异种金属复杂体系阴极保护电位场有限元建模

海洋防腐工程中受阴极保护金属构筑物表面的电位电流分布常常是不均匀的,而金属表面的电位电流只有在一定范围内才能使构筑物受到有效和适当的保护.尤其是复杂而庞大的海洋钢结构物(如滨海电厂钛管凝汽器)阴极保护系统的设计和监测较复杂,此阴极保护下电化学场的计算,对评价阴极保护效果,优化阴极保护设计有重要意义.采用电化学场中的拉普拉斯(Laplace)方程,使用四节点四面体和合适的形状函数对水室表层和复杂结构体系周围场域进行离散.用有限元计算法,通过对各单元的分布和整个求解区域的总和,建立了两种不同金属组成复杂结构体系的三维有限元数学模型.     

海洋平台复杂节点阴极保护电位分布的有限元法计算

了解阴极保护电位分布是合理设计阴极保护工程的必要条件和评价阴极保护效果的重要依据。本文应用有限元素法(FEM)计算海洋平台复杂节点表面的阴极保护电位分布。在实验室通过边界条件试验建立数学模型,计算海水中被保护的I,Y,K型复杂节点电位分布情况。计算结果与测量结果吻合得很好,说明FEM能够应用于海洋平台复杂节点阴极保护电位分布的计算,所获得的边界条件合理。     

MATLAB在海底管线阴极保护电场计算中的应用

海洋钢结构阴极保护电场的数值模拟仿真和计算是当前海洋腐蚀、阴极保护研究和工程实践中一个重要的研究方向。研究海底管线的腐蚀状态就必须准确测定管线表面的电位分布,而实际测量中深海管线表面电位分布难以直接测量。构建了海水中钢管线的阴极保护数学模型,采用以边界元法为基础的数值计算方法,利用Matlab开发了均匀电解质中电位分布的计算软件,实测中通过对腐蚀电场海水区域环境电场的测量,就可实现不接触测量管线表面电位的目的。最后通过海洋实测验证了计算结果的可靠性,证明了基于Matlab的数值仿真计算引入阴极保护设计中是行之有效的。     

高锰铝青铜在流动海水中阴极保护参数的研究

采用稳态动电位极化法测量了螺旋桨材料ZQAl12-8-3-2高锰铝青铜在静态和流动海水中的极化曲线,分析了其在流动海水中的腐蚀电化学行为,解析了最小保护电位、最大保护电位、最小保护电流密度等阴极保护参数,其在海水中的保护电位范围为-0．45～0．72V,最大保护电位在常规阴极保护范围内没有限制,流动海水中的最小保护电流密度比静态时增加几十倍,为海水中螺旋桨阴极保护设计及应用提供参考数据。     

光电化学阴极保护技术研究进展

海洋环境下的金属面临着非常严峻的腐蚀问题,必须采取措施进行防护.光电化学阴极保护是一种绿色环保的新型防腐蚀技术,受到了广泛的关注.本文简要阐述了光电化学阴极保护技术的原理以及对光阳极的要求;详细介绍了以二氧化钛为代表的几种常见光阳极材料及其不同改性方法;此外还介绍了兼具储能与阴极保护功能的光阳极,它有望实现暗态下连续保护的目标;最后讨论了光电化学阴极保护技术的发展趋势.     

X80钢在含有SRB的海水溶液中阴极保护准则适用性

通过表面观察及电化学方法研究X80钢在含有SRB的海水溶液中阴极保护准则的适用性,测试结果表明:腐蚀控制因素为阳极控制,对金属施加阴极极化第5天降低金属腐蚀速度主要通过增大金属表面SRB的附着电阻和电荷转移电阻实现;而施加阴极极化第10天,阴极保护主要通过改变金属表面电荷转移电阻控制腐蚀速度,且阴极极化电位越大控制效果越好。无阴级保护的金属试样腐蚀产物较多且附着力差,施加阴极保护的金属试样腐蚀产物较少且附着力较强。阴极保护的确能对存在SRB的海水溶液环境中X80钢起到阴极极化作用,但极化5 d时传统的阴极保护准则中-850 mV_CSE(即-770 mV_SCE)电位未达到85%的保护要求,-950 mV_CSE(即-870 mV_SCE)电位刚刚能满足保护要求;而极化10 d时2种极化电位下保护度都有所下降且都不能满足保护要求,因此还需要进一步实验确定其合适的阴极保护电位。     

