技和组织、管理、协调能力。对U10领域的专家、粉丝以及反对者来说，“阿波罗11”号登月也意义非凡。多年以来，在这次史诗级的空间旅行中，一直有关于UFO的报告和照片流传。     

具有无源控制空腔时正激波/湍流附面层干扰的数值模拟

采用雷诺平均N-S方程和B/L代数湍流模型计算了具有无源控制空腔时正激波/湍流附面层干扰流场。计算与实验结果的比较表明,本文方法可较准确地预测激波结构、激波与附面层干扰区流动基本特征及波后流动分离状态、激波位置、波前马赫数等参数。      

测量燃烧室内温度时的热辐射修正

我们在进行某一环形燃烧室扇形形试验件的试验研究时,用热电偶测量了燃烧室内的温度分布。一般来说,热电偶不能获得与热燃气同样的温度,这是因为热电偶和周围环境有着辐射能量的交换。通常是热电偶节点向冷的壁面辐射能量。在稳态时,燃气通过对流传热向热电偶节点提供能量来平衡这一损失。这就是说,热电偶节点测得的温度较燃气的真实温度要低,这一温差就是由辐射热损失造成的。下面介绍对此热辐射损失进行修正的一个简化方法。      

21世纪士兵的新装备——微型无人飞行器

由于高能量储备和微型精确飞行控制技术的突破性进展,一种供士兵用的比鸟还小的微型侦察无人机已被列入美国国防研制计划     

高速空间光通信系统的研究动态

文章介绍了高速空间光通信系统在大气光通信和卫星光通信领域的研究发展动态,分析了高速空间光通信系统中有关关键技术,尤其是提高数据速率的DWDM、IOM以及EDFA等器件在长距离通信中的应用等技术,同时还涉及了自由空间光通信中大气光通信系统的可行性问题。     

Microbially induced iron precipitation associated with a neutrophilic spring at Borra Caves, Vishakhapatnam, India

The present investigation uncovers various pieces of evidence for the possible biologically induced mineralization in iron mats associated with a pH-neutral spring in the Borra caves, Vishakhapatnam, India. Electron microscopy [scanning electron microscopy (SEM) and transmission electron microscopy (TEM)] demonstrated large numbers of (i) hollow tubes (diameter ～1?μm) resembling sheaths of the iron-oxidizing bacteria Leptothrix, (ii) thin (diameter <1?μm) solid fibers of uncertain origin, (iii) nanoscale subspherical to irregularly shaped particles encrusting tubes and fibers, and (iv) aggregates of broken and partially disintegrated sheaths, fibers, and particles embedded in extracellular polymeric substances (EPS) occasionally including microbial cells. X-ray microanalyses by energy dispersive spectroscopy (EDS) revealed that the mat accumulated largely Fe but also smaller amounts of Si and traces of P and Ca. Particles rich in Si and Al (possibly kaolinite) and Ca (carbonate) were also observed. High-resolution TEM/EDS of unstained ultrathin sections suggests that microbial sheaths were highly mineralized by amorphous to cryptocrystalline Fe-rich phases and less frequently by other fine-grained and fibrous authigenic claylike minerals. Total number of microorganisms in the iron mats was 5.8×10(5) cells, g sed(-1) (wet weight). Analysis of the 16S rRNA gene diversity revealed microorganisms assigned to eight different phyla [Proteobacteria (62%), Chloroflexi (8%), Bacteroidetes (7%), Planctomycetes (1%), Actinobacteria (5%), Acidobacteria (6%), Nitrospira (1%), Firmicutes (5%)]. Within the Proteobacteria, Betaproteobacteria was the predominant class, which accounted for 28% of the sequences. Within this class some obvious similarities between the obtained sequences and sequences from other cave systems could be seen, especially sequences affiliated with Leptothrix, Siderooxidans, Crenothrix, Comamonadaceae, Dechloromonas, and many uncultured Betaproteobacteria. Four (4%) of the sequences could not be assigned to phylum level but were affiliating with the candidate division TM7 (2%), candidate division OP11 (1%), and candidate division WWE3 (1%). The results allow us to infer a possible relationship of microbial sheaths, EPS, and the iron precipitates to microbial community diversity in the Borra cave springs. Understanding biogenic iron oxides in caves has important astrobiological applications as it provides a potential tool for the detection of extraterrestrial life.     

Abundance and diversity of microbial inhabitants in European spacecraft-associated clean rooms

The determination of the microbial load of a spacecraft en route to interesting extraterrestrial environments is mandatory and currently based on the culturable, heat-shock-surviving portion of microbial contaminants. Our study compared these classical bioburden measurements as required by NASA's and ESA's guidelines for the microbial examination of flight hardware, with molecular analysis methods (16S rRNA gene cloning and quantitative PCR) to further develop our understanding of the diversity and abundance of the microbial communities of spacecraft-associated clean rooms. Three samplings of the Herschel Space Observatory and its surrounding clean rooms were performed in two different European facilities. Molecular analyses detected a broad diversity of microbes typically found in the human microbiome with three bacterial genera (Staphylococcus, Propionibacterium, and Brevundimonas) common to all three locations. Bioburden measurements revealed a low, but heterogeneous, abundance of spore-forming and other heat-resistant microorganisms. Total cell numbers estimated by quantitative real-time PCR were typically 3 orders of magnitude greater than those determined by viable counts, which indicates a tendency for traditional methods to underestimate the extent of clean room bioburden. Furthermore, the molecular methods allowed the detection of a much broader diversity than traditional culture-based methods.     

The PROCESS experiment: an astrochemistry laboratory for solid and gaseous organic samples in low-earth orbit

The PROCESS (PRebiotic Organic ChEmistry on the Space Station) experiment was part of the EXPOSE-E payload outside the European Columbus module of the International Space Station from February 2008 to August 2009. During this interval, organic samples were exposed to space conditions to simulate their evolution in various astrophysical environments. The samples used represent organic species related to the evolution of organic matter on the small bodies of the Solar System (carbonaceous asteroids and comets), the photolysis of methane in the atmosphere of Titan, and the search for organic matter at the surface of Mars. This paper describes the hardware developed for this experiment as well as the results for the glycine solid-phase samples and the gas-phase samples that were used with regard to the atmosphere of Titan. Lessons learned from this experiment are also presented for future low-Earth orbit astrochemistry investigations.