高性能高强砼的设计推荐规程

高性能高强砼是目前国际上发展起来的一种新技术，国外较步较早，并已有了各自的设计规范。本文仅对此作一简单的介绍，以供国内的同仁们参考和借鉴。     

采用实时MTI处理的双通道雷达系统的飞行试验结果

讨论了实时空时自适应处理（STAP）的两种应用：首先是STAP可以用来抑制杂波和干扰；此外可以用由STAP获得的杂波滤波系数来确定SAR图像中动目标的正确位置。给出了这种实时STAP技术的结果和动目标重新定位技术的结果。用实际SAR数据和测量期间所记录的动目标验证了杂波抑制质量和动目标重新定位精度。     

DAIS航空电子软件研制技术

软件研制技术的主要目的是产生正确的工作软件.把本文提供的技术应用于一个完整的软件工程研制计划时,可降低产品的价格和寿命期费用,同时保持了高可靠性。空军 DAIS 计划担负着降低军用航空电子系统的研制、维护和寿命期费用的任务.DAIS 系统提供了一种硬件配置,该配置便于硬件维修、更换和增长.高级软件(HOS)提供一种产生高可靠性软件的方法,此软件是建立在一种高级的设计和开发基础上的.HOS 原理应用于 DAIS 系统,产生了标准的航空电子软件设计和管理方法,该设计方法建立了一个与 DAIS 目标相一致的软件结构标准;该管理方法提供了一种严格受控的、安排很好的软件开发过程,该过程受配置管理方案、开发和验证方法及自动生成文件支持。这里没有给出另一些软件费用因素是:软件的获得过程、人力的安排和组织、航空电子系统方案和支援软件的可移植性。这些费用因素是重要的,因为处理得不合理时,有时会发挥不出好的开发技术的益处。本文假定这些因素不影响 DAIS 航空电子软件所使用的技术。     

煤油在超声速气流中非定常横向喷射的实验观察

本文目的是研究煤油在超声速气流中非定常横向喷射问题,并与静止和亚声速气流中的结果进行对比。改造普通油嘴并采用单次高压燃油喷射系统,得到不同延时的流场阴影照片。结果表明：在超声速气流中,射流柱破碎是由迎风面的表面波引起的,破碎点位于表面波的波谷。雾化过程过分四个区域。射流激波由近射流柱的迎风面,并在人壁反射,非定常喷射的波系演化复杂。煤油在亚声速气流中喷射,不存在射流激波,破碎点沿射流柱上移,穿透深     

空间激光通信技术最新进展与趋势

空间激光通信技术已成为现代超宽带卫星通信技术发展的新焦点。详细介绍了美国、欧洲和日本在空间激光通信技术领域的最新研究进展和发展规划,重点介绍他们正在开发的第2代空间激光通信系统的主要性能指标和采用的新技术,深入分析了国际空间激光通信技术的发展趋势,为我国开展相关研究提供借鉴和思路。     

航天飞机指控中心Unix工作站中专家系统的实时数据获取

最具代表性的美国技术杰作之一可能是位于德克萨斯州休斯顿的约翰逊航天中心的航天指挥控制中心(MCC)。该中心各指挥室经历了美国技术史上许多重大事件,如首次登月、营救天空实验室以及首次发射航天飞机。60年代初MCC首次启用时,的确是技术杰作。然而该设施自阿波罗任务后只进行过不大的改进。直到最近,它仍然维持着以单主机的结构,     

Modelling of Geomagnetic Storm Effects in the Ionosphere of East Asia

This paper presents simulated results of the ionospheric behavior during few geomagnetic storms,which were occurred in the different seasons. The numerical model for ionosphere-plasmasphere coupling was used to interpret the observed variation of ionosphere structure. Reasons why the positive storms are dominant in the winter whereas the negative ones are dominant in the summer season present the special interest for the mid-latitude ionosphere. A theoretical analysis of the processes controlling the ionospheric response to the geomagnetic storms has showed a good agreement between the simulated results and measurements, as well as the crucial role of the neutral composition variations to fit the calculated and the observed ionospheric parameters.      

Hydrogeologic controls on episodic H2 release from precambrian fractured rocks--energy for deep subsurface life on earth and mars

Dissolved H(2) concentrations up to the mM range and H(2) levels up to 9-58% by volume in the free gas phase are reported for groundwaters at sites in the Precambrian shields of Canada and Finland. Along with previously reported dissolved H(2) concentrations up to 7.4 mM for groundwaters from the Witwatersrand Basin, South Africa, these findings indicate that deep Precambrian Shield fracture waters contain some of the highest levels of dissolved H(2) ever reported and represent a potentially important energy-rich environment for subsurface microbial life. The delta (2)H isotope signatures of H(2) gas from Canada, Finland, and South Africa are consistent with a range of H(2)-producing water-rock reactions, depending on the geologic setting, which include both serpentinization and radiolysis. In Canada and Finland, several of the sites are in Archean greenstone belts characterized by ultramafic rocks that have under-gone serpentinization and may be ancient analogues for serpentinite-hosted gases recently reported at the Lost City Hydrothermal Field and other hydrothermal seafloor deposits. The hydrogeologically isolated nature of these fracture-controlled groundwater systems provides a mechanism whereby the products of water-rock interaction accumulate over geologic timescales, which produces correlations between high H(2) levels, abiogenic hydrocarbon signatures, and the high salinities and highly altered delta (18)O and delta (2)H values of these groundwaters. A conceptual model is presented that demonstrates how periodic opening of fractures and resultant mixing control the distribution and supply of H(2) and support a microbial community of H(2)-utilizing sulfate reducers and methanogens.     

Microbial populations in Antarctic permafrost: biodiversity, state, age, and implication for astrobiology

Antarctic permafrost soils have not received as much geocryological and biological study as has been devoted to the ice sheet, though the permafrost is more stable and older and inhabited by more microbes. This makes these soils potentially more informative and a more significant microbial repository than ice sheets. Due to the stability of the subsurface physicochemical regime, Antarctic permafrost is not an extreme environment but a balanced natural one. Up to 10(4) viable cells/g, whose age presumably corresponds to the longevity of the permanently frozen state of the sediments, have been isolated from Antarctic permafrost. Along with the microbes, metabolic by-products are preserved. This presumed natural cryopreservation makes it possible to observe what may be the oldest microbial communities on Earth. Here, we describe the Antarctic permafrost habitat and biodiversity and provide a model for martian ecosystems.