非缓坡非均匀流场中多向不规则波传播数学模型的建立

根据线性波动的叠加原理和波浪方向谱理论,在文献[1]的非缓坡非均匀流场的规则波基本方程的基础上,推导出了非缓坡非均匀流场中的多向不规则波传播变形的偏微分方程,并使用有限差分方法建立了数学模型。该模型避开了求解波动势函数的困难,直接求解波动能量的空间分布,可采用简单的有限差分数值方法求解,对空间步长没有限制,适合非缓坡复杂地形及存在流场的情况下大面积波浪场(波高和波向)的计算。     

单相谐振MOSFET逆变电源的研究

给出一种用于中频感应加热装置的ＭＯＳＦＥＴ逆变电源,在ＭＯＳＦＥＴＲ 控制信号方面,提出了一种新的控制方法,即正弦波控制法,它能够自动地产生“死区时间”,对于避免同桥壁上,下管子直通有可靠的作用,中详细叙述了装置主电路和控制电路的并给出试验波形。     

Free Propagation of Wave in Viscoelastic Cables with Small Curvature

IntroductionDynamicbehaviorsofcablesandcable structureshaveattractedtheattentionofmanyresearchers .Therehavebeenmanyreports[1 5 ] ontheproblemsofnaturalfrequencies ,freevibrations,andstabilitybehaviorsofcablesandcablestructures .Manyavailabletechniques ,s…     

城市道路不规则交叉口渠化设计

不规则交叉口是城市交通的瓶颈,合理的渠化设计是提高不规则交叉口通行能力的重要途径,但国内针对不规则交叉口渠化的研究较少,且缺乏系统性。文章分析了不规则交叉口渠化的基本思路,从交通调查、现状问题分析、渠化设计及方案评价等4个方面提出了不规则交叉口渠化的基本步骤．并结合VISSIM仿真软件对渠化方案进行评价,论证方案的合理性。     

直立圆柱体内孤立波载荷特性数值模拟

以三类内孤立波理论(KdV、eKdV和MCC)的适用性条件为依据,将内孤立波诱导上下层深度平均水平速度作为入口条件,采用Navier-Stokes方程为流场控制方程,建立了两层流体中内孤立波对直立圆柱体强非线性作用的数值模拟方法.结果表明,数值模拟所得内孤立波波形及其振幅与相应理论和实验结果一致,并且直立圆柱体内孤立波水平力、垂向力及其力矩数值模拟结果与实验结果吻合.直立圆柱体内孤立波载荷由波浪压差力、粘性压差力和摩擦力构成,其中摩擦力很小,可以忽略;对于水平力,其波浪压差力与粘性压差力量级相当,流体粘性的影响显著;对于垂向力,粘性压差力很小,流体粘性影响可以忽略.此外,直立圆柱体对内孤立波的波形及其诱导流场的影响很小,因此采用Morison公式和傅汝德—克雷洛夫力分别计算其内孤立波水平力和垂向力是可行的.     

异形钢桥塔高程精密测量技术

针对传统桥塔高程测量方法受场地、环境等因素影响较大无法满足异形桥塔高程测量要求的问题,本文结合永定河特大桥桥塔高程测量的实际需求,提出了一种基于正负压力变送器测量桥塔倾斜端口高差的方法,并介绍其计算分析方法.全站仪地面竖向高程传递+端口正负压力变送器测量倾斜端口高程的测量方法克服了传统方法中要求测试端口基本平直的限制;温度引起的液态水密度变化会对压力变送器测量高差的精度产生较大影响;通过测量已知基准点高差反算液体密度取值可减小温度影响产生的误差;该测量方法能够满足高度大于100 m的异形桥塔高程精确、快速测量的要求.     

实船耐波性试验数据快速分析方法研究

针对实船耐波性试验数据不规则性强、数据量大的特点,研究了包括有效数据采样、数据中心化、快速傅里叶变换（FFT）、幅值统计分析等环节在内的耐波性试验数据快速分析方法,成功开发耐波性试验数据分析系统,直接由原始试验结果分析得到舰船在海浪中的运动响应幅度统计值,并将原始记录及分析结果的曲线和数据导出,生成Excel等形式的文件,大大简化了试验数据处理过程,提高了效率。     

Asymmetry of Columbia River tidal plume fronts

Columbia River tidal plume dynamics can be explained in terms of two asymmetries related to plume-front depth and internal wave generation. These asymmetries may be an important factor contributing to the observed greater primary productivity and phytoplankton standing crop on the Washington shelf. The tidal plume (the most recent ebb outflow from the estuary) is initially supercritical with respect to the frontal internal Froude number F_R on strong ebbs. It is separated from the rotating plume bulge by a front, whose properties are very different under upwelling vs. downwelling conditions. Under summer upwelling conditions, tidal plume fronts are sharp and narrow (< 20–50 m wide) on their upwind or northern side and mark a transition from supercritical to subcritical flow for up to 12 h after high water. Such sharp fronts are a source of turbulent mixing, despite the strong stratification. Because the tidal plume may overlie newly upwelled waters, these fronts can mix nutrients into the plume. Symmetry would suggest that there should be a sharp front south of the estuary mouth under summer downwelling conditions. Instead, the downwelling tidal plume front is usually diffuse on its upstream side. Mixing is weaker, and the water masses immediately below are low in nutrients. There is also an upwelling–downwelling asymmetry in internal wave generation. During upwelling and weak wind conditions, plume fronts often generate trains of non-linear internal waves as they transition from a supercritical to a subcritical state. Under downwelling conditions, internal wave release is less common and the waves are less energetic. Furthermore, regardless of wind conditions, solition formation almost always begins on the south side of the plume so that the front “unzips” from south to north. This distinction is important, because these internal waves contribute to vertical mixing in the plume bulge and transport low-salinity water across the tidal plume into the plume bulge.F_R and plume depth are key parameters in distinguishing the upwelling and downwelling situations, and these two asymmetries can be explained in terms of potential vorticity conservation. The divergence of the tidal outflow after it leaves the estuary embeds relative vorticity in the emerging tidal plume water mass. This vorticity controls the transition of the tidal plume front to a subcritical state and consequently the timing and location of internal wave generation by plume fronts.     

Wave energy assessments in the Black Sea

The present work aims to evaluate the wave energy resources in the Black Sea basin. The study is focused on the western part of the sea, which is traditionally considered as being more energetic. In order to give a first perspective of the wave climate, a medium-term wave analysis was carried out using in situ measured data. As a further step, a wave prediction system was implemented for the Black Sea. This was based on the simulating waves near-shore model, which is used for both wave generation and near-shore transformation. This methodology has the advantage that a single model covers the full scale of the modelling process. Various tests were performed considering data measured at three different locations. Special attention was paid to the whitecapping process, which is still widely considered to be the weak link in deep water wave modelling. Comparisons carried out against measured data show that the wave prediction system generally provides reliable results, especially in terms of significant wave heights and mean periods. By increasing the resolution in geographical space, the field distributions of wave energy were analysed for both high and average wave conditions. The analysis and the wave prediction system developed are a prerequisite for further investigations extended in time and with increased resolution in the near-shore direction.     

双层开孔消浪板结构消能性能分析

双层开孔消浪板是一种新型消能结构，其结构通过上层开孔板和下层实心板两部分来解决结构的消能问题．文中通过模型试验的方法来验证结构的消能性能，同时，对双层开孔消浪板结构在规则波作用下的消能系数随3个主要影响因子（相对板宽B／L，相对开孔A／A0，波陡H／L）变化的结果进行分析．通过分析和比较消能系数与影响因子之间的相互关系，证明双层开孔消浪板结构具有较好的消能效果．