喷射成形过程中雾化锥体的温度场与质量场

本文着重研究了喷射成形过程中雾化锥体的温度场与质量场的测定方法，进一步测定了纯铝及ＺＱＳｎ６－６－３青铜的温度场和质量场，并讨论了其特征。     

三角形速度场解析平面变形辊拔与辊挤

文章对平面变形辊拔与辊挤问题建立了运动许可的三角形速度场并获得上界解析解。该解与 Avitzur 以连续速度场得到的上界解进行比较表明,有时本文解法可得到更低的上界值。     

缓凝砂浆螺旋输送理论研究

缓凝预应力筋包覆装置是将新型独特的缓凝材料应用于预应力混凝土体系的一种施工设备．通过对缓凝砂浆的流变性能分析，建立了螺旋输送物理模型，运用粘性流体力学的运动微分方程研究缓凝砂浆螺旋输送的速度场和流率，从而对其装置的设计和运行参数的合理选择提供了理论依据．     

原子光谱线变宽的因素分析

分别从经典理论和量子理论的不同角度论述了使原子光谱线变宽的各种主要因素:由于能量的不确定关系导致的自然致宽;多普勒致宽;碰撞致宽;因碰撞过程中原子能级变化而导致的压力致宽、场致宽等.通过分析,阐明了实际光谱线与理想光谱线的不同及其原因.     

PEAK COVARIANCE STABILITY OF A RANDOM RICCATI EQUATION ARISING FROM KALMAN FILTERING WITH OBSERVATION LOSSES

We consider the stability of a random Riccati equation with a Markovian binary jump coefficient. More specifically, we are concerned with the boundedness of the solution of a random Riccati difference equation arising from Kalman filtering with measurement losses. A sufficient condition for the peak covariance stability is obtained which has a simpler form and is shown to be less conservative in some cases than a very recent result in existing literature. Furthermore, we show that a known sufficient condition is also necessary when the observability index equals one.     

2006年秋末一次连续性降雪天气过程诊断分析

对连续性降雪过程进行了综合分析,提出了该类降雪过程的预报着眼点。     

煤矿工程出水预测主要方法探讨

随着煤矿生产逐渐向深部发展，煤矿水害事故对煤矿安全生产的威胁越来越严重。本文由简到繁地介绍了有效地预测煤矿涌水量的地下工程出水预测的考虑多场耦合的几种主要方法，包括考虑渗流与应力耦合的解析法、考虑渗流与应力耦合的经验解析法，考虑渗流与应力耦合的数值方法．考虑渗流-应力-温度耦合环境的数值方法和基于反演分析的考虑渗流-应力-温度耦合环境的数值方法。     

A theoretical model for mid-and low-latitude ionospheric electric fields in realistic geomagnetic fields

The geomagnetic fields, which play important roles in the ionospheric dynamo, can greatly affect the global distribution of ionospheric electric fields, currents and other ionospheric electrodynamics phenomena. In the study of ionospheric electrodynamics phenomena, such as the longitudinal variations of ionospheric electric fields, the non-dipolar component of the geomagnetic fields must be taken into account. In this paper, we deduce a theoretical electric field model for ionospheric dynamo at mid- and low-latitude which adopt a modified magnetic apex coordinates system. In the new electric field model, the geomagnetic fields can be calculated from either the IGRF model or the dipole field model, and the neutral winds and conductivities are calculated based on empirical models. Then the dynamo equation for the electric potential is finally solved in terms of the line-by-line iteration method, and the ionospheric electric fields and currents are derived from the calculated potential. Our model can reproduce the main features of the ionospheric electrodynamics processes, so it will be a useful tool for the investigation of the upper atmosphere and ionosphere.