近60年莱州湾东部砂质海岸地貌的时空动态

doi:DOI:10.3969/J.ISSN.0253-4193.2017.09.009

YIC-IR > 中国科学院海岸带环境过程与生态修复重点实验室 > 海岸带环境过程实验室

	近60年莱州湾东部砂质海岸地貌的时空动态
其他题名	Spatial and temporal dynamics of sandy coastal geomorphology in the east of Laizhou Bay over recent 60years
	战超 ; 于君宝; 王庆 ; 栗云召 ; 周迪
发表期刊	海洋学报
ISSN	0253-4193
	2017-09-15
卷号	39 期号:9 页码:90-100
关键词	sandy coast shoreline subaqueous slope geomorphic evolution anthropogenic activities 砂质海岸海岸线水下岸坡地貌演变人类活动
DOI	DOI:10.3969/J.ISSN.0253-4193.2017.09.009
产权排序	(1) 中国科学院烟台海岸带研究所; (2) 鲁东大学滨海生态研究院; (3) 中国科学院大学
作者部门	海岸带环境过程实验室
英文摘要	Based on the results of field surveys,the spatial and temporal dynamics of sandy coastal geomorphology along the eastern Laizhou Bay over the last 60years was investigated using the comprehensive methods of digital shoreline analysis,remote sensing and geographic information system technologies.The data mainly derived from the nautical charts,topographic maps and high resolution remote sensing images which measured and imaged in different periods.The results show that there are significant spatial-temporal variations in both the sandy coast shoreline migration and the subaqueous slope erosion-deposition evolution along the eastern Laizhou Bay.The alternate regulation of forward and backward for shoreline migration is caught in this study.There is a remarkable non-linear characteristic in the time process.The proportion of the erosional shoreline is fluctuated and phased from 1959to 2013.The average annual evolution rate of eroded coast is divided into two stages by 1985.The erosion rate decreased from the maximum value of 4.95m/a(during the period of 1959-1969)to minimum value 1.97m/a (1969-1985)at prophase.In the late period,the erosion rate increased from 1.97m/a to 4.43m/a(1985- 1998),and the coast was in serious erosion state since then.The characteristics of shoreline migration in four headland bays are not consistent with overall trend.At the same time,the scouring strips distribute alternating with the silting of the subaqueous slope.The trend of scouring and silting evolution was basically opposite in the same coast between the periods of 1959-1985and 1985-2008.Further analysis indicate that there are 5alternations of erosion and deposition and the changes of rate of erosion and siltation,under the control of geomorphic effects of anthropogenic activities such as sediment trapping by reservoirs,fishing culture in supratidal zone and coastal engineering, in the east of Laizhou Bay during recent 60years.
中文摘要	在野外考察的基础上,以不同时期测量和成像的海图、地形图和高分辨率遥感影像为数据源,综合使用数字岸线分析、遥感、地理信息系统等方法,对近60年来莱州湾东部砂质海岸(界河口-刁龙嘴)地貌演变进行研究。结果表明,研究期内莱州湾东部岸线迁移和水下岸坡冲淤存在强烈的时空差异。岸线迁移表现为冲淤进退交替发生,其在时间过程上具有非线性的显著特点。1959-2013年,侵蚀岸线所占比例波动起伏,具有阶段性。侵蚀岸段年均演变速率以1985年为界分成两个阶段,前期由极大值4.95m/a(1959-1969年)锐减至极小值1.97m/a(1969-1985年),后期由1.97m/a增大到4.43m/a(1985-1998年),之后均处于高强度侵蚀。岸线迁移空间分布的差异性主要表现在4个岬湾的岸线变迁特征与莱州湾东岸岸线整体变迁并不一致。同时,水下岸坡冲淤条带大体相间分布,同一岸段1959-1985年和1985-2008年的冲淤演变趋势基本相反。进一步分析表明最近60年来,莱州湾东部砂岸在水库拦沙、潮上带工厂化水产养殖、大型海岸工程等人类活动的地貌效应共同控制下,发生了5次岸线淤积前进与侵蚀后退以及冲淤速率大小的交替。
文章类型	Article
收录类别	CSCD
语种	中文
关键词[WOS]	Oceanography
研究领域[WOS]	Oceanography ; 海洋学
CSCD记录号	CSCD:6058434
引用统计
文献类型	期刊论文
条目标识符	http://ir.yic.ac.cn/handle/133337/24284
专题	中国科学院海岸带环境过程与生态修复重点实验室_海岸带环境过程实验室中国科学院海岸带环境过程与生态修复重点实验室_海岸带信息集成与战略规划研究中心中国科学院海岸带环境过程与生态修复重点实验室_滨海湿地实验室
作者单位	1.中国科学院烟台海岸带研究所; 2.鲁东大学滨海生态研究院; 3.中国科学院大学
推荐引用方式 GB/T 7714	战超,于君宝,王庆,等. 近60年莱州湾东部砂质海岸地貌的时空动态[J]. 海洋学报,2017,39(9):90-100.
APA	战超,于君宝,王庆,栗云召,&周迪.(2017).近60年莱州湾东部砂质海岸地貌的时空动态.海洋学报,39(9),90-100.
MLA	战超,et al."近60年莱州湾东部砂质海岸地貌的时空动态".海洋学报 39.9(2017):90-100.