Chaboche热粘塑性损伤模型的应用研究

本文讨论了Chaboche粘塑性模型的材料参数确定问题,提出了一种简单实用的模型参数确定方法,并用本文提出的方法确定了TiAl材料的Chaboche模型参数,并用这些参数进行了不同应变率下的拉伸模拟计算、不同应力下的蠕变模拟计算和CT试样在阶梯载荷下的蠕变模拟计算。     

Physical Causes of Solar Variability – Discussion Session 1b

This report is divided into three parts: Section 1 gives a short introduction and a summary of the topics discussed. Section 2 is a position statement by J. Kuhn on the interpretation of the irradiance measurements, while Section 3 gives a position statement by M. Schüssler discussing observations of stars that could be useful for understanding solar variability.     

Status and Perspectives in Protective Design

Starting with an introduction into the field of hypervelocity impacts, an overview over current research in the area of protection against space debris is given. Trends and strategies to further develop know-how in protection technology are then discussed. One purpose is to demonstrate that improvements in shield efficiency can be expected. To achieve this aim, a strategy is outlined which tries to avoid the adjustment of numerical and material parameters by fits to penetration experiments. Instead, it is suggested to determine material parameters from carefully selected laboratory tests, covering a broad range of strains, strain rates and stress states. Knowledge of the dynamic material behaviour can then be used for the development of new shield concepts by means of numerical simulation.     

Road-map assisted ground moving target tracking

Tracking ground targets with airborne GMTI (ground moving target indicator) sensor measurements proves to be a challenging task due to high target density, high clutter, and low visibility. The exploitation of nonstandard background information such as road maps and terrain information is therefore highly desirable for the enhancement of track quality and track continuity. The present paper presents a Bayesian approach to incorporate such information consistently. It is particularly suited to deal with winding roads and networks of roads. The target dynamics is modeled in quasi one-dimensional road coordinates and mapped onto ground coordinates using linear road segments taking road map errors into account. The case of several intersecting roads with different characteristics, such as mean curvature, slope, or visibility, is treated within an interacting multiple model (IMM) scheme. Targets can be masked both by the clutter notch of the sensor and by terrain obstacles. Both effects are modeled using a sensor-target state dependent detection probability. The iterative filter equations are formulated within a framework of Gaussian sum approximations on the one hand and a particle filter approach on the other hand. Simulation results for single targets taken from a realistic ground scenario show strongly reduced target location errors compared with the case of neglecting road-map information. By modeling the clutter notch of the GMTI sensor, early detection of stopping targets is demonstrated     

Ionospheric and field-aligned current systems in the auroral zone: a concise review

During the last few years our knowledge about the real three-dimensional current flow in the auroral zone has been significantly increased due to new improved measurements, especially those made by ground-based magnetometer networks, coherent and incoherent auroral radars, sounding rockets and low-altitude satellites. Combination of two or even more of those data sets (e.g. electron densities and electric and magnetic fields) allowed for a rather accurate determination of the distribution of Hall, Pedersen and Birkeland currents in the auroral zone. In this review an attempt is made to summarize the present knowledge about the distribution of conductivity, electric field and current flow in the auroral zone as well for the large-scale electrojet systems as for the comparatively smaller current systems associated with quiet and active aurora, i.e. discrete arcs, auroral break-ups, westward travelling surges and omega bands.     

Hypersaline microbial systems of sabkhas: examples of life's survival in "extreme" conditions

Life and living systems need several important factors to establish themselves and to have a continued tradition. In this article the nature of the borderline situation for microbial life under heavy salt stress is analyzed and discussed using the example of biofilms and microbial mats of sabkha systems of the Red Sea. Important factors ruling such environments are described, and include the following: (1) Microbial life is better suited for survival in extremely changing and only sporadically water-supplied environments than are larger organisms (including humans). (2) Microbial life shows extremely poikilophilic adaptation patterns to conditions that deviate significantly from conditions normal for life processes on Earth today. (3) Microbial life adapts itself to such extremely changing and only ephemerally supportive conditions by the capacity of extreme changes (a) in morphology (pleomorphy), (b) in metabolic patterns (poikilotrophy), (c) in survival strategies (poikilophily), and (d) by trapping and enclosing all necessary sources of energy matter in an inwardly oriented diffusive cycle. All this is achieved without any serious attempt at escaping from the extreme and extremely changing conditions. Furthermore, these salt swamp systems are geophysiological generators of energy and material reservoirs recycled over a geological time scale. Neither energy nor material is wasted for propagation by spore formation. This capacity is summarized as poikilophilic and poikilotroph behavior of biofilm or microbial mat communities in salt and irradiationstressed environmental conditions of the sabkha or salt desert type. We use mainly cyanobacteria as an example, although other bacteria and even eukaryotic fungi may exhibit the same potential of living and surviving under conditions usually not suitable for life on Earth. It may, however, be postulated that such poikilophilic organisms are the true candidates for life support and survival under conditions never recorded on Planet Earth. Mars and some planets of other suns may be good candidates to search for life under conditions normally not thought to be favorable for the maintenance of life.     

Erdbeobachtende missionen—Anforderungen und konzepte

(Earth Observation Missions—Requirements and Concepts)—Ten years ago, on 23 July 1972. NASA launched the first satellite specifically designed for Earth observation. With Landsat 1 the importance and attractiveness of remote sensing from space increased worldwide.The paper presents in an overview former remote sensing missions with their applications and the system elements required for gathering Earth observation information. Main elements are the sensors (optical, microwave, and other instruments), the platforms (satellites, space stations, aircraft and Earth based stations) and their orbits.It is shown how these elements are interrelated and which constraints must be considered for planning an Earth observation mission. The feasibility, the amount of hard- and software, the costs, and the performance of a system are decisive for the realization of a satellite concept.Examples for different concepts investigated to date at Dornier System are given; included is the first ESA Remote Sensing Satellite ERS-1, which is now under definition at Dornier System, the main contractor of ESA.     

The near-Earth plasma sheet: An AMPTE/IRM perspective

During the last five years, statistical studies using plasma measurements made by the AMPTE/IRM satellite have lead to a better understanding of the structure and dynamics of the near-Earth plasma sheet between about 10 and 20R _E. The most notable new findings are: (1) the adiabatic non-isentropic behavior of the tail plasma during quiet times; (2) the strong non-adiabatic heating of ions and electrons during substorms and the strong coupling of the ion and electron temperature withT _i/T_i7; and (3) the high-speed flow bursts which carry most of the tail plasma transport. Moreover, it became clear that it is the central plasma sheet, and not the plasma sheet boundary layer, which is most affected by substorm activity.