热带海洋学报 ›› 2011, Vol. 30 ›› Issue (4): 58-65.doi: 10.11978/j.issn.1009-5470.2011.04.058cstr: 32234.14.j.issn.1009-5470.2011.04.058

• 海洋地质学 • 上一篇    下一篇

伶仃洋表层沉积物特征及其泥沙运移趋势

肖志建,  李团结,  廖世智   

  1. 国家海洋局南海工程勘察中心,  广东  广州 510300
  • 收稿日期:2010-01-12 修回日期:2010-07-16 出版日期:2011-09-05 发布日期:2011-09-08
  • 通讯作者: 肖志建(1979—), 男, 江西省峡江县人, 工程师, 硕士, 主要从事河口海岸环境研究。E-mail:75698368@qq.com
  • 作者简介:肖志建(1979—), 男, 江西省峡江县人, 工程师, 硕士, 主要从事河口海岸环境研究。E-mail:75698368@qq.com
  • 基金资助:

    国家海洋局青年基金项目(2009211);  国家海洋局南海分局局长基金项目(0516);  我国近海海洋综合调查与评价专项底质调查
    项目(908-01-CJ15)

Surface sediment characteristics and transport trend in Lingdingyang Bay of the Pearl River Estuary

XIAO Zhi-jian, LI Tuan-jie, LIAO Shi-zhi   

  1. South China Sea Marine Engineering Surveying Center, SOA, Guangzhou 510300, China
  • Received:2010-01-12 Revised:2010-07-16 Online:2011-09-05 Published:2011-09-08

摘要:

根据伶仃洋表层沉积物的粒度分析资料,  探讨表层沉积物的特征,  并在此基础上应用 Gao-Collins 粒径趋势
分析方法(GSTA 模型)分析了伶仃洋表层沉积物的泥沙净输运趋势。结果表明,  伶仃洋表层沉积物共有 6 种类型,
其中以黏土质粉砂分布最广泛。受径流、潮流、波浪和陆架水入侵等多种动力作用,  伶仃洋表层沉积物颗粒在北
面最粗,  南面次之,  中间最细,  东面略粗,  西面略细;  分选由中部向东、西两岸逐渐变好,  但总体分选差;  不同级
配的泥沙分布和沉积特征存在差异。伶仃洋泥沙运移规律较复杂,  泥沙呈现出向西南输运的总趋势;  内伶仃洋四
周泥沙受各种力作用,  呈现出顺时针方向的环流运移,  中心区域为最大浑浊带,  泥沙以垂直落淤为主。 淇澳岛以南
至澳门半岛以东海域受粉砂和黏土向西扩散影响,  泥沙向西运移。大屿海峡及外伶仃岛附近海域为高盐水入侵通
道,  泥沙向西北运移。

关键词: 沉积特征,  , 粒度参数,  , 泥沙输运, } 运移趋势, 珠江河口, 伶仃洋, GSTA 模型

Abstract:

The authors analyzed surface sediment characteristics of Lingdingyang Bay in the Pearl River Estuary based on 230
bed material samples collected in December 2004. Sediment transport trends were identified by the grain-size trends calculated
using the Gao-Collins Grain Size Trend Analysis Model (GSTA model). The results indicate that there are six types of bed
materials in the Lingdingyang Bay, with clayey silt being the dominant type. Under the influences of runoff, tidal current, wind
waves, and salty water, the bed sediments in the northern zone are the coarsest; those in the southern zone are coarse; those in
the middle zone are the finest; and those in the eastern zone are a little coarser than those in the western zone. The sorting of
bed sediment becomes better and better from the middle zone to both the east coast and the west coast, but the total sorting is
poor. The spatial distribution and deposition characteristics of different grain-size sediments are different. The patterns of the
sediment transport in the Lingdingyang Bay are very complex, but the total sediment transport trend is southwestward. Under
the influences of various forcing, the sediments around the inner Lingdingyang Bay take on a clockwise rotation circumfluence
transport; the center zone of the inner Lingdingyang Bay is the maximum turbidity zone and the sediments mostly deposit
vertically. Under the influences of slit and clay diffusing westward, the sediments in the southern zone of Qi’ ao Island and the
eastern zone of Macau Peninsula transport to the west. The Dayu Strait and its adjacent sea area of outer Lingding Island are
the main inlets of high salinity water, and the sediments transport to the northwest.

Key words: sediment characteristics, grain-size parameter, sediment , transport, grain-size trend, Pearl River Estuary, Ling-dingyang Bay, GSTA pattern