爆炸冲击载荷下典型机身结构动响应及破坏

确定满足适航要求的最小风险炸弹位置,必须研究爆炸冲击载荷下机身结构动响应及破坏模式。以某型飞机典型机身结构为研究对象,采用LS-DYNA商用软件,建立了爆炸冲击载荷下机身典型结构动响应数值模型。采用控制变量法分析了爆炸物当量、爆炸冲击距离以及爆炸冲击位置对典型机身结构动响应及破坏模式的影响,同时研究了损伤后典型机身结构的剩余强度。研究结果表明,造成机身结构有效破坏的爆炸物临界当量与爆炸冲击距离密切相关;爆炸冲击距离对典型机身结构损伤及剩余强度影响不明显;典型机身结构筋条位置对剩余强度影响较大。在此基础上,提出了表征剩余强度的无量纲系数,并建立了剩余强度无量纲系数与爆炸物当量及爆炸冲击距离之间的函数关系。     

A stationary bow shock model for plasmas: The spherical blunt obstacle problem

We present an analytic model of a stationary bow shock which describes the interaction between a supermagnetosonic ambient wind and an obstacle with spherical-like frontal shape. We develop expressions for the bow shock’s geometry and the physical properties of the plasma sheath as functions of the upstream conditions. The solution is limited to magnetic fields parallel to the upstream velocity. The model allows to use any value of the upstream alfvenic and sonic Mach numbers and the polytropic index (γ$\gamma$), pointing out the influence of γ$\gamma$ for the magnetosheath compression and the bow shock shape. When both Mach numbers are small, the upstream magnetic field intensity affects also the bow shock shape. We compare our results with other models finding important consistencies. We also compare our results with in-situ data, we fund a reasonable qualitative agreement; however, it seems that our model underestimates the magnetosheath size.     

Numerical modeling of propagation of breaking nonlinear acoustic-gravity waves from the lower to the upper atmosphere

Acoustic-gravity waves (AGWs) observed in the upper atmosphere may be generated near the Earth’s surface due to a variety of meteorological sources. Two-dimensional simulations of vertical propagation and breaking of nonlinear AGWs in the atmosphere are performed. Forcing near the Earth’s surface is used as the AGW source in the model. We use a numerical method based on finite-difference analogues of fundamental conservation laws for solving atmospheric hydrodynamic equations. This approach selects physically correct generalized solutions of the wave hydrodynamic equations. Numerical simulations are performed in a representative region of the Earth’s atmosphere up to altitude 500 km. Vertical profiles of temperature, density, molecular viscosity and heat conductivity were taken from the standard atmosphere model MSIS-90 for January. Calculations were made for different amplitudes and frequencies of lower boundary wave forcing. It is shown that after activating the tropospheric wave forcing, the initial pulse of AGWs may very quickly propagate to altitudes of 100 km and above and relatively slowly dissipate due to molecular viscosity and heat conduction. This may increase the role of transient nonstationary waves in effective energy transport and variations of atmospheric parameters and gas admixtures in a broad altitude range.     

Effects of sintering temperature and time on defect evolution and compression properties of Ti-Al3Ti laminated composites

For metal-intermetallic laminated composites, various types of defects often occur during the preparation process. This paper studied the evolution and formation mechanism of defects,such as pores, tunnel cracks, and delamination cracks in Ti-Al₃Ti laminated composites prepared by vacuum hot-pressing method. Moreover, quasi-static and dynamic compression tests were performed to study the effects of pores and delamination cracks on the compression properties of the composites. The resu...     

连续旋转爆震波细致结构及自持机理

基于化学非平衡流解耦方法和详细化学反应机理,在0.1mm的网格尺度下对连续旋转爆震波内流场和爆震波平掠惰性气体界面的传播过程进行了数值模拟。详细分析了连续旋转爆震波的空间结构,由于在出口侧无几何约束,受一系列稀疏波的影响,旋转爆震波强度受到不同程度的削弱,形状也发生了相应的变化。爆震波平掠惰性气体界面时的流场分布与连续旋转爆震波结构极为类似,对比研究了波前可燃气体层高度对爆震波结构和传播过程的影响,当爆震波高度较小时,其抵御惰性气体侧稀疏波衰减的能力弱,波阵面严重变形,爆震波解耦。若爆震波要稳定自持传播,其必须要达到一定的临界高度来抵御稀疏波的影响。     

