纳米压痕实验微米级深度硬度下降现象的研究(英文)

本文针对均匀材料微米级压痕深度,分析接触深度、接触面积、载荷以及加载时间几种因素对实验数据的影响,结合有限元数值模拟,说明压头几何缺陷、接触深度与接触面积的处理并不是造成微米级压痕硬度随压深增大而下降的主要原因,最可能的原因是材料的蠕变特性。进行了不同最大压深实验显示连续刚度法(CSM)将强化蠕变特性对硬度曲线的影响,证明造成该现象的重要原因是纳米压痕实验的实验方法问题。     

形貌和空间对PAEK增韧BMI树脂及其碳纤维复合材料层压板韧性和冲击损伤阻抗的影响(英文)

通过对热塑性树脂PAEK增韧BMI树脂的玻璃化转变行为,相形貌和断裂韧性,以及对采用"离位"概念增韧的T700/BMI复合材料的层间形貌及其冲击后压缩强度(CAI)的分析,研究了微结构-性能之间的关系,发现特征相分离形貌随着PAEK的含量而变化。特别探索了PAEK-BMI复相体系的相形貌与断裂韧性之间的关系,得到的断裂机理解释了复合材料层压板的分层和冲击损伤行为。有关"离位"增韧的机理、以及扩散控制的相行为等还需要继续研究。     

威布尔分布三参数估计的模糊—随机方法

提出了威布尔分布三参数估计的模糊－随机方法，并对蒙特卡罗方法产生的随机样本进行了验证，结果表明，求得的参数估计值十分接近理论值。     

嵌套网格粘性流动数值模拟用于风洞洞壁干扰研究

运用嵌套网格技术和Navier Stokes数值模拟对机翼半模和翼身组合体试验时风洞的四壁干扰进行综合模拟、评估和修正。计算格式在空间上采用中心有限体积离散 ,在时间上采用多步Runge Kutta时间步长格式进行积分。计算结果证明了该方法的可行性和优越性。     

Decomposition of sodium formate and L- and D-alanine in the Pampas de La Joya soils: Implications as a new geochemical analogue to Martian regolith

The organic compounds on the Martian surface are still undetectable by the previous Viking mission that has been sent to Mars even though they are expected to be there by exogenous and/or endogenous synthesis. The high abiotic reactivity has been the most acceptable explanation for the apparently absence of organic matter in the regolith.     

Plasma Morphology at Mars. Aspera-3 Observations

A total of about of 400 orbits during the first year of the ASPERA-3 operation onboard the Mars Express spacecraft were analyzed to obtain a statistical pattern of the main plasma domains in the Martian space environment. The environment is controlled by the direct interaction between the solar wind and the planetary exosphere/ionosphere which results in the formation of the magnetospheric cavity. Ionospheric plasma was traced by the characteristic “spectral lines” of photoelectrons that make it possible to detect an ionospheric component even far from the planet. Plasma of solar wind and planetary origin was distinguished by the ion mass spectrometry. Several different regions, namely, boundary layer/mantle, plasma sheet, region with ionospheric photoelectrons, ray-like structures near the wake boundary were identified. Upstream parameters like solar wind ram pressure and the direction of the interplanetary electric field were inferred as proxy from the Mars Global Surveyor magnetic field data at a reference point of the magnetic pile up region in the northern dayside hemisphere. It is shown that morphology and dynamics of the main plasma domains and their boundaries are governed by these factors as well as by local crustal magnetizations which add complexity and variability to the plasma and magnetic field environment.     

