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Deflection of ice cover caused by an underwater body moving in channel

机译:由水下体在通道中移动引起的冰盖的偏转

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摘要

Deflections and strains in an ice cover of a frozen channel caused by an underwater body moving under the ice with a constant speed along the channel are studied. The channel is of rectangular cross section, the fluid in the channel is inviscid and incompressible. The ice cover is clamped to the channel walls. The ice cover is modeled by a thin viscoelastic plate. The underwater body is modeled by a three-dimensional dipole. The intensity of the dipole is related to the speed and size of the underwater body. The problem is considered within the linear theory of hydroelasticity. For small deflections of the ice cover the velocity potential of the dipole in the channel is obtained by the method of images in leading order without account for the deflection of the ice cover. The problem of moving dipole in the channel with rigid walls provides the hydrodynamic pressure on the upper boundary of the channel, which corresponds to the ice cover. This pressure distribution does not depend on the deflection of the ice cover in the leading approximation. The deflections of the ice and strains in the ice plate are independent of time in the coordinate system moving together with the dipole. The problem is solved numerically using the Fourier transform, method of the normal modes and the truncation method for infinite systems of algebraic equations.
机译:研究了由沿着通道的恒定速度在冰下移动的水下体移动引起的冷冻通道的冰盖中的抗弯和菌株。通道是矩形横截面,通道中的流体是无胶片和不可压缩的。夹层夹在通道壁上。冰盖由薄粘弹性板材建模。水下体由三维偶极模拟。偶极子的强度与水下体的速度和尺寸有关。在水力弹素的线性理论内被认为是问题。对于冰覆盖冰的小偏转,通过在未考虑冰盖的偏转的情况下,通过以领导顺序的图像的方法获得频道中偶极子的速度电位。具有刚性壁的通道中移动偶极子的问题在通道的上边界上提供了流体动力学压力,其对应于冰盖。该压力分布不依赖于冰盖在前导近似的偏转。冰板中的冰和菌株的偏转与坐标系的时间与偶极子一起移动。使用傅里叶变换,正常模式的方法和代数方程的无限系统的截断方法来数值求解问题。

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