本期要文(可全文下载)

黄河三角洲大汶流自然保护区的土地利用与岸线变化分析

展开
  • 1. 中国地质调查局滨海湿地重点实验室,青岛266071;
    2. 国土资源部海洋油气资源与环境地质重点实验室,青岛266071
赵广明(1984-),男,助理研究员,研究方向为生态环境遥感。E-mail:guangming_210@163.com

收稿日期: 2012-10-15

  修回日期: 2013-01-23

  网络出版日期: 2013-06-17

基金资助

大地调项目(1212010611402);国土资源部公益性行业基金(201111023);国土资源部海洋油气资源与环境地质重点实验室基金项目(MRE2012030);海洋地质保障工程项目( GZH201200503)。

Analysis of Land Use and Shoreline Changes at the Dawenliu Nature Reserve of Yellow River Delta Based on Remote Sensing

Expand
  • 1. Key Laboratory of CoastalWetlands, China Geologic Survey, Qingdao 266071, China;
    2. Key Laboratory of Marine Hydrocarbon Resource and Geology, Ministry of Land and Resources, Qingdao 266071, China

Received date: 2012-10-15

  Revised date: 2013-01-23

  Online published: 2013-06-17

摘要

本文选择黄河三角洲大汶流自然保护区为研究对象,以多时相遥感影像,对土地利用类型进行解译分析。同时,以平均低潮线作为分析基线,提取海岸线变化信息。结果表明:1996-2009年研究区面积净增13.35km2。各种土地利用类型中滩涂所占面积最大,养殖池所占比例最小,但增幅明显。芦苇地面积后期增长迅速,指示研究区生态环境趋向转好。自然因素(黄河来水来沙量)和人类活动(黄河调水调沙工程,湿地恢复工程,滩涂规模开发以及人类开垦造田)是研究区土地利用类型变化的直接驱动力。1976-2009年研究区海岸净造陆面积217.14km2,沙嘴变幅为29.2km。黄河入海水沙量和滨海区的海洋潮流条件共同影响着海岸线的变迁。

本文引用格式

赵广明, 叶思源, 高茂生, 丁喜桂, 袁红明, 王锦 . 黄河三角洲大汶流自然保护区的土地利用与岸线变化分析[J]. 地球信息科学学报, 2013 , 15(3) : 408 -414 . DOI: 10.3724/SP.J.1047.2013.00408

Abstract

By the support of remote sensing (RS) and geographic information system (GIS) technology, Dawenliu Nature Reserve of Yellow River Delta (YRD) was picked as the study objective, which is located at Dongying City of Shandong Province. The multi-temporal Landsat images were used as the data source, which were registered to the high precision GIS database, matched each other and with the database, and all the images have the same coordinate system. Four corrected images (1996/2000/2005/2009) were used for land use interpretation, and seven images (1976/1981/1986/1996/2000/2005/2009) were extracted for the information shoreline change, regarding mean low tide level as the analysis baseline. The results show that the land area increased 13.35km2 from 1996-2009. Tidal flat made up the largest proportion in all the land use types and culture ponds were the smallest, which significantly increased. The reed area rapidly increased during the late period, which indicated that eco-environment trended to get better. Coast was divided into siltation coast, erosion coast and steady coast. From 1976 to 2009, 373.92km2 was silted, 156.78 km2 eroded, and net accretion area was 217.14km2. Both the natural factors, such as Yellow River zero flow, and human activities, such as Yellow River water and sediment regulation project, wetland restoration projects, tidal flat development and the construction of a large number of farms, had rendered big influence on the distribution of land use types in the study area. Meanwhile, runoff and sediment of Yellow River and ocean dynamic worked together to change shoreline. Therefore, combing the data of runoff and sediment of Yellow River, tide and ocean dynamic, comprehensive analysis on shoreline evolution will be an important focus in future. Temporal and spatial variation of land use and shoreline evolution interacted each other, so linkage mechanism between healthy assess of land use and shoreline change will be a basic monitoring content of the nature reserve in future.

参考文献

[1] 尹延鸿.现代黄河三角洲海岸的冲淤及造陆速率[J].海洋地质动态,2003,19(7):13-18.

[2] 王红,宫鹏,刘高焕.黄河三角洲土地利用/土地覆被变化研究现状与展望[J].自然资源学报,2004,19(1):112-118.

[3] 赵广明,叶思源,李广雪.卫星遥感在湿地研究中的应用[J].海洋地质动态,2007(12):28-33.

[4] 宗秀影,刘高焕,乔良玉,等.黄河三角洲湿地景观格局动态变化分析[J].地球信息科学学报,2009,11(1):91-97.

[5] 张高生,王仁卿.现代黄河三角洲生态环境的动态监测[J].中国环境科学,2008,28(4):380-384.

[6] 王海梅,李政梅,韩国栋,等.黄河三角洲土地利用及景观的动态分析[J].水土保持通报,2007,27(1):81-85.

[7] 汪小钦,王钦敏,刘高焕,等.黄河三角洲油田集中区土地利用演化的遥感分析[J].地球信息科学,2002,4(4):75-79.

[8] 栗云召,于君宝,韩广轩,等.基于遥感的黄河三角洲海岸线变化研究[J].海洋科学,2012,36(4):99-106.

[9] 薛允传,马圣媛,周成虎.基于遥感和GIS的现代黄河三角洲岸线变迁及发育演变研究[J].海洋科学,2009,33(5):36-40.

[10] 崔步礼,常学礼,陈雅琳,等.黄河水文特征对河口海岸变化的影响[J].自然资源学报,2006,21(6):957-964.

[11] 杨伟,陈沈良,陈小英,等.现代黄河三角洲河口段海岸线演变特征[J].人民黄河,2010,32(10):13-20.

[12] 刘高焕,汉斯·德罗斯特.黄河三角洲可持续发展图集[M].北京:测绘出版社,1997.

[13] 赵广明,李广雪,曹克伟,等.基于RS和GIS 的黄河三角洲北部湿地保护区的生态环境变化[J].海洋地质前沿,2011,27(2):29-33.

[14] 马妍妍.现代黄河三角洲海岸带环境演变[D].青岛:中国海洋大学,2008.

[15] 王开荣.黄河调水调沙对河口及其三角洲的影响和评价[J].泥沙研究,2005(6):29-33.

[16] 李小涛,黄诗峰,杨海波,等.新水沙环境下得黄河三角洲湿地资源动态变化研究[J].水利水电技术,2007,11(38):18-21.

[17] 曹景华,王志秀,王学义.黄河三角洲实施“生态湿地恢复工程”[J].走向世界,2004(2):38-40.

[18] 彭俊,陈沈良.近60 年黄河水沙变化过程及其对三角洲的影响[J].地理学报,2009,64(11):1353-1362.

[19] 常军,刘高焕,刘庆生.黄河三角洲海岸线遥感动态监测[J].地球信息科学,2004,6(1):94-98.

[20] 常军,刘高焕,刘庆生.黄河口海岸线演变时空特征及其与黄河来水来沙关系[J].地理研究,2004,23(5):339-346.

[21] 陈小英,陈沈良,李九发.黄河三角洲孤东及新滩海岸侵蚀机制研究[J].海岸工程,2005,24(4):2-8.

文章导航

/