波浪作用下沙波的运动速度和沙波床面的底沙输移

根据沙波床面底沙运动特点,引用二阶Stokes波浪理论,推导出波浪作用下沙波运行速度计算公式,并给出沙波床面上底沙输移的计算公式.公式计算结果与水槽试验结果吻合很好.     

基于点云特征提取的波浪增阻预报及对比研究

目的为在设计阶段快速预报船舶波浪增阻,提出一种基于点云特征提取的神经网络模型——波浪增阻点云预报模型。方法以S60船为例,与传统的基于主要设计参数的模型预报进行对比;参照船模试验结果,分析点云预报模型在准确性和稳定性等方面的优势,探讨利用静水阻力预训练优化模型的方法。结果结果显示,基于点云特征提取的波浪增阻预报模型在全部5艘S60母型船上的预报结果的决定系数R² = 0.74～0.90,而基于主要设计参数的模型会在部分船型中失效。结论所做研究可为船舶波浪增阻预报提供新的思路和方法,有利于在设计阶段充分考虑波浪增阻的影响从而有利于设计和优化船型。     

随机波浪联合折射绕射数学模型

基于波浪能量谱理论,导出了考虑底摩擦的复杂地形能量谱的联合折射绕射数学模型,在能量谱为单一频率组成波时,模型则简化为规则波的联合折射绕射方程.实际计算结果表明:本文提出的随机波浪联合折射绕射数学模型是合理的,在浅水区应该考虑底摩擦作用.     

多阶底部上的垂直可渗透结构斜海洋波的阻尼研究(英文)

Oblique ocean wave damping by a vertical porous structure placed on a multi-step bottom topography is studied with the help of linear water wave theory. Some portion of the oblique wave, incident on the porous structure, gets reflected by the multi-step bottom and the porous structure, and the rest propagates into the water medium following the porous structure. Two cases are considered: first a solid vertical wall placed at a finite distance from the porous structure in the water medium following the porous structure and then a special case of an unbounded water medium following the porous structure. In both cases, boundary value problems are set up in three different media, the first medium being water, the second medium being the porous structure consisting of p vertical regions-one above each step and the third medium being water again. By using the matching conditions along the virtualvertical boundaries, a system of linear equations is deduced. The behavior of the reflection coefficient and the dimensionless amplitude of the transmitted progressive wave due to different relevant parameters are studied. Energy loss due to the propagation of oblique water wave through the porous structure is also carried out. The effects of various parameters, such as number of evanescent modes, porosity, friction factor, structure width, number of steps and angle of incidence, on the reflection coefficient and the dimensionless amplitude of the transmitted wave are studied graphically for both cases. Number of evanescent modes merely affects the scattering phenomenon. But higher values of porosity show relatively lower reflection than that for lower porosity. Oscillation in the reflection coefficient is observed for lower values of friction factor but it disappears with an increase in the value of friction factor. Amplitude of the transmitted progressive wave is independent of the porosity of the structure. But lower value of friction factor causes higher transmission. The investigation is then carried out for the second case, i.e., when the wall is absent. The significant difference between the two cases considered here is that the reflection due to a thin porous structure is very high when the solid wall exists as compared to the case when no wall is present. Energy loss due to different porosity, friction factor, structure width and angle of incidence is also examined. Validity of our model is ascertained by matching it with an available one.     

Damping of Oblique Ocean Waves by a Vertical Porous Structure Placed on a Multi-step Bottom

Oblique ocean wave damping by a vertical porous structure placed on a multi-step bottom topography is studied with the help of linear water wave theory. Some portion of the oblique wave, incident on the porous structure, gets reflected by the multi-step bottom and the porous structure, and the rest propagates into the water medium following the porous structure. Two cases are considered： first a solid vertical wall placed at a finite distance from the porous structure in the water medium following the porous structure and then a special case of an unbounded water medium following the porous structure. In both cases, boundary value problems are set up in three different media, the first medium being water, the second medium being the porous structure consisting ofp vertical regions-one above each step and the third medium being water again. By using the matching conditions along the virtualvertical boundaries, a system of linear equations is deduced. The behavior of the reflection coefficient and the dimensionless amplitude of the transmitted progressive wave due to different relevant parameters are studied. Energy loss due to the propagation of oblique water wave through the porous structure is also carried out. The effects of various parameters, such as number of evanescent modes, porosity, friction factor, structure width, number of steps and angle of incidence, on the reflection coefficient and the dimensionless amplitude of the transmitted wave are studied graphically for both cases. Number of evanescent modes merely affects the scattering phenomenon. But higher values of porosity show relatively lower reflection than that for lower porosity. Oscillation in the reflection coefficient is observed for lower values of friction factor but it disappears with an increase in the value of friction factor. Amplitude of the transmitted progressive wave is independent of the porosity of the structure. But lower value of friction factor causes higher transmission. The investigation is then carried out for the second ca     

