袁鹏, 刘林, 司先才, 谭俊哲, 杜修茂, 王树杰. 波流耦合环境下潮流能水轮机阵列对区域潮流特性影响研究[J]. 太阳能学报, 2021, 42(9): 439-445. DOI: 10.19912/j.0254-0096.tynxb.2019-0576
引用本文: 袁鹏, 刘林, 司先才, 谭俊哲, 杜修茂, 王树杰. 波流耦合环境下潮流能水轮机阵列对区域潮流特性影响研究[J]. 太阳能学报, 2021, 42(9): 439-445. DOI: 10.19912/j.0254-0096.tynxb.2019-0576
Yuan Peng, Liu Lin, Si Xiancai, Tan Junzhe, Du Xiumao, Wang Shujie. STUDY ON INFLUENCE OF TIDAL TURBINE ARRAY ON REGIONAL TIDAL STREAM CHARACTERISTICS UNDER WAVE-CURRENT COUPLING[J]. Acta Energiae Solaris Sinica, 2021, 42(9): 439-445. DOI: 10.19912/j.0254-0096.tynxb.2019-0576
Citation: Yuan Peng, Liu Lin, Si Xiancai, Tan Junzhe, Du Xiumao, Wang Shujie. STUDY ON INFLUENCE OF TIDAL TURBINE ARRAY ON REGIONAL TIDAL STREAM CHARACTERISTICS UNDER WAVE-CURRENT COUPLING[J]. Acta Energiae Solaris Sinica, 2021, 42(9): 439-445. DOI: 10.19912/j.0254-0096.tynxb.2019-0576

波流耦合环境下潮流能水轮机阵列对区域潮流特性影响研究

STUDY ON INFLUENCE OF TIDAL TURBINE ARRAY ON REGIONAL TIDAL STREAM CHARACTERISTICS UNDER WAVE-CURRENT COUPLING

  • 摘要: 通过将Delft3D-FLOW和WAVE模块在线耦合,建立斋堂岛海域的三维波流双向耦合模型,并通过动量损失的方式等效模拟潮流能水轮机阵列,以此为基础研究波流耦合环境下潮流能水轮机阵列对区域潮流特性的影响。结果表明:水轮机阵列放置后,区域海域水位变化最大可达约2 cm,流速变化最大可达约0.4 m/s;在波流耦合环境下,沿岸区域以及水流流过水轮机阵列和海峡后的交汇区域水位和流速变化较大,且表层和中层流速变化更为明显,波浪带来的区域潮位变化约为1 cm,表层和中层流速变化约为0.25 m/s。

     

    Abstract: Using Delft3D online coupling,the Delft3D FLOW and WAVE modules are coupled to establish a three-dimensional bidirectional wave-current coupling model in the sea of Zhaitang Island,and the impact to the waters due to the operation of a turbine was emulated by adding a momentum loss term in the equations of the model. Then,the influence of the tidal current turbine array on the regional tidal field is studied under the environment. The results show that:after the turbine array is placed,the water level change in the regional sea area can reach up to 2 cm,and the flow speed can reach up to 0.4 m/s. In the wave-flow coupling environment,the water level and flow speed of the coastal area and the intersection of the water flow through the turbine array and the strait change greatly,and the surface and middle flow speed changes are more obvious. The tidal level change caused by the waves is about 1 cm,and the surface and middle flow speed changes are about 0.25 m/s.

     

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