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1.
斜向不规则波对直墙作用的实验研究 总被引：5，自引：1，他引：5
通过长峰不规则波和方向波谱对直墙作用的实验研究 ,分别给出了每延米斜向不规则波波浪力与正向力之比 ,方向波谱波浪力与斜向长峰不规则波波浪力之间的关系 ,通过与规则波实验结果的比较给出了斜向规则波与不规则波波浪力之间的相对关系 ;并对斜向不规则波的反射系数与正向波时的变化作出了分析 相似文献
2.
本文应用有限元数值分析方法求解了不规则波作用下抛石基床上圆柱墩底部的渗流力.抛石基床内的渗流阻力采用了非线性的Forchheimer方程,同时还考虑了基床以外海床土内的渗流特性.为了验证所得到的数值解,进行了模型试验,两者吻合良好.应用所编程序,进行了大量计算以研究一些主要参数的影响.文中还对不规则波与规则波作用下渗流力的比值作了较为深入的分析,对此比值得到了一个可供工程实际应用的简化计算模式,从而可以简化不规则波作用下渗流力的计算. 相似文献
3.
不规则波越波量的实验研究 总被引：4，自引：0，他引：4
本文试验研究了不规则波在斜坡式和直墙式海堤或护岸上的越波量,给出了计算无因次越波量的公式,研究了斜堤堤坡和波谱宽度对越波量的影响。还探讨了利用概率分布法由规则波越波量计算不规则波越波量的可行性. 相似文献
4.
本文叙述了利用现有各类规则波造波机产生不规则波的简易方法。不规则的波模拟是通过模拟波谱来实现的。文中叙述了模拟波谱的基本原理。作为不规则电压信号的输入装置,先后采用了四种系统:即1、单机头发报机与继电器组系统;2、微处理机作为控制系统;3、单板计算机系统;4、磁带记录器系统。文中对模拟所得的不规则波作了谱分析及统计分析,并与靶谱作了比较。最后还对各系统的经济效益作了讨论。 相似文献
5.
本文研究立波作用下的层流、紊流边界层内的流速和传质速度,并采用谱法将传质速度推广到不规则波情况.根据实验与计算分析,研究了床面边界层内传质速度在堤前冲刷中的应用.研究结果表明,在传质速度的峰值附近形成底沙的冲刷坑;由于不规则波作用下堤前传质速度的峰值沿程递减,因此相应冲刷坑的深度沿程减少. 相似文献
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7.
p-y 曲线法常用于水平静力受荷桩的分析，但海洋工程中的桩基除静力外还承受波、流等循环荷载作用，将静力 p-y曲线直接用于循环荷载下桩基的设计研究时，往往会产生误差。本文梳理了水平循环荷载作用下 p-y 曲线模型的研究成果，
按照得到循环 p-y 曲线的不同方式，将其分为总体调整法和参数修正法。在参数修正法中，根据修正时考虑的因素不同，分为考虑荷载特性的修正和考虑桩土相互作用的修正。最后通过对循环荷载作用下 p-y 曲线研究现状的总结对比，评价了不同方法的特点，讨论了当前研究存在的问题并给出了建议。 相似文献
8.
本文提出了用频谱法计算不规则波和同向水流对孤立桩柱共同作用力的方法。对计算波流力有关的统计量,如流中的波谱、速度谱、力谱和相应的均方根值等提出了计算公式。文中,用算例对系统的传递函数、力谱及波——流力的大小作了分析和比较。指出,在波——流场中建造桩柱结构物时,必须考虑波——流共同作用的动力响应.而采用谱法求不规则波和流共同作用力是较简单和适用的。 相似文献
9.
本文用谱分析方法对方柱群墩结构在不规则波作用下的相互影响进行了计算。研究了在不同入射波向时每个方墩的群墩影响系数随墩距变化的规律并与折算圆墩的结果进行了比较。入射波谱采用Ｂｒｅｔｓｃｈｎｅｉｄｅｒ谱。计算结果表明方柱墩群与折算圆柱墩群的群墩影响系数较为接近且随着墩间距的增加趋近于孤立墩情形。 相似文献
10.
