Ridge Loads on Wind Turbine Structures

K. Croasdale, N. Allyn
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引用次数: 1

Abstract

Wind turbine towers are being planned in ice covered regions subject to pressure ridges (e.g. the Great Lakes). Conical collars are often employed to reduce ice loads from level ice and their associated dynamics. For level ice, downward breaking cones have some advantages. It is not clear if this is the case for pressure ridges. This paper presents an improved method for ridge loads on wind turbines with downward breaking cones and makes comparisons with upward breaking cones. First year pressure ridges can be formidable ice features and usually control design ice loads in the sub-Arctic. Important components of a ridge creating ice loads are the consolidated layer at the surface (which is considered as solid ice) and the ridge keel below consisting of ice rubble, but much thicker. The load due to the consolidated layer is usually derived as if it is thick level ice. On a cone, methods for level ice assume it can be idealized as a plate on an elastic foundation (the water) and equations have been developed for upward and downward breaking cones. But for a ridge on a downward cone, to break the consolidated layer downwards requires it to be pushed into the keel rubble below. This will have a different foundation modulus than water buoyancy. A method is developed to account for this difference. The method uses an iterative approach to determine the point of breaking of the consolidated layer (and associated load) accounting for the ridge geometry, keel rubble shear strength, the flexural strength of the consolidated layer and the buoyancy forces. The keel loads on the vertical shaft below the conical collar are based on the method currently in ISO 19906 (2010) but modified to add the effect of additional rubble in the keel from breaking the consolidated layer downwards. In examples, it is shown that the breaking force can be about twice that of breaking the consolidated layer without the keel present. This might be seen as a disadvantage for downward breaking cones vs upward breaking. However, it is also shown that the clearing forces on an upward cone are higher; which tends to balance out the lower breaking force. Example loads are given on typical wind turbine bases due to typical ridges. Upward and downward breaking configurations are compared. The paper provides new methods for ice loads due to ridges acting on wind turbine structures not currently covered by existing methods.
风力涡轮机结构的脊荷载
风力涡轮机塔正计划建在受压力脊影响的冰雪覆盖地区(例如五大湖)。锥形环常用于减少水平冰的冰负荷及其相关的动力学。对于水平冰,向下破碎锥有一定的优势。目前尚不清楚压力脊是否也是如此。本文提出了一种改进的下破锥风力机脊荷载计算方法,并与上破锥进行了比较。第一年的压力脊可能是可怕的冰特征,通常控制着亚北极地区的设计冰负荷。山脊产生冰荷载的重要组成部分是表面的固结层(被认为是固体冰)和下面由冰碎石组成的脊龙骨,但要厚得多。固结层所产生的荷载通常被认为是厚的水平冰。对于圆锥体,水平冰的方法假设它可以理想化为弹性基础(水)上的板,并且已经开发了向上和向下破坏圆锥体的方程。但对于一个向下的圆锥上的山脊来说,要想向下打破固结层,就需要把它推到下面的龙骨碎石上。这将有一个不同的基础模量比水浮力。人们开发了一种方法来解释这种差异。该方法使用迭代方法来确定固结层的破裂点(以及相关载荷),该方法考虑了脊的几何形状、龙骨碎石的剪切强度、固结层的弯曲强度和浮力。锥形接箍下方竖井上的龙骨载荷基于ISO 19906(2010)中目前的方法,但进行了修改,以增加龙骨中额外的碎石向下破坏固结层的效果。算例表明,在没有龙骨存在的情况下,破坏力约为破坏固结层时的两倍。这可能被视为向下打破锥体与向上打破的缺点。然而,也表明,向上锥体上的清除力更大;这样就能平衡较低的断裂力。在典型的风力机基座上,由于典型的脊线,给出了示例载荷。比较了向上和向下的破碎形态。本文提供了一种新的方法来计算由于脊对风力涡轮机结构的作用而产生的冰荷载,而现有的方法尚未涵盖这种冰荷载。
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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