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作 者:陈纯[1] 黄玉新 韩志远[1] 杨华[1] CHEN Chun;HUANG Yu-xin;HAN Zhi-yuan;YANG Hua(Tianjin Research Institute for Water Transport Engineering,National Engineering Laboratory for Port Hydraulic Construction Technology,Key Laboratory of Engineering Sediment,Ministry of Transport,Tianjin 300456,China;Shanghai China Communications Water Transportation Design&Research CO.LTD.,Shanghai 200092,China)
机构地区:[1]交通运输部天津水运工程科学研究所,港口水工建筑技术国家工程实验室,工程泥沙交通行业重点实验室,天津300456 [2]上海中交水运设计研究有限公司,上海200092
出 处:《水道港口》2021年第3期318-322,327,共6页Journal of Waterway and Harbor
基 金:国家重点研发计划资助(2018YFC0809600,2018YFC0809602);中央级公益性科研院所基本科研业务费项目(TKS20200201)。
摘 要:以深圳至中山通道沉管隧道基槽工程为背景,建立二维水动力泥沙数学模型,采用现场实测资料进行验证,预测了大风过程基槽内的回淤分布。结果表明,基槽开挖后,最大下挖深度约30 m,大风过程引起的基槽淤积明显,回淤分布特征为中间大、两头小,最大淤厚为0.78 m。Based on the foundation tank project of the sinkhole tunnel in Shenzhen to Zhongshan channel,a two-dimensional hydrodynamic sediment mathematical model was established,and the field data were used to verify the results.The dredging distribution in the base tank was predicted.The results show that the maximum depth of excavation is about 30 m after excavation,the sedimentation of the foundation tank caused by the gale process is obvious,and the dredging distribution is characterized by a large middle and small two ends,and the maximum thickness is 0.78 m.
分 类 号:U65[交通运输工程—港口、海岸及近海工程]
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