Computation of Total Forces and Moments of Bodies of Revolution Moving Beneath the free Surface

Y. Hong
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Abstract

The accurate prediction of the total forces and moments of a body of revolution which is moving beneath the free surface with and without an angle of attack is one of the important areas in ship hydrodynamics. The experiments to measure these forces and moments were undertaken in the past by several researchers. The experimental results of forces and moments for a body of revolution near the free surface were reported in Reference 1 for various angles of attack and depths. Those of deep submergence were given in References 2, 3, and 4 for different angles of attack. Although there are many other published papers on the measurement of forces and moments, only the results of References 1-4 are used in this paper to compare with the predicted results. The total forces and moments consist of two parts in the present method; namely the inviscid part and the viscous part. The inviscid part of the forces and moments is computed using three-dimensional potential theory. The body boundary condition is exact and the free-surface condition is linearized. The body surface is discretized with many surface elements and the unknown strengths of the source and sink at each surface element are assumed to be constant. The velocities at surface elements are computed and saved for later computation of the viscous forces and moments. The viscous part of the forces and moments is computed with the application of the boundary layer theory for laminar and turbulent flows. The method developed by Young (Reference 5) is used to compute the total drag of bodies of revolution. It is assumed in this method that there is no flow separation. The axial force is computed with this method. The lateral force and pitching moment are computed under the assumption that there is separation in the two-dimensional cross flow. The boundary layer equation is solved to the separation point and the friction force is integrated to compute frictional drag. Furthermore, it is assumed that a constant pressure is acting on the two-dimensional section beyond the separation point.
在自由表面下运动的旋转体的总力和力矩的计算
在有攻角和无攻角情况下在自由水面下运动的旋转物体的总力和力矩的准确预测是船舶流体力学的重要研究领域之一。测量这些力和力矩的实验过去是由几位研究人员进行的。参考文献1报道了在不同攻角和深度下,在自由表面附近旋转物体的力和力矩的实验结果。深沉时不同攻角的数值见文献2、3、4。虽然关于力和力矩测量的论文已经发表了很多,但本文只使用参考文献1-4的结果与预测结果进行比较。在本方法中,总力和力矩由两部分组成;即无粘性部分和粘性部分。用三维位势理论计算了力和矩的非粘性部分。体边界条件是精确的,自由曲面条件是线性化的。将物体表面离散为多个面元,并假设每个面元处的未知源和汇强度为常数。计算了表面单元处的速度,并将其保存下来,以便以后计算粘性力和力矩。应用层流和紊流的边界层理论计算了力和力矩的粘性部分。采用Young(参考文献5)提出的方法计算公转体的总阻力。该方法假定不存在流动分离。用该方法计算了轴向力。在二维横流存在分离的假设下,计算了横流的侧向力和俯仰力矩。将边界层方程求解到分离点,并将摩擦力积分计算摩擦阻力。此外,假定在分离点以外的二维截面上有恒定的压力作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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