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海岸沙坝剖面和滩肩剖面特征研究

张洋 邹志利 苟大荀 罗年鹏 尹晶

张洋, 邹志利, 苟大荀, 罗年鹏, 尹晶. 海岸沙坝剖面和滩肩剖面特征研究[J]. 海洋学报, 2015, 37(1): 147-157. doi: 10.3969/j.issn.0253-4193.2015.01.015
引用本文: 张洋, 邹志利, 苟大荀, 罗年鹏, 尹晶. 海岸沙坝剖面和滩肩剖面特征研究[J]. 海洋学报, 2015, 37(1): 147-157. doi: 10.3969/j.issn.0253-4193.2015.01.015
Zhang Yang, Zou Zhili, Gou Daxun, Luo Nianpeng, Yin Jing. Experiment study on evolution and geometrical characteristics of sandbar profile and berm profile[J]. Haiyang Xuebao, 2015, 37(1): 147-157. doi: 10.3969/j.issn.0253-4193.2015.01.015
Citation: Zhang Yang, Zou Zhili, Gou Daxun, Luo Nianpeng, Yin Jing. Experiment study on evolution and geometrical characteristics of sandbar profile and berm profile[J]. Haiyang Xuebao, 2015, 37(1): 147-157. doi: 10.3969/j.issn.0253-4193.2015.01.015

海岸沙坝剖面和滩肩剖面特征研究

doi: 10.3969/j.issn.0253-4193.2015.01.015
基金项目: 国家自然科学基金(51079024);国家创新群体基金(51221961)。

Experiment study on evolution and geometrical characteristics of sandbar profile and berm profile

  • 摘要: 通过物理模型实验研究了海岸沙坝剖面和滩肩剖面的形成和演化过程,给出了稳定的沙坝剖面和滩肩剖面的几何特征。实验中考虑了两种初始坡度(1:20和1:10)和不同波高的规则波和不规则波,讨论了不同初始坡度海岸上破碎波空间分布特征。结果表明,沙坝产生后存在向岸和离岸两种运动形态,但最终将停留在稳定位置。稳定的沙坝剖面对应不同初始坡度和波浪存在不同的大沙坝和小沙坝分布。沙坝剖面由长时间小波高波浪序列作用后可转化为稳定滩肩剖面,该剖面不依赖于波浪和初始坡度。实验也给出了平衡剖面与理论曲线的对比以及剖面上泥沙粒径的分布。
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出版历程
  • 收稿日期:  2013-11-09
  • 修回日期:  2014-08-22

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