以不规则波在缓变地形和缓变流场水域的折射-绕射理论以及风浪的成长、衰减理论为基础,得到近岸区不规则波成长模型。结合近岸波浪特性和海洋工程应用的实际情况,建立综合考虑海岸、折射、白浪、底摩擦、流、风和非线性作用诸因素的近岸不规则波数值计算模型。该模型具有二维波谱特性及实用性。文章力图使模式更合理地反映近岸波浪的传播、成长和衰减规律,而整个计算工作量则较小,可在微型电子计算机上得以实现。 相似文献
11.
DETERMINATION OF THE DIRECTION AND VELOCITY OF INTERNAL TIDE WAVE BY MEANS OF MEASUREMENTS AT SINGLE STATION 总被引：1，自引：0，他引：1
In this paper, the method for determining the direction and velocity of internal tide wave is proposed. The main points are as follows: (1) starting with the continuity equation of incompressible fluid and taking the isotherm whose balance position is situated in the middle of the thermocline as the interface of two-layer ocean, one can get an equation of variations of average total current in the lower and upper layers; (2) WTide (Z) in the above-mentioned equation is expressed in first-order approximation; (3) the internal tide waves are treated as wave packets. Thus, one finds out a statistical relation, AΔu BΔv =ζ, which correlates the average shear effect caused by the internal tide wave with the isothermal fluctuation. The direction and velocity of the wave can be drawn from the formulae: (((1=Arctg (A/B), C1=1/(H0(A2 B2)~1/2).The calculated results agree, in the main, fairly well with two sets of observations at station L3. 相似文献
12.
Wen Shengchang 《海洋学报(英文版)》1988,7(1):1-16
In this part ot the paper theoretical wind-wave spectra nave been derived oy (I) expressing the spectrum in series composed of exponential terms; (2) assuming that the spectrum satisfies a high order linear ordinary differential equation; (3) introducing proper parameters in the spectrum; and (4) making use of some known charateristics of wind-wave spectrum, for instance, the law governing the equilibrium range. The spectrum obtained contains the zero order moment of the spectrum m0, the peak frequency ω0 and the ratio R =ω/ω0 (ω being the mean zero-crossing frequency) as parameters. The shape of the nondimensional spectrum S(ω) = ω0S(ω)/m0(ω=ω/ω0) changes with R and theoretically reduces to a Dirac delta function δ(ω-1) when R = 1. A spectrum of simplified form is given for practical uses, in which R is replaced by a peakness factor P=S(1). 相似文献
13.
The effects of free-surface waves on the floating structures are of great importance in the offshore industry. Among the six degrees of motions of a surface ship the absence of restoring forces in surge, sway and yaw led to critical situations for moored ships in the recent times. The order of forces in horizontal plane and their exciting frequencies are matters of interest. The resonance with the presence of moored chains led to many accidents in the recent past. The lines in dry conditions may not give good damping and in wet condition they may trigger the system to chaotic motions and jumps. Two different loading conditions of a container ship model are tested with waves in laboratory conditions in two different drafts. The mooring lines are chosen as per scale law and the energy under the response spectrum is determined from the plots. The results give new insights into the movement of a berthed ships subjected to waves. Response of the moored ship to different loading conditions in different water depths are discussed in this paper. The paper gives the order of energy due to first-order and slowly varying movement of a berthed container model in a towing tank. 相似文献
14.
The transfer of liquid bulk through flexible transfer lines can be accomplished despite relatively large ship motions. For this reason, open sea berth terminals have replaced conventional harbors in many places. The thorough understanding of moored ships dynamics when subjected to waves, wind and currents, combined with the use of flexible dolphins, flexible fenders, asymmetric constant-tension winches and nylon tails permit us to design open sea berth terminals for relatively exposed areas. The design of an integrated system of marine sensors to continuously monitor all the critical elements-ship motion and mooring and fender forces-will enhance the operational procedure whilst insuring safe operations. A berth code can then be established for insuring the maximum efficiency of the terminal on the basis of the measurement of these critical elements. 相似文献
15.
