利用开尔文-纽曼近似的二阶差频波流加载

Farid P. Bakti, Moo-Hyun Kim
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摘要

Kelvin & Newman引入了一种线性化方法,将电流(或前进速度)效应纳入大型细长浮体的衍射和辐射波场。K-N法假设有稳定的远场电流,而忽略了由于物体存在而产生的稳定势场。当弗劳德数比较小,体型比较修长(∂∂x≪∂∂,∂∂z),海况温和时,这种方法被证明是可靠的。对于典型的fpso和船型船来说,在典型的当前(或前进速度)条件下,这一要求是可以满足的。一些研究表明,电流的存在可能会改变一阶流体动力系数,如一阶衍射力、附加质量和辐射阻尼。电流也导致了二阶缓慢变化的漂移力的变化。然而,电流对二阶差频力的影响还有待研究。通过将Kelvin-Newman近似扩展到二阶,并在频域中求解,在提高格式精度的同时节省了计算时间。二阶二次力是本研究的主要焦点,因为它是总二阶差频力的主要贡献者,特别是在对角线附近。通过将开尔文-纽曼波流相互作用方法实现到波的二阶,我们可以评估开尔文-纽曼波流相互作用公式在各种海况下的性能。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Second Order Difference Frequency Wave-Current Loading Using Kelvin-Newman Approximation
Kelvin & Newman introduced a linearization method to include the current (or forward speed) effect into the diffraction & radiation wave field for large-slender floating bodies. The K-N method assumes a steady far-field current while disregarding the steady potential field due to the presence of the body. The method is proven to be reliable when the Froude number is relatively small, the body shape is relatively slender (∂∂x≪∂∂y,∂∂z), and the sea condition is mild. This requirement is fulfilled for typical FPSOs and ship-shaped vessels in a typical current (or forward speed) condition. Several studies suggested that the presence of the current might change the first order hydrodynamic coefficients such as the first order diffraction force, added mass, and radiation damping. Currents also contributed to a change in the second-order slowly-varying drift force. However, the effect of current in the second-order difference-frequency force is yet to be investigated. By expanding the Kelvin-Newman approximation up to the second order, and solving the problem in the frequency domain, we can save computational time while expanding the accuracy of the scheme. The second order quadratic force is the main focus of this study, since it is the main contributor to the total second order difference frequency forces especially near the diagonal. By implementing the Kelvin-Newman wave current interaction approach up to the wave’s second order, we can assess the performance of the Kelvin-Newman wave current interaction formulation in various sea conditions.
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