山东半岛东南部典型砂质岸滩季节性演化及控制因素探讨——以海阳万米海滩为例

解航, 杨怡红, 朱龙海, 张晓东, 胡日军, 尹砚军, 冷星. 山东半岛东南部典型砂质岸滩季节性演化及控制因素探讨——以海阳万米海滩为例[J]. 海洋地质与第四纪地质, 2022, 42(1): 57-67. doi: 10.16562/j.cnki.0256-1492.2021042301
引用本文: 解航, 杨怡红, 朱龙海, 张晓东, 胡日军, 尹砚军, 冷星. 山东半岛东南部典型砂质岸滩季节性演化及控制因素探讨——以海阳万米海滩为例[J]. 海洋地质与第四纪地质, 2022, 42(1): 57-67. doi: 10.16562/j.cnki.0256-1492.2021042301
XIE Hang, YANG Yihong, ZHU Longhai, ZHANG Xiaodong, HU Rijun, YIN Yanjun, LENG Xing. Seasonal evolution of the typical sandy coast of southeastern Shandong Peninsula and controlling factors—Take the 10 000-meter beach in Haiyang as an example[J]. Marine Geology & Quaternary Geology, 2022, 42(1): 57-67. doi: 10.16562/j.cnki.0256-1492.2021042301
Citation: XIE Hang, YANG Yihong, ZHU Longhai, ZHANG Xiaodong, HU Rijun, YIN Yanjun, LENG Xing. Seasonal evolution of the typical sandy coast of southeastern Shandong Peninsula and controlling factors—Take the 10 000-meter beach in Haiyang as an example[J]. Marine Geology & Quaternary Geology, 2022, 42(1): 57-67. doi: 10.16562/j.cnki.0256-1492.2021042301

山东半岛东南部典型砂质岸滩季节性演化及控制因素探讨——以海阳万米海滩为例

  • 基金项目: 国家自然科学基金项目“山东半岛海湾对泥沙的捕获机制——以威海湾为例”(41776059);山东省自然科学基金项目“近50年来山东半岛滨海沙滩侵蚀演变的定量评价及其影响因素”(ZR2019MD037)
详细信息
    作者简介: 解航(1994—),男,硕士研究生,主要从事海洋沉积动力地貌学研究,E-mail:554812239@qq.com
    通讯作者: 朱龙海(1979—),男,教授级高级工程师,主要从事海洋沉积动力地貌学研究,E-mail:zhulonghai@ouc.edu.cn
  • 中图分类号: P736.21

Seasonal evolution of the typical sandy coast of southeastern Shandong Peninsula and controlling factors—Take the 10 000-meter beach in Haiyang as an example

More Information
  • 根据2018年秋季至2019年夏季4个季节的海滩剖面形态测量和表层沉积物粒度分析结果,研究了海阳万米海滩地形和表层沉积物粒度季节变化特征,探讨了控制研究区砂质岸滩季节性演化的因素。结果表明:连理岛-东村河口以西海滩剖面形态在强动力和弱动力条件下分别呈“上蚀下淤”和“下冲上塑”特征,夏季台风造成的滩肩侵蚀量大于冬季风,在滩面形成的沙坝数量多、规模小且离岸距离较之冬季风更远。连理岛-东村河口处海滩剖面形态整体呈淤积状态,且在强动力条件下的淤积量大于弱动力条件。连理岛-东村河口以东海滩剖面形态的季节性变化幅度小于以西海滩,同时滩肩顶剖面形态在夏季出现明显下凹特征。表层沉积物粒度特征变化同样呈现东西差异的特点,秋季到冬季,西侧海滩表层沉积物粒度变粗、分选变差,而东侧海滩变细、分选基本不变;冬季到春季,海滩表层沉积物粒度总体变细、分选较好;夏季变化趋势与冬季相似,但变化幅度有所差异。人工岛和港口等海岸工程建设是导致海滩剖面形态和表层沉积物粒度东西差异的主导因素;波浪和台风事件等是控制砂质岸滩季节性演化的主要动力因素;潮汐作用、旅游开发等人类活动也对岸滩演化造成一定影响。

  • 加载中
  • 图 1  研究区地理位置及取样站位图

    Figure 1. 

    图 2  研究区海滩地形测线

    Figure 2. 

    图 3  连理岛-东村河以西、以北海滩剖面图

    Figure 3. 

    图 4  连理岛-东村河以东海滩剖面图

    Figure 4. 

    图 5  研究区海滩表层沉积物平均粒径、分选系数季节变化图

    Figure 5. 

    图 6  研究区岸滩时空演化控制因素示意图

    Figure 6. 

    图 7  台风“利奇马”过境期间研究区风向变化[37]

    Figure 7. 

    表 1  研究区海滩滩肩表层沉积物取样起止点坐标

    Table 1.  Coordinates of starting and ending points for surface sediments sampling on beach berms in the study area

    起点终点
    纬度经度纬度经度
    T136°41′39.33″N121°12′55.47″E36°41′36.05″N121°12′56.07″E
    T236°41′16.52″N121°11′38.61″E36°41′14.79″N121°11′39.75″E
    T336°40′47.13″N121°10′41.74″E36°40′45.61″N121°10′42.83″E
    T436°40′16.59″N121°09′23.52″E36°40′15.24″N121°09′24.40″E
    T536°39′09.94″N121°07′24.05″E36°39′06.58″N121°07′26.55″E
    T636°38′14.81″N121°06′18.86″E36°38′10.93″N121°06′22.96″E
    下载: 导出CSV

    表 2  研究区海滩滩肩表层沉积物分选等级季节变化

    Table 2.  Seasonal variation of sorting coefficient of berm surface sediments in the study area

    T1T2T3T4T5T6
    较好中等较好较好中等
    中等中等中等较好较好较好
    较好较好较好较好较好较差
    较差中等较差较好较好
    下载: 导出CSV

    表 3  研究区海滩滩面表层沉积物分选系数季节变化

    Table 3.  Seasonal variation of sorting coefficient of beach surface sediments in the study area

    T1T2T3T4T5T6
    较好中等较差较好中等中等
    较差中等较差中等较好
    较好较差中等较好较好较好
    较好较好较好
    下载: 导出CSV

    表 4  2018年秋季至2019年冬季研究区波浪和风场变化

    Table 4.  Wave and wind field changes in the study area from autumn 2018 to winter 2019

    2018年秋季2018年冬季2019年春季2019年夏季
    有效波高/m0.720.930.750.74
    平均波向NNENWSSWSSE
    平均风速/(m/s)1.572.821.302.48
    风向NNWNNWSSWS
    下载: 导出CSV

    表 5  研究区2018年秋季至2019年冬季浪潮作用指数计算结果

    Table 5.  Calculation results of wave action index from autumn 2018 to winter 2019 in the study area

    2018年秋季2018年冬季2019年春季2019年夏季
    H1/10/m0.921.190.960.95
    MHW/m1.180.921.071.32
    MLW/m–1.08–1.31–1.16–0.91
    /m2.272.212.212.18
    K1.021.341.071.07
    下载: 导出CSV
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出版历程
收稿日期:  2021-04-23
修回日期:  2021-06-02
刊出日期:  2022-02-28

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