福建安海湾表层沉积物粒度特征及其现代沉积过程分析

李东义; 徐勇航; 王爱军; 郑斌鑫; 李国刚

doi:10.14027/j.cnki.cjxb.2015.04.011

ISSN 1000-0550 CN 62-1038/P

高级搜索

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

福建安海湾表层沉积物粒度特征及其现代沉积过程分析

李东义, 徐勇航, 王爱军, 郑斌鑫, 李国刚

文章导航 > 沉积学报 > 2015 > 33(4): 724-734

李东义, 徐勇航, 王爱军, 郑斌鑫, 李国刚. 福建安海湾表层沉积物粒度特征及其现代沉积过程分析[J]. 沉积学报, 2015, 33(4): 724-734. doi: 10.14027/j.cnki.cjxb.2015.04.011

引用本文:

LI DongYi, XU YongHang, WANG AiJun, ZHENG BinXin, LI GuoGang. Analysis of Surface Sediment Grain Size Characteristics and Modern Sedimentary Process in Fujian Anhai Gulf[J]. Acta Sedimentologica Sinica, 2015, 33(4): 724-734. doi: 10.14027/j.cnki.cjxb.2015.04.011

Citation:

LI DongYi, XU YongHang, WANG AiJun, ZHENG BinXin, LI GuoGang. Analysis of Surface Sediment Grain Size Characteristics and Modern Sedimentary Process in Fujian Anhai Gulf[J]. Acta Sedimentologica Sinica, 2015, 33(4): 724-734. doi: 10.14027/j.cnki.cjxb.2015.04.011

引用本文:

Citation:

福建安海湾表层沉积物粒度特征及其现代沉积过程分析

doi: 10.14027/j.cnki.cjxb.2015.04.011

1.
国家海洋局第三海洋研究所海洋与海岸地质环境开放实验室福建厦门 361005;
2.
国家海洋局北海分局北海海洋工程勘察研究院山东青岛 266033

基金项目: 福建省自然科学基金(编号:2014J01158)、国家海洋局第三海洋研究所基本科研业务费(编号:海三科2014015)与国家自然科学基金项目(批准号:41076035)联合资助 ②国家海洋局第三海洋研究所. 泉厦漳城市联盟高速公路工程水文观测与分析研究报告[R].2013.

详细信息

作者简介:
李东义男 1981年出生硕士助理研究员海洋沉积学、沉积动力学 E-mail:lidongyi1981@163.com

中图分类号: P736.21

计量

文章访问数: 818
HTML全文浏览量: 5
PDF下载量: 1126
被引次数: 0

Analysis of Surface Sediment Grain Size Characteristics and Modern Sedimentary Process in Fujian Anhai Gulf

1.
Open Lab of Ocean and Coast Environment Geology, Third Institute of Oceanography, S.O.A, Xiamen, Fujian 361005;
2.
North China Sea Branch of the State Oceanic Administration, Beihai Offshore Engineering Survey Institute, Qingdao, Shandong 266033

摘要

摘要: 通过对福建安海湾表层沉积物的粒度分析和对比,应用系统聚类分析、粒径趋势模型和切应力计算公式,探讨了研究区粒度的分布特征、沉积环境分区、表层沉积物输运趋势及其影响因素.研究结果表明,研究区包括6种表层沉积物类型,以黏土质粉砂和粉砂为主,沉积物大体呈现自海湾两侧潮滩向潮汐通道变粗的分布趋势.表层沉积物粒度的分布特征与水动力条件和物质来源密切相关,湾口附近及湾内深槽内,细颗粒的沉积物被再悬浮带走,粗颗粒的含量增大;在湾内潮滩上,悬浮物质因水动力作用逐渐减弱发生分选沉降,形成向岸变细的横向分异.海湾外泥沙随潮流不断地向海湾东侧岸滩运移,海湾周边陆源来沙由湾顶部往湾口方向下泄,两者是导致表层沉积物出现明显的顺时针方向汇聚趋势的原因之一;表层沉积物的输运趋势、悬浮泥沙的输运、潮滩植被与湾口沙嘴的遮蔽效应共同影响了研究区内浅滩地形的形成和变化.研究区可分为四类沉积环境区,以潮滩和潮汐通道环境为主,不同沉积区内的粒度参数、粒级频率和敏感粒级均有差异,动力条件差异和不同物源的影响程度是现代沉积环境格局的主要影响因素.
- 粒度 /
- 沉积环境 /
- 沉积动力 /
- 粒径趋势分析
Abstract: Surface sediments in Fujian Anhai gulf were collected and analyzed by grain size laser particle sizer. The grain size distribution characteristics, sedimentary environment partition, trend of surface sediment transport and its influencing factors were discussed by application system clustering analysis, grain size trend model and the formula of shear stress. The results shows that surface sediment include six types of sediment, give priority to the two main types which are clayey silt and silty sand. The grain size trends to coarse form tidal flat in both sides of the bay to the tidal channel. The grain size distribution characteristics are closely related to the hydrodynamic and material source. The fine particles material were removed by resuspension near the bay mouth and in tidal channel, lead to the content of coarse particles increased. On the tidal flat in the bay, the selective deposition of suspended material happen due to the hydrodynamic effect weakened, formed the horizontal differentiation which particles material become more finer toward the shore. The transportation to the east side tidal flats of the suspended sediment carried by the tide current form the outside bay, and the discharge of terrigenous sediment derived from surrounding the gulf towards the top of the bay to the bay mouth, can influence the migration trend of sediment shows obviously clockwise convergence. The formation and change of the shoals are affected by the migration trend of sediment and transport of suspended sediment together with vegetation and the shading effect of the sand spit in bay mouth. The study area can be divided into four types of sedimentary environment, give priority to tidal flat and tidal channel environment. The grain size parameters, frequency and sensitive fraction have difference in different sedimentary environment. The modern pattern sediment environment is mainly impacted by hydrodynamic difference and the influence of different material source.
- grain size /
- sedimentary environment /
- sediment dynamics /
- grain size trends analysis

HTML全文

参考文献(0)

[1]	胡京九, 张虎才, 常凤琴, 李婷, 蔡萌, 段立曾, 张龙吴, 张扬. 程海表层沉积物粒度空间分布特征及其影响因素 . 沉积学报, 2020, 38(2): 340-348. doi: 10.14027/j.issn.1000-0550.2019.032
[2]	乔大伟, 王红亮. 基于粒度小波变换分析的四川盐源盆地沉积特征及其对盆地形成演化的指示意义 . 沉积学报, 2019, 37(4): 713-722. doi: 10.14027/j.issn.1000-0550.2018.165
[3]	林镇坤, 王爱军, 叶翔. 南流江河口水下三角洲表层沉积物端元分析及其沉积动力环境意义 . 沉积学报, 2019, 37(1): 124-134. doi: 10.14027/j.issn.1000-0550.2018.113
[4]	周建超, 吴敬禄, 曾海鳌. 新疆乌伦古湖沉积物粒度特征揭示的环境信息 . 沉积学报, 2017, 35(6): 1158-1165. doi: 10.14027/j.cnki.cjxb.2017.06.007
[5]	李华勇, 张虎才, 陈光杰, 常凤琴, 段立曾, 王教元, 卢慧斌, 吴汉, 胡葵. 云南高原湖泊表层沉积物粒度特征及环境指示意义 . 沉积学报, 2017, 35(3): 499-507. doi: 10.14027/j.cnki.cjxb.2017.03.008
[6]	吴汉, 常凤琴, 张虎才, 李华勇, 蒙红卫, 段立曾, 刘东升, 李楠, 朱梦姝. 泸沽湖表层沉积物粒度空间分布特征及其影响因素 . 沉积学报, 2016, 34(4): 679-687. doi: 10.14027/j.cnki.cjxb.2016.04.008
[7]	宗娴, 石学法, 葛晨东, 邹建军, Sergey Gorbarenko, 乔淑卿, 董智. 日本海百年来沉积速率及粒度指示意义 . 沉积学报, 2016, 34(3): 516-522. doi: 10.14027/j.cnki.cjxb.2016.03.009
[8]	. 汕头近岸海域表层沉积物粒度特征及其输运趋势 . 沉积学报, 2014, 32(2): 314-324.
[9]	. 乌梁素海湖泊沉积物粒度特征及其环境指示意义 . 沉积学报, 2013, 31(04): 646-652.
[10]	舒强. 苏北盆地浅钻沉积物磁化率与粒度记录的末次冰消期以来的环境变化 . 沉积学报, 2009, 27(1): 111-117.
[11]	闵凤阳. 深圳湾西北部海域表层沉积物的分布特征及输运趋势 . 沉积学报, 2009, 27(4): 714-722.
[12]	刘红. 长江口表层沉积物粒度时空分布特征 . 沉积学报, 2007, 25(3): 445-455.
[13]	谢昕. 古环境研究中深海沉积物粒度测试的预处理方法 . 沉积学报, 2007, 25(5): 684-692.
[14]	邢云. 潮滩表层沉积物磁性特征的季节性变化及其对沉积动力作用的响应：以杭州湾北岸为例 . 沉积学报, 2007, 25(2): 267-273.
[15]	舒强. 苏北盆地XH1＃钻孔沉积物磁化率与粒度组分相关性变化特征及其意义研究 . 沉积学报, 2006, 24(2): 276-281.
[16]	汪勇. 陕北红碱淖沉积物粒度特征所揭示的环境变化 . 沉积学报, 2006, 24(3): 349-355.
[17]	王爱军, 汪亚平, 杨旸. 江苏王港潮间带表层沉积物特征及输运趋势 . 沉积学报, 2004, 22(1): 124-129.
[18]	张瑞生, 王华, 吴冲龙. 抚顺盆地沉积动力学特征及其聚煤意义 . 沉积学报, 2001, 19(3): 375-380.
[19]	刘晓东, 鹿化煜, 安芷生. 利用黄土沉积速率与粒度的相关性建立黄土序列年龄的新方法 . 沉积学报, 1999, 17(1): 145-148.
[20]	魏文寿. 沙漠表层粒度与水热变化的环境效应分析──以古尔班通古特沙漠为例 . 沉积学报, 1998, 16(1): 152-156.

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 818
HTML全文浏览量: 5
PDF下载量: 1126
被引次数: 0

福建安海湾表层沉积物粒度特征及其现代沉积过程分析

doi: 10.14027/j.cnki.cjxb.2015.04.011

1. 国家海洋局第三海洋研究所海洋与海岸地质环境开放实验室福建厦门 361005;

2. 国家海洋局北海分局北海海洋工程勘察研究院山东青岛 266033

作者简介:
李东义男 1981年出生硕士助理研究员海洋沉积学、沉积动力学 E-mail:lidongyi1981@163.com

收稿日期: 2014-06-30
修回日期: 2014-11-07
刊出日期: 2015-08-10

中图分类号: P736.21

关键词:

粒度 /

沉积环境 /

沉积动力 /

粒径趋势分析

摘要: 通过对福建安海湾表层沉积物的粒度分析和对比,应用系统聚类分析、粒径趋势模型和切应力计算公式,探讨了研究区粒度的分布特征、沉积环境分区、表层沉积物输运趋势及其影响因素.研究结果表明,研究区包括6种表层沉积物类型,以黏土质粉砂和粉砂为主,沉积物大体呈现自海湾两侧潮滩向潮汐通道变粗的分布趋势.表层沉积物粒度的分布特征与水动力条件和物质来源密切相关,湾口附近及湾内深槽内,细颗粒的沉积物被再悬浮带走,粗颗粒的含量增大;在湾内潮滩上,悬浮物质因水动力作用逐渐减弱发生分选沉降,形成向岸变细的横向分异.海湾外泥沙随潮流不断地向海湾东侧岸滩运移,海湾周边陆源来沙由湾顶部往湾口方向下泄,两者是导致表层沉积物出现明显的顺时针方向汇聚趋势的原因之一;表层沉积物的输运趋势、悬浮泥沙的输运、潮滩植被与湾口沙嘴的遮蔽效应共同影响了研究区内浅滩地形的形成和变化.研究区可分为四类沉积环境区,以潮滩和潮汐通道环境为主,不同沉积区内的粒度参数、粒级频率和敏感粒级均有差异,动力条件差异和不同物源的影响程度是现代沉积环境格局的主要影响因素.

English Abstract

Analysis of Surface Sediment Grain Size Characteristics and Modern Sedimentary Process in Fujian Anhai Gulf

1. Open Lab of Ocean and Coast Environment Geology, Third Institute of Oceanography, S.O.A, Xiamen, Fujian 361005;

2. North China Sea Branch of the State Oceanic Administration, Beihai Offshore Engineering Survey Institute, Qingdao, Shandong 266033

Received Date: 2014-06-30
Rev Recd Date: 2014-11-07
Publish Date: 2015-08-10

Keywords:

Abstract: Surface sediments in Fujian Anhai gulf were collected and analyzed by grain size laser particle sizer. The grain size distribution characteristics, sedimentary environment partition, trend of surface sediment transport and its influencing factors were discussed by application system clustering analysis, grain size trend model and the formula of shear stress. The results shows that surface sediment include six types of sediment, give priority to the two main types which are clayey silt and silty sand. The grain size trends to coarse form tidal flat in both sides of the bay to the tidal channel. The grain size distribution characteristics are closely related to the hydrodynamic and material source. The fine particles material were removed by resuspension near the bay mouth and in tidal channel, lead to the content of coarse particles increased. On the tidal flat in the bay, the selective deposition of suspended material happen due to the hydrodynamic effect weakened, formed the horizontal differentiation which particles material become more finer toward the shore. The transportation to the east side tidal flats of the suspended sediment carried by the tide current form the outside bay, and the discharge of terrigenous sediment derived from surrounding the gulf towards the top of the bay to the bay mouth, can influence the migration trend of sediment shows obviously clockwise convergence. The formation and change of the shoals are affected by the migration trend of sediment and transport of suspended sediment together with vegetation and the shading effect of the sand spit in bay mouth. The study area can be divided into four types of sedimentary environment, give priority to tidal flat and tidal channel environment. The grain size parameters, frequency and sensitive fraction have difference in different sedimentary environment. The modern pattern sediment environment is mainly impacted by hydrodynamic difference and the influence of different material source.

引用本文:

Citation:

全文HTML

下载: 全尺寸图片幻灯片

返回文章

用微信扫码二维码

分享至好友和朋友圈

x 关闭永久关闭

2023年地质事件沉积研究新进展国际学术研讨会（第一号通知）

留言板

福建安海湾表层沉积物粒度特征及其现代沉积过程分析

doi: 10.14027/j.cnki.cjxb.2015.04.011

作者简介:
李东义男 1981年出生硕士助理研究员海洋沉积学、沉积动力学 E-mail:lidongyi1981@163.com

计量

Analysis of Surface Sediment Grain Size Characteristics and Modern Sedimentary Process in Fujian Anhai Gulf

计量

目录

福建安海湾表层沉积物粒度特征及其现代沉积过程分析

doi: 10.14027/j.cnki.cjxb.2015.04.011

1. 国家海洋局第三海洋研究所海洋与海岸地质环境开放实验室福建厦门 361005;

2. 国家海洋局北海分局北海海洋工程勘察研究院山东青岛 266033

作者简介:
李东义男 1981年出生硕士助理研究员海洋沉积学、沉积动力学 E-mail:lidongyi1981@163.com

English Abstract

Analysis of Surface Sediment Grain Size Characteristics and Modern Sedimentary Process in Fujian Anhai Gulf

1. Open Lab of Ocean and Coast Environment Geology, Third Institute of Oceanography, S.O.A, Xiamen, Fujian 361005;

2. North China Sea Branch of the State Oceanic Administration, Beihai Offshore Engineering Survey Institute, Qingdao, Shandong 266033

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

福建安海湾表层沉积物粒度特征及其现代沉积过程分析

doi: 10.14027/j.cnki.cjxb.2015.04.011

作者简介: 李东义 男 1981年出生 硕士 助理研究员 海洋沉积学、沉积动力学 E-mail:lidongyi1981@163.com

计量

出版历程

Analysis of Surface Sediment Grain Size Characteristics and Modern Sedimentary Process in Fujian Anhai Gulf

计量

出版历程

目录

福建安海湾表层沉积物粒度特征及其现代沉积过程分析

doi: 10.14027/j.cnki.cjxb.2015.04.011

1. 国家海洋局第三海洋研究所海洋与海岸地质环境开放实验室 福建厦门 361005; 2. 国家海洋局北海分局北海海洋工程勘察研究院 山东青岛 266033

作者简介: 李东义 男 1981年出生 硕士 助理研究员 海洋沉积学、沉积动力学 E-mail:lidongyi1981@163.com

English Abstract

Analysis of Surface Sediment Grain Size Characteristics and Modern Sedimentary Process in Fujian Anhai Gulf

1. Open Lab of Ocean and Coast Environment Geology, Third Institute of Oceanography, S.O.A, Xiamen, Fujian 361005; 2. North China Sea Branch of the State Oceanic Administration, Beihai Offshore Engineering Survey Institute, Qingdao, Shandong 266033

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
李东义男 1981年出生硕士助理研究员海洋沉积学、沉积动力学 E-mail:lidongyi1981@163.com

1. 国家海洋局第三海洋研究所海洋与海岸地质环境开放实验室福建厦门 361005;

2. 国家海洋局北海分局北海海洋工程勘察研究院山东青岛 266033

作者简介:
李东义男 1981年出生硕士助理研究员海洋沉积学、沉积动力学 E-mail:lidongyi1981@163.com

1. Open Lab of Ocean and Coast Environment Geology, Third Institute of Oceanography, S.O.A, Xiamen, Fujian 361005;

2. North China Sea Branch of the State Oceanic Administration, Beihai Offshore Engineering Survey Institute, Qingdao, Shandong 266033