首页> 外文会议>International conference on port and ocean engineering under arctic conditions >RUBBLE ICE TRANSPORT ON ARCTIC OFFSHORE STRUCTURES (RITAS), PART Ⅱ: 2D SCALE-MODEL STUDY OF THE LEVEL ICE ACTION
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RUBBLE ICE TRANSPORT ON ARCTIC OFFSHORE STRUCTURES (RITAS), PART Ⅱ: 2D SCALE-MODEL STUDY OF THE LEVEL ICE ACTION

机译:北极海洋结构(RITAS)上的碎冰运输,第二部分:碎冰作用的二维尺度模型研究

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A model scale experiment on the interaction between level ice and an arctic offshore structure with a downward bending hull was conducted in April 2012 in the large ice tank of HSVA. The experiments investigate the different mechanical processes contributing to the ice action. The present paper is completed by a companion paper "Rubble Ice Transport on Arctic Offshore Structures (RITAS), part I: Model scale investigation of level ice action mechanisms". Detailed investigations on special aspects of the level ice action mechanisms are presented in "Rubble Ice Transport on Arctic Offshore Structures (RITAS), part III: Analysis of scale model rubble ice stability" and "Rubble Ice Transport on Arctic Offshore Structures (RITAS), part IV Tactile sensor measurement of the level ice load on inclined plate". The structure, a so called buoyancy box, is inclined at the waterline and promotes a downward bending failure of the level ice. Two-dimensionality is introduced by limiting the panel width to 1 meter with two transparent Lexan plates allowing monitoring of the ice breaking and accumulation process. Several parameters are varied: ice thickness, ice density, ice velocity. A tactile sensor is installed on the ice breaking area of the structure to monitor the local waterline ice loads. During each interaction tests, the volume and buoyancy of the rubble accumulated on the structure are measured for derivation of the rubble porosity. The waterline ice load is oscillating. The experimental results show that the magnitude of the load peaks increases. The rubble is subjected to a rotating motion and to a series of collapse events. Increased buoyancy forces reduce the rubble porosity.
机译:2012年4月,在HSVA的大型冰罐中进行了水平冰与具有向下弯曲船体的北极近海结构之间相互作用的模型规模实验。实验研究了促冰作用的不同机械过程。本论文由配套论文“北极离岸结构上的碎冰运输(RITAS),第一部分:液面冰作用机理的模型规模研究”完成。有关“层冰作用机制”特殊方面的详细研究,请参见“北极离岸结构上的碎石冰运输(RITAS),第三部分:尺度模型碎石冰稳定性的分析”和“北极离岸结构上的碎石冰运输(RITAS)”,第四部分触觉传感器测量斜板上的冰负荷水平”。该结构,即所谓的浮力箱,在水线处倾斜,并促进了层冰的向下弯曲破坏。通过使用两个透明的Lexan板将面板宽度限制为1米来引入二维,从而可以监控破冰和积冰过程。几个参数是变化的:冰的厚度,冰的密度,冰的速度。触觉传感器安装在结构的破冰区域上,以监视局部水线的冰负荷。在每个相互作用测试过程中,测量堆积在结构上的瓦砾的体积和浮力,以推导瓦砾的孔隙率。水线的冰负荷正在振荡。实验结果表明,负载峰值的幅度增加了。瓦砾经受旋转运动和一系列塌陷事件。增大的浮力降低了瓦砾的孔隙率。

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