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国土资源遥感  2018, Vol. 30 Issue (3): 189-195    DOI: 10.6046/gtzyyg.2018.03.26
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1979—2012年莱州湾南岸海水入侵与区域海岸线变动时空耦合分析
蒙永辉, 王集宁, 张丽霞, 罗梅
山东省地质环境监测总站,济南 250014
An analysis of spatial-temporal coupling relationship between seawater intrusion and regional coastline changes in south coast of Laizhou Bay from 1979 to 2012
Yonghui MENG, Jining WANG, Lixia ZHANG, Mei LUO
Shandong Province Geological Environment Monitoring Station, Jinan 250014, China
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摘要 

在整合区域海水入侵历史观测数据的基础上,结合现代遥感综合观测手段,开展莱州湾南岸海水入侵时空动态变化过程和海岸线历史变迁耦合机制研究。完成了1979―2012年区域海岸线的多期遥感监测和区域咸水入侵锋线演化的时间过程与空间特征数字重建,并引入端点速率法(end point ratio,EPR)分析模型对二者的时空耦合关系进行了探索研究。研究结果表明: ①区域海水入侵经历了由快到慢的变化过程,1990年以后入侵速率明显减缓,入侵锋线基本稳定在1995年锋线附近,且2008―2012年入侵锋线局部发生后退; ②区域海岸线除局部人工造陆导致岸线向海扩张外,区域海岸以蚀退型为主; ③海水入侵锋线变化与海岸线进退二者之间在时空上存在强耦合关系,相关系数达到0.407,显著性水平P<0.01(双侧)。研究结果可为区域海水入侵的预防和治理提供数据支撑和科学依据。

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蒙永辉
王集宁
张丽霞
罗梅
关键词 海水入侵海岸线动态变化耦合机制    
Abstract

Based on the regional seawater intrusion observation data and the remote sensing integrated observation data, the authors examined spatio-temporal dynamic change characteristics and mode of seawater intrusion and coastline evolution in the south coast zone of Laizhou Bay. Firstly, multi-period remote sensed images were used for monitoring of the regional coastline changes from 1979 to 2012. And then, the temporal and spatial features of seawater intrusion were reconstructed by digital vectorization from the historical filed survey maps. On the basis of above information, the EPR model was introduced and the spatial-temporal coupling mechanism between the seawater intrusion and coastline changes was studied and analyzed. Some conclusions have been reached: ① The regional seawater intrusion experienced a change process from rapid to slow, and the rate of invasion was slowing down after 1990. The front of intrusion line was stable since 1995 and retreated from 2008 to 2012. ② The coastal coastline is dominated by the coastal retreating coastline, besides the local artificial coastline. ③ There is a strong coupling relationship between the change of seawater intrusion frontline and coastline in time and space. The correlation coefficient is 0.407, at the significant level of P less than 0.01 (bilateral). The research results can provide data support and scientific basis for regional seawater intrusion prevention and control.

Key wordsseawater intrusion    coastal line    dynamic changes    coupling mechanism
收稿日期: 2017-01-04      出版日期: 2018-09-10
:  TP79  
基金资助:山东省地质勘查项目“黄河三角洲高效生态经济区(潍坊)海(咸)水入侵调查与监控预警系统建设报告”(鲁勘字[2011]14号)
作者简介: 蒙永辉(1980-),男,硕士,高级工程师,主要从事区域水文地质工程地质环境地质综合勘查等方面研究。Email: mengyonghui1122@126.com。
引用本文:   
蒙永辉, 王集宁, 张丽霞, 罗梅. 1979—2012年莱州湾南岸海水入侵与区域海岸线变动时空耦合分析[J]. 国土资源遥感, 2018, 30(3): 189-195.
Yonghui MENG, Jining WANG, Lixia ZHANG, Mei LUO. An analysis of spatial-temporal coupling relationship between seawater intrusion and regional coastline changes in south coast of Laizhou Bay from 1979 to 2012. Remote Sensing for Land & Resources, 2018, 30(3): 189-195.
链接本文:  
https://www.gtzyyg.com/CN/10.6046/gtzyyg.2018.03.26      或      https://www.gtzyyg.com/CN/Y2018/V30/I3/189
Fig.1  研究区位置 (影像底图为TM B4(R),B3(G),B2(B)假彩色合成影像)
卫星 传感器 轨道号/行号 获取日期 空间分辨率/m
Landsat-3 MSS P130/R034 1979-05-27 60
Landsat-5 TM P120/R034 1990-09-20 30
Landsat-5 TM P120/R034 1995-03-26 30
Landsat-5 TM P120/R034 2001-10-12 30
Landsat-7 ETM+ P120/R034 2003-05-11 30
Landsat-8 OLI P120/R034 2013-05-30 30
Tab.1  用于海岸线监测的遥感数据
Fig.2  技术流程图
Fig.3  EPR局部垂直(纵向)断面建模计算示意图
Fig.4  1979―2012年莱州湾南岸海水入侵锋线动态过程(影像底图为TM B3(R),B2(G),B1(B)假彩色合成影像)
Fig.5  EPR空间动态分布图
Fig.6  1979―2013年区域海岸线变迁图(影像底图为MSS B3(R),B2(G),B1(B)假彩色合成影像)
Fig.7  1979―2012年莱州湾南岸岸线与海水入侵锋线变化速率图
(图中Y轴表示基准岸线,正值表示向海方向,负值表示向陆地方向)
状况 均值 最小值 最大值 相关系数 P
海岸蚀退 -10.441 -124.02 191.14
海水入侵 -177.226 -435.28 -33.24 0.407** 0.000
Tab.2  岸线蚀退与海水入侵变化量统计与耦合关系分析
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