The application of directional waves in design processes has clearly received much interest during recent years. Thus, in model testing with moored ships and offshore structures, significant deviations have been revealed between results obtained in traditional uni-directional wave trains and those obtained in directional wave fields. Whether the same tendency is valid in connection with the design of rubble mound breakwaters is studied in the present project. A breakwater with a front slope of 1:2 is tested at the scale 1:40. The weight and diameter of the stones in the core, filter and armour layers were carefully selected, and the sources of scatter in repeated tests were minimized. Furthermore, the incident wave energy was accurately adjusted to keep the same level in both uni-directional and directional waves. For the actual rubble-mound breakwater unambiguous results were obtained. When uni-directional waves were applied, the damage increased by 30–50% relative to the directional wave situation. 相似文献
16.
measurements by a circular array consisting of 18 wave gauges in a large wave tank, directional spectra of wind-generated waves in deep water are systematically determined by using maximum likelihood method The investigations reveal that the angular spreading of the wave energy is consistent with cos2s(θ/2) proposed by Longuet-Higgins et al.(1963, Ocean Wave Spectra, 111-136), if the bimodal distributions of wave energy are not taken into account. Bimodality occurring on higher frequency than peak frequency is too rare to affect our whole resalts. Surprisingly, a much broader directional spreading than that of the field, which is interpreted by the strongly nonlinear energy transfer because of the very young waves in laboratory, is found. The parameter s depends on frequency in the same way as observed by Mitsuyasu et al.(1975, Journal of Physical Oceanography, 5, 750-760) and Hasselmann et al.(1980, Journal of Physical Oceanography, 10, 1264-1280) in the field, and the relationship between the four nondimensional parameters sm, fo, b1 and b2, determining the directional width, and ū10 (corresponding to the inverse of wave age) are given respectively. The observed distributions are found to agree well with the suggestion of Donelan et al.(1985, Philosophical Transaction of Royal Society of London, A315, 509-562) when applied to field waves. 相似文献
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18.
Stig E. Sand 《Coastal Engineering》1982,6(3):195-208
In recent years the group-induced long waves have received an enhanced degree of attention. Especially in nearshore regions, the long waves can be of considerable height, and consequently the influence on harbour resonance, on the operation of ship terminals, on moorings of large vessels, etc. is obviously very important. It is the grouping of natural wave fields that generates the long waves, and they are proportional to the square of the short-wave height. Therefore, the expressions for the long-wave elevations can be found to include the short-wave components of the wave field and a second-order transfer function. This function is presented in a diagram with dimensionless parameters. For practical purposes a formula for rough estimate of the long-wave height is proposed.The second-order equations show that the long waves are determined by the difference of the wave-number vectors of the short waves. This is shown to imply that the spread of the long waves is larger than that of the short waves, and that the wave lengths of the long waves are dependent on the short-wave spread. Hereby it is possible to change the long-wave lengths, which seems to be a quality of great practical importance.The long waves are also expressed in spectral terms. That is, a formula for the directional long-wave spectrum is shown to comprise the transfer function squared and the short-wave amplitudes and phases. 相似文献
19.
Noriyuki Iwata 《Journal of Oceanography》1971,27(3):102-108
Two-dimensional ocean wave spectrum developing under the atmospheric surface pressure fluctuations is linearly correlated with that of wind pressure itself, so that angular distribution of energy of ocean surface waves can be determined by directional properties of surface pressure fluctuations with the same frequency to the surface wave.From empirically determined spectral formula of the atmospheric surface pressure fluctuations the coefficients of Fourier series expanded around mean direction of wind are analytically integrated, from which r.m.s. angular distribution, spectral peakedness and long-crestedness are calculated, compared with previously proposed empirical formulae and observations carried out by ultrasonic current meter. 相似文献