简单控制规律下涡喷发动机特性的研究

研究了用于无人飞行器上使用的小推力级涡喷发动机在简单控制规律下的多种重要特性。通过计算横模拟方法，重点研究某型发动机的设计点性能装订方法、不同进口温度条件下发动机的稳定工作裕度以及发动机能够适应的飞行包线，并揭示了发动机的一些潜在的缺点。计算结果在发动机设计、生产和使用过程中有重要的指导意义。     

基于运动嵌套网格的前飞旋翼绕流N-S方程数值计算

 通过求解 Navier-Stokes方程数值模拟了直升机旋翼前飞非定常流场。为了模拟包括旋转、周期性变距和周期性挥舞的非定常运动,采用了一种能够快速完成重叠网格间流场信息交换的运动嵌套网格方法。空间上采用中心平均的有限体积法进行离散,时间方向应用含隐式子迭代的双时间法推进求解。为了验证程序的正确性,数值计算了一有升力悬停流场,旋翼桨叶表面压力分布的计算值与实验值吻合很好。     

Response of the ionospheric F-region in the Brazilian sector during the super geomagnetic storm in April 2000 observed by GPS

The response of the ionospheric F-region in the equatorial and low latitude regions in the Brazilian sector during the super geomagnetic storm on 06–07 April 2000 has been studied in the present investigation. The geomagnetic storm reached a minimum D_st of −288 nT at 0100 UT on 07 April. In this paper, we present vertical total electron content (VTEC) and phase fluctuations (in TECU/min) from GPS observations obtained at Imperatriz (5.5°S, 47.5°W; IMPZ), Brasília (15.9°S, 47.9°W; BRAZ), Presidente Prudente (22.12°S, 51.4°W; UEPP), and Porto Alegre (30.1°S, 51.1°W; POAL) during the period 05–08 April. Also, several GPS-based TEC maps are presented from the global GPS network, showing widespread and drastic TEC changes during the different phases of the geomagnetic storm. In addition, ion density measurements on-board the satellite Defense Meteorological Satellite Program (DMSP) F15 orbiting at an altitude of 840 km and the first Republic of China satellite (ROCSAT-1) orbiting at an altitude of 600 km are presented. The observations indicate that one of the orbits of the DMSP satellite is fairly close to the 4 GPS stations and both the DMSP F15 ion-density plots and the phase fluctuations from GPS observations show no ionospheric irregularities in the Brazilian sector before 2358 UT on the night of 06–07 April 2000. During the fast decrease of D_st on 06 April, there is a prompt penetration of electric field of magnetospheric origin resulting in decrease of VTEC at IMPZ, an equatorial station and large increase in VTEC at POAL, a low latitude station. This resulted in strong phase fluctuations on the night of 06–07 April, up to POAL. During the daytime on 07 April during the recovery phase, the VTEC observations show positive ionospheric storm at all the GPS stations, from IMPZ to POAL, and the effect increasing from IMPZ to POAL. This is possibly linked to the equatorward directed meridional wind. During the daytime on 08 April (the recovery phase continues), the VTEC observations show very small negative ionospheric storm at IMPZ but the positive ionospheric storm effect is observed from BRAZ to POAL possibly linked to enhancement of the equatorial ionospheric anomaly.     

Effects observed in the ionospheric F-region in the South American sector during the intense geomagnetic storm of 14 December 2006

This investigation presents observations related to the generation of equatorial ionospheric irregularities (also known as equatorial spread F (ESF)) including ionospheric plasma bubbles and dynamic behavior of the ionospheric F-region in the South American sector during an intense geomagnetic storm in December 2006 (a period of low solar activity). In this work, ionospheric sounding observations and GPS data obtained between 13 and 16 December 2006 at several stations in the South American sector are presented. On the geomagnetically disturbed night of 14 and 15 December, ionospheric plasma bubbles were observed after an unusual uplifting of the F-region during pre-reversal enhancement (PRE) period. The unusual uplifting of the F-region during PRE was possibly associated with prompt penetration of electric field of magnetospheric origin. During the geomagnetic disturbance night of 14 and 15 December, strong oscillations due to the propagation of traveling ionospheric disturbances (TIDs) by the Joule heating in the auroral region were observed in the F-region at São José dos Campos (SJC, 23.2°S, 45.9°W; dip latitude 17.6°S), Brazil, and Port Stanley (PST, 51.6°S, 57.9°W; geom. latitude 41.6°S). The VTEC-GPS observations presented on the night of 14 and 15 December 2006 show both positive and negative storm phases in the South American sector, possibly due to changes in the large-scale wind circulation and changes in the O/N₂ ratio in the southern hemisphere, respectively.