潮汐通道

  • 网络tidal inlet;tidal channel
潮汐通道潮汐通道
  1. 潮汐通道系统动力地貌演变的数值模拟研究进展

    Advances in morphodynamic modeling of tidal inlet systems

  2. 水东潮汐通道的落潮三角洲处于均衡状态。

    We may consider that the ebb delta of Shuidong tidal inlet is in a balance condition .

  3. 胶州湾潮汐通道地貌体系

    Geomorphologic System in the Jiaozhou Bay Tidal Inlet

  4. 潮汐通道外泄水流喷射扩散对拦门沙形成的作用

    The Effect of Outflow Jet on the Formation of Entrance Bar in Tidal Inlet

  5. 潮汐通道口拦门沙航道的淤积计算

    Prediction of sedimentation for the navigation channel of a tidal inlet with mouth bar

  6. 浙江东部潮汐通道地区水下滑坡的类型及特征

    Classification and features of subaqueous landslide in the tidal channel region off Zhejiang Province

  7. 潮汐通道边坡潮流垂向结构及其底床冲淤数值模拟

    Vertical distribution of tidal current over side slope of channel and numerical model of its bottom deposition and erosion

  8. 口门内潮汐通道深槽泥沙净搬运趋势指向湖。

    The net transport trending of the sediments in the tidal channel within the channel mouth is towards the lagoon .

  9. 此外,对河流-潮汐通道截弯取直也导致了红树林死亡和海岸侵蚀。

    Making a cutoff of the river-tidal channel near the shore caused the death of the mangroves and shore erosion .

  10. 浙北近海潮汐通道地区水下滑坡分布及成因机制研究

    A study of the distribution and mechanism of subaqueous landslides in the tidal channel region of the northern inshore , zhejiang

  11. 而平台区由于设计管径仅为潮汐通道区的三分之一,其极限冲刷长度远小于潮汐通道区。

    Because the pipeline diameter in platform is one third of that in tidal channel , so the limit scour length is less .

  12. 本文介绍了黄海海底辐射沙洲与潮汐通道的可视模型以及建模的方法。

    Visual models and its forming methods of submarine radiative sandbar and tide channal in the Yellow Sea have been introduced in this paper .

  13. 对沙坝泻湖海岸潮汐通道的稳定性进行分析,探讨南方沙坝泻湖水道稳定的工程措施。

    This paper analyzes the stability of tidal waterway on the coast of sandbank and lagoon and discusses the engineering measures for the stability of sandbank and lagoon waterway in Southern China .

  14. 由于水流的非正向入射,潮汐通道地貌体系不对称,潮流三角洲在湾内东侧发育、在湾外东北侧发育。

    The obliquely inflowing current forms an asymmetric geomorphologic system in the tidal inlet , the tidal deltas are more developed on the east side of inner bay and on the northeast side of outer bay .

  15. 本文将波流实时耦合模式应用于潮汐通道理想算例,并按实时耦合、离线耦合模式分别对该算例进行了模拟,分析了波流相互作用下波浪场及流场的变化规律。

    The concurrent wave-current coupling model has been applied in an idealized case of tidal inlet , which is also simulated by offline coupling model . The change of wave field and current field has been analyzed .

  16. 在分析潮汐通道地区水下滑坡的区域环境的基础上,对水下滑坡的分类、结构特征、发育规模和形成时代进行了研究。

    Based on the analysis of regional environment conditions of the tidal channel region off Zhejiang Province , detail studies are carried out on the classification , structure features , dimensions and forming time of subaqueous landslides .

  17. 胶州湾属基岩海湾型潮汐通道,湾口内、外发育较为典型的涨、落潮流三角洲,地貌体系较为完整。

    The Jiaozhou Bay is a tidal inlet of bedrock bay type , the typical flood and ebb tidal deltas are developed inside and outside the bay mouth , and the geomorphologic system in the bay is complete .

  18. 其中岛群区依据潮汐通道的发育程度又划分为3个亚区:1舟山群岛北区、2舟山群岛南区、3南部岛群区。

    The islands region can be subdivided into three sub regions again according to the development degree of tidal channels : ⅲ 1 northern region of the Zhoushan Islands ,ⅲ 2 southern region of the Zhoushan Islands , and ⅲ 3 region south of Zhoushan Islands .

  19. 结果表明,由于华南弧形海岸遮蔽岸段发育有潮汐通道,湾内存在少量沿岸输沙等因素,致使判定准则并不能用于预测华南弧形海岸的稳定与侵蚀状况。

    The results show that the rules cannot be applied to forecast stability and erosion of the arc-shaped coasts in South China owing to the existence of tidal inlets in the shadow zones and a little alongshore sediment transportation within the arc-shaped bays in South China .

  20. 通过对水下滑坡的分布规律及潮汐通道的冲淤特征的分析,得出了潮汐通道的冲淤变化而引起的坡度增大是滑坡产生的主要诱发因素等结论。

    Based on the study of the distribution of landslides and the alteration of erosion and deposition in the tidal channels , a conclusion can be drawn that the increasing of gradient caused by the alteration of erosion and deposition is the main triggering factor to cause failures .

  21. 研究结果表明土体失稳主要分布于、2区的潮汐通道中,且以通道深槽边坡、通道凹岸、通道交汇处以及通道中的残留高地边缘等部位最为常见。

    Research results suggest that many instabilities exist in tidal channels of ⅱ and ⅲ 2 regions , what is more , the deep troughs of the channel , concave bank , conjoining of channels and margins of relict salients in channels are the positions where the instabilities concentrate .