| 注册
首页|期刊导航|海洋地质前沿|南海中沙大环礁表层沉积物的粒度特征和输运趋势

南海中沙大环礁表层沉积物的粒度特征和输运趋势

徐国强 王勇智 杜军 闫文文 李平 周润生

海洋地质前沿2026,Vol.42Issue(9):57-66,10.
✕
海洋地质前沿2026,Vol.42Issue(9):57-66,10.DOI:10.16028/j.1009-2722.2026.012

南海中沙大环礁表层沉积物的粒度特征和输运趋势

Grain size characteristics and transport trends of surface sediments in Zhongsha Atoll,South China Sea

徐国强 1王勇智 1杜军 1闫文文 1李平 1周润生2

作者信息

  • 1. 自然资源部第一海洋研究所,青岛 266061
  • 2. 自然资源部南海调查中心,广州 510500
  • 折叠

摘要

Abstract

In addition to the growth of hermatypic corals,the accumulation of coral sand is also a significant factor in shaping atoll topography.The grain size of 17 surface sediment samples collected from the shallow wa-ters of the Zhongsha Great Atoll in the South China Sea were analyzed,the seabed-based current was observed at five stations,and the sediment transport trends were also analyzed to understand the erosional and depositional status of the atoll,providing a theoretical basis for the preservation of atoll topography.Results indicate that the sediments consist of three types:gravelly sand,sandy gravel,and sand-bearing gravel,and they were transported via mainly rolling and saltation.In addition,the hydrodynamic environment,the Great Atoll region was divided into three sedimentary environment zones.Zone A(sandy transition zone):Located on the eastern and northwest-ern sides of the outer ring of the Great Atoll,dominated by gravelly sand,representing a high-energy reef flat sedi-mentary environment.Zone B(gravel accumulation zone):Stretching in NW-SE along the Luba Ansha-Manbu Ansha-Haijiu Ansha in the central part of the Great Atoll,composed of chiefly sandy gravels.This zone serves as the primary source of coarse-grained materials for the atoll,indicating rapid,near-source,mixed accumulation processes.Zone C(sand-loss zone):Located at Bohu Ansha in the southwestern part of the Great Atoll,composed of mainly sand-bearing gravel.This zone is characterized by sandy sedimentation and sorting under the influence of strong currents.While hydrodynamics in Zones A and B could transport only a small amount of fine sediments,the maximum current velocity in Zone C could exceed the threshold of sediment motion,resulting in the loss of coral sand.In the future,local monitoring shall be strengthened,and appropriate measures shall be taken to pre-vent sediment loss.

关键词

粒度分析/粒度参数/输运趋势/沉积动力/中沙大环礁

Key words

grain size analysis/grain size parameters/transport trends/sedimentary dynamics/Zhongsha Atoll

分类

海洋科学

引用本文复制引用

徐国强,王勇智,杜军,闫文文,李平,周润生..南海中沙大环礁表层沉积物的粒度特征和输运趋势[J].海洋地质前沿,2026,42(9):57-66,10.

基金项目

国家科技基础资源调查专项课题"中沙群岛及邻近海域海洋水动力环境调查"(2018FY100102) (2018FY100102)

海洋地质前沿

1009-2722

访问量0
|
下载量0
段落导航相关论文