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浙江朱家尖岛东南沙滩群地形年际变化特征及影响因素

汪拾金 张一鸣 王致辉 胡鹏 董超 李薇

海洋地质前沿2025,Vol.41Issue(8):1-12,12.
海洋地质前沿2025,Vol.41Issue(8):1-12,12.DOI:10.16028/j.1009-2722.2024.172

浙江朱家尖岛东南沙滩群地形年际变化特征及影响因素

Inter-annual morphological evolution characteristics and impact factors of the southeastern sandy beaches of Zhujiajian Island,Zhejiang Province

汪拾金 1张一鸣 2王致辉 3胡鹏 4董超 5李薇2

作者信息

  • 1. 东海实验室,舟山 316021||浙江省海洋地质调查大队,舟山 316021
  • 2. 浙江大学海洋学院,杭州 310058
  • 3. 浙江省海洋地质调查大队,舟山 316021
  • 4. 浙江大学海洋学院,杭州 310058||浙江大学舟山海洋研究中心,舟山 316021
  • 5. 浙江省水文地质工程地质大队,宁波 315000
  • 折叠

摘要

Abstract

To investigate the morphological evolution characteristics and impact factors of the southeastern sandy beaches in Zhujiajian,Zhejiang,six topographic surveys of bed profiles were conducted from November 2012 to November 2015.Results show that the beach morphology exhibited significant seasonal variations before beach nourishments.Specifically,the period from post-typhoon to the end of winter was featured by extensive accretion in upper and middle beach,with a maximum accretion height of 0.97 m.Meanwhile,the top and bottom of the beaches showed slight erosion,with erosion depths generally less than 0.3 m.Beach berms was formed as shown in the northern Dongsha and southern Nansha profiles.From spring to pre-typhoon season,the middle beach was eroded while the upper and lower beach were silted up,with the maximum erosion depth and accretion height of approximately 0.8 and 0.5 m,respectively.During the typhoon season,intense erosion occurred in the upper and middle parts of the beaches,with maximum erosion depth exceeding 1.0 m,while the lower parts experienced ac-cretion,with maximum accretion height around 0.45 m,forming typical storm profiles.From November 2012 to November 2015,significant inter-annual morphological changes were observed in the southern Dongsha and northern Nansha with local erosion depths exceeding 1.0 m,which indicates erosion risks.In contrast,Qiansha,Lisha,and Qingsha exhibited dynamic equilibrium state with morphological changes ranged between-0.6 m and 0.4 m.Additionally,the morphological evolution of the beaches was jointly controlled by tides and waves,during which geomorphological conditions and human activities further influenced the morphological features.Dongsha,being less sheltered by headlands,experienced stronger hydrodynamic forces and more intense morphological changes.Human activities may contribute to the erosion in Dongsha and Nansha,highlighting the importance of scientifically design of artificial structures to maintain the natural dynamic balance of the beaches.

关键词

朱家尖岛/沙滩/地形变化/水动力/人类活动

Key words

Zhujiajian Island/sandy beach/morphological evolution/hydrodynamic/human activity

分类

海洋科学

引用本文复制引用

汪拾金,张一鸣,王致辉,胡鹏,董超,李薇..浙江朱家尖岛东南沙滩群地形年际变化特征及影响因素[J].海洋地质前沿,2025,41(8):1-12,12.

基金项目

东海实验室开放基金(DH-2022KF0221) (DH-2022KF0221)

中央自然灾害防治体系建设项目(2023330053) (2023330053)

浙江省地质专项资金项目(2023013) (2023013)

国家自然科学基金(12272349,52339005) (12272349,52339005)

海洋地质前沿

OA北大核心

1009-2722

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