异种金属材料磁脉冲焊接技术

通过对磁脉冲焊接技术结合机理的阐述,采用5A03Al-5A06Al、1050Al-AZ31Mg异种金属材料进行焊接试验.对所得的焊接接头进行气密性试验和剥离试验,检测其结合质量;结合光学显微镜,对比分析Al-Al、Al-Mg焊接接头的微观形貌特点;并采用SEM/EDS分析界面附近的元素分布;最后通过硬度试验,检测接头界...     

Lower ionosphere response to external forcing: A brief review

There are two ways of external forcing of the lower ionosphere, the region below an altitude of about 100 km: (1) From above, which is directly or indirectly of solar origin. (2) From below, which is directly or indirectly of atmospheric origin. The external forcing of solar origin consists of two general factors – solar ionizing radiation variability and space weather. The solar ionization variability consist mainly from the 11-year solar cycle, the 27-day solar rotation and solar flares, strong flares being very important phenomenon in the daytime lower ionosphere due to the enormous increase of the solar X-ray flux resulting in temporal terminating of MF and partly LF and HF radio wave propagation due to heavy absorption of radio waves. Monitoring of the sudden ionospheric disturbances (SIDs – effects of solar flares in the lower ionosphere) served in the past as an important tool of monitoring the solar activity and its impacts on the ionosphere. Space weather effects on the lower ionosphere consist of many different but often inter-related phenomena, which govern the lower ionosphere variability at high latitudes, particularly at night. The most important space weather phenomenon for the lower ionosphere is strong geomagnetic storms, which affect substantially both the high- and mid-latitude lower ionosphere. As for forcing from below, it is caused mainly by waves in the neutral atmosphere, i.e. planetary, tidal, gravity and infrasonic waves. The most important and most studied waves are planetary and gravity waves. Another channel of the troposphere coupling to the lower ionosphere is through lightning-related processes leading to sprites, blue jets etc. and their ionospheric counterparts. These phenomena occur on very short time scales. The external forcing of the lower ionosphere has observationally been studied using predominantly ground-based methods exploiting in various ways the radio wave propagation, and by sporadic rocket soundings. All the above phenomena are briefly mentioned and some of them are treated in more detail.     

Gravitational wave detection on the Moon and the moons of Mars

The Moon and the moons of Mars should be extremely quiet seismically and could therefore become sensitive gravitational wave detectors, if instrumented properly. Highly sensitive displacement sensors could be deployed on these planetary bodies to monitor the motion induced by gravitational waves. A superconducting displacement sensor with a 10-kg test mass cooled to 2 K will have an intrinsic instrument noise of 10⁻¹⁶ m Hz^−1/2. These sensors could be tuned to the lowest two quadrupole modes of the body or operated as a wideband detector below its fundamental mode. An interesting frequency range is 0.1–1 Hz, which will be missed by both the ground detectors on the Earth and LISA and would be the best window for searching for stochastic background gravitational waves. Phobos and Deimos have their lowest quadrupole modes at 0.2–0.3 Hz and could offer a sensitivity h_min ? 10⁻²² Hz^−1/2 within their resonance peaks, which is within two orders of magnitude from the goal of the Big Bang Observer (BBO). The lunar and Martian moon detectors would detect many interesting foreground sources in a new frequency window and could serve as a valuable precursor for BBO.     

几种超声速非常规压缩系统的研究

根据斜激波和膨胀波理论,数值计算得到给定非常规压缩型面所形成的弯曲激波型面和壁面静压分布,同Fluent计算结果进行比较。应用Fluent软件,计算了等压力梯度设计非常规曲面压缩二元进气道、常规等熵压缩二元进气道和三楔压缩二元进气道设计点性能。研究结果表明:数值计算得到的弯曲激波型面与Fluent计算结果吻合较好。等压力梯度设计的非常规压缩型面壁面静压均匀上升,有利于防止壁面附面层分离;其压缩面长度比等熵压缩面缩短21.6%,减轻了进气道的重量。