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CHARACTERISTIC LEVELS OF STRONGLY NONLINEAR EXTREME WAVE LOAD EFFECTS

机译:强非线性极端波荷载作用的特征水平

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Offshore structures are typically required to withstand extreme and abnormal load effects with annual probabilities of occurrence of 10~(-2) and 10~(-4) respectively. For linear or weakly nonlinear problems, the load effects with the prescribed annual probabilities of occurrence are typically estimated as a relatively rare occurrence in the short term distribution of 100 year and 10 000 year seastates. For strongly nonlinear load effects, it is not given that an extreme seastatc can be used reliably to estimate the characteristic load effect. The governing load may occur as an extremely rare event in a much lower seastate. In attempting to model the load effect in an extreme seastate, the short term probability level is not known nor is it known whether the physics of the wave loading is captured correctly in an extreme seastate. Examples of such strongly nonlinear load effects are slamming loads on large volume offshore structures or wave in deck loads on jacket structures subject to seabed subsidence. Similarly, for structures which are unmanned in extreme weather, the governing load effects for the manned structure will occur as extremely rare events in a relatively frequent seastate. The present paper is concerned with the long term distribution of strongly nonlinear load effects. Using a simple point estimate of the wave elevation correct to second order and a crest kinematics model which takes into account the possibility of wave breaking, the long term distribution of drag load on a column above the still water level is studied and compared with a similar loading model based on second order kinematics which does not include the effect of wave breaking. The findings illustrate the challenges listed above. Model tests are useful in quantifying strongly nonlinear load effects which cannot be calculated accurately. But only a relatively small number of seastates can be run in a model test campaign and it is not feasible to estimate short term responses far beyond the three hour 90% fractile level. Similarly, Computational Fluid Dynamics (CFD) is increasingly useful in investigating complex wave induced load effects. But only a relatively small number of wave events can be run using CFD, a long term analysis of load effects cannot in general be carried out. It appears that there is a class of nonlinear problems which require a long term analysis of the load effect in order for the annual probability of occurrence to be estimated accurately. For problems which cannot be estimated by simple analytical means, the governing wave events can be identified by long term analysis of a simple model which capture the essential physics of the problem and then analysed in detail by use of CFD or model tests.
机译:海上结构通常需要承受极端和异常载荷的影响,每年的发生概率分别为10〜(-2)和10〜(-4)。对于线性或弱非线性问题,通常将具有指定年发生概率的负载效应估计为在100年和10000年海域的短期分布中相对罕见的事件。对于强烈的非线性载荷效应,没有给出可以可靠地使用极限静压来估算特征载荷效应的假设。在低得多的海域中,控制负载可能是极为罕见的事件。在尝试对极端海况下的载荷效应进行建模时,未知短期概率水平,也不知道是否在极端海况下正确捕获了波浪载荷的物理性质。这种强烈的非线性载荷效应的例子包括大体积海上结构的猛击载荷或受海床沉陷影响的夹层结构的甲板载荷波动。类似地,对于在极端天气中无人值守的结构,有人值守结构的控制负载效应将在相对频繁的海域中作为极为罕见的事件发生。本文关注强非线性载荷效应的长期分布。使用校正到二阶的波高的简单点估计以及考虑了破波可能性的波峰运动学模型,研究了静水水位以上柱上阻力的长期分布,并将其与类似方法进行了比较。基于二阶运动学的载荷模型,其中不包括波浪破碎的影响。调查结果说明了上面列出的挑战。模型测试可用于量化无法精确计算的强烈非线性载荷效应。但是在模型测试活动中只能运行相对少量的海况,并且无法估计远远超过三小时90%的脆性水平的短期响应。同样,计算流体动力学(CFD)在研究复杂波引起的载荷效应中越来越有用。但是,使用CFD只能运行相对较少的波浪事件,通常无法对载荷效应进行长期分析。似乎存在一类非线性问题,需要对负载效应进行长期分析,以便能够准确估算年度发生概率。对于无法通过简单分析方法估算的问题,可以通过对简单模型进行长期分析来识别控制波事件,该模型可以捕获问题的基本物理原理,然后使用CFD或模型测试进行详细分析。

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