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作 者:呼文佳 王世圣 赵晶瑞 HU Wenjia;WANG Shisheng;ZHANG Jingrui(CNOOC Research Institute Co.,Ltd.,Beijing 100028,China)
机构地区:[1]中海油研究总院有限责任公司,北京100028
出 处:《海洋工程》2022年第6期125-132,共8页The Ocean Engineering
基 金:“十三五”国家科技重大专项课题“深水平台工程技术”(2016ZX05028-002)。
摘 要:为揭示张力腿平台涡激运动响应规律,采用数值模拟与模型试验相结合的方法研究了全水深系泊张力腿平台涡激运动响应。根据张力腿平台主尺度参数,按照几何相似制作了水池试验模型,在满足运动相似和动力相似的条件下开展了均匀流、剖面流模型试验,并将模型试验结果与数值模拟结果进行了对比,验证了数值模拟与模型试验结果的一致性。分析结果表明在均匀流作用下张力腿平台涡激运动的锁定区间在5.5<U_(r)<8.5,来流角对涡激运动影响较大。剖面流作用下平台涡激运动规律与均匀流作用基本一致,但剖面流造流引起的能量分散,使平台在XY平面的运动轨迹变得不规律,系泊系统提供的回复力对涡激运动幅值有抑制作用,来流角和流速对张力腿或立管模态影响明显。论文得到结论对于张力腿平台的工程设计有一定借鉴意义。In order to obtain the TLP vortex-induced motion response mechanism,the method of combining numerical simulation and model experiment was used to study the response of TLP vortex-induced motion in a full-water depth mooring.According to the main scale parameters of TLP,the test model was made according to the geometric similarity.And under the conditions of similar motion and similar dynamics,a joint model test of uniform flow,profile flow and wave flow was carried out.The model test results were compared with the numerical simulation results to verify the consistency between the numerical simulation and the model test.The analysis results show that the locking interval of TLP vortex-induced motion is 5.5<U_(r)<8.5,and the incoming flow angle has a greater impact on the vortex-induced motion.The vortex-induced motion law of the platform under the action of the profile flow is basically consistent with that of the uniform flow.However,the energy dispersion caused by Creating profile flow makes the motion trajectory of the platform in the XY plane irregular.The restoring force provided by the mooring system has an inhibitory effect on the amplitude of vortex-induced motion.Incoming flow angle and flow velocity have obvious influence on tension leg or riser mode.The conclusions obtained from the research have certain reference significance for the research and design of TLP.
关 键 词:张力腿平台 张力腿 涡激运动 模型试验 数值模拟 均匀流 剖面流
分 类 号:P751[交通运输工程—港口、海岸及近海工程] U661.32[天文地球—海洋科学]
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