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摘要:
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针对崖门航道所在海域水流、地形及泥沙特点,从悬移质不平衡输沙方程出发,导出估算挖槽回淤的计算公式,根据实测资料和潮流数值计算确定其中主要参数,并用1990年崖门试挖槽回淤资料确定公式中待定的综合系数。在此基础上估算了航道浚深不同方案的回淤强度与回淤量,并结合实际对结果进行了分析,结果表明航道回淤总体上并不严重,航道及所在海域基本上处于平衡微淤状态。
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Based on the characteristics of flow, topography and sediment of the sea area where Yamen waterway is located, the formula for assessment of the waterway's sediment deposition is derived from the equation of non-equilibrium sediment transport of suspended material. The major parameters are determined from the numerical simulation of tidal and field data. And the general coefficient is determined from the sediment deposition data of Yamen waterway's dredging up which is as a trial in 1990. Based on all of these, various projects' deposition strength and quantity are calculated and the solutions are analyzed, combining the observed data. Solutions show that the deposition of Yamen waterway is not significant. The sea area where the waterway located is in a balance state and little deposition.
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基金项目:
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国家自然科学基金(40476039);;
教育部科学技术研究重点项目(03095)资助
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作者简介:
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参考文献:
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[1] 上海航道勘察设计研究院.崖门5000吨级出海航道整治工程水文测验技术报告[R].2003年.
[2] 河海大学海岸及海洋工程研究所,广东省航道勘测设计科研所.西江崖门出海航道工程可行性研究(综合报告)[R].1992.
[3] JTJ213-98,海港水文规范[S].
[4] 李安中.横跨挖槽中流速变化及回淤预报[J].河海大学学报,1993,(1).
[5] 罗肇森.珠江崖门口拦门沙航道开发模型试验研究[A].内河航道整治工程技术交流大会文集[C].北京:人民交通出版社,1998.
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