椭圆余弦波浅水变形实用计算法（I）——对《海港水文规范》的一个补充

尽管线性波浪理论不适宜应用在近岸浅水海域,但我国《海港水文规范》中波浪浅水变形的计算方法仍是建立在线性波浪理论的基础上,且没有考虑外界因素（如风和海底摩擦）的影响。为弥补上述不足,基于波浪传播过程中能量守恒的原理建立了一个波浪浅水变形的数值模型,该模型采用椭圆余弦波假定,并考虑了风和海底摩擦对波能的增加和损耗作用。在该数值模型基础上,分析大量工况下的计算结果,提出了便于工程设计初期用于确定近岸波浪要素的浅水变形实用计算方法（PCM）     

缓坡海岸平均沿岸流实验研究与数值模拟

沿岸流研究对海岸工程具有重要的应用价值。为了更深入地研究沿岸流特征,文章对1∶100和1∶40两个较缓坡条件下的沿岸流进行了实验研究,弥补了现有实验研究主要针对较陡坡情况,不具有代表性的弊端,并通过数值模拟进一步阐述了缓坡情况下的平均沿岸流不同于陡坡情况下的物理机理。主要特色与创新有：第一、通过物理模型实验研究发现了1∶100坡度地形条件下存在不同于1∶40坡度情况下的平均沿岸流速度分布特征：前者海岸一侧平均沿岸流分布呈下凹趋势,而后者呈上凸的趋势。第二、通过平均沿岸流数值模型对1∶100和1∶40缓坡沿岸流的不同特征进行数值模拟,找出了影响平均沿岸流速度剖面特征的主要因素为破波带内波高分布和水底摩擦力表达式的选取不同,且对后者更为敏感。1∶100坡度海岸沿岸流速度剖面可由水流型水底摩擦力来计算出,而1∶40坡度海岸沿岸流速度剖面可由波浪型水底摩擦力来计算出。第三、在此基础上进一步给出了缓坡情况下二次破碎波高和波浪增减水的分布特征。     

0-1型BEM与VOF方法耦合模型的研究与应用

文章讨论了近年来出现的波浪耦合数值模型,并建立了一个前域采用考虑底摩阻的0-1型BEM方法,后域采用VOF方法的双向耦合的波浪数值模型(0-1BEM+VOF模型)。应用模型计算了平缓岸坡上规则波的传播与破碎,并通过与物模试验的结果进行对比,表明了0-1BEM+VOF波浪耦合数值模型可以很好地模拟波浪的传播与强非线性变形,验证了该模型的有效性和准确性。     

双层通道中可渗透底部起伏的波浪散射(英文)

The scattering of plane surface waves by bottom undulations in channel flow consisting of two layers is investigated by assuming that the bed of the channel is composed of porous material. The upper surface of the fluid is bounded by a rigid lid and the channel is unbounded in the horizontal directions. There exists only one wave mode corresponding to an internal wave. For small undulations, a simplified perturbation analysis is used to obtain first order reflection and transmission coefficients in terms of integrals involving the shape function describing the bottom. For sinusoidal bottom undulations and exponentially decaying bottom topography, the first order coefficients are computed. In the case of sinusoidal bottom the first order transmission coefficient is found to vanish identically. The numerical results are depicted graphically in a number of figures.     

Wave Scattering by Porous Bottom Undulation in a Two Layered Channel

The scattering of plane surface waves by bottom undulations in channel flow consisting of two layers is investigated by assuming that the bed of the channel is composed of porous material. The upper surface of the fluid is bounded by a rigid lid and the channel is unbounded in the horizontal directions. There exists only one wave mode corresponding to an internal wave. For small undulations, a simplified perturbation analysis is used to obtain first order reflection and transmission coefficients in terms of integrals involving the shape function describing the bottom. For sinusoidal bottom undulations and exponentially decaying bottom topography, the first order coefficients are computed. In the case of sinusoidal bottom the first order transmission coefficient is found to vanish identically. The numerical results are depicted graphically in a number of figures.     

FPSO内孤立波载荷实验观测及理论预报模型研究

利用大型密度分层水槽开展了下凹型内孤立波作用在FPSO上的载荷特性系列实验;并依据实验工况,考虑KdV、eKdV和MCC内孤立波理论的适用性条件,数值研究了FPSO内孤立波载荷成分构成;基于实验结果和载荷成分构成,建立了FPSO内孤立波载荷的理论预报模型.研究表明:FPSO内孤立波水平载荷由粘性力和Froude-Krylov力组成,而垂向载荷主要为垂向Froude-Krylov力;Froude-Krylov力可通过动压力沿FPSO浮体湿表面积分得到,粘性力则通过经实验回归的摩擦系数Cf、形状修正因数K乘以内孤立波诱导水质点切向速度沿FPSO浮体湿表面积分得到.系列实验结果得出:摩擦系数Cf和形状修正因数K与雷诺数Re、KC数和流体层深度比h1/h有关;摩擦系数与Re呈自然对数关系;而形状修正因数K与KC数呈幂函数关系.理论预报模型预报的水平载荷、垂向载荷结果均与系列实验和数值结果吻合较好,并且发现随着内孤立波振幅的增加,载荷幅值近乎线性增加,而且上层流体深度对水平力幅值有明显的影响.