基于耦合边界元法的水下目标低频声散射特性

基于耦合声学边界元理论对水下目标低频声散射特性进行仿真研究。为了验证此数值方法准确性,对水中弹性球壳在平面波入射下的反向散射特性进行数值计算。结果表明,散射声场的数值计算结果和解析解较好吻合。在此基础上,本文探究刚性BeTSSi-Sub[1]和弹性BeTSSi-Sub的全向散射特性,对比发现,刚性BeTSSi-Sub的目标强度大于弹性BeTSSi-Sub的目标强度。通过对形状不同弹性的BeTSSi-Sub的目标强度对比发现,在低频段潜艇上舵对潜艇目标强度的影响比上层建筑的影响大。     

带有挡板的注液舱室地震响应分析（英文）

In thispaper, the effects of a rigid baffle on the seismic response of liquid in a rigid cylindrical tank are evaluated. A baffle is an annular plate which supplies a kind of passive control on the effects of ground excitation. The contained liquid is assumed incompressible, inviscid and has irrotational motion. To estimate the seismic response, the method of superposition of modes has been applied. To analyze the rigid tank response, Laplace's equation is considered as the governing equation of the fluid domain, in both time and frequency domains. The boundary element method(BEM) is employed to evaluate the natural modes of liquid in a cylindrical tank. To gain this goal, the fluid domain is divided into two upper and lower parts partitioned by the baffle. Linearized kinematic and dynamic boundary conditions of the free surface of the contained liquid have been considered.     

边界控制方法在DVR样机研制中的应用

动态电压恢复器（DVR）可在供电电压发生电压下陷时维持负载电压稳定,以保护敏感负载。由于在正常电力系统中,电压下陷故障出现的频率相对不高,使得DVR的利用率较低。将一种基于二阶开关平面理论的边界控制器应用于DVR系统,使其既可用于电压下陷补偿又能用于稳态下电压电能质量控制,大大提高了设备利用率。通过预测DVR逆变器的某次开关动作后,其系统状态矢量的运动轨迹可得到上述二阶开关平面。将该平面作为状态轨迹沿理想开关平面运动的上界,可约束轨迹使其趋向理想工作点。为考察其动态特性,应用上述控制器的DVR样机针对源端谐波畸变和伴有畸变的下陷电压波形进行了补偿试验。结果证实上述边界控制方案可获得优于其它一些控制策略的谐波补偿效果。     

新型分油机中的参数变量对分离效果的影响

介绍了传统分油机与新型分油机结构等特征.考虑到油、水二相的密度差,使它们在高速旋转时所受的离心力不同,因而在半径方向油、水分离.根据这一原理,对新型分油机建立相应的物理模型、数学模型并进行求解,得出影响分离效果的技术参数,经比较与实测数据相符.     

浸没边界格子Boltzmann方法的改进及转动圆柱绕流模拟

针对浸没边界格子Boltzmann方法计算效率不足的问题,提出一种改进浸没边界格子Boltzmann方法。通过使用作用力格子Boltzmann模型,并简化流固耦合作用力的计算方法,使计算流程得到简化,同时,对比原方法转动圆柱绕流计算结果,计算时间缩短一半以上,提高了数值计算效率。结合改进算法研究转动圆柱绕流的流场升阻力系数、压力系数、流场速度等流体参数场随转速比的关系,揭示了一定的转动圆柱绕流动力学规律。研究结果表明,改进方法准确可靠。     

基于宏观基本图的路网多子区状态一致协同控制

针对基于宏观基本图(MFD)的路网多子区协同控制未考虑各子区拥堵状态差异性及均衡性的问题，本文提出以多子区状态可达一致为目标的子区边界状态反馈控制设计方法. 首先，基于路网 MFD模型建立路网多子区协同模型；进一步，基于部分变量稳定性理论，设计多子区状态可达一致的边界状态反馈控制律.在此基础上，考虑子区拥堵状态的差异性，设计了子区间的协同控制策略，快速缓解子区拥堵状态；同时，提出子区边界输入流的分配优化策略.最后，以潍坊市实际路网为背景建立仿真模型.实验结果表明，本文方法可实现子区交通流分布的均衡性，快速缓解子区拥堵状态，较大幅度地提升路网运行效率.     

奇摄动三阶非线性边值问题

利用微分不等式技巧和Volterra型积分算子，研究了三阶非线性奇摄动边值问题εx^(3)=f(t,x,x′,w(ε）x^(3)，ε），g（x′（0），x″（0）=0，x（1）=A，x′（1）=B的存在性及渐近估计。     

桥梁结构连同地基的整体计算方法

本文提出将桥梁上部结构、下部结构和基础连同地基整体计算的方法     

Initial results from long-term measurements of atmospheric humidity and related parameters in the marine boundary layer at two locations in the Gulf of Mexico

Measurements of boundary layer moisture have been acquired from Rotronic MP-100 sensors deployed on two NDBC buoys in the northern Gulf of Mexico from June through November 1993. For one sensor, which was retrieved approximately 8 months after deployment, the post- and precalibrations agreed closely and fell well within WMO specifications for accuracy. The second sensor operated continuously from June 1993 to February 1997 (3.5 years). Buoy observations of relative humidity and supporting data were used to calculate specific humidity and the surface fluxes of latent and sensible heat. Specific humidities from the buoys were compared with observations of moisture obtained from nearby ship reports, and the correlations were generally high (0.7–0.9). Surface gravity wave spectra were also acquired. The time series of specific humidity and the other buoy parameters revealed three primary scales of variability, small (h), synoptic (days), and seasonal (months). The synoptic variability was clearly dominant and occurred primarily during September, October, and November. Most of the synoptic variability was due to frontal systems that dropped down into the Gulf of Mexico from the continental US followed by air masses which were cold and dry. Cross-correlation analyses of the buoy data indicated that: (1) the moisture field was highly coherent over distances of 800 km or more in the northern Gulf of Mexico; and (2) both specific humidity and air temperature served as tracers of the motion associated with propagating atmospheric disturbances. These correlation analyses also revealed that the prevailing weather systems generally entered the buoy domain from the South prior to September, but primarily from the North thereafter. Spectra of the various buoy parameters indicated strong diurnal and semidiurnal variability for barometric pressure and sea surface temperature (SST) and lesser variability for air temperature, wind speed and significant wave height. The surface fluxes of latent and sensible heat were dominated by the synoptic events which took place from September through November with the transfer of latent heat being primarily from the ocean to the atmosphere. Finally, an analysis of the surface wave observations from each buoy, which included calculations of wave age and estimates of surface roughness, indicate that major heat and moisture flux events coincide with periods of active wave growth, although the data were insufficient to identify any causal relationships.     

改进振动法在地下工程动力时程计算中的应用

地下工程受到周围土体的约束作用,其动力反映与地面工程有所区别,如将源于地面工程的振动法用于地下工程的动力时程计算分析,需要进行相应的改进.文章通过计算分析发现,振动法用于地下工程动力时程计算时,在计算模型边界条件和波动传播时间效应方面不能反映波动对地下工程作用的实质;通过对比分析,在这两个方面对常规振动法进行了改进;提出了适用于地下工程动力时程计算的改进振动法.该方法的计算模型采用左右两侧粘弹性底部固定的人工边界条件,波动输入采用能够反映波动传播时间效应的分层加速度动态输入法,其计算分析结果与理论解吻合较好,适用于地下工程的动力时程计算分析.