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Steel catenary riser (SCR) is the transmission device between the seabed and the floating production facilities. As developments move into deeper water, the fatigue life of the riser can become critical to the whole production system, especially due to the vortex-induced vibration (VIV), which is the key factor to operational longevity. As a result, experimental investigation about VIV of the riser was performed in a large plane pool which is 60 m long, 36 m wide and 6.5 m deep. Experiments were developed to study the influence of current speed and seabed on VIV of SCR. The results show that amplitudes of strain and response frequencies increase with the current speed both in cross-flow (CF) and in-line (IL). When the current speed is high, multi-mode response is observed in the VIV motion. The amplitudes of strain in IL direction are not much smaller than those in CF direction. The seabed has influence on the response frequencies of riser and the positions of damage for riser.  相似文献   
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华南及南海北部地区瑞利面波层析成像   总被引:2,自引:1,他引:1       下载免费PDF全文
基于华南及周边地区106个宽频带地震台站多年记录的MS≥5.0中浅源地震事件,开展瑞利面波层析成像和速度结构特征研究,获得了华南大陆及南海北部地区10~100s瑞利波群速度分布图像和典型剖面下方地壳上地幔速度结构,为理解该地区构造演化和深部过程提供约束.考虑到实际地震射线的覆盖情况以及华南地区主要构造的主体展布特征,本文同时采用传统的规则网格剖分和平行主要构造走向的非规则网格剖分方法,分别进行分格频散反演,开展了不同参数化方案对反演结果影响的对比分析研究.基于瑞利面波层析成像结果,进行了典型剖面横波速度结构反演,重建了华南地区由内陆至南海海域主要构造单元的壳幔横波速度结构.研究结果表明,扬子和华夏块体地壳上地幔结构特征差异显著,扬子块体地壳和岩石圈厚度均大于华夏地块,且扬子块体上地幔顶部速度较华夏块体低,岩石圈厚度在雪峰山造山带下方发生过渡和转换;南海北部陆缘和南海海盆上地幔速度较高且形态相对完整,表现为非火山型大陆边缘和已停止扩张海盆的壳幔结构特征.  相似文献   
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