大电流密度下阴极产物膜的探讨

在室内和现场不同大电流密度下形成阴极产物膜，通过观察膜的形貌、厚度、强度、分析成份，对其进行电位衰变试验、阴极极化试验、生锈试验及维持保护电流试验，进行分析比较，同时对涂层和阴极保护联合防腐时涂层破损、剥落处阴极产物膜的形成，及其对电流密度、保护电位的影响作了探讨。本文还对阴极产物膜的应用价值，以及在阴极保护中应用的可能性作了阐述。     

重力式码头过大位移和不均匀沉降质量通病防治

结合烟台港三突堤集装箱码头工程施工,对重力式码头过大位移和不均匀沉降的现象、成因和危害进行了分析总结,并提出防治措施,取得了明显效果。     

阴极保护时碳钢的交流阻抗特性和最佳防蚀电位

测定了在3.5％食盐水中碳钢的法拉第交流阻抗,其结果与理论解析结果一致。阴极保护的实际效率(保护效率p和保护电流利用率q的乘积即r=p×q)在腐蚀电位E′_(cor)附近表现出最大值,这个电位可以认为是阴极保护的最佳保护电位。由于法拉第交流阻抗值容易被测得,为此提出了一种对阴极保护系统进行监测管理的一种新方法。     

动态海水中保护电位对钙质沉积层形成的影响

采用恒电位阴极极化和线性极化法研究了天然海水中不同动态条件、不同初始保护电位下,阴极保护初期碳钢表面钙质沉积层的形成规律.扫描电镜( SEM)和能谱X-射线分析(EDX)分析了保护后碳钢表面的产物.结果表明:-800 mV(vs.SCE,下同)保护电位下,在静态和动态海水中碳钢表面形成的钙质沉积层质量都较差;-900 mV保护电位下,静态海水中形成致密的钙质沉积层,动态下钙质沉积层形成困难;-1 000 mV保护电位下,静态和动态海水中都形成良好的钙质沉积层.随流速增大,阴极保护电流密度显著增大,钙质沉积层中Ca/Mg比值增加;动态条件下,较负的保护电位,有利于阴极保护初期钙质沉积层的形成.     

A coupled debris flow–turbidity current model

In the last decade, offshore pipeline engineering extended its action field to very deep waters and continental slopes. This implied the necessity to deal with continental slope instability and mass gravity flows. Mass gravity flows are rare and have random occurrence; therefore, considering also the technical difficulties, the direct measurement of the phenomena is practically impossible. This has encouraged the development of physical and numerical models for investigating the characteristics and intensity of the phenomena (Proc. OTC Conf., Houston, TX (2000); Proc. 19th OMAE Conference, New Orleans, LA (2000)). In order to provide design activities with reliable predictive tools, two numerical models, one for debris flows and the other for turbidity currents, have been developed. The two models are coupled by the bottom boundary conditions of the turbidity current model that depends on the instantaneous velocity of the debris flow model. The two models used together provide a tool for the evaluation of a mass gravity flow event starting as a debris flow and evolving into a turbidity current.     

Numerical Modeling of Wave and Current Interaction in the Tidal Inlet Area

This paper investigates the phenomena of wave refraction and diffraction in the slowly varying topography, as well as the current deflection due to wave actions. A numerical model is developed based on depth integrated mean continuity equation and momentum equations, and a 3rd-order wave equation which governs the wave diffraction, refraction and interaction with current. Examples to examine the above model are given comparing with the laboratory data or the numerical results of other researchers. An example simulating the inlet area shows the interesting velocity field which may be used as a pioneer to further study on the nearshore hydrodynamics and sedimentation.     

环台湾岛海域冬季水文要素的数值模拟

本文利用POM模式对环台湾岛海域冬季的水文要素进行了数值模拟,对有代表性的水平环流、温度场和上升流三个要素所进行的分析表明:模式再现了台湾岛东岸的高温高盐强流速区即黑潮,黑潮在冬季并无直接进入台湾海峡的分支存在;西岸的东北向流在冬季各个层次上都存在,台湾东北部的冷涡模拟与实况较为一致。温度场和上升流的分布与水平环流有很好的对应关系。本文还进一步验证了前人的一些研究成果,并对一些特殊物理现象的成因进行了定性解释。     

胶南东部近岸海域实测海流分析及潮流场数值模拟

基于2005年胶南东部近岸海域的测流资料,分析了该海域的海流、潮流及余流特征,在此基础上,进行了潮流场的数值模拟,展现了M2分潮的潮波系统、潮流椭圆分布、最大流速分布和逐时潮流场。计算结果与实测结果符合良好,较好地反映出该海域M2分潮潮流场时空分布的基本特征。对该海域的水动力状况有了更进一步了解,为胶南近岸海域的环境保护规划的制定提供了科学依据。     

单点系泊潜标系统动力学建模与姿态分析

通过对单点系泊潜标进行动力学分析,利用集中质量法建立系统的动力学模型,编制Matlab仿真程序,通过数值模拟获取不同海流条件下,分析潜标系统的姿态。文中将一个典型潜标系统的浮球、锚链、重力锚等部件,利用集中质量法简化为节点,通过模拟真实环境中的海流流速在垂直方向的分布,设计1～5 m/s的流速剖面分布。将节点的物理参数和海流参数代入仿真程序中,得到各节点的姿态、节点间张力以及重力锚与海底摩擦力等数据。分析仿真结果,海流流速与节点的偏降、节点间的张力以及重力锚与海底的摩擦力成正比,仿真结果与实际情况相符。文中设计的建模方法和仿真程序可以为单点系泊潜标的总体设计、姿态估算、锚系配置提供工程参考。     

粤东甲子海域潮波异常和南海北部潮波的传播

从南海潮波数值模拟潮能通量的结果中,勾勒出南海北部潮波的传播路径,显示出众多的路径分支。分析表明南海北部陆架包括北部湾海区,仅获得太平洋传入潮能的一小部分,因而南海北部沿岸的潮汐潮流都表现得比较弱。由于复杂的地形,导致了潮波传播路径指向不同方向。文章通过实测资料以及潮波的传播路径,特别讨论了粤东甲子站附近的潮波异常现象,并指出流向台湾海峡南口的分支和流向珠江口、广州湾的分支之间的潮能辐散,可能是造成甲子站附近潮性系数特别大以及潮汐潮流性质迥异现象的重要原因之一。     

Impacts of Different Dynamic Factors on the Saltwater Intrusion in the Northern Branch of the Yangtze Estuary

A 3-D baroclinic numerical model is established to study the temporal and spatial distribution of salinity in the Northern Branch(NB) of the Yangtze Estuary(YE) in response to river runoff, wind and currents. The idealized,process-oriented studies show that the lower river runoff in the dry season is the main driving factor for the spilling over from the NB to the Southern Branch(SB). The NB takes longer time to get in dynamic stable state compared with the SB, as the runoff transfers from the wet season to the dry season. The vertical stratification intensity of the NB has obvious periodic phenomena in the dry season, and the stratification strength is enhanced under the action of low runoff and north wind, which further weakens the vertical transport of water. Momentum balance analysis suggested that the landward net flux increases when considering the influence of the moderate north wind, and the landward flux will enhance if considering the boundary current during the spring tide. With the influence of the boundary current, increases the average salinity of the NB, as well as the intrusion degree from the NB to the SB.This indicates that the nearshore ocean current of the Yellow Sea is an important factor affecting the saltwater intrusion in the NB of the YE.     

Nonlinear effects at the initial stage of tsunami-wave development

An analytical solution to shallow-water nonlinear equations determining the height of tsunami waves leaving the source is obtained. The initial water-level displacement in the source and the distribution of particle velocities are set. The numerical solution showed that analytical estimates fit well with source characteristics varying in a broad range, even if the waves produced by the source collapse.     

Experimental and numerical investigation of sloshing using different free surface capturing methods

We investigated the use of numerical methods to predict liquid sloshing phenomena in a moving tank and compared our results to model test measurements. The numerical techniques for the free surface, based on the so-called finite Volume-of-Fluid (VoF) approach, comprised an incompressible VoF method, an incompressible coupled Level-Set and Volume-of-Fluid (clsVoF) method, and a compressible VoF method. We assessed the capability of these three numerical methods to achieve suitable numerical predictions of sloshing phenomena, specifically, air pockets and bubbles on the free surface inside a test tank. To observe the described sloshing phenomena, we simulated tank motions leading to well defined single impact wave motions. We performed repeated physical tests for validation purposes. Computed velocity and pressure time histories were compared to experimental data we obtained from Particle Image Velocimetry (PIV) and pressure sensor measurement. Grid sensitivity and turbulence model studies were performed. We demonstrated that the compressible VoF method was the most suitable method to obtain accurate predictions of sloshing phenomena.     

Stochastic Analysis Method of Sea Environment Simulated by Numerical Models

1 .IntroductionNumericalmodelsmostwidelyusedforseaenvironmentandsedimenttransportfocusonsolvingseriesofdifferentialequations .Theinputandoutputofanumericalmodelareconsideredasdecisivefactors .Butinrealitythecausesofnaturaleventssuchasmeteorological,astronomical,oceanograph ic ,geomorphologicandgeophysicalfactorsarerandom .Therearemanyuncertaintiesinvolvedininputfactorsinnumericalmodels .Correspondinglytheoutputsofnumericalmodelsarealsorandom .There fore ,theoutputparametersofnumericalmodelsca…