山东半岛静海湾及邻近海域悬沙时空分布格局

海洋地质与第四纪地质 Pub Date : 2013-02-17 DOI:10.3724/SP.J.1140.2012.06009

Xiao Liu, Xiuli Feng, Jie Liu, Lin Lin

{"title":"山东半岛静海湾及邻近海域悬沙时空分布格局","authors":"Xiao Liu, Xiuli Feng, Jie Liu, Lin Lin","doi":"10.3724/SP.J.1140.2012.06009","DOIUrl":null,"url":null,"abstract":"Suspended sediment concentration(SSC),as the basis for sediment flux balance,is an important parameter in marine sedimentology.Based on the survey and hydrological observations at 10 stations in the Jinghai Bay and its adjacent waters,SSC in different layers is calculated,and the SSC horizontal and vertical distribution patterns and the transportation of suspended sediment are analyzed.Data show that SSC changes with the variation of tide current and runoff,and increases from the surface to the bottom and from southwest to northeast.The mechanism of longitudinal suspended sediment transport shows that sediments move toward the land and Wuleidao Bay where flood tide dominates,but move towards the sea near the Changhuikou area where ebb tide dominants.","PeriodicalId":18188,"journal":{"name":"海洋地质与第四纪地质","volume":"32 1","pages":"9-15"},"PeriodicalIF":0.0000,"publicationDate":"2013-02-17","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Spatial and Temporal Distribution Pattern of Suspended Sediment in the Jinghai Bay and Adjacent Waters, Shandong Peninsula\",\"authors\":\"Xiao Liu, Xiuli Feng, Jie Liu, Lin Lin\",\"doi\":\"10.3724/SP.J.1140.2012.06009\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Suspended sediment concentration(SSC),as the basis for sediment flux balance,is an important parameter in marine sedimentology.Based on the survey and hydrological observations at 10 stations in the Jinghai Bay and its adjacent waters,SSC in different layers is calculated,and the SSC horizontal and vertical distribution patterns and the transportation of suspended sediment are analyzed.Data show that SSC changes with the variation of tide current and runoff,and increases from the surface to the bottom and from southwest to northeast.The mechanism of longitudinal suspended sediment transport shows that sediments move toward the land and Wuleidao Bay where flood tide dominates,but move towards the sea near the Changhuikou area where ebb tide dominants.\",\"PeriodicalId\":18188,\"journal\":{\"name\":\"海洋地质与第四纪地质\",\"volume\":\"32 1\",\"pages\":\"9-15\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2013-02-17\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"海洋地质与第四纪地质\",\"FirstCategoryId\":\"1089\",\"ListUrlMain\":\"https://doi.org/10.3724/SP.J.1140.2012.06009\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"海洋地质与第四纪地质","FirstCategoryId":"1089","ListUrlMain":"https://doi.org/10.3724/SP.J.1140.2012.06009","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}

引用次数: 0

摘要

悬沙浓度(SSC)是海洋沉积学中的重要参数，是泥沙通量平衡的基础。基于静海湾及邻近海域10个站点的调查和水文观测，计算了静海湾各层的SSC，并分析了SSC的水平和垂直分布格局以及悬沙的输运。数据表明，SSC随潮流和径流的变化而变化，从表面到底部，从西南到东北增加。纵向悬沙输运机制表明，泥沙向以涨潮为主的陆地和五雷岛湾移动，向以退潮为主的长会口附近海域移动。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

查看原文本刊更多论文

Spatial and Temporal Distribution Pattern of Suspended Sediment in the Jinghai Bay and Adjacent Waters, Shandong Peninsula

Suspended sediment concentration(SSC),as the basis for sediment flux balance,is an important parameter in marine sedimentology.Based on the survey and hydrological observations at 10 stations in the Jinghai Bay and its adjacent waters,SSC in different layers is calculated,and the SSC horizontal and vertical distribution patterns and the transportation of suspended sediment are analyzed.Data show that SSC changes with the variation of tide current and runoff,and increases from the surface to the bottom and from southwest to northeast.The mechanism of longitudinal suspended sediment transport shows that sediments move toward the land and Wuleidao Bay where flood tide dominates,but move towards the sea near the Changhuikou area where ebb tide dominants.

求助全文

通过发布文献求助，成功后即可免费获取论文全文。去求助

来源期刊

海洋地质与第四纪地质

CiteScore

0.10

自引率

0.00%

发文量

4176

期刊介绍： Marine Geology and Quaternary Geology launched in 1981 is a bimonthly academic journal sponsored by Qingdao Institute of Marine Geology, China Geological Survey, and published by the Science Press, China.The journal aims to publish original, cutting-edge, and explorative scientific results in the field of marine geology and sea-land Quaternary geology. The journal focus on reporting the latest research achievements supported by National Natural Science Foundation Project, National Key Project and International Cooperation Project, with priority to the results in China seas, global ocean and three poles, and the comparative study results between offshore and land, regional and global